M/S. DHARMENDRA CHATURBHAI KHABHATI (DCK)

Village‐OZ, Tal.: Karjan, Dist.: Vadodara‐393105. (M) 9824421292. E‐mail: [email protected]

DCK/DEAC/EC/01/2018 Date: 02/08/2018

To, District Level Expert Appraisal Committee (DEAC), The Geologist, Department of Geology & Mining, Collectorate Compound, Vadodara.

Subject: Application for Environmental Clearance for the Ordinary (Ordinary Bricks) Clay Mines Admeasuring 04.82.06 Ha. At Sr. No: 344,1060,1061,1271,1272,1273,1274,1275, 1276,1277,1307,1308,1309,1314,1315,1316,1324,1325,1326,1327,1328,1331,Village‐OZ, Tal.: Karjan, Dist.: Vadodara‐393105.

Respected Sir, With reference to the above subject and circular form MoEF “In case of mining activity at any less than 5 ha lease areas require Environmental Clearance form DEIAA as per MoEF Circular Dated – 15/01/2016”. We require obtaining the Environmental Clearance.

We herewith apply (in Form‐1M) for environmental clearance with the Form – 1M, prefeasibility study report, Project details and other supporting documents.

We request your good selves to kindly consider our case in earliest committee meeting and grant us the recommendation / Environmental Clearance.

Thanking You,

Sincerely Yours, For DHARMENDRA CHATURBHAI KHABHATI(DCK).

Authorised Signature Dharmendra C. Khabhati

FORM-1M APPLICATION FOR MINING OF MINOR MINERALS UNDER CATEGORY ‘B2’ FOR LESS THAN TO FIVE HECTARE

Basic information

Sr. No. Item Details

DHARMENDRA CHATURBHAI KHABHATI(DCK) (04.82.06 ha)

1 Name of the Project

Ordinary Clay Mining at Survey No. –344, 1060,1061,

1271,1307, 1308,1309,1314, 1315, 1316,1324,1325,

1326,1327,1328,1331,

Village: OZ ,TaL: Karjan , Dist: Vadodara‐393105. 1 21°51'53.38"N 73° 09'18.52"E

2 21°51'45.46"N 73° 09'13.24"E

3 21°51'11.11"N 73° 09'50.49"E

4 21°51'14.55"N 73° 09'54.08"E

Location / site (GPS Co-

2 ordinates):

Size of the Mining Lease

3 04.82.06 ha

(Hectare):

4 Capacity of Mining Lease (TPA): 240000 TPA

5 Period of Mining Lease: 10 Years

6 Expected cost of the Project: 10 Lacs

Mr. Dharmendra Chaturbhai Khabhati

7 Contact Information: Ordinary Clay Mining

Village: OZ ,Tal: Karjan, Dist: Vadodara‐393105.

Environment Sensitivity

SI No Areas Distance in Kilometer

Distance of project site from nearest rail or road bridge Narmada River – 0.3 km 1

over the concerned River, Rivulet, Nallah etc.

Distance from infrastructural facilities OZ – 1.13 . km

Raliway – 11.5 km. Railway line Palej

– 10.7 km. National Highway NE‐48(NH‐8)

State Highway No

Major District Road No

2 Any other Road Nareshwar Road – 1.36 km

Electric transmission line pole or tower Not Applicable

Canal or check or reservoirs or lake or ponds Mini Canal – 3.76 km

In-take for drinking water pump house Not Applicable

Intake for Irrigation canal pumps Not Applicable

Areas protected under international conventions, national Not Such area available within 15

3 or local legislation for their ecological, landscape, cultural

km.

or other related value

Areas which are important or sensitive for ecological Not Such area available within 15 4 reasons - Wetlands, watercourses or other water bodies,

km.

coastal zone, biospheres, mountains, forests

Areas used by protected, important or sensitive species of

Not Such area available within 15 km. 5 flora or fauna for breeding, nesting, foraging, resting, over

wintering, migration 6 Inland, coastal, marine or underground waters Not Applicable

Not Such area available within 15

7 State, National boundaries km.

Routes or facilities used by the public for access to

8 Not Applicable recreation or other tourist, pilgrim areas

9 Defence installations Not Applicable

Densely populated or built-up area, distance from nearest 10 OZ – 1.13 km.

human habitation

Areas occupied by sensitive man-made land uses 11 OZ Primary School: 1.13 km.

(hospitals, schools, places of worship, community acilities)

Areas containing important, high quality or scarce

12 resources (ground water resources, surface resources, Not Applicable

forestry, agriculture, fisheries, tourism, minerals)

Areas already subjected to pollution or environmental

13 damage. (those where existing legal environmental Not Applicable

standards are exceeded)

Areas susceptible to natural hazard which could cause the

project to present environmental problems (earthquakes, 14 Flooding in heavy rain

subsidence, landslides, erosion, flooding or extreme or

adverse climatic conditions)

Is proposed mining site located over or near fissure / 15 No. Not Applicable

fracture for ground water recharge

Whether the proposal involves approval or clearance

under the following Regulations

or Acts, namely:-

(a) The Forest (Conservation) Act, 1980;

16 Not Applicable

(b) The Wildlife (Protection) Act, 1972;

(c) The Coastal Regulation Zone Notification, 2011.

If yes, details of the same and their status to be given.

17 Forest land involved (hectares) Not Applicable

Whether there is any litigation pending against the project

and/or land in which the project is propose to be set up?

(a) Name of the Court 18 (b) Case No. Not Applicable

(c) Orders or directions of the Court, if any, and its

relevance with the proposed project.

“I hereby given undertaking that the data and information given in the application and enclosures are true to the best of my knowledge and belief and I am aware that if any part of the data and information submitted is found to be false or misleading at any stage, the project will be rejected and clearance give, if any to the project will be revoked at our risk and cost.”

Date: 02‐08‐2018 Place: VADODARA

DHARMENDRA CHATURBHAI KHABHATI C/o Dharmendra Khabhati Village: OZ Tal.: Karjan, Dist: Vadodara.

Signature of the applicant With Name and Full Address (Project Proponent/Authorized Signatory)

PROJECT DETAILS – ORDINARY CLAY MINING PROJECTS

Sr.

Details Particulars

No.

DHARMENDRA CHATURBHAI KHABHATI(DCK) 1 Name of Lease Holder

Sur. No. 344,1060,1061,1271,1272,1273,1274,1275,1276,

1277,1307,1308,1309,1314,1315,1316,1324,1325,1326, 2 Location address 1327,1328,1331, Village‐ OZ, Tal: Karjan,

Dist: Vadodara‐393105.

4.82.06 hectare

Northing Easting

21°51'53.38"N 73° 09'18.52"E 21°51'45.46"N 73° 09'13.24"E 3 Lease Area (Hectares) 21°51'11.11"N 73° 09'50.49"E Co‐ordinates of the lease area 21°51'14.55"N 73° 09'54.08"E

21°51'31.24"N 73° 09'38.33"E

21°51'28.61"N 73° 09'33.41"E

Please refer Annexure for coordinates map.

Ownership of Land

4 Private land

(Govt. / Private Land)

Status of Operation (New Project or

5 Existing project operating since New Project

______)

Status of Lease (Lease no., date of Registration for excavation of mining clay

(bricks manufacturing) as per the

6 issues / renewal, lease period, date of existing rules of mining has been done at geology

application for lease renewal, etc.) and mining department.

7 Name of Mineral Ordinary Clay

8 Ordinary Clay Reserve (MT) 512000 MT

Rate of Mining of Ordinary Clay

9 240000 MT/Year

(MT/Year)

10 Life of Mine 10 years

Weather project involves forest land,

11 No, This project does not involve any forest land.

If yes, status of diversion of forest land

12 Applicability of CRZ notification,2011 Not applicable

ENVIRONMENTAL SETTING

If located within 15 km, aerial distance

13 ‐‐

of the lease area from the nearest:

i. National Park / Wildlife

None

Sanctuary / Biosphere Reserve

ii. Reserve Forest /Protected

None

Forest:

OZ–1.13 km iii. Human Habitation:

iv. Railway Line: Palej:‐ 11.5 Km

v. Road: NH 48(NH‐8) – 10.7 km

vi. Notified / Protected

None

Archaeological sites:

vii. Social infrastructures, e.g. School(OZ) ‐ 1.13 km

School, hospital, historic / Temple(OZ) – 1.10 km

cultural / religious places etc.: Hospital(Palej) – 10.7 km

Presently there is no land use for any activities.

After grant of lease and EC. proponent will start land

14 Present land use of lease area. use for mining activities. The mining method will be

open cast mining and there will be permanent

change in land pattern.

As observed from nearby wells water table level in

the area is at around 30‐40 mts. Mining will not

reach up to that depth. Further There is no nallah 15 Geo‐Hydrological features existing near the clay area. The rain water

collected in pit, which recharge the area

It was observed that wind direction is

16 Predominant wind direction

predominantly from North & North East direction

Flora: Details on riparian vegetation, Baval

17 endemic / endangered species of flora Fauna: / fauna in the area Cow, Buffalo, sheep, Goat, Camel

No endangered species of flora / fauna in the area.

Width and condition of access road (

18 3.0 to 4.0 m aces road

pucca) to the lease area.

DETAILS ON MINING / EXCAVATION ACTIVITIES

Requirement of Power supply and its

19 No power requirement

source

Requirement of Water supply and its Requirement of water will be 5.0 KLD. and source is

20 source bore well nearby project area

Type of mining (Manual / Semi –

21 Semi ‐ mechanized

mechanized / Mechanized)

Equipment to be used (bulldozers, List of the equipment to be used.

22 hydraulic excavators, JCB, scrapers, 1. hydraulic excavators

loaders, diesel pumps, etc) 2. trolley mounted tractor

As it is open cast mining, manual as well as semi

mechanized methods will be used.

Ordinary Clay mining will be an open cast mining

Details of method of working with activity; in the first phase top soil will be removed

23 phasing of activates (sequence of and stacked for plantation purpose. Than

mining operations) overburden will be removed and stacked at

earmarked place.

It is open cast mining project and there is no need to Explosives, detonators to be used 24

use explosives and detonators.

Details of drilling, blasting 25 No drilling, blasting is required.

Safety measures at the time of 26 blasting N.A

Over burden in lease area will be in the form loose top soil and weathered upper layer of rocks. The soil

Details of Over Burden (OB) removal excavated will be dumped & preserved in the area 27 and stacking ear marked for soil dump & the dumping will be

carried out in the phase banner upto the height of

3m. This preserved soil will be used for plantation.

Height and width of benches and its 28 slop Bench of height 1 mt will be prepared

Data of the CGWB (Central Ground Water Board) for 29 Depth of ground water table (Meters) ground water table is mentioned is about 30 to 35

mts.

Maximum depth of working will be 3mts. No ground Maximum depth of working (Meters) 30 water intersection will be made. weather it will intersect ground water

table 31 Land use pattern of the lease area Non agriculture area for clay mining

32 Man power Requirement 8 to 9 person

33 No. of working days in year 250 days

34 Time of working hours in a day 6.00 AM. to 6.00 PM. / Sunrise to Sunset

ENVIRONMENTAL MANAGEMENT PLAN AND C.S.R. ACTIVITES Measures proposed for protection of

environmental attributes like , riparian Please refer in prefeasibility report for proposed 35

vegetation, water, air , human health impacts and mitigation.

etc.

Measures for control of noise, 36 vibration and fly rock problems due to Blasting is not required

blasting

Mitigation:

Details on transportation route & • Water is sprayed periodically to wet the road.

measures proposed for control of • Plantation of trees along the roads to help reduce 37

fugitive emission during the impact of dust in the nearby villages.

transportation • PUC certified heavy vehicles will be used for

transportation.

Plan for tree plantation in riparian As per attached Environment Management Plan. area / road sides in at least 20% of 38

lease area, numbers & types of species

and budgetary outlay for the same.

As per current mining plan there is no need for Plan, if any, for restoration / restoration or reclamation of mine, however at the

39

reclamation end of entire mine of life, area mined out will be

reused for agriculture purpose.

The proposed project will generate employment

opportunity for the local inhabitants. As a part of

Proposed CSR Activities and budgetary CSR activity, the proponent will expend approx.

40

outlay for the same. Rs.8000.00 annually for medical checkup camp,

scholarship to school students, drinking water

cooler etc.

41 NA Provision of fencing the pits in case of

use as water reservoir No green belt proposed. However plantation in Plan for green belt development, area lease area will be carried out as per attached of green belt, no & types of species to Environment Management Plan 42 be planted and budgetary outlay for

the same

Date: 02/08/2018 Place: Vadodara.

Signature of the Applicant (Dharmendra Chaturbhai Khabhati)

PREFEASIBILITY STUDY REPORT For

ORDINARY CLAY MINING PROJECT

BY

M/S. DHARMENDRA CHATURBHAI

KHABHATI

LOCATED AT VADODARA

AT

VILLAGE: OZ,

TALUKA: KARJAN, DIST.:VADODARA-393105

AUGUST 2018

1

INDEX

Sr. Section Details Page No. No. 1 Details of Proposed Project 3 1.1 Need of the Project 3 1.2 Screening Category 3 1.3 Location of the Proposed Project 4 1.4 Process Technology 6 1.5 Product Details 7 1.6 Cost of Proposed Project 7 1.7 Permission from Authorities 7 1.8 Resources Requirement 8 1.8.1 Raw Material 8 1.8.2 Electricity 8 1.8.3 Water 8 1.8.4 Fuel 8 1.8.5 Man Power 8 1.8.6 Land 8 1.8.7 Equipment / Machinery / Vessel / Reactor 9 1.9 Pollution Potential 9 2 Anticipated impact based on project operations on receiving Environment 10 2.1 Population 10 2.2 Flora and Fauna 10 2.3 Water 10 2.4 Air 11 3 Mitigation Measures 12 3.1 Wastewater Treatment and Disposal 12 3.2 Air Pollution Control Measures 12 3.3 Noise Control Measures 13 3.4 Solid /Hazardous Wastes Management System 13 3.5 Greenbelt Development 14 3.6 Hazards and Safety Measures 14 3.6.1 Mining safety guide 15 3.6.2 Excavation 16 3.6.3 Transportation Safety 17 3.6.4 Haulage (Pulling & Shifting) 18 3.6.5 The key points to ensure safety 18 3.6.6 Good Housekeeping 18 4 Environment Management Plan 19

2

1. Details of Proposed Project:

1.1. Need of the Project

The proposed mining project falls in the Vadodara District of South in the Gujarat State.

Gujarat is the one of the largest contributors of Industrial Growth in the nation.

The mining project will be done on Non–Agricultural land. For such type of mining project, the survey is being carried out by Geology Department of government to evaluate the probable reserve.

This natural clay from India are generally used in flooring, wall cladding, vanity tops and to pave the floors of large commercial complexes, hospitals, airports, shopping malls, railway station, parks etc.

1.2. Screening Category:

The mining of Bricks earth was not covered under environmental laws, since most of the bricks earth extraction work in the country is having mining activities in area less than 5 hectares and Ministry of Environment and Forests (MoEF), New Delhi had exempted areas less than 5 hectares for obtain environmental clearance. Now as per MoEF office memorandum dated 18th May, 2012, all the mining activities irrespective of the mining area are required to get Environmental Clearance form them before starting any mining activity and as per Office memorandum dated 24th June, 2013 and No. J-13012/12/2013-IA-II (I) dated 24th December, 2013 the acitvityies of borrowing/excavation of ordinary earth up to an area less than 5 hectares, comes under category ‘B2”. And Ministry of Environment and Forest and Climate change in pursuance of amendment dated 15-01-2016 has issued a notification no. S.O. 190 (E) dated 20-01-2016 Annexure ‘II’ constitutes the District Level Environment Impact Assessment Authority (DEIAA), for grant of

3

Environmental clearance for Category ‘B2’ Projects for mining of minor minerals, for all the districts in the country.

As per EIA Notification 14th September, 2006 & O.M. No-L-11011/47/2011-IA.II (M) dated 24 th June 2013 the proposed project falls under Schedule 1(a) & Category “B-2”.

As per MoEF office Memorandum no. L-11011/47/2011-IA.II (M) dated 24th June 2013 following conditions shall be followed during the mining activity:

 The activity associated with burrowing/excavation of brick earth and ordinary earth for purposed of brick manufacturing, construction of road, embankments etc. shall not involve blasting.

 The burrowing /excavation activity shall be restricted to a maximum depth of 2 M below general ground level at the site.

 The burrowing/excavation activity shall be restricted to 2 M above the ground water table at the site.

 A minimum distance of 15 m form any civil structure shall be dept form the periphery of any excavation area.

1.3 Location of the Proposed Project:

Project location is at Survey No. 344,1060,1061,1271,1272,1273,1274,1275,1276, 1277, 1307, 1308, 1309, 1314,1315,1316,1324,1325,1326,1327,1328,1331, Village-OZ, Tal.: Karjan, Dist.: Vadodara- 393105. The break-up of proposed Mining clay lease area is given as table no.1

Sr.No. Survey No. Address of Mining Area location (Hectares)

1 344,1060,1061,1271,1272,1273,1274, Village-OZ, Tal.: Karjan, 4.82.06 1275,1276, 1277, 1307, 1308, 1309, Dist.: Vadodara-393105. 1314,1315,1316, 1324,1325,1326, 1327, 1328,1331

4

The mining area is 04.82.06 Hactare Latitude 21.51’28.79 N & Longitude 73.09’38.64 E.

India Gujarat

Vadodara Location Site

5

Location site:

1.4 Process Technology (Manufacturing Process)

• Thorny bushes will be removed. Top soil should be removed and stored at boundary of the Mines. Remaining soil will be dig out and stored at the Mines site for refilling at the closer time.

• Earth-moving equipment such as scrapers and mechanical shovels are used to extract the clay. This clay is blending after transported from the pit by truck. The materials are stockpiled to enable blending of the various types of clay. The clays are fed separately by manually into mixing of clays follows to water addition.

• Than material is mixed in high-speed rollers which complete the grinding process. Bricks are hand formed, pressed or extruded into their final shape. The method used to shape the bricks affects their final appearance and texture, and sets certain limitations on the handling methods employed during manufacture. Wet clay bricks then pass though drying process.

• In the brick-making process, the clay is refined and water is added in order to mould the brick. Before the bricks can be fired, they must be dried properly in sun light to minimize the moisture up to 8% of volume for the clamp kiln. This wet bricks are fired in

6

conventional kiln process. Lignite is used as fuel. After complete the process, cool it & remove the finished bricks from the kiln. Generally next batch will be start after first batch.

• All around the excavated mines pit the Proper wire fencing is required to avoid falling of kids, cattle etc.

• Regular servicing of equipments/machineries will be carried-out to reduce Noise level.

Restoration Plan:

Including landscaping proposals, phasing and proposal for reuse of the area after quarrying or will be used as water reservoir and supply the water those who require.

Ancillary Work:

Transportation route will be marked for traffic regulation. Office building, stores for newly purchased spare parts as well as for used oil and tyre-tubes.

1.5 Product Details:

Mining of Ordinary Clay area.

SR NO. NAME OF PRODUCTS MONTHLY QUANTITY

1 MINING OF ORDINARY CLAY 20000 MT/MONTH

1.6 Cost of Project

The approx cost of the proposed project will be Rs. 10 Lac.

The details of the cost of the project is given delow:

Land & Building and

Plant & Machinery Rs. 10 Lcas

1.7 Permission from Authorities: Details are given in attached documents.

7

1.8 Resources:

As the proposed project will be required resource for production. The details of the resources given hereunder,

1.8.1 Raw Material requirement

1.8.2 Electricity

1.8.3 Water

1.8.4 Fuel requirement

1.8.5 Manpower

1.8.6 Land

1.8.7 Equipment / Machinery

1.8.1 Raw Material requirement

The project under consideration is project for Ordinary (Ordinary Bricks) Clay Mines for ecavation of soil clay so need of raw material will use like Natural clay, Water, Agro waste & fly ash. The final product will be Bricks which shall be marketed directly by road to various destinations.

1.8.2 Electricity

Source of Power supply: 5 HP, company Limited (MGVCL).

1.8.3 Water

Fresh water requirement will be 5000 Lit/Day for the proposed project. Out of this 2000 L/Day will be used for domestic purpose, 3000 L/Day for Dust Control Sprinkling System and greenbelt development purpose

1.8.4 Fuel Requirement

Not applicable

1.8.5 Man power

The proposed mining activity will provide employment of 6-9 full time person approximately.

1.8.6 Land

Project land is Private Land.

8

1.8.7 Equipment/ Machinery:

1. Wagon drill machine

2. Dozzer

3. JCB/Poclain

4. Crusher with conveyor belt

5. Water sprinkler system

6. Trucks for transportation of material

1.9 Pollution Potential:

1.9.1 Air Emission: Dust Emission during Mining, Transportation & which will be controlled by water sprinkling and development of Greenbelt area.

1.9.2 Industrial Water Pollution: Nil.

1.9.3 Hazardous Wastes Generation: Nil.

9

2. Anticipated impact based on project operations on receiving Environment

2.1 Population:

The project is micro level enterprise. Hence, the magnitude of impact is negligible. No influx of population is anticipated as only local labor shall be deployed.

2.2 Flora and Fauna:

No endangered Spp. Or forest within 10 KM radius. Surrounding land is wasteland. No farming in the surrounding. Very negligible impact on flora & fauna.

2.3 Water:

2.3.1 Water Consumption

2.3.2 Wastewater Generation

2.3.3 Rain Water Harvesting

2.3.1 Water Consumption:

2.3.2 Waste Water Generation:

Fresh water requirement will be 5000 L/Day for the proposed project. Out of this 2000 L/Day will be used for domestic purpose, 3000 L/Day for Dust Control Water Sprinkler and Greenbelt Development purpose. The detail breakup of the water consumption is given hereunder in Table:

The water consumption & waste water generation details:

Sr. Category Water Cosumption kl/day Waste water generation kl/day No.

1 Domestic 2.0 1.0

2 Industrial a. Processing 3.0 NIL

Total - INDUSTRIAL 3.0 NIL

Total – DOMESTIC + 5.0 1.0 INDUSTRIAL

10

1. There shall be no generation of industrial effluent from the Brick manufacturing and other ancillary industrial operations.

2. The quantity of the domestic waste water (sewage) shall not exceed 1000 lits/day.

3. Sewage shall be disposed in to the soak pit/septic tank system.

2.3.3 Rain Water Harvesting:

As the water is the basic natural resources and towards the step to resource conservation, rain water harvesting system is integrated in the project. Rain water will be percolate from the sides and the balance collected rain water will be lifted out and stored at storage tank for water sprinkling and greenbelt development.

2.4 Air:

The Impact on the air quality is divided in to two categories:

A. Impact on air quality during Mining phase

B. Impact on air quality during Transportation phase.

A. Impact on Air Quality during Construction Phase:

Minimum amount of air pollution will occur due to fly dust during Mining Phase.

B. Impact on Air Quality during Operation Phase:

Sources of Air Pollution

Dust generation during Mining, Transportation and Crushing/Screen of Minerals.

Impact on Environment

Minor increase of particulate matters in local environment.

11

3. Mitigation Measures:

Mitigation Measures

The proposed unit will provide adequate Environmental Management Plan to assure the regular and efficient working / operation of the same. The details of Environment Plan are described here under:

Objectives:

Regular and efficient working of the Operation with acceptable minimum Environmental Impact.

• To conserve the environment.

• To check and maintain the record of the environmental parameters for the further improvement of the process and environment.

• To comply with the Act, Rules, Notifications directly applicable to the Environment Management.

3.1 Wastewater Treatment System and Disposal:

A) Domestic Wastewater:

The generated 1000 Lit./Day of domestic waste water will be drained in to the Soak pit through septic tank.

B) Industrial Wastewater:

No industrial waste water will be generated from process as well as ancillary operations.

3.2 Air Pollution Control Measures:

A. Air pollution Control Measures during Construction Phases:

Minimum amount of air pollution will occur due to fly dust during construction of buildings which will be controlled by water sprinkling. Impact is Temporary and Short Term in nature.

B. Air pollution Control Measures during operation Phases:

Sources of Air Pollution

Dust generation during Mining, Transportation etc.

12

Impact on Environment:

Minor increase of particulate matters in local environment.

Control Measures:

• Sprinkling of water at Mining Area, Transportation etc.

• Adequate plantation will be provide to prevent dust dispersion.

Haul roads:

• All the haul and service roads shall be mettled and well maintained.

• Un-mettled haul roads shall be free of ruts and pot holes.

• All haul roads and surface roads shall be regularly sprayed with water.

• Plantation alongside haul roads (avenue plantation) shall be carried out done.

• Mined material receiving pits are shall be located close to the quarry to reduce the haul length of the dumper.

Overburden:

• Non-operative dumps shall be subjected to technical and biological reclamation.

• Plantation over and around over burden dumps shall be carried out to ensure stability of slopes, prevention of dust by wind action and soil erosion during the run off.

• Wetting of surface of O. B. dump shall be regularly practiced.

3.3 Noise Control Measures:

There are few potential sources such as Pump Operation, Vehicular Movement, etc. which would generate noise. Proper maintenance of all the equipments will be taken. Adequate encloser of stone crushing machine will be provided as well as personal protective equipment (PPE) like: ear muffs/ earplugs shall be given to workers during working.

3.4 Solid/Hazardous Wastes Management System

No hazardous waste generation

13

3.5. Greenbelt Development

In order to mitigate the air pollutants and to attenuate the noise generated by the plant and Also improving the ecology and aesthetics of the area, the unit will develop greenbelt area on the periphery of lease area.

3.6 Hazards and Safety Measures:

• All the personnel at the plant will be made aware about the operation hazards and risk associated with them.

• Safe work practices will be adopted to ensure the control of hazards during operation and maintenance.

• The workers will be made aware about the hazards associated with manual handling and operation.

• Safety measures in the form of ‘DO’ and ‘Don’t Do’ will be displayed at strategic locations especially in local language.

• Good housekeeping will be maintained in the Mining area.

• The required PPEs for each area/operation should be identified and the necessary PPEs, like, helmets, goggles, hand gloves, mask, suit, safety belts, ear muff and plug, etc. will be provided to the personnel.

• The plant will check and ensure that all instruments provided in the plant are in good condition and documented.

• First Aid box will be provided within the plant.

• List of important telephone numbers will be displayed at prominent location in the plant. Lease Holder Machine Operator Helper/ Labour

• All the accidents and incidents if any will be recorded, investigated and analysed in the proposed plant.

• Safety awareness program and trainings of the worker will be carried out to motivate the workers to increase the safety level at personal level.

Occupational Health Aspect: As per govt. standard all facilities will be provided.

Safety Precautions:

• Adequate fencing would be provided against protection of human beings and animals in deep pit of mine.

14

3.6.1 Mining Safety Guide:

Company will follow the below guidelines during Mining Activity:

Area wise hazards:

• Bulk storage of raw material – Hazard of dust

• Crusher/Screen plant- Dust emission, Noise generation

• Mixtures and drives – Crush injuries

• Loading and unloading – Dust

• Transportation – Air pollution because of fossil fuel combustion and dust emission too.

• Drilling- Dust emission

General Considerations:

1. Adequate lighting,

2. Ventilation to supply fresh air,

3. Electricity,

4. Dust control i.e. Controlling dust within safe limits,

a) Rock dust containing silica and quartz may cause silicosis.

b) It is advisable to use Electrostatic filters to reduce air pollution.

5. Continuous safety of people at work,

6. Survey of hazards of fall of persons, soil, material, etc.

7. Warning signs and notices,

8. Safe means of access,

9. Emergency generators,

10. Sufficient lighting will be provided for night work,

11. Means of escape and ladder from bottom to top will be provided in addition to any mechanical means of ingress and egress,

12. Employment of trained workers and further training to them,

15

13. Safe guarding of dangerous parts of machinery,

14. Proper drainage and de-watering system (if require),

15. Wet drilling for dust control,

16. Separate transport vehicles for explosives and detonators, separate storage facility beyond 100m from lease area and their separate magazines,

17. Lubricating oils, grease and rope dressings will be kept in closed metal containers,

18. Lighting arresters will be provided on the surface,

19. Emergency lighting to function for a long time (to escape safely) will be provided,

20. To avoid any damage or accident during natural calamities like cyclone, flood, cloud bursting, earthquake, etc. sound construction of housing facility will be provided to workers,

21. Medical center with first-aid facilities will be provided,

22. Important telephone numbers (Police, Ambulance, Fire, nearest Primary Health Center)

Personal Protection Equipments:

1. Helmets

2. Gum-boots

3. Face shield

4. Hand gloves

5. Safety goggles

6. Full body harness

3.6.2 Excavation:

General precautions for any excavation or underground work are:

1. Stability of ground

2. Position of public utility services such as electric or telephone cables, water, sewers line, etc. (Relocation, isolation or protection of underground utilities should be done with due permission.)

16

3. Effect on adjoining building, structure, roadways, bridges, etc.

4. No load or vehicles should be moved or stacked near the edge of excavation to prevent the side- collapsing.

5. All sides will be fenced by barrier at least up to 1m and danger notice, red signal and light will be provided. Sides of all excavation must be sloped to a safe angle not steeper than the angle of repose of a particular soil/rock.

6. Cutting will be done from top to bottom. No undercutting of side will be allowed.

7. Road barrier at a distance will be provided if road is to be blocked.

3.6.3 Transportation Safety:

1. Vehicles must be checked for:

a) Warning sirens,

b) Horns (loud and clear),

c) Lights (head-lights, tail-lights),

d) Signals,

e) Reverse alarm,

f) Vehicles will not run overloading and over speeding

g) Smokeless locomotives will be used.

2. Other important considerations:

a) Rules for driving will be enforced

b) Cabins of excavators in quarries will be partially closed and drivers should be supplied air mask

c) Water spray to dusty processes and to conveyor belts including their drives and transfer points.

17

3.6.4 Haulage (pulling and shifting):

• Material carried out mechanically.

• Workers will not be transported along with the material.

• Speedy removal of derbies, refuse and trash.

• Safe and adequate walkways.

3.6.5 The key points to ensure safety are:

a) Clearing employees from the mining area,

b) Effective access control,

c) Efficient communications,

d) Training

3.6.6 Good Housekeeping:

The term Good Housekeeping is often loosely understood as simple floor cleaning or broom stick operation. But it has even wider meaning including up keeping of all industrial activities in orderly manner to minimize the accidents due to improper planning, placement, arrangement, handling, etc. everywhere in industrial premises. “Place for everything and everything on proper place”. So, Good housekeeping at quarry site will greatly reduce unsafe conditions and so risk of accidents.

18

4.Environment Management Plan:

The proposed unit will provide/prepare an adequate Environmental Management Cell to assure the regular and efficient working /operation as given here below:

• The Environment Management Plan (EMP) is required to ensure sustainable development in the area of the proposed project. Hence it needs to be all encompassive plans for which the industry, Government, Regulating agencies like Pollution Control Board working in the region and more importantly the population of the area need to extend their co-operation and contribution. • Mitigation measures for each of the activities causing the environmental impact.  • Monitoring plans for checking activities and environmental parameters and monitoring responsibilities.  • Role responsibilities and resource allocation for monitoring.  • Following sections describes the environment management plan proposed for site clearing and Mining phases.    MITIGATION MEASURES:-

• Each of the activities during production phase is critically Reviewed for suggestion of mitigation measures. Based on This the Table 1 to 6 gives the mitigation measures for the Activities considered being causing significant Environmental impacts during production phase of every Year.

19

Table: - 1 Environment Management Plan:-

Activity Environmental Mitigation Remarks Impacts

Mining Water spraying by Implementation process sprinkle to control responsibility: Project micro particles of Proponent Air mineral and dust. Ensure uses of personal protective equipments. (PPE's)

No waste water management. Water Install proper facilities to prevent rain / storm water.

Ensure uses of personal protective Land equipments (PPE's). Manage proper storage of bricks

Ensure proper maintenance of Noise machinery to reduce noise level

20

Table: - 2 Environment Management Plan:-

Activity Environmental Mitigation Remarks

Impacts

Storage of all the Air To be stored in Implementation Waste materials Water accordance with responsibility: and products. Land the rules and Project Proponent regulation of the As per Department.

Separate storage area for products.

Install proper facilities to prevent

rain / storm water

contamination

during the storage

of solid prepared

products.

Trained / approved

transports will be

given work for the

transportation of the products.

Land Well maintained vehicles will be used. Metalled Road for vehicle movement. Top soil will be conserved and be utilized for greenbelt on area.

21

Table: - 3 Environment Management Plan:-Other Facilities:-

Activity Environmental Mitigation Remarks

Impacts

Toilets Water Ensure proper Implementation sewage disposal. responsibility: Project Proponent Development and Air. Ensure maintenance of Land development and green belt maintenance of proper green belt as

proposed.

Direct / Indirect Socio- economic Continue policy of Employment issue local employment according to the skill and availability

Environmental Monitoring Plan:-

Environment monitoring plan is given in table 5 as follows: Table No. 4

Sr.No. Activity Schedule Air Pollution Monitoring

1 Ambient air monitoring of parameters specified Once every Calendar Year by GPCB in their air consents from time to time within the Proposed premises

Water Pollution Monitoring

1 No waste water Produced N.A. Solid Waste Generation Monitoring / Record Keeping

1 No Solid Waste Generation. N.A.

22

Expenditure on Environmental Matters:-

The following table gives the expenditure to be incurred by Proponent on environmental matters. Table No. 5

Sr. Description Approximate Approximate

No. Recurring cost per Capital Cost annum (Rs. In lacs) (Rs. In Lacs)

1 Air pollution control 0.40 0.50

2 Water pollution control 0.10 ---

3 Environment monitoring and 0.45 0.55 management

4 Solid and hazardous waste 0.10 -- management

5 Noise pollution control 0.10 0.20

6 Occupational health 1.00 1.10

7 Green belt 0.80 0.90

Total 2.95 3.25

23

Table No. 6: vegetation

Name of Sensitive / Height No. of Amount to the trees tolerant to Threes to be Spent air be planted pollution

Neem Tolerant 10-15 m 10 0.30 Lacs

Asopalav Tolerant 10-15 m 10

Peepal Tolerant 10-15 m 10

Local species Tolerant 5-10 m 10

Total 40 0.30 Lacs

24

M/S. DHARMENDRA CHATURBHAI KHABHATI (DCK)

Village-OZ, Tal.: Karjan, Dist.: Vadodara-393105. (M) 9824421292. E-mail: [email protected]

MINING PLANT IS NOT APPLICABLE....

For DHARMENDRA CHATURBHAI KHABHATI(DCK).

Authorised Signature Dharmendra C. Khabhati

M/S. DHARMENDRA CHATURBHAI KHABHATI (DCK)

Village-OZ, Tal.: Karjan, Dist.: Vadodara-393105. (M) 9824421292. E-mail: [email protected]

Environmental Impact Assessment:

We are applied for Ordinary Clay Mining project which lease area is 04.82.06 ha (which is < 25 ha) and under B2 Category. So, TOR (Terms of Reference), Public Hearing, and EIA is not applicable. DISTRICT SURVEY REPORT

1. INTRODUCTION

Vadodara district with 7548.50 Sq km area, is located central part of mainland Gujarat, lies between 21°49‟19” and 22°48‟37” north latitude and 72°51‟05”and 74°16‟55” east longitude. It falls in the Survey of India, degree sheets numbered 46B, 46F, 46J & 46G. The district is bounded in north & northeast by Anand, Panchmahals & Dahod districts, in east & in south east by Madhya Pardesh & Maharashtra State, in south east by Narmada district & in south & in west by Bharuch district. Vadodara city, the district headquarter is about 100 km south of Ahmedabad, is well connected to other parts of the State & Country by network of highways and railway network. (Location Map, Fig No. 1).

Location Map of Vadodara District

Major Road - Highways

t

c

i

r Railway Lines

t 0km 10km 20km D

s a

i h o

d D D P i a s

n t c r d i h c

m t n h

al a s

Di s n t

ri

c

t

A

Vadodara

h es d ra P ya dh

Ma

B

h a N

r a u t r

c ic e m a

h t a r

is d t h D D a s

i a s h r t c D u i a e r s h

i a t

c h r a t i B c

t M

Figure 1. Location map of Vadodara district

Vadodara district is divided 12 taluaks. Details of the Talukas, their urban & rural areas and numbers of revenue villages & towns etc., are given in Table – 1 Map showing its administrative units as Taluka & their headquarter is given as Fig –2. Table : 1 Details of Taluka area & Nos. of Towns & Villages

Sr. Taluka Area Urban Rural No. No. No

(Sq.km) (Sq.km) (Sq.km) Town Villages

1 Chhota Udaipur 765.4563 4.0099 761.4464 1 144

2 Dabhoi 632.1895 23.82 608.3695 1 118

3 Jetpur 805.64 4.4098 801.2302 1 212

4 Karjan 601.8724 15.7094 586.163 1 93

5 Kawant 607.762 2.0399 605.7221 1 132

6 Naswadi 535.1656 0 535.1656 0 219

7 Padra 534.7288 12.8331 521.8957 1 82

8 Sankheda 722.6128 31.8354 690.7774 3 182

9 Savli 791.9973 0 791.9973 0 137

10 Shinor 292.5048 16.1894 276.3154 1 40

11 Vadodara 693.4307 213.8801 479.5506 9 91

12 Vaghodiya 565.1405 15.0595 550.081 1 95

Total 7548.5007 339.7865 7208.7142 20 1545

Figure No. 2 Administrative Unit Map – Vadodara District

22.75 Map of Vadodara District

Admn. Units & District / Taluka HQ

Talluka HQ. District HQ

Savli

22.5

0 km 10 km 20 km

Jetpur Pavi

Vadodara

Vaghoriya Chota Udaipur

22.25

Padra

Sankheda

Dabhoi

Kawant Karjan Naswadi

22

Sinor

73 73.25 73.5 73.75 74 74.25

1.1. DEMOGRAPHIC PERTICULARS According to the 2001 census, total population of

Vadodara District is 3,639,775 persons. Out of these District Area

nearly 53.47 % of Rural Population is spread in 1545 5%

villages having total areas of 7208.71 sq.km while 46.53

95 % of urban population spread is in 20 towns & 11 urban %

agglomerate, having total areas of 339.78 sq,km. The

density of population in rural area is 268 persons per

Rural Urban

sq.km while in urban area it is around 5,029 persons per

sq.km while as a whole district it is 489 persons per sq.km.

(Table 2). As per 2001 census report, Vadodara taluka area is one of the most urbanized talukas of the State, have 87.49 % urban population with average population density of 6,978 persons per Sq.km.

Table No.2 Area & Population

Area in Hectares (2001 Census) District Population Urban 720871.42

Rural 33978.65

Total District 754850.07 47%

Population Nos. (2001 Census)

Urban 1932976

Rural 1708826 53%

Total District 3641802

Population Density ( Nos / hectares)

Urban 268 Rural Urban

Rural 5029

Total District 482

The district had decadal growth of population of around 28 % during 1961 to 1981, which declined to around 20 % during last two decades. (Figure 3)

Figure : 3 Decannial Growth of Population

4.00 35.00

3.50 30.00

3.00

25.00

2.50

20.00

2.00

15.00

1.50

10.00

1.00

Decannial Growth % Population In Million In Population

5.00

0.50

0.00 0.00

1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

The tribal population of Vadodara district is mostly located in eastern hilly terrain of the districts, which is a continuous part of tribal belt of Gujarat State covering all boarder areas along neighboring States of

Details of ST, SC & General Population Madhya Pradesh &

Maharashtra. As per 2001

4000000 3641802

census, percentage of tribal

3000000 2470124

population to total population

2000000

is 26.56 % while percentage 967393

1000000 204285 of scheduled caste population

0 to total population is 5.61 %

Total ST SC General

while rest, 67.83 % is general

population.

1.2. LAND USE PATTERNS, IRRIGATION & AGRICULTURE 1 Seasons & Crops Record , Vadodara District -year 2001-02, has been refereed for land use, irrigation & agriculture statistics of the district.

1.4.1. Land Use Patterns As per Seasons & Crops Record, 7,52,776 hectares of land is accounted for land use record. Brief account of land use classification for the district, in general, is given in table No.3 . Table No. 3 Land Use Classification of Vadodara District (2001-02)

Sr No Land Use Classification Area in Hectare 1 Area Reported for Land Use 7,52,776 2 Forest 79,667 3 Total Uncultivable area 1,25,931 4 Culturable Waste 6,724 5 Cultivated Area ( 1 - 2 – 3 – 4 ) 5,40,454 6 Cultivable Area ( 5 + 4 ) 5,47,178 7 Current Fallow 20,188 8 Net Area Sown ( 5 -7) 5,20,266 9 Area Shown More Than Once 43,777 10 Total Cropped Area ( 8 + 9 ) 5,64,043 11 Net Area Irrigated 1,99,808 12 Area Irrigated More Than Once 36,052 13 Gross Area Irrigated ( 11 + 12 ) 2,35,860

Land Use Category

Cropped & Irrigated Area

547,178

600000 520,991 Cultivable

500000 547,178

400000 Uncultiva 72% ble

300000

125,931 199,808

200000 17%

100000

Forest in Hecatres Area 0 79,667 Cultivable Net Cropped Net Irrigated 11%

1.4.2. Irrigation 1 Table No. 4 Structure for Irrigation & Other Uses Details of water supply sources and irrigation structures etc., and area Sr.No Structure Nos. irrigated by various sources are in table 1 Tank for Irrigation 24

No. 4 while details of area irrigated by 2 Non Irrigation Tank 1,569 surface & ground water resources are 3 Canal No. / Length km 7 / 65 given in table No 5 4 Lift Irrigation Sources 4

5 Tube Wells for Irrigation 1,676

6 Dug Wells for Irrigation 18,015

7 Domestic Wells 9,773

8 Abandoned Wells 3,056

9 No. of Oil Engines 7,564

10 No. of Electric Pump 12,933

1 Land Use & Season –Crop Record – Vadodara District – Year 2001-02 – Agriculture Directorate, Government of Gujarat.

1 Table No. 5 Details of Irrigated Areas

Irrigated Area (Hectares) Source

Irrigation by Sources

Net MTO * Gross

Tanks 3,642 523 4,165 5%

Canals 4,073 745 4,818

Lift & Flow Irrigation 2,283 238 2,521

Total Surface Water 9,998 1,506 11,504

95%

Govt. Tube Wells 19,029 3,086 22,115 Ground Water Irri Pvt. Tube Wells 71,705 6,867 78,572 Surface Water Irri

Dug Wells 99,076 24,593 123,669

Total Ground Water 189,810 34,545 224,355

Total Irrigated Area 199,808 36,052 235,860

* MTO – more than once

1.4.3. Agriculture The district areas have varied agriculture crops, both food crops & non food crops. Main food crops consist of food grains such as paddy, wheat, jowar, bajra, maize etc., and

pulses. Other food crops are 500 sugarcane, fruits &

400 vegetables. Non food crops

100 fodder etc. As per Season & 300 consists of cotton, oil

200 ground nut, castor, tobacco,

1 0 Crops Records, there were

Kharif 5,64,043 hectares of gross

Rabi

Hot area under various crops in

the district, out these

Gross Cropped Area Gross Irrigated Area

2,35,860 hectares were

under irrigated crops. Figure

Hot seasons. Details of areas shows further subgroups under Kharif, Rabi & under various food crop & non food crop of the district are given in table No 6 Table No .6 Details of Areas under Food & Non-food Crops & Irrigation

Kharif Rabi Hot Total

Irrigated Area * 70413 47604 5448 123465

Food Crop : Paddy,

Wheat & other cereals, Non Irrigated 179389 20153 0 199542

pulses, vegetables, Area*

Total Cropped fruits etc. 249802 67757 5448 323007

Area *

Non Food Crop : Irrigated Area * 99409 5593 7393 112395

Cotton, Oil seeds,

Non Irrigated tobacco, fodder etc. 126309 2332 0 128641

Area*

Total Cropped

225718 7925 7393 241036

Area*

Gross Cropped Area * 475520 75682 12841 564043

Gross Irrigated Area * 169822 53197 12841 235860

* Area in Hectares

1.14.4. Urban and Industrial area

Vadodara district is one of the most industrially developed areas the state. It has many Strategic Industries, such as oil refinery, petrochemical complex, fertilizers, and heavy water project etc., located around areas of Vadodara Taluka. Other important industries are of metal product, rubber& plastic, non- metallic mineral product, pharmaceuticals, engineering & machinery parts etc. Besides these, there are many industrial notified area in various Taluka areas of the district of which 8 are established and managed by Gujarat Industrial Development Corporation Ltd. (GIDC Ltd).

2. HYDROMETEOROL OGY

2.1. CLIMATE Vadodara district area, in general, being located south of Tropic of Cancer and in transition zone of heavy rainfall areas of South Gujarat and arid areas of North Gujarat plains, have sub-tropical climate with moderate humidity. The various season of the year are (a) monsoon - middle of June to October, (b) winter - November to February, and (c) summer – March to June. From March onward the temperature starts rising till it reaches maximum, as high as 41° C in some parts of the district. January is the coldest month of the year.

There is a Indian Meteorological Department (IMD) station located at Baroda (Vadodara), where observation of climatic data is recorded since 1900. Details of this climatological data is given in table No. 2.1 and same is depicted graphically in figure No. 2.1

Table No. 2.1 - Climatological Data of IMD Station –( Baroda) - Vadodara

Max Solar

Mini Wind Sun

Temp Humidity Rad. Eto Rainfall

Month Temp Spd. shine

(Deg.C (%) (MJ/m2/ (mm/d) (mm)

(Deg.C) Kmpd (Hours)

) d)

January 30.30 12.00 50.00 65.80 9.10 17.23 3.02 1.20

February 33.00 13.80 43.00 67.50 9.70 20.07 3.81 0.60

March 37.10 18.40 36.50 69.10 10.20 23.16 4.88 2.20

April 40.20 22.90 36.50 79.00 10.80 25.75 6.03 0.90

May 40.90 26.50 44.50 143.20 10.90 26.38 7.46 4.40

June 37.10 27.00 63.50 169.50 7.10 20.62 5.97 146.80

July 32.70 25.70 80.00 138.20 4.40 16.51 4.11 297.60

August 31.50 25.00 82.00 116.80 4.50 16.32 3.82 284.70

September 33.20 24.30 74.50 83.90 6.90 18.87 4.28 141.70

October 36.00 21.30 58.00 49.40 9.30 20.24 4.12 22.00

November 34.30 16.70 52.50 49.40 9.40 18.02 3.24 16.20 December 31.20 13.40 55.00 59.20 9.10 16.50 2.83 4.40

Total ------922.70

Average 34.79 20.58 56.33 90.92 8.45 19.97 4.46 -

Figure No 2.1 - Plot of Climatological Data – (Baroda) –Vadodara IMD Station

90.00 350.00

80.00

300.00

70.00

250.00

60.00

200.00 50.00

40.00 150.00

30.00

100.00

20.00

Climatiological Parameter Climatiological Rainfall 50.00

10.00

0.00 0.00

January March May July September November

Rainfall (mm) Max Temp (°C) Min Temp (°C) Rel Humidity (%) Eto (mm/d)

3. GEOMORPHOLOGY

3.1. PHYSIOGRAPHY Vadodara district forms a part of the great Gujarat plain. The eastern portion of the district comprising the Chhota Udepur, the Kavant, the Jambughoda and the Naswadi taluka is hilly terrain with several ridges, plateaus and isolated relict hills have elevation in range of 150 to 481 m amsl. The south eastern plateau have the highest peaks of the district – Amba Dungar & Mandai Dongar 637 m amsl. The rest of the district, the western & southern part, comprising of Mahi & Narmada Doab, is a level plain with gentle undulating terrain have elevation in range of 120 to 20 m amsl . The overall elevation ranges from 610m in east to 20 m amsl in south-west

The most of the western part, comprising of Mahi – Narmada Doab and northern alluvial plain is more or less level terrain, have elevation in range from 20 to 80 m amsl. There are some linear tracts, along Mahi, Viswamitre, Dhadahar and Orsang rivers, have ravine landforms, with typical head ward erosional featured gully formation in soft alluvium. The banks of the Mahi has high vertical cliff , 10 to 25 m height, generally on left bank; same way left bank of the Narmada also has high cliff of 10 to 20 m high on right bank. All such features of Mahi-Narmada Doab, like ravine features, high cliff along banks and entrenched meandering courses with dry and wide sandy river bed of intermediate independent river systems of the Dhadhar & its tributaries indicate mature river stage and also tectonic uplift of Doab portion in Recent geological past.

The central part of the district is low level undulating plain with low level plateau and few relict hills. The area between the Unch and the Orsang river have aeolian low level stabilized dune with rolling topography. The hilly terrains of north - eastern part have residual hill features with more or less flat topped plateau. Except few volcanic peaks – Phenai Mata Hills and Amba Dungar, all have plateau or ridge type features and are few tens of meter height than surrounding rocky dissected plain. The highest plateaus are in south eastern part of the district, marked with rift valley of the Narmada River towards south. Figure No. 3.1 The physiographic map of the district

22.75

Map of Vadodara District

Physiograpy

Mud Flats Ravines

Northern 22.5 0km 10km 20km Alluvial

Plain

North - Eastern

Hilly Terrain

Intermediate 22.25 Ridges - Plateaue &

- Undulating Plains &

i Relict Hills

h a Low Level Plateau

a d

a

M m

r b

a a

o

a &

22 N st e e r u

D r o ea

F t

la P

h

A ig

H

73 73.25 73.5 73.75 74 74.25

3.2. DRAINAGE

The Narmada and the Mahi are the chief rivers of the district, flow along the northwestern and southern boundary respectively while independent small river system of the Dhadhar with its numerous tributaries flow in south central part of the district. Broadly, the entire district, as a River Basin is divided into these three basin, namely the Narmada, the Mahi Basin and the Dhadhar. The Mesari, the Goma and the Karad are the small rivers flowing northwest part of the district, are tributaries of , and are part of the Mahi Basin. The Jambuva, the Surya, the Viswamitre and the Dhadhar, which flow through central part of the district and empty into the Gulf of Khambat, are part of the Dhadhar Basin. The eastern and the southern part of the district, drained by the Narmada River and its tributaries, like the Unch, the Heran, the Dev, the Orsang, the Karjan, the Aswan and the Bhukhi, constitutes the Narmada basin. (Drainage & Basin Map in figure No. 3.2)

Figure No. 3.2 Drainage & Basin Map of Vadodara District

22.75 Map of Vadodara District

Drainage & Basin

Mahi Basin Dhadhar Basin Narmada Basin

22.5

0km 10km 20km

r

e

iv

R r r i e

v iv h R

g

22.25 a i R an

r rs

i t M m er O iv

a r R

w ha h d ha

i s D

er

n Riv

ra

He

22

r

e v r i e R iv

a R d a a d

rm a

a rm N a

N 73 73.25 73.5 73.75 74 74.25

3.3. SOILS The soils2 of Vadodara district can be broadly classified into three groups. They are black soils, alluvial soils and hilly soils. Soil map of the district is given as figure no 3.3.

Figure No. 3.3 Soil Map of Vadodara District

22.75 Map of Vadodara District Soil Map

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

Aluvium Soil Deep Black Soil Legend Medium Black Soil Shallow Black Soil Hilly Soil

2 Technical Bulletin- Revised (No. 11) – May 1992 ; Agriculture Information, Directorate of Agriculture, Government of Gujarat, Ahmedabad.

4. HYDROLOGY

4.1. SURFACE WATER RESOURCES Vadodara district has huge potential of Surface Water Resources, but the irrigation potential created through various sources was only 11,504 hectare according to 1 Season & Crops Report (2001-02) . Till 2003, scope of canal irrigation was limited in spite of the fact that the district has the advantage of having two major river, the Narmada and the Mahi on its borders, besides smaller rives like the Viswamitri, the Orsang, the Heran, the Dadhar etc. Recently, water of the Narmada river have been harnessed by Sardar Sarovar Dam and consequently large part of the district now forms a part of Narmada Canal Command. The dam constructed on Mahi at Kadana and Weir at Wanakbori did not produced any direct surface water resources benefit for irrigation in parts of Vadodara district as such Mahi Project command areas falls in neighboring Anand & Kheda district. However, surface water release, from Kadana Dam through Wanakbori weir during lean season, satisfy huge demands of Vadodara City and surrounding many Strategic Industrial Units for their domestic and industrial requirement.

Besides these two major rivers, other rivers of the district such as the Orsang and the Heran do sustain some base flow upto February / March which is being utilized for supplement irrigation at places along their course at suitable places.

5. GEOLOGY

5.1. STRATIGRAPHIC SET UP The rocks of the Vadodara district shows an age from Proterozoic to Recent but a striking features of the district stratigraphy is the total absence of Paleozoic, and the development of only the uppermost Mesozoic rocks. The south westerly extended Precambrian basement of Peninsular India, the oldest rocks of Proterozoic age, are exposed in eastern and north eastern part of the district. Post Cretaceous sediments & major volcanic rocks rest over this south westerly extended Precambrian basement. Post Cretaceous sediments, Infratrappean and Intratrappean are exposed as scattered inliers while younger volcanic rocks unit as Deccan trap is well represented and so are the Tertiary and Quaternary, though the Tertiary records are not complete and fully exposed. The stratigraphic outline of the district is given in table no. 5.1.

Table No. 5.1 Stratigraphic outline of the Vadodara District

Continental sediments – fluvio-marine, fluvial and aeolian Quaternary Marine and fluvio-marine sediments Tertiary

……………………………………Unconformity……………………………………………….

Basalts of the Deccan Trap with associated differentiates and Upper Cretaceous to Lower intrusive bodies Eocene

……………………………………Unconformity……………………………………………….

Marine, fluvio-marine and fluvial sediments Cretaceous

……………………………………Unconformity……………………………………………….

Crystalline rocks -Metasediments associated with granite, Precambrian (Aravalli) gneiss and other mafic rocks 5.2. SUBSURFACE GEOLOGY 5.2.1. Exploration Details The boreholes drilled by CGWB and erstwhile ETO, as a part of Ground Water Exploration work, in various parts of Vadodara district have revealed the sub surface geological formation in the district. ETO have drilled few boreholes in parts of the district and adjoining Bharuch & Kheda during under various program. Then CGWB have drilled 14 Boreholes in ‟Outfall Area of Narmada Project‟ (1972-1978) in parts of Vadodara district & Bharuch district. Then under piezometer construction program, few bore holes were drilled in parts of Padara, Karjan, Dabhoi, Vadodara & Savli Taluka areas during 1988 -90. Recently exploration in hard rock areas of northern & eastern parts of the district has been under progress since 2002-04. Map showing locations of all such sites is given as figure No. 5.1

Figure No. 5.1 Location of Exploratory Wells & Piezometers

EW & OW

22.75 Map of Vadodara District

Vejpur

Location of EW & PZ

EW

EW PZ

EW -1 -3 Sandhsal

EW & OW Section Line Rasulpur EW Vasanpur EW Pz - 1-2

Nava Wankaner Moti Bhadol 0km 10km 20km 22.5 Gahntiyal Pz - 1-2

EW & OW

Sankarda Khed Karmsiya

Pz -- II Pz Pz - 1-2

Vadodara Ii Chota udepur

Raypura EW EW

22.25 Pz - 1-2 EW

Pz - 1-2 Palaswada Tawa

Ghayaj Alamgir EW EW & OW EW 1-4

Pz Chitral Sarsvani EW 1-2 Akoti Karanjwant EW EW 1-2 Tokri Mobha EW EW EW

Pz - 1-3EW Chatral Pz EW

Bamangam EW Bhakha Gozariya HandodKurai EW Vadoj Kharmada Reand Pz - 1-2 EW EW Pz - 1-2 Palasni EW 1-7 Raysingpura Teantalao

Kurali 22 Timbarva Segwa EW & OW EW 1 -2 Niasariya EW

Kia Tanakhala Pz - 1- 2 Maletha

EW Haldarwa

Malod

73 73.25 73.5 73.75 74 74.25

6. HYDROGEOLOGY

6.1. OCCURRENCE & DISTRIBUTION OF GROUNDWATER In Vadodara district area, groundwater occurs both as unconfined and confined conditions. Saturated zones of unconsolidated shallow alluvium and weathered zones, shallow depth jointed and fractured rocks forms unconfined aquifers, whereas multilayered aquifer below impervious clay horizons in alluvium formation and interflow zones of basalts, inter-trappean beds, deep seated fracture zones, shear zones in basalts, granites and gneisses give rise to semi confined to confined conditions.

Generally the water table follows topographic configuration. The depth to water is greater in upland areas whereas in valley portion and shallow grounds, the levels are very close to surface. In hilly terrain of eastern, north- east and south-east part of the district, spring zones are seen in stream river section; also along the section of the Mahi, the Narmada and the Orsang rivers. The piezometric surface, mainly in alluvium areas of western half the district also follows the gentle gradient corresponding to subsurface configuration of deep aquifer zones.

In major part of the district, in north and almost in eastern half of the district, the hard rocks, such as phyllite, schist, granite, gneiss, basalt and other sediments such as sandstone, limestone etc., form aquifers, whereas multilayered alluvium deposits form aquifer system in remaining central, south-central and western half

of the district. The weathered basalts, granite, gneiss etc., covered by soil / muram and the valley fill & piedmont deposits forms potential aquifer in the vicinity of rivers and on vast undulating plains adjacent to hilly terrain but their regional continuity and extent are limited due to heterogeneous nature of deposits with limited thickness and as such rarely exceed a few square kilometers. Map showing general hydrogeology of the district is given as figure no. 6.1.

Figure 6.1 Hydrogeological Map of Vadodara District.

Plate No. I

GUJARAT

VADODARA DISTRICT

LEGEND HYDROGEOLOGY Aluvium - Sand, silt, caly,

gravels, kankars, etc.

Large to moderate yield prospect ; Tube wells & dug cum bore

22.75 Discharge : 750 to 1500 lpm

Quality variable slight brackish

to saline at depth

SCALE

0KM 5KM 10KM 15KM 20KM Deccan trap- Basalts,

& Infratrappean Moderate to low yield prospect ;

Dug & dug cum bore - EM & Oil engine

Discharge : 100 to 500 lpm

Quality good ; with in

permissible limit

22.5

Granite - Gneiss

& Meta Sediments,

Schist, Phyllite, Quartzite,

Dolomite, etc.

Low to medium yield prospect ;

Dug well with oil engine & EM Discharge : 50 to 200 lpm ;

Quality good ; with in

permissble limit

National Hydrograph Network Station

22.25

GW Exploration Site

Raingauge Station

Water Body & Stream / River course

0

Water Table contour 5 0

0 0 EC - Iso Con line 2 0

0 Isohyets 8 22

73 73.25 73.5 73.75 74 74.25 Vadodara District Hydrogeology Report (2005) P.R.Gupte - Jr. Hydrogeologist

6.2. GROUND WATER STRUCTURES Vadodara district area has varied ground water extraction structures, appropriate to different hydrogeological units and necessity. Various types of dug wells (DW) are common to both alluvial / soft rock areas and also in hard rock areas. In unconsolidated formation the depth of dug well is few meter to more than 25 m; while in hard rock areas, generally their depth depends upon weathering zone, through which they have curbing and below it have naked zone. With declining water levels along with rapid development, bore well of 30 to 90 m depth are drilled at bottom of dried up dug well section and such well are termed as dug cum bore well (DCB well), are common in both unconsolidated & consolidated formation of the district. In consolidated rock units, especially in Deccan Trap areas, horizontal bores at the bottom of the well, with gentle gradient towards well are common. Large dia, collector type wells, generally for regional water supply or for industrial uses are common in sandy beds of Mahi and Orsang rivers. To meet large demands bore well / tube wells are common structures. There are shallow bore wells up to 60 to 80 m depth both in consolidated and unconsolidated areas. Such bore well, in hard rock areas are drilled for hand pump and also for irrigation purposes. In unconsolidated arrears, in areas of Quaternary

alluvial deposits having deep aquifer, deep tube wells up to 200 m depth are common.

6.3. GROUNDWATER REGIME MONITORING Ground water regime monitoring is the basic component of groundwater management, and it is carried out in parts of Vadodara district through National Hydrograph Network Stations (NHNS or NHS). NHSs are observation wells, consisting of dug wells and purpose built bore wells – known as piezometers. There are 36 NHS as shown in Map of NHS in figure no 6.1. Through these observation wells ground water levels are monitored four times of each year. Water samples are collected during pre-monsoon period i.e., during May monitoring and is subjected to complete chemical analysis to know its chemical constituents

Figure No. 6.1 Map showing location of NHS

Map of Vadodara District

22.75

Vejpur2 Location of NHS

Chhaliyar Wells Piezometers

Rasulpur

Nava WankanerGothada 22.5 0km 10km 20km Kevadi

Juna samalya

Tundav Vadala

Jojh Sankarda

Asoj Karamasiya

Chisadia

Asala

Ghamodi Ferkuva

Pavi

Baroda

Vadodara Ii ChhotaChotaudepur

Raypura Baroda1 Saidal Suskal

22.25 Patiyapura Bodeli

Pitha Alladpur

Amreshwar Makni

Ghayaj

Govindpura Bhindol Panwad

Chitral Kalitalavdi Chavaria

Vega Tokri

Masor Dabhoi Baladgam

Devat (thadgam)

Handod Vadoj Waghach Vagudan Saidivasana

Naswadi1 Sengpur

Kurali 22 Segwa Moti chikhali

Kaprali

Sinor

Haldarwa

73 73.25 73.5 73.75 74 74.25

6.3.1. Water Level Map Various maps prepared on the basis of available data of NHS monitoring and other data, incorporated from the systematic and reappraisal hydrogeological surveys carried out in the district areas, are described as follows.

6.3.1.1.Water Table Map The figure 6.2 shows the water table map in the district. The movement of ground water in general, from north-east highland to south-west and western low lying Mahi Rive estuary zone. In north – east areas and also along area along Mahi & Narmada River in west and south, the counters show effluent nature of all streams, rivulets and rivers. The gradient is steep in eastern hilly terrain, a hard rock terrain. It becomes gentler towards central and western part of semi-consolidated to un-consolidated formation areas. Figure No. 6.2 Water Table Map

Map of Vadodara District

22.75

Water Table - Phreatic

GW Flow

Water Table

Direction

m amsl 25 22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

6.3.1.2.Piezometric Surface Map

The figure 6.3 shows the piezometric surface map, in the areas having deep aquifer system, on the basis of data collected during the systematic and reappraisal surveys. The piezometric surface range from 40 m amsl in north central to 0 m amsl in southwest corner of the district. Groundwater through (below -10 m amsl) observed in southwestern part of the district where ground water development through deep aquifer is high.

Figure No. 6.3 Piezometric Surface Map

Map of Vadodara District

22.75 Water Table - Confined

GW Flow Water Table

Direction

m amsl 25

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

7. GROUND WATER RESOURCES ESTIMATION 3 Estimation of Ground Water Resources for Gujarat State (GWRE-2002) has been carried out by the Government of Gujarat as per the „Ground Water Resources 4 Estimation Methodology GEC –1997‟ set up by Ministry of Water resources, Government of India. The ground water resources of Vadodara district are as follows.

As per GWRE 2002, ground water recharge during monsoon season has been computed using water level fluctuation method and compared with recharge by the infiltration factors. Depending upon percent deviation value, Gross Recharge has been calculated as per the recommended methodology. Besides rainfall, the recharge due to seepage from canal, return flow from irrigation, recharge from tanks, ponds & water conservation structures, etc. were also considered. The total annual recharge was obtained as the sum of the monsoon and non-monsoon periods comes out to be 1053.03 MCM per year. It has been decided to keep a provision at rate 5 % of the annual ground water recharge, when water table fluctuation method is followed for the computation. Making provision of 52.65 MCM (@ 5 %) for environmental /runoff purposes, net annual ground water availability is worked out to be of 1000.37 MCM per year.

The level of ground water development in an area is taken as the ratio of existing gross ground water draft for all uses to available ground water recharge and it is expressed as %. Thus the level of ground water development at year 2002, in all the taluka of the Vadodara district computed range from 23.00 % to 103.11 %. The average for district is 53.50 %. As per GWRE 3 norm, the units of assessment (talukas) can be categorized for ground water development in different categories such as Safe, Semi-critical, Critical and Over Exploited, based on the stages of ground water development and the long-term trend of pre and post monsoon ground water levels. Level of Ground Water Development and Categorization for all talukas of Vadodara district and as a whole district is given in table no. 7.1.

Table No. 7.1 Level of Groundwater development - Vadodara district

Existing Gross

Available Ground Level of Ground

Name of Ground Water Category

Water Recharge in Water Development

Taluka Draft for all uses in

MCM / Year ( % )

MCM / Year

Chhota 55.61 26.93 48.42 Safe

Udepur

Dabhoi 123.52 84.91 68.74 Safe

Karjan 161.31 137.71 85.37 Semi Critical

Kavant 29.36 19.14 65.20 Safe

Naswadi 34.19 12.17 35.59 Safe

Padra 113.01 77.73 68.78 Safe

Pavi Jetpur 99.96 60.45 60.47 Safe

Sankheda 66.26 35.96 54.27 Safe

Savli 71.35 37.56 52.65 Safe

Sinor 80.99 64.76 79.96 Semi Critical

3 Report on Estimation of Ground Water Resources and Irrigation Potential in Gujarat State, GWRE- 2002, (June – 2004 ) by NWR, WS & K Department, Government of Gujarat, Gandhinagar 4 Report of the Ground Water Resources Estimation Committee ( June 1997), Ministry of Water Resources, Government of India. Vadodara 100.99 104.12 103.10 Over Exploited Vaghoriya 63.84 14.69 23.01 Safe Total 1000.38 676.13 67.59 Safe

8. HYDROCHEMISTRY

The Vadodara district has main three hydrogeological provinces, Aravalli terrains, Deccan trap & associated Cretaceous sediments terrains and Alluvium areas. Each terrain also have varied hydrological regime, as shown in basin map. During the course of systematic and reappraisal hydrogeological surveys water sample were collected from the wells inventoried in all these ares. Further water samples are also collected periodically from National Hydrograph Stations in the district. On the basis of chemical analysis of such water samples hydrochemistry of shallow and deeper aquifers are describe as follows.

8.1. QUALITY OF SHALLOW GROUND WATER It is observed that the quality of ground water in shallow aquifer varies as per the nature of underlying formation. Generally in hard rock areas of eastern part overall quality is uniform, good in nature, whereas in western part, in alluvium area quality varies widely, have high concentration of dissolved ions (TDS).

Based on the analytical results of about 100 samples distributed throughout the district, collected during various surveys (1994-95), map depicting areal distribution of electrical conductance (Iso-con map), measures of dissolved ions, in phreatic aquifer is prepared and given as figure No.8.1

Fig. No. 8.1 Iso-con map of Vadodara district

22.75

Map of Vadodara District

Iso-con : Phreatic Aquifer

22.5

0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

4000µS /cm 3000µS /cm 2000µS /cm 1000µS /cm 0µS /cm

The Iso-con map (Fig. 8.1) reveals that E.C. of ground water varies from less than 380 µS /cm to more than 4000 µS/cm in the district In central part of Mahi- Narmada Doab where thickness of alluvium is limited (14-40m) and is underlain

by Tertiary sediments, have ground water quality with relatively high electrical conductance (more than 3000 µS /cm). Similarly in some localized pockets of alluvium area, overlying Deccan trap rocks, in parts of Vaghoriya, Vadodar & Dabhoi Taluka areas also have high EC groundwater. In in areas of consolidated formations – hard rock areas and also along Mahi river alluvium zone, ground water with EC less than 2000 µS /cm are observed. The high EC areas in south central part have formation having inherent salinity.

An iso-chloride (Iso- chloride) map for the phreatic aquifer is also prepared and presented in fig no. 8.2, shows gradual variation in chloride content from east to west. However , in major part of the district chloride content is less than 250 ppm, which gradually increase westward and towards Mahi Estuary zone reaches to highest of 2800 ppm.

Figure No. 8.2 Iso-chlor map of Vadodara district

Map of Vadodara District

22.75

Chloride : Phreatic Aquifer

22.5

0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

2000 mg/l 1500 mg/l 1000 mg/l 500 mg/l 250 mg/l 0 mg/l

8.2. QUALITY OF DEEP GROUND WATER The quality of ground water in the confined a1quifer has been determined by analysis of water samples collected during various surveys. Study of exploratory boreholes geophysical logs also reveals the nature of formation water quality at various depths. Plot of electrical conductance of deep aquifer water samples shows that in major part of confined aquifer zones, ground water is within range of 2000 µS / cm range. More than 2000 µs / cm are observed in areas where Tertiary formation is at depth. Towards east, in Padra Taluka area and southeast of Vadodara city also have high mineralized ground water at depth. Deterioration of ground water quality is observed from central part of the district to the eastern fringe at Mahi Estuary zone. 8.3. HYDROCHEMICAL REGIME Based on the study of hydrochemical nature of ground water, the district can be divided into following distinct areas, such as i) Areas with fresh ground water at all levels : In this category are included area where ground water is fresh with in 200 m explored depth, both in phreatic as well as confined aquifer, which can be used for irrigation and domestic consumption. ii) Areas with fresh ground water overlain by saline ground water: In this category phreatic ground water quality with high mineral content is underlain by relatively low mineralized ground water. iii) Area with fresh ground water is underlain by saline ground water: In this category phreatic ground water quality with low mineral content is underlain by relatively highly mineralized ground water. iv) Areas with saline ground water at all levels : Map showing all such spatial variation of ground water quality regime is given below as figure no. 8.3 & 8.4.

Figure No. 8.3 Iso-Con map – Confine Aquifer – Vadodara District

22.75

Map of Vadodara District

EC : Confined Aquifer

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

3000 µS/cm 2000 µS/cm 1000 µS/cm 0 µS/cm

Figure No. 8.4 Spatial variation of ground water quality – Vadodara district

22.75 Map of Vadodara District Spatial Variation of GW Quality

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

Fresh GW at all level GW Saline at deep level GW Saline at shallow level GW saline at all level

8.4. WATER POLLUTION Vadodara district is one of the highest industrialized districts in the state. The noteworthy notified industrial areas are IPCL Complex (Petrochemicals & Oil Refinery), GSFC Complex, Nandesari Complex and other industrial estates. 5 Gujarat Pollution Control Board (GPCB) , in their survey found that rapid industrialization and concurrent urbanization have had adverse impact on vital environment parameters like water and air of these areas. It was observed that different analytical values, in terms of pH, TDS, DO, BOD, COD, NH3N and NO2 + NO3 , for rivers of the district, namely Mahi, Mini, Vishwamitri and Dhadhar have crossed the critical levels to become harmful for living flora and fauna.

8.5. VULNERABAL AREA

8.5.1. Vulnerability of shallow aquifer to pollution Large part of the Vadodara district is urbanized and also have industrial activities. In event of uncontrolled development and lack of adequate infrastructure for effective treatment and safe disposal of effluents and solid waste, these areas would be prone to ground water pollution. These may ultimately result in deterioration of ground water quality, mostly in phreatic zones in down gradient areas. A map showing vulnerability to ground water & surface water bodies, as consequence of pollution in urban & industrial zones, in the basic three groups (high, moderate and low) is given as figure no. 8.5.1. The area of circle is proportional to sources of pollution (size of urban & industrial areas).

5 A report on the status of air and water of Gujarat (May 1988), GPCB, Gandhinagar. Figure No. 8.5.1 Vulnerability of Industrialization & Urbanization

22.75 Vulnerability Map : Vadodara District Vulnerability of Industrialisation & Urbanisation Vulnerability to Surface Water & Ground Water

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

Legend Polluted Streach Low Moderate High of River

8.5.2. Vulnerability of ground water to saline ingress Under natural system, two main rivers of the district, the Mahi & the Narmada has tidal ingress up to few kilometers inland from their estuarine zone. With construction of major dam on Mahi (1970), there has been drastic reduction in flow of river in down stream area of dam. Coupled with ever increasing high ground water development, the base flow is reducing drastically since last two decades and ultimately tidal water ingress came several kilometers inland. Same situation is likely to be envisaged in areas of Narmada River after completion SS Dam in next few years. With basis attributes of base flow data of rivers, rate of ground water development, aquifer disposition & water level & quality data etc., a map showing vulnerability to ground water source of saline ingress in the basic three groups (high, intermediate and low) is given as figure no. 8.5.2 Figure No. 8.5.2 Vulnerability of salinity ingress

Vulnerability Map : Vadodara District

22.75

Vulnerability of Salinity Ingress

Vulnerability to Inland Area

Low Moderate High

22.5 0km 10km 20km

22.25

22

73 73.25 73.5 73.75 74 74.25

8.6. SCOPE OF CONJUNCTIVE USE The conjunctive use of surface and ground water resources is one of the indispensable aspects of sustainable water resource management strategy. In the Vadodara district the main source for irrigation (2002-03) is ground water, which has already high rate of development. Further development of ground water resources for agriculture or for any other sector, in few highly developed Taluka of western half is likely to cause environment imbalance. With commencement of Narmada Project Irrigation, the stress on ground water resources is likely to lessen and there is a great scope to use conjunctively both surface and ground water resources for sustainable development of the district area.

8.7. SCOPE OF ARTFICIAL RECHARGE The Vadodara district area has moderated to high rate of ground water development, mainly in areas of western part where multilayer aquifer system exists. This area has come under Narmada Irrigation Command since last two years. There is likely to have surplus surface water resources in various stretches of canal command which can be diverted to numerous tanks & dray rivulets of the areas which will help to recharge subsurface dry aquifers. With efficient water management practice, seepage losses and any other surplus water can be diverted to amiable or purposes build structure for artificial recharge.

9. GROUND WATER DEVELOPMENT & MANAGEMENT

9.1. PRESENT GROUND WATER DEVELOPMENT The estimation of ground water resources of the Vadodara district (2002) show that present ground water development in the district is about 676 MCM, out of which nearly 70 MCM accounted for domestic and industrial purposes while remaining 606 is for irrigation. Taken as a whole district, level of ground water development is about 67 %. 9.1.1. Urban & Rural Water Supply Scheme Urban and rural water supply of the district is partly based on the ground water as well as surface water sources. Most of the urban areas and also rural area water supply schemes in western half of the district, where unconsolidated formation (alluvium) constitutes main aquifer, are based on surface water sources. The Mahi River is the main source of surface water supply. Major water requirements of many regional water supply schemes of rural areas, Vadodara city and many industrial unit of western part of the district are meet through series of in-take wells (Collector Wells) constructed in river beds. Part of the remaining requirement is augments through local ground water sources. Contrary to this scenario, main source for domestic need in central and remaining eastern half of the district is meet through local ground water resources and augmented partially by surface water sources. In unconsolidated formation area tube wells are the main sources while in hard rock area, dug wells & DCB wells used as ground water sources for domestic need. All the rural areas, mostly the tribal area scattered helmets, have hand- pump (shallow depth (40-80 m) as main local source of drinking & domestic need. 9.1.2. Groundwater for Irrigation Ground water is most reliable source of irrigation in the district & constitutes nearly 95 % of irrigation sources (2002-03). Moreover, groundwater constitutes more than 70% to 100 % of total cropped areas of the district during Rabi & Summer season. During Kharif season (monsoon) it is mainly used as supplementary but as a reliable source of irrigation in events of failures of required rainfall spell during vital stage of crop development. During remaining two seasons of Rabi & Summer, it is difficult to satisfy full demand of irrigation in want of other source (rainfall), ground water is sparsely used for less water intensive food crops & for vegetable, fruits or mainly cash crops or essential fodder for livestock. Tube wells are the main sources in the unconsolidated formation in western half of the district while dug wells and DCB wells are the main sources in remaining hard rock areas of the district.

9.2. FEASIBLE GROUND WATER STRUCTURES 9.2.1. Hard Rock Area – Consolidated Formations Development prospects in this area are more complicated because of the heterogeneity of the formations, non uniformity in the degree and nature of weathered zone and variations in degree and nature of fracturing. Favorable hydrogeological situations in such areas are in the form of valley fill materials, pediplain with weathered residuum and low lying hilly terrain crisscrossed by the lineaments. Almost eastern half of the district have such terrain, in which two mode of development are feasible namely i) the traditional Dug cum Bore well (DCB well) and ii) moderate depth Bore Well (BW).

The dimension of DCB well varies in Deccan Trap & Granite /Gneiss areas. In former it have medium diameter of 2 to 4 m with suitable depth (8 to 12 m) tapping the weathered residuum and with additional 50 to 100 mm dia bore well at the bottom, either vertical or two-three sets of slightly horizontal bores with gentle gradient toward well. In granite – gneiss areas, dug well section in general, have large diameter (4 to 8 m) with one or two vertical bores at the bottom the dug well.

The bore wells having diameter of 200 to 150 mm and depth in range of 120 m 200 m appears feasible in hard core areas. There appear to be fairly good prospects for moderate depth bore wells in Deccan Trap areas. Ground Water exploration carried out by CGWB ( 2004-05) have indicated possibility of tapping potential deep fracture system as a sustained source of water supply. As a point source for drinking water in such difficult areas, about 100 numbers may be attempted. Considering the resource potential of the hard rock terrain about 7,000 irrigation wells (dug & DCB type) are recommended in first phase such that, properly located, designed , constructed and energized bore well may be able to command an area of 2.5 hectare. Construction of remaining 7000 structures may be taken after accessing development of first phase program.

9.2.2. Alluvium – Soft Rock Area – Unconsolidated Formation Level of ground water development in unconsolidated formation areas, mainly in Vadodara, Padra, Sinor & Karjan Taluka is highest ( 80 to 100 %). Ground water, in general occurs in semi confined to confine condition in deep 40 to 300 m) depth multilayered aquifer system. The phreatic zone, at most palace is

dry or unsaturated to sustain pumping. Main ground water strictures are in form of medium depth (80 to 250 m) tube wells. The depth and yield of tube wells varies as per aquifer disposition. Considering the resource potential of the unconsolidated formation, about 800 irrigation tube wells of 150-200 m depth are recommended in first phase such that, properly located, designed , constructed and energized bore well may be able to command an area of 10 to 15 hectare.

9.3. GROUND WATER MANAGEMENT Management ground water resources in Vadodara district has to be viewed against the backdrop of varied & complementary economy scenario, i.e., agrarian economy of rural areas and industrial economy of urban and semi –urban areas. Both scenarios are marked by stifled growth due to non availability of vital water resources at critical juncture; i.e. for raising rabi & hot season crops in agrarian economy and for crucial need & sustenance, during lean season, of industrial and urban economy. Although, it may be prudent to mention that the present status of ground water development for the whole district is about 67.6 % of the net utilizable recharge, more attention has to be focused for conserving the groundwater endowed with dependability, less cost, better quality, possibility for time bound development and as a „Safe Point Source‟ for drinking and related purposes. Various aspects of emerging issues of Water Resources Management, with emphasis on ground water and related environment issues, for both agrarian economy of rural areas and industrial economy of urban and semi –urban areas in context of water resources of the Vadodara district are discusses as follows

9.3.1. Agrarian Economy of Rural Areas A critical examination of source wise Net irrigated Area of the Vadodara district , during both Kharif & Rabi seasons, clearly bring out the severe limitations of surface water irrigation as contrast to near reliable nature of ground water irrigation. Before commencement of Narmada Irrigation Project, total canal irrigation in Vadodara district, year 2001-02 accounted for 5 % of the gross irrigated area. These figures are likely to be increased substantially after reliable supply of surface water supply by Narmada Irrigation Project. It will drastically improve ground water resource scenario, which is facing severe stress due to ever increasing demand since decades. During year 2001- 02, contribution of ground water resources during Kharif, Rabi and Summer season were 36 %, 70 % and 100 % respectively. With input of additional surface water of Narmada Irrigation Project, stress on ground water resources will be lessening considerably.

9.3.2. Industrial Economy of Urban and Semi –Urban Areas One of the most significant urban changes in Vadodara district areas has been the growth of cities to unprecedented sizes. Although rapid urban change during last few decades is often viewed as an uncontrolled flood of people, but there is an economic logic underpinning global urban trends The great migrations of people from rural to urban areas all over the district, during last few decades are proof of their power to attract and dazzle with their promise of a better life. Meeting the water needs of fast-growing cities with competing demands from commercial, domestic and industrial users have put great pressures on freshwater resources. The scenario of such degradation and

depletion of freshwater resources would threaten the very livelihood of cities and the sustainability of economic and social development

It is observed that, in general, many urban water systems are poorly maintained, and often large quantity is lost in distribution. Many urban residents and especially the poor get irregular or no water supplies, and no sanitation. For the urban poor, this lack of access to safe water and basic sanitation may cause widespread ill-health that would further limit their productive capabilities. At the same time, revenue collection for much of the urban institutes with poor infrastructures is poor which further restrict operation, maintenance and investment funds for expansion. The scenarios of such are threatening the very livelihood of cities and the sustainability of economic and social development. New ways of responding to rapid change and making the urban environment sustainable should be explored, especially through better management and service pricing, greater participation of community groups and women, and creative partnerships between public and private sector enterprises. Better management of resources in and around urban centers is therefore a major challenge to the administrators all over such areas.

9.3.3. Aspect of Urban Hydrogeolgy Vadodara district has 5 % of area termed as Urban Area with 47 % population of the district. Amongst various talukas (blocks) of the district, Vadodara Taluka with 21,388 hectares area (31 % of Taluka) and with 14,92,398 persons (87 % of the Taluka) with population density of 6,978 persons per sq.km., is most Urbanised area of the district. Most of the urbanized areas lies in western half of the district, relies both, almost equally on surface water supply and ground water supply. The scope of further ground water development in Vadodara, Padra & Karjan Taluka area is limited as these areas is underlain by inferior quality ground water at depth their existing level of development has reached to a critical stage. Besides this natural constraint of limited & poor aquifer potential, other aspects of anthropogenic activities of urban and industrial development, as described follows, demand careful ground water management strategy.

 As a consequent to urbanization & concurrent industrialization, overall demands of water are increasing and cause decline of agriculture in such area. There is extreme disproportionate ratio of agriculture area vs. urban areas in western part of the district.   Problems relating to inadequate sewerage disposal and industrial waste are posing great environmental hazards in small urban areas, resulting into degradation and depletion of freshwater resources. Natural stream courses of Mini, Vishwamitri & Dhadhar, down to urban & industrial areas have been converted into effluent disposal channels. Many fresh water bodies, tanks in low-lying areas, have become puddles of sewerage water in many towns of the district. Quality of such fresh water bodies are degraded to such an extent, in terms of BOD, COD 5 requirement , too support aquatic flora & fauna.   In addition to pollution problem, an urban & industrial activity greatly increases the consumptive use of water and precludes water recycling, thereby contributing disproportionately to water scarcity. Huge

withdrawal of surface water (base flow) of Mahi River in northwest border of the district for urban and industrial requirement, which ultimately disposed as effluent to the sea, ultimately result dry river bed in downstream portion. This has been explanation to more ingress of tidal water inland & deterioration of already dwindling scare groundwater resources of the area.

 The competitive demands of all three, agriculture, urban and industrial sector encroach upon vital demand of environment, which is degraded in most of the urban & industrial areas of Vadodara district.

9.4. STRATEGY FOR GROUND WATER DEVELOPMENT Based on the scenario of present ground water development and its management aspects and feasible structures, as discussed above, a comprehensive strategy for stepping for optimum utilization of available resource potential may be undertaken. With the concept of “Conjunctive Use for Sustainable Water Resource Management”, large irrigation requirement as well as domestic & industrial need would be satisfied through „Narmada Canal‟ water. With more focus on other complementary aspect of development, i.e. conservation of water resources, mainly ground water resources, both in space and time such that it can be used efficiently with surface water resources, concept of conjunctive use can be effectively implemented with optimum development strategy. In canal command, conjunctive use management should be such that cumulative draft of ground water should never exceed annual replenisher recharge as per guideline of National Water Policy. Moreover, unilateral development of surface water, without adequate planning for utilization of available ground water, which often leads to undesirable situations like water logging and related soil salinity problems, should be avoided. There are many such areas, prone to water logging, are identified during „Pre Irrigation Study‟ by the State Government. As per the guideline of NWP every effort has to be made for proper integration and dovetailing of any surface water development especially in canal command areas such so that environment hazards like water logging can be eliminated. At the same time, through adequate back up from the ground water reservoir, duration of canal operation can be extended.