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Hkkjr Ljdkj Dsunzh; Ty Vk;Ksx Tyo [kaM&3 Volume-III dsoy dk;kZy; mi;ksx gsrq ( ) (FOR OFFICIAL USE ONLY) Hkkjr ljdkj GOVERNMENT OF INDIA MINISTRY OF JAL SHAKTI t y ’fDr ea=ky; ty lalk/ku unh fodkl vkSj xaxk laj{k.k foÒkx , DEPARTMENT OF WATER RESOURCES, RIVER DEVELOPMENTdsUnzh; & GANGAty vk;ksx REJUVENATION CENTRAL WATER COMMISSION tyo"kZ iqfLrdk WATER YEAR BOOK twu 2018 ebZ 2019 ( - ) (June 2018 - May 2019) cSrj.kh] lqcZ.kjs[kk ,oa cw<kcyax csflu BAITARANI, SUBARNAREKHA & BURHABALANG BASIN Tky foKkuh; izs{k.k ifjeaMy HYDROLOGICALHkqous j OBSERVATION CIRCLE ’o (BHUBANESWAR) September: 2019 [kaM&3 Volume-III tyo"kZ iqfLrdk WATER YEAR BOOK twu 2018 ls ebZ 2019 ( ) (June,2018 – May,2019) cSrj.kh] lqcZ.kjs[kk ,oa cw<kcyax csflu BAITARANI, SUBARNAREKHA & BURHABALANG BASIN FOREWORD Proper assessment, analysis and compilation of hydro -meteorological data are essential for planning and management of precious water resources, which is vital not only for economic development but also for providing basic needs for such a large population of our country. Water reaches the land -mass through precipitation, a part of which evaporates, a portion of it percolates into ground as natural ground water and the excess runoff flows through rivulets and rivers and drain into the sea. Central Water Commission (CWC), an apex technical Organisation of Government of India for surface water resources, carries out systematic collection of hydro -meteorological data and assessment of surface water as one of its prime functions. Hydro-meteorological observation stations have been established by CWC in almost all the river basins of India in a phased manner. These are further modernised and strengthened under various schemes. In the process, additional Divisions, Circles and Regional offices have been set up on a basin-wise concept. All the east flowing rivers in-between the Ganga and the Godavari basins (Mahanadi, Subarnarekha, Brahmani, Baitarani, Vamsadhara Rushikulya, Burhabalang, , Nagavali and Sarada) have been identified as Mahanadi and Eastern Rivers Basin dealt by Mahanadi and Eastern Rivers Organisation (MERO), CWC, Bhubaneswar. Hydrological Observation Circle (HOC), Bhubaneswar is responsible through Mahanadi Division (MD), Burla and Eastern Rivers Division (ERD), Bhubaneswar for hydrological observation and flood forecasting activities in these 9 river basins flowing mainly through Odisha along with its neighbouring states of Jharkhand, Chhattisgarh, Andhra Pradesh and West Bengal. There are a total of 119 observation stations under MERO. Sy stematic gauge and discharge observations are regularly conducted at 50 hydrological stations (out of the above 119) throughout the year. Sediment, Water Quality and Meteorological data are also observed at some of the stations. After scrutiny and checking , the collected & processed data is published in the form of Water Year Books through “SWDES”, custom made software for hydrological data processing. This Water Year data Book contains Hydrological data, Sediment data and Water Quality data for the hydrolo gical year 2018-19. Water Year Book pertaining to the Hydrological Observation Circle, CWC, Bhubaneswar is published in four volumes.Volume-I incorporates data of Mahanadi basin, Volume -II contains data of Brahmani basin, Volume -III of Subarnarekha, Burhabalang & Baitarani basins and Volume-IV of Rushikulya, Vamsadhara, Nagavali and Sarada basins. Each Volume contains Discharge data as Section -I, Sediment data as Section-II and Water Quality data as Section-III for respective river basins This Volume-III covers Subarnarekha, Burhabalang & Baitarani river basins for Water Year 2018-19. Hydrological, sediment and water quality data for nine sites and three effluent stations alongwith features and other important statistical information.The efforts by the officers and staff of HOC, CWC, Bhubaneswar and staff of ERD, CWC, Bhubaneswar under the leadership of Dr. D.R. Mohanty, Executive Engineer, in collection of data and bringing out this publication is highly commendable. The guidance and encouragement from Shr i A.Nayak, Chief Engineer, MERO, Bhubaneswar and help of officials of the Chief Engineer’s office are duly acknowledged. Place: Bhubaneswar (S.K. Samal) Date: September, 2019 Superintending Engineer Hydrological Observervation Circle Central Water Commission Bhubaneswar LIST OF ABBREVIATIONS USED: General: CWC : Central Water Commission H.P. : Hydrology Project IMD : India Meteorological Department msl : mean sea level Q : Discharge in Cumecs WL : Water level in metres Type of station: G : Gauge (Water Level) D : Discharge (Average discharge passing across a cross section of the river S : Sediment (suspended sediment load) Q : Water Quality Units: m : meter mm : milli meter km : kilometer s : second MCM : million cubic meters MT : metric tonne g : gramme l : litre CONTENTS (VOLUME-III) BAITARANI, SUBARNAREKHA & BURHABALANG BASINS SI NO. SUBJECT PAGE No. 1 BAITARANI Basin Description 1-6 2 CHAMPUA 7-31 3 ANANDPUR 32-57 4 SUBARNAREKHA Basin 58-64 Description 5 MURI 65-84 6 ADITYAPUR 85-110 7 JAMSHEDPUR 111-136 8 GHATSILA 137-162 9 FEKOGHAT 163-170 10. JAMSHOLAGHAT 171-178 10 RAJGHAT 179-188 11 GOPIBALLAVPUR 190-200 12 GHATSILA ROAD BRIDGE 201-209 13 BARIDHI NALA 210-218 14 KULPATANGA 219-227 15 BURHABALANG Basin 228-232 Description 16 NH-5 GOVINDPUR 233-254 BAITARANI BASIN BAITARANI BASIN 1. GENERAL 1.1 Introduction Baitarani is one of the important east flowing rivers of peninsular India, falling into Bay of Bengal. Major portion of its catchment lies in the state of Orissa and a small patch of the upper reach lies in Jharkhand. The river originates from the hill ranges of Keonjhar district of Orissa near Mankarancho village at an elevation of about 900 m. The total catchment area of this basin is 10,982 sq. km. The basin is situated approximately between East longitudes of 8510' to 8703' and between North latitudes of 2035' to 2215'. The basin is surrounded by the Brahmani basin on the south and west, the Subarnarekha basin on the north, the Burhabalang and the Bay of Bengal on the east. The river is flashy in nature, having a total length of 355 km, with the upper reach upto Anandpur in the hilly region. There is a considerable fall in elevation from RL 367 m at Champua to RL 28 m at Anandpur. State-wise distribution of the catchment area is tabulated below: State-wise Catchment area distribution Catchment Area (sq. Percentage of total Sl. No. Name of State km) catchment area 1. Jharkhand 736 6.7 2. Orissa 10,246 93.3 Total 10,982 100.0 Basin Map of Baitarani river system showing the various hydrological and hydro meteorological observation stations maintained by CWC, State Governments and India Meteorological Department, is enclosed herewith. Central Water Commission is maintaining 10 sites (including seasonal rainfall site at Thakurmunda which remains operative only during monsoon), out of which 2 are of GDSQ type, 7 are of G type and 1 is RF type. 1.2 River system Details of the tributaries which join Baitarani River on both sides are tabulated below: Length Catchment area Percentage of total Name of River River/Tributary (km) (sq.km) catchment area Baitarani Main stream 355.00 4112.45 37.45 Mohida Left Tributary 33.99 222.74 2.03 Baradpara Left Tributary 49.88 331.52 3.02 Kangira Left Tributary 40.00 458.43 4.17 Orarai Right Tributary 72.41 821.03 7.48 Korribhandhan Left Tributary 88.50 116.29 1.07 Deo Left Tributary 78.84 722.61 6.58 Kanjhari Right Tributary 59.53 497.69 4.53 Sita Right Tributary 38.62 505.05 4.60 Kusal Right Tributary 59.53 530.95 4.83 Kusai Right Tributary 78.84 870.24 7.92 Salandi Left Tributary 144.00 1793.00 16.32 Total 10982 100.00 1 1.3 Climatic Characteristics The basin receives most of the rainfall from the South-West monsoons during the period from June to October. Summer months from March to May are highly humid. Moderate cold winter is experienced from November to February. The average annual rainfall for the basin is approximately 1450 mm. The maximum temperature varies from 25 to 380 C and the minimum from 12 to 240 C. 1.4 Geology The rocks of the basin belong to the iron ore series of the Upper Dharwar system of the Archean group. There is intrusion of Epidorite with some Quartzite and at higher altitudes; intrusions of Hematite-Quartzite are seen. In the Zonal area of the Sundargarh district, Shales, Phyllites and Dolomites are found. At some places, Hematite deposits are seen over layers of Shale and Manganese. In the hills and forests between the Dhenkanal border and Anandpur, Quartzites, Shales, Phyllites, Granites and Genesis are also found 1.5 Site Details Details of water storage/ diversion structures in the Baitarani Basin are as below: Sl. Name of Project River Status No. 1. Akhuapada System Baitarani Existing 2. Remal Remal (Tributary of Kusei) Existing 3. Salandi Salandi (Tributary of Baitarani) Existing 4. Kanupur Baitarani Under Construction 5. Deo Baitarani Existing 6. Kusei (Tributary of Baitarani) Existing 7. Kanjhari Baitarani Existing 8. Integrated Anandpur Barrage Baitarani Under Construction 2. STREAM FLOW DATA 2.1 Methodology Area-velocity method is generally adopted for measuring discharge at sites. Cup type current meter is used to measure the velocity of the flow and the depth is measured by using sounding rod for depths upto 3 m and by log line beyond 3 m. Discharge by area velocity method is being observed once in a day starting at 0800 Hrs. at all the sites except on Sundays and holidays. Besides, silt and water quality observation are also being carried out at Anandpur and Champua sites of CWC. The observed stage and discharge figures for each season (monsoon and non-monsoon) are plotted and a mean Stage vs Discharge curve is drawn, giving due attention to the scattered points with reference to area, velocity etc.
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