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Physicochemical Assessment and Water Quality of Surface Water in Chandel and Tengnoupal Districts, Manipur for Domestic and Irrigational Uses
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 08 Issue: 01 | Jan 2021 www.irjet.net p-ISSN: 2395-0072 Physicochemical Assessment and Water Quality of Surface Water in Chandel and Tengnoupal Districts, Manipur for Domestic and Irrigational Uses Herojit Nongmaithem*1, Maibam Pradipkanta Singh2 & Sujata Sougrakpam3 1-3Geological Survey of India, SU: MN, Imphal office, Imphal, 795004 ---------------------------------------------------------------------***--------------------------------------------------------------------- Abstract: The study aims to validate the water quality for domestic and irrigational uses based on the physico chemical properties of the surface waters in parts of Chandel and Tengnoupal districts of Manipur. The sources of the dissolved constituents in the samples suggest Mg-Ca-HCO3-Cl as the dominant hydro-facies and are magnesium bicarbonate water types. The dominant geochemical process that governs the water chemistry is rock weathering dominance. WQI of the water samples ranges from 76.18 to 155.33 and is well within the limits of the BIS and WHO guidelines for drinking water. All the samples are suitable for irrigational uses based on the determined values of EC, TDS, SSP and SAR. Hence, these perennial rivers and streams hold the potential to provide uninterrupted supply of drinking and irrigational water to Chandel, Tengnoupal, Kakching and Thoubal districts of Manipur without any major treatment. Keywords: Physico-chemical, hydrochemical facies, Water Quality, Manipur 1. Introduction Urbanisation catalyst the human dependency on the water consumption either for domestic or irrigational uses. Rivers and streams show spatial heterogeneity in the physico-chemical indices which enable to categorize the water for different uses or to detect toxicity. -
Th Alexander Singh.Pmd
Current World Environment Vol. 8(1), 93-102 (2013) Seasonal Variation of Some Physico-chemical Characteristics of Three Major Riversin Imphal, Manipur: A Comparative Evaluation TH. ALEXANDER SINGH1, N.SANAMACHA MEETEI2, and L. BIJEN MEITEI* 1Research Scholar, CMJ University, LaitumkhrahShillong, Meghalaya -793 003. 2Directorate of Environment, Imphal East - 795 010, Manipur. *Directorate of Environment, Porompat, Imphal East-795 005, Manipur. DOI : http://dx.doi.org/10.12944/CWE.8.1.10 (Received: March 22, 2013; Accepted: April 10, 2013) ABSTRACT Documentation on water quality based on seasonal distribution pattern of physic-chemical characteristics of the three major rivers flowing in Imphal, Manipur were carried out during July, 2011 to June, 2012. Three main seasons were classified based on the ombothermicinformation for ten years weather data of Imphal. Significant seasonal variations of the different parameters were observed and the study has a great valuein terms of river ecosystem as well as water quality in different seasons. Key words: Anthropogenic, Eutrophication, Allochthonous, Seasonal variation, River ecosystem, population growth, pollution. INTRODUCTION rivers are polluted (Sahu, 1991). The physico- chemical characteristics are also greatly affected Water, by means of its physical, chemical due to discharge of domestic, municipal, industrial and biological characteristics, reflects the and other several factors like religious offerings, significance as potent ecological factor and quality recreational and constructional activities in the for sustenance. However, the increasing catchments areas ( Pandaet al.,1991). Hill and anthropogenic influences in recent years, in and Webb (1958) reported that rainfall pattern influences around aquatic ecosystem and their catchment in changing the physical and chemical environment areas have contributed to a large extent to various of water and helps in increasing input of pollutants. -
73Rd Meeting
Government of India Ministry of Development of North Eastern Region --------- Minutes of the 73rd Meeting of the NLCPR Committee held at 1100 Hrs on 22.09.2009 under the Chairmanship of Secretary, M/o DoNER in Committee Room No.243-A, Vigyan Bhavan Annexe New Delhi. Present 1. Shri Jarnail Singh, Secretary, Ministry of Development of North Eastern Region…..In Chair. 2. Shri P.K. Pattanaik, Joint Secretary, Ministry of DoNER. 3. Mrs. Anjuly Chib Duggal, Joint Secretary (PF-I), Department of Expenditure 4. Shri Naveen Verma, Joint Secretary (NE), MHA 5. Dr. R.K. Vats, JS&FA, DoNER 6. Shri Sarvan Kumar, Director, Planning Commission. 7. Shri D.D. Mathur, Consultant, Planning Commission. Mrs. Firoza Mehrotra, Special Consultant (SP-NE), Planning Commission granted leave of absence. Following Officers were also present as special invitees: Shri Rajesh Kumar (Director), Shri P.R. Meshram (Director), Shri B.B. Samaddar (Deputy Secretary), Shri K. Guite, Joint Director (IFD), Shri Ajay Kumar (Section Officer) and Shri S.K. Saha (Section Officer), Ministry of DoNER. The Committee met and deliberated on the Agenda items. Following observations and recommendations were made: Item No.1: Confirmation of Minutes of 72nd Meeting of the NLCPR Committee held on 28.08.2009 Minutes of the 72nd Meeting were confirmed. **** Item No.2: Action taken report of decisions / recommendations made by NLCPR Committee in the 72nd Meeting held on 28.08.2009 The Committee noted that the Minutes for 72nd Meeting have been issued on 28.08.2009 and action has been taken by the Ministry of DoNER on the decisions/ recommendations made by the NLCPR Committee in that meeting. -
Flood Risk Reduction of Rupnarayana River, Towards Disaster Management
aphy & N r at og u e ra G l Das and Bandyopadhyay, J Geogr Nat Disast 2015, 5:1 f D o i s l a Journal of a s DOI: 10.4172/2167-0587.1000135 n t r e u r s o J ISSN: 2167-0587 Geography & Natural Disasters ResearchResearch Article Article OpenOpen Access Access Flood Risk Reduction of Rupnarayana River, towards Disaster Management–A Case Study at Bandar of Ghatal Block in Gangetic Delta Biplab Das* and Aditya Bandyopadhyay Indian Institute of Engineering Science and Technology, Shibpur, India Abstract The paper discussed the present state of flood at a junction point between two rivers at Bandar of Ghatal block in Gangetic delta and proposed a technological solution to reduced vulnerability of flood. While annual floods have the potential to wreak havoc on unprepared communities, spoil crops and endanger food security, they also play a vital role in agriculture. Flood Management and Mitigation is designed to minimize negative flood-related impacts while preserv- ing the benefits. Flood mitigation involves the managing and control of flood water movement, such as redirecting flood run-off through the use of floodwalls and flood gates, rather than trying to prevent floods altogether. It also involves the management of people, through measures such as evacuation and dry/wet proofing properties for example. The pre- vention and mitigation of flooding can be studied on a number of levels: individual properties, small communities and whole area or towns or cities. The costs of protection rise as more people and property are protected. The most effective way of reducing the risk to people and property is through the production of flood risk maps. -
Pethia Arunachalensis, a New Species of Small Barb (Teleostei: Cyprinidae) from Arunachal Pradesh, India
Rec. zool. Surv. India: Vol 119(4)/ 328-333, 2019 ISSN (Online) : 2581-8686 DOI: 10.26515/rzsi/v119/i4/2019/142213 ISSN (Print) : 0375-1511 Pethia arunachalensis, a new species of small barb (Teleostei: Cyprinidae) from Arunachal Pradesh, India Bungdon Shangningam1*, Laishram Kosygin1 and Basudhara Roy Chowdhury2 1Zoological Survey of India, Freshwater Fish Section, 27 J. L. Nehru Road, Kolkata – 700 016, West Bengal, India; [email protected], [email protected] 2Paribesh Unnayan Parishad, South 24 Parganas, Sagar Island, West Bengal – 743 373, India; [email protected] Abstract Pethia arunachalensis, a novel cyprinid species, is described from the Nao-dhing River, Brahmaputra Basin, Arunachal Pradesh, India. The new species is diagnosed in having an incomplete lateral line, 6-7 lateral-lined pored scales, absence of barbels and a distinct black caudal spot. A key to the species of the genus Pethia established in the Ganga-Brahmaputra drainage is provided. Keywords: Brahmaputra Basin, India, Noa-dhing, Pethia Introduction During a freshwater faunal survey in the Arunachal Pradesh, eight specimens of Pethia were collected in The cyprinid genus Pethia Pethiyagoda et al., 2012 the Nao-dhing River at Miao. Further examination and includes small freshwater fishes distributed in India, comparison with known members of Pethia revealed the Bangladesh, Bhutan, Myanmar, Nepal, Pakistan, and Sri species to be unnamed and new to science, which we Lanka. Members of the genus are characterised by the herein described as Pethia arunachalensis sp. nov. distinctive colour form comprising of a spot on humeral and caudal peduncle; absence of rostral barbels; absent or Material and Methods minute maxillary barbels; dorsal-fin with 3 to 4 simple and 8 branched rays, last simple dorsal-fin ray rigid and Fishes were fixed in 10% formalin and preserved in serrated posteriorly; 3 simple and 5 branched anal-fin rays; 70% ethanol. -
River System of Manipur
RIVER SYSTEM OF MANIPUR There are three main river system of Manipur a) The Barak system b) The Manipur system c) The Chindwin system THE BARAK SYSTEM ➢ The Barak river and its tributaries – Irang , Makru, Tuivai And Jiri – flow through the northern and western hills of the state, and have a total catchment area of 9,042 sq. km. this forms approximately 40.5 percent of the state. ➢ From its source at Liyai Khullen in Manipur’s Senapati district at an elevation of 2331 meter and its flows downward , the river receives a lot of streams and it flows west between Manipur and Nagaland, then southwest to Assam where it leaves India and enters Bangladesh. ➢ The Barak river is the biggest river and longest river of the state. It rises in the southern spures of Japho and flows in a south westerly direction. At Tipaimuk (Pherzawl district), it joins the Tuivai river and take a sharp bend towards north, to join the Jiri river. ➢ The Makru and Jiri river are right bank tributaries of Barak river. These rivers rIses from the hills in the south of the Barail ranges and flows more or less in parallel course. ➢ The Irang is the most important tributary of the Barak river. It rises from the northern part of the western hills and seperates the Tamenglong and Churachandpur districts. The Leimatak river falls into the Irang river. Barak river at Tipaimukh Barak river at Senapati Irang river at Tamenglong (Pherzawl) MANIPUR RIVER SYSTEM ➢ Manipur valley is transverse by the major rivers viz. Imphal, Iril, Thoubal, Sekmai, Wangjing, Khuga, Chakpi, Nambul etc which falls directly into or indirectly connects with Imphal river which later known as Manipur river. -
Effect of Turbulent Structures on the Riverbank Erosion Due to Tidal Incuence: a Case Study from the Rupnarayan River, Eastern India
J. Earth Syst. Sci. (2021) 130:62 Ó Indian Academy of Sciences https://doi.org/10.1007/s12040-021-01554-w (0123456789().,-volV)( 0123456789().,-vol V) Effect of turbulent structures on the riverbank erosion due to tidal inCuence: A case study from the Rupnarayan River, eastern India 1 1, 1 2 VIKAS KUMAR DAS ,KOUSTUV DEBNATH *, SAYAHNYA ROY ,KRISHNENDU BARMAN , 1 1 SUNIL HANSDA and BIJOY SINGHA MAZUMDER 1Fluid Mechanics and Hydraulic Laboratory (FMHL), Department of Aerospace Engineering and Applied Mechanics, Indian Institute of Engineering Science and Technology (IIEST), Shibpur 711 103, India. 2Department of Applied Mathematics with Oceanology and Computer Programming, Vidyasagar University, Midnapore 721 102, India. *Corresponding author. e-mail: debnath˙[email protected] MS received 18 April 2020; revised 29 November 2020; accepted 3 December 2020 For understanding the sediment removal mechanism from the bank face, Beld measurements of the dominating turbulent Cow structures under the inCuence of Cood and ebb tide were carried out at the middle reach 98 km upstream of the mouth of Rupnarayan River, India where the bank erosion activity was highly dynamic. Measurement of the three-dimensional temporal variation of velocity was carried out using a 16-MHz Micro-ADV during the transition period of Cood to ebb tide. Results from the present Beld study depict that during the transition of the onset of the ebb tide, the velocity Beld showed reduced values that gradually acquired negative values at the near bank region. This manifested the existence of an anti-clock circulation during Cood tide and clock-wise circulation during ebb tide at the near bank Cow Beld. -
Vishwanath Genus Glyptothorax 1443.Pmd
NEW DESCRIPTION ZOOS' PRINT JOURNAL 22(3): 2617-2626 FISHES OF THE GENUS GLYPTOTHORAX BLYTH (TELEOSTEI: SISORIDAE) FROM MANIPUR, INDIA, WITH DESCRIPTION OF THREE NEW SPECIES W. Vishwanath 1 and I. Linthoingambi 2 Department of Life Sciences, Manipur University, Canchipur, Imphal 795003. India Email: 1 [email protected]; 2 [email protected] plus web supplement of 3 pages ABSTRACT included G. platypogonoides, G. trilineatus, G. manipurensis, G. cavia, Sisorid catfishes of the genus Glyptothorax of Manipur, India is and G. sinense in his list of fishes of the state. G. platypogonoides revised. Glyptothorax ngapang sp. nov., G. granulus sp. nov. and G. is now spelled G. platypogonides (Roberts, 1989; Tan & Ng, 2000). chindwinica sp. nov. are described from Chindwin basin of the state. Characteristic differences in the new species include: G. Subsequent reports of Hora & Mukerji (1935), Hora (1936), ngapang sp. nov. in its well tuberculated skin and slender caudal and Menon (1953) from the state did not include any peduncle; G. granulus sp. nov. in having granulated skin and representative of the genus. thoracic adhesive apparatus width 78.9-85.0% its length; and G. Examination of several collections from different parts of chindwinica sp. nov. in having large head, depth at nape 55.8- Manipur included six species of Glyptothorax of which three 56.7% HL, teeth on upper jaw as broad patch, lateral extent of lower jaw tooth band more than that of upper, and thoracic from Chindwin basin are undescribed. They are described adhesive apparatus with a shallow pit in the centre. G. here as new species, viz., Glyptothorax granulus sp. -
Action Plan for Rejuvenation of River Rupnarayan Tamluk, West Bengal
Action Plan for Rejuvenation of River Rupnarayan Tamluk, West Bengal Priority – V Nodal Agency Municipal Engineering Directorate Department of Urban Development & Municipal Affairs Government of West Bengal Approved by River Rejuvenation Committee, West Bengal (constituted in compliance to the order of the Hon’ble National Green Tribunal) Submitted to Central Pollution Control Board, Delhi SEPTEMBER, 2020 Action Plan for Rejuvenation of River Rupnarayan Executive Summary Sl. Description of Item Details 1. Name of the identified polluted river RiverRupnarayan 2. Identified polluted stretch of the river Kolaghat to Benapur 3. Total length of the polluted river 20 KM (approximately) Towns in the catchment of the polluted stretch of the 4. Bagnan, Kolaghat, Tamluk river 5. Is river is perennial Perennial No. of drains contributing to pollution and names of 6. Three (3) major drains 1. Sankarara Khal 2. Narayanpur Khal 3. Pairatunga Khal Whether ‘River Rejuvenation Committee’ (RRC) Yes. 7. constituted by the State Govt./UT Administration and If 07.01.2019 so, Date of constitution of ‘RRC’ Tamluk 8. Major Towns on the banks of the river with population Population = 65,306 (Census, 2011) Total water consumption and sewage generation in Total water consumption =13.24 MLD a. MLD Total sewage generation = 8.37 MLD Total no. of existing STPs and the totalcapacities in b. Nil MLD Gaps in sewage treatment in MLD and no. of towns c. Town=1, Gap=8.37 MLD not having STPs d. Total MSW generation in TPA 19710 TPA Existing treatment and disposal facilities and total e. NIL capacity Major industrial estates located with total no. -
Flood Hazard Zonation of Manipur Valley, Manipur
FLOOD HAZARD ZONATION IN MANIPUR VALLEY FINAL REPORT Submitted to : NRDMS DIVISION DEPT. OF SCIENCE AND TECHNOLOGY Govt. of India TECHNOLOGY BHAVAN NEW MEHRAULI ROAD NEW DELHI – 110016 Submitted by: MANIPUR SCIENCE & TECHNOLOGY COUNCIL CENTRAL JAIL ROAD IMPHAL - 795001 C O N T E N T S 1. INTRODUCTION 2. OBJECTIVES 3. FLOOD RECORDS 4. METEOROLOGICAL DATA ANALYSIS 5. RAINFALL FREQUENCY FOR IMPHAL 6. SLOPE ASPECT 7. GEOMORPHOLOGY AND HYDROGEOMORPHOLOGY 8. SOIL EROSIONAL PATTERN 9. DRAINAGE ANALYSIS OF MANIPUR VALLEY 10. SLOPE AND DRAINAGE COMBINE ANALYSIS 11. SURVEY REPORT 12. STAGE-DISCHARGE RELATION 13. DISCUSSION 14. RECOMMENDATION Introduction Manipur Valley (Imphal Valley) located in the central part of the State is nearly oval shaped valley. It virtually comprises of four districts viz. Imphal East, Imphal West, Bishnupur and Thoubal districts. The total geographical area of the valley is 1900 sq. km. that falls within the parallels N 24°16′ to N 25°2′ and meridians E 93°41′ to E 94°9′. It is approximately 60-65 km. long and 30-35 km. wide. Physiographically the terrain is an elevated plain surrounded from all sides by structural hills of disang formation. Flood is a primary natural hazard in the area during monsoon season damaging the crops and properties of the people. Flash flood occurred almost every year during rainy season due to poor drainage condition. The primary causes of flood in Manipur Valley are heavy run off and less infiltration in degraded watersheds in the upper reaches of the rivers during rainy seasons in the valley. Manipur Valley is traversed by the major rivers viz., Imphal, Iril, Thoubal, Sekmai, Wangjing, Khuga, Chakpi, Nambul etc. -
India River Week – North East @?>D
State of India’s Rivers for India Rivers Week, 2016 (Non Brahmaputra) Authors Santon Laishram Jiten Yumnam India River Week – North East @?>D Contents OVERVIEW OF BARAK RIVER SYSTEM AND OTHER MINOR RIVERS FLOWING TO BURMA AND BANGLADESH ........7 1. Barak River System .........................................................................................................................................7 2. Minor rivers of North East draining into Myanmar and Bangladesh .............................................................8 DESCRIPTION OF RIVERS IN BARAK RIVER BASIN .......................................................................................................9 3. Rivers of Manipur ...........................................................................................................................................9 3.1 Barak River ................................................................................................................................................. 10 3.2 Manipur River ............................................................................................................................................ 11 4. Rivers of Meghalaya .................................................................................................................................... 12 4.1 Myntdu River ............................................................................................................................................. 13 4.2 Someshwari River: .................................................................................................................................... -
Penaeid Shrimp and Giant Prawn Seed Collection from Rupnarayan River in Purba Medinipur, West Bengal, India
Penaeid shrimp and giant prawn seed collection from Rupnarayan River in Purba Medinipur, West Bengal, India Subrato Ghosh 122/1V, Monohar Pukur Road, P.O. Kalighat, Kolkata – 700026, West Bengal Email: subratoghosh2007@rediff mail.com; subratoff [email protected] Operating a net. River Rupnarayan River is located at a distance of 135 km from the sea. Almost every year, the river inundates its two banks during the peak The Rupnarayan River has its origin near Ghatal town of the rainy season in July-September. in Paschim Medinipur District of West Bengal, where the Dwarakeswar River is joined by the Shilabati. The Shrimp seed collection methods from inundated Rupnarayan joins the Hooghly River at Geonkhali in Purba river bank Medinipur District after completing a 78-80 km course. The Rupnarayan is famous for the highly-priced hilsa Tenualosa The practice of collecting penaeid shrimp seed (post-larvae ilisha; adults move upstream for spawning and are caught by and juvenile) and prawn seed (Macrobrachium sp.), the fi shermen in stationary gill nets at Kolaghat and other places. latter to a much lesser extent, from inundated agricultural The Rupnarayan River forms the eastern boundary of Purba fi elds comprising small individual plots located on western Medinipur with Howrah, fl ows along this region down to Bay bank of the Rupnarayan river at Kharui, Gujarkharui, Gobra of Bengal. Being a part of Hooghly estuary, the lower reaches and Jamitta villages has become a supplementary source of of this river are aff ected by semi-diurnal tides from the Bay of income for local agricultural communities.