Ground Water Prospects
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L E G E N D GROUND WATER PROSPECTS MAP RECHARGE MAP UNIT RECHARGE G R O U N D W A T E R P R O S P E C T S GEOLOGICAL SEQUENCE / GEOMORPHIC DEPTH TO STRUCTURES ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) ROCK TYPE CONDITIONS ( HYDROGEOMORPHIC UNIT / LANDFORM WATER LEVEL SUITABLE & AQUIFER MATERIAL HOMOGENEITY UNIT ) BASED ON TYPE OF WELLS DEPTH RANGE YIELD RANGE QUALITY OF GROUND PRIORITY AVAILABILITY IN THE UNIT REPRESENTED IN PRE / POST- MONSOON SUITABLE OF WELLS OF WELLS WATER WATER OF WATER & SUCCESS PT = PERCOLATION TANK R E M A R K S THE MAP WITH (AVERAGE IN METERS) ( SUGGESTED ) ( EXPECTED ) IRRIGATED CD = CHECK DAM ALPHANUMERIC CODE RATE OF WELLS POTABLE (P) ( PROBLEMS / LIMITATIONS ) ( RAINFALL & OTHER LS = LOOSE SEDIMENTS NON - POTABLE (NP) AREA NB = NALA BUND RW = RECHARGE WELL PR = PERMEABLE ROCK DW = DUG WELL MIN - MAX ( in LPM or m / day) ( PROBABILITY ) ( REPRESENTED IN SOURCES ) DT = DESILTING OF TANK NO. OF WELLS FIR = FISSURED ROCK RW = RING WELL ( INDICATE REASONS IF ( APPROX . RANGE ( REPRESENTED IN RP = RECHARGE PIT ( COLOUR INDICATES THE MAP WITH OBSERVED FR = FRACTURED ROCK BW = BORE WELL ( IN METERS ) NON POTABLE ) IN PERCENTAGE ) Kilometers VERY HIGH SD = SUBSURFACE DYKE YIELD RANGE AND THE MAP WITH WR / = WEATHERED ROCK / TW = TUBE WELL NUMERIC CODE ) HIGH WM WEATHERED MATERIAL DBW / = DUG CUM-BORE WELL / RS = RECHARGE SHAFT HATCHING INDICATE ALPHABETIC CODE ) MODERATE IR = IMPERIVIOUS ROCK DTW DUG CUM-TUBE WELL ST = STORAGE TANK 0 1 2 3 4 5 © DEPTH RANGE) LOW SCM = SOIL CONSERVATION MEASURES SCALE - 1 : 50,000 MAP SHEET NO. 79B/5 HUGLI, NORTH 24 PARGANAS & NADIA DISTRICTS, WEST BENGAL s Channel Bar Groundwater prospects very high CB111 t No well observed Excellent LS TW 5-10 m Very High P Nil Not Required " i (CB) 400-500 LPM with high recharge potential. Gaharpur " Jatrasiddhi )" Birpara Kotalpara Methigere s " "Halusai " Recharge structures not required. "Amtola 10/113 o Hediapota Char Beliamath Dakshinpara Kantalia ! " "Jaypur "Konchati " " D Lijirio " p Jangal Purushuttampur " Nandidanga Rahimpur Patna " "Aymapara " " " e " " " "Hansghara " Bhairabpur " Magraganja Dakshin 6/130 16/155 Tribeni D 10/154 Tapanpur " "! ! Baikunthapur R Ghoshpara ! Ramnathpur D D" Jadupatichar D " " "Natunganja ) Kapashtikri " " Saguna y Sultangachha Sultanpur E 6/130 a "Bangopal FP111 Tribeni " ! d "Rathtala 6/101 V D ! "Dingalpara D" I " Banshbagan t " Khein " Lichutala Akna Puranpota " L1 4/143 n " " R Majherchar ! Ox-bow Lake Baral Basudebpur e Groundwater potential below Shalukgarh " Magra Kalyani D" No well observed LS TW 10-15 m Very High Not Required " " OL111 Very Good 200-300 LPM P Nil Paranchapur Islampur Chandmari s (OL) " "Sekhpara " " surface water level. e "Meria Madaripur Shibpur 4/150 ) " 8/119 4/155 r Y Alikhoja " " y ! ! D! Kasundipara D" P " " D )Ï" Raghunathpur a L Sudarsan Gajaghanta / " Uropukur 12/95 " Milchita D Jharerpara " Hosenabad " Kalyani Rs " ! "Sankhonagar n Alluvium 6/98 D H " Sonatikri " t " o ! Sangrampur " Dingalhat" Kulia (Sand Dominant) n DDantra " Chhatimtola " i Parul G " Dhokradaha Dhokradaha t Barapara e (111) " Bil Keshabpur " " a " "Gaula Ayma " s Saptagram O Kanchrapara Donarpara " 4/130 e " ! m " "Haldarpara GayeshpurD r Kantudanga O r Ayma "Ghoshpur 1 " " Namajgar Krishnagebatti P Goaljor o Samsara " ! ( Groundwater prospects very high 6/98 Manipur H " D " " 8/60 " F Meander Scar LS Khatni 7/110 D! K5 MS111 No well observed Good TW 10-15 m 200-250 LPM High P Nil Not Required with high recharge potential. Polba " ! "Bhoagachhi (MS) D i "Chaupala K " Recharge structures not required. 16/120 " Atpukur Jhanpa Trishbigha 10/107 Rathtala Bedibhaban a " " Banshbaria h "! n ! " "Mallikerbag 6/120 D a D" " t Sarangpur "Dhuliara " t Adi ! a Mithapukur D a l "Nalbona "Telipukur N Saptagram r Mirkhila a " " d Baral Bara i i Malimpur Kataganja " 12/107 " g Ochai Kaladharpur" Khejuria Bahirbag Kanpur " ! " Tegharia " Bhatua D " a Sekhpara " Chandanpur " Bijpur Layanpur Barola h " Paunan " " " " " Dakshin Khamarpara !" Kanchrapara " ! B " Shira " Krishnapur D "Jatarpur D " hajipur " 8/85 " 14/107 / " Palladaha Satrapara Gokulpur Shunka Badul " i Barakpur " " l " " Chhoto 10/86 NP Nawpara g Belgare " Khejuria 12/95 Pirpara Manasadapara Flood Plain Groundwater prospects very high Kelorpara ! Ishwarbaha ! (As) " D u No well observed D8/195 " " FP111 (FP) Very Good LS TW 100-200 m 250-350 LPM Very High 38 Not Required with high recharge potential. " Kanpa [At shallow Rajhat Debanandapur H " " Keota "Halisahar MS111 Recharge structures not required. "Hadilpur Sahaganja " Sahapur Ampala Colony depth] " Chautara " Bhaturia " (Keota) Charapal "Balitana Barnapara " " " "Balikukhari " Kantadanga Baldeghata " 8/185 " " ! "Khashbati D " Island " Balagar Dharampur Amnan Manushpur Chakla Chanrali " " " " 11/75 Chak Tayarbagan Latbagan " " " Gotu 15/125 Kona D! Khamarpara " Palashi / Ichhpur Banseye " " " " " ! Bandel r Muriguri Kazidanga " D" Chendua " 10/67 Jetia Kalora u Ramnagar " Gandhi " Elespur D"! Halisahar 1" Nagdaha K14 " Colony Bikramnagar p Naldanga n " )" Alluvium Harit " b " " o "Panchpota Bali Balibhara Dariala Backswamp " Majhipa"ra i Nil Areas of low groundwater potential. Bhuto e (Clay Dominant) No well observed Poor Panchrakhi " " BS12 t TW Low Not Required " Purushottambati " " Hajinagar (BS) LS 60-70 m 40-50 LPM Derui Alinagar " d P Better potential at greater depths. " a (12) " Kedarnagar Narayanpur " Khasbati Newabila u " m " " Bishwashwarbati " Bijna Panchrakhi Ghatpukur r Kaswara " Kodalia Imambara " s Petiti Akna Garifa Ashoknagar " Bhagabatitala " " " o Arsallapatti " " a " 12/158 " Hooghly " " 7/78 " F Benabharui " B Sugandha "! " " ! Malancha i Haripur Barabandh " D D 10/82 Shibdaspur / Kapasdanga ) " " ! Biharipalli h 7/165 " a Gotu " " D e !" 10/107 Gauripur " s Kanagar n DPanjipukur Ranirbheri " "Loharpara Jadunathbati Madarpuli 8/213 w " ! o e Patul t " D Kulihanda " D! Maheshwarbati K " " c Khanarhat a " " " - Birendranagar 1 "Amarpur o Jete a K Atisara l " " Maheshpur Dharmapur " 9/110 " Narayanpara " Rajendrapur / g " Jagannathbati o "Gurjala Kamdebpur " Chinsura J6 ! a Chakpara " Shimla D n " " 8/110 H " " r Rabindranagar ! a " 12/94 D Shalidaha e " Mamudpur u Alluvium Jadabpur Dadpur Raypara "! 10/75 Debhog G Areas of very high groundwater " " D t Binodpur ! / Abandoned Channel " s No well observed Very Good TW P i Very High 4.22 D" " AC13 a (Sand,Silt & Clay) LS 10-15 m Not Required Naihati Budhuria 250-300 LPM potential at shallow depth.Most r (AC) Dhuma Miar Beg " n " " L (13) suitable for extraction of groundwater. i Pantra u Pado " Payradanga " Payan " Maynadanga Bara o Birendranagar " Ranagachha Goalapara " g " h " " i " " t 2 "Erenga Kharuabazar Ramchandanpur C " Deulpara a y H 12/95 " / Premnagar p 12/110 l N "Jarura ! Haldidanga " l h DDebipur r ! Amdabad " " " 1 " D a a " Dagachhia Kamarpara H Jetrapota g Surerpukur " J i E / S JM a Pathalia " Dubirbheri Naldanga " 6/200 " Bhushnara " ( " Nima a d ! " b " Kanthalpara "Kuliagar D Kantapukur ! d Kachua a D l " m Taldanga " Dagachhia " 7/190 Shankarbati " N " a " G " Hamidpur a h i a i Bibih"at r N a d t Talpukur M i " / Khoshalpur Anantapur a Kolagar " " i Aricharbheri " Ugli " Bekubpur " w Bura A " " s " 9/105 Napara / NP a Shibtola Madrail d r Laroa Bhatpara ! Bhabagachhi Alluvium Alluvial Plain 10 / 7 Areas with high Arsenic and Iron " a Balitipa a D" " n (As&Fe) RW " Narayanpur " Dhopaghata " S " " " " Younger Good High APY13 r (Sand and Silt) 150-250 m Bolpur a LS 37 Barai 10/70 D! 9/80 100 TW 200-300 LPM concentration.Potable water Bharta"rchak [At shallow Low u Mahishati " ! K (113) (APY) available at deeper depth. " " D " depth] Khalisani k Panchpota " 9/70 Rajarbathan 10/165 Khalis"ani Ganja 9/110 Shashipur " ! s " " D" 10/107 NoaparaD! Chandanipukur " D"! Katadanga " Babubazar Narayanpur Khidirpur n Khanpukuria D! Belkuli Benipukur 10/110 12/155 " " " " a Bainchipota " ! Kankinara ! Kaliara " Bonobazar D" D Panpur P K " Phirgapara Baijala Nafar " Baghabatipur " " 8/75 Swetpur 9/107 Chandra " u " (Nabagram) ! Kutubpur ! Prabhakarkati " D D" " "Chandannagar 6/95 Sundia Srirampur Bahirpur Beleghata " n " " " Bagdanga 6/107 Gopalbati ! " Sthirpara F F " " Jugipukur Urdubazar D " Chankia Kaipukuria D! t " " These are fault / fracture zones, which generally act as conduits for movement of ground water in hard rocks. Along these zones, the yields are significantly higher and wells are likely to be sustainable for longer duration. However, the inferred fractures need to be confirmed by detailed ground surveys. "Daipukur " i Bejra Digra 8/154 " " ! "Bolorampur 10/150 D" N Altara Hekampur " Hatkhola Mandalpara ! " "Laskarpur " Abhirampur " P Anandanagar "Mankundu RS D D D Q Q P a Shankarpur "Jagatnagar " 6/30 These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. d i Surpara " " 8/95 D Q Q P P a 9/107 Jagaddal ! 10/85 D d D ! Taherpur" " " N ! Chhutipur APY113 ! D a D " Madhabpur Gondalpara Atpur D Rautara n i " " a " " Mukundapur K Barasat " " Abantipur Khosalpur "Nutangram Keutia Badpur " Shibpur " Mankundu Gouri Colony Sankar 8/95 " " N.B.-The depth range and yield range of wells may vary within the unit because of certain inhomogeneities. Fractures/Lineaments which are clearly observed / inferred from the satellite image are indicated on the map. There could be some obscured fractures which also influence the ground water prospects. " ! " ! ! Katalpur "Padmanavapur K17 Paikpara " Hindusthan D Biadyadharpur D