Ground Water Prospects
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L E G E N D GROUND WATER PROSPECTS MAP MAP UNIT GEOMORPHIC DEPTH TO RECHARGE G R O U N D W A T E R P R O S P E C T S RECHARGE GEOLOGICAL SEQUENCE / STRUCTURES ROCK TYPE UNIT / LANDFORM WATER LEVEL CONDITIONS ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) ( HYDROGEOMORPHIC SUITABLE & UNIT ) BASED ON TYPE OF WELLS HOMOGENEITY PRE / POST- MONSOON AQUIFER MATERIAL DEPTH RANGE YIELD RANGE QUALITY OF PRIORITY AVAILABILITY SUITABLE IN THE UNIT GROUND REPRESENTED IN (AVERAGE IN METERS) OF WATER OF WELLS OF WELLS WATER THE MAP WITH & SUCCESS WATER PT = PERCOLATION TANK R E M A R K S ( SUGGESTED ) ALPHANUMERIC CODE ( EXPECTED ) RATE OF WELLS POTABLE (P) IRRIGATED CD = CHECK DAM ( PROBLEMS / LIMITATIONS ) NON - POTABLE (NP) AREA NB = NALA BUND NO. OF WELLS ( RAINFALL & OTHER LS = LOOSE SEDIMENTS = DUG WELL 3 RW = RECHARGE WELL ( REPRESENTED IN DW MIN - MAX ( PROBABILITY ) ( REPRESENTED IN OBSERVED SOURCES ) PR = PERMEABLE ROCK RW = RING WELL ( in LPM or m / day) DT = DESILTING OF TANK FIR ( INDICATE REASONS IF ( APPROX . RANGE ( COLOUR INDICATES THE MAP WITH THE MAP WITH = FISSURED ROCK BW = BORE WELL NON POTABLE ) RP = RECHARGE PIT FR ( IN METERS ) IN PERCENTAGE ) Kilometers YIELD RANGE AND NUMERIC CODE ) ALPHABETIC CODE ) = FRACTURED ROCK TW = TUBE WELL VERY HIGH SD = SUBSURFACE DYKE HATCHING INDICATE WR / = WEATHERED ROCK / DBW / = DUG CUM-BORE WELL / HIGH RS = RECHARGE SHAFT WM DEPTH RANGE) WEATHERED MATERIAL DTW DUG CUM-TUBE WELL MODERATE ST = STORAGE TANK 0 1 2 3 4 5 © IR = IMPERIVIOUS ROCK LOW SCM = SOIL CONSERVATION MEASURES SCALE - 1 : 50,000 Cut-off Meander No Well Observed Very Good RW CM111 LS 10-15 m 200-300 LPM Very High P Nil Potable water available at shallow (CM) TW Not Required MURSHIDABAD DISTRICT, WEST BENGAL s depth. MAP SHEET NO. 78D/4 t " " i Lalipali Chorgachhi s " 16/34 Saundighi MS111 " " ! o Nidhia D 14/34 Baliabhboti D! 14/34 " p D! Boara Baranagar A4 14/45 M23 " 15/34 e " Rambhadrapur 16/34 ! ! " ! D D ª Bharat Chordighi " D 15/73 Korai " (! Chanda "Ladmadanga y ! "Krishnapur Ghuguriadanga 15/34 Korgram ª E " a " " ! Mahalo " d D "Chyongbela Suki Poranpur" 14/34 " t Targram Asanpur Groundwater prospects very high " ! Dobhadanga n (! Nanoch D " ! Choukibela Meander Scar No Well Observed 16/34 " ( " High P Nil e Good RW 10-15 m 200-250 LPM Not Required (! E ! Kamodda E MS111 (MS) LS with high recharge potential. ! D Milki " s E Tentulia D ! 15/34 TW Recharge structures not required. 16/34 Palasi ! e " Beruli " 14/34 18/34 " ( D ! 16/34 r "Nimgram D Taldanga 14/34 ! ! E "Narandanga " D D D! P Diara / "Mehenadanga " ) y " Ashundighi " n ! Bilol 16/34 " Masjidpur ( " a Samtalpara o Alluvium ! i "Baniyapara " E D D ! Garsama "Chandabagh t (Sand Dominant) Tiknara Nagara ( " Benipur " a Ikrol " t (111) " Bishnupur E n "Buradanga " m e 14/34 r "Chanak s D! o NP " e 16/34 F Flood Plain RW 16/35 Khajuria Nagara r 17 / 12 Areas with high Arsenic ! (! i Very Good Very High (As) 100 ! FP111 P TW 400-600 LPM D Karjora "Samtalpara (FP) LS 80-100 m Low D Mubarakpur h concentration. Recharge of Kharikadanga " ( " " "Kusmor E 1 [At shallow t "Purbagram 10/45 shallow aquifer suggested. 16/53 Siara Kethar a depth] " " ! ! "D r ª 20/34 Shusinidanga i Pasla Majhigram ! g " D "Amar " N ! a H " ( Haripur h 18/34 3 E 17/34 4 ! B D ! "Talapahar "Bati D "Ramanandapur / " 15/34 Kiriteswari Jakhirabagh i Jaychandpur 17/34 " l Taluyadanga " ! Bogdanga )" Kanfala ! D " 14/40 9/34 g " D "Damrul Budhyadanga ! ! u Panchgram " D D Flood Plain 19 / 12 Groundwater prospects very high " (! " (! (! Jarulia H Very Good " Binodpur Mukundabagh (FP) LS <30 m 250-350 LPM Very High with high recharge potential. ! E ! " TW P E E ( "Manjhipara D FP111 23 Not Required 17/45 "Udaijol Itor ! 72 "Dangapara Vidyabati " 20/34 14/34 ( Recharge structures not required. ! Dakshingram E )" ª " ! " E 18/34 D! " ! Kishorpur D Phalsabagh D 10/34 "Sajaimati "Muramara Gura (! " Ghughudanga ! " Pathanpara M16 E Jafrabad 16/34D Paisanda " "Nabagram 20/58 " "Sahebnagar "Chak Shilgram n " " ! 22/55 Bara Satlakshmi ª Matradanga " " o Kachubari 16/34 " ! Narayanpur Bathan i Mominabad ! D " " "Ramdanga Palaspukur " Bahala D Bholadanga " t Uste " Simanapara " 12/34 " a " ! m Chupor " Dhamua G D " (! r Alluvium 14 / 9 a Kaliganj E Backswamp M17 " o Nil 14/34 m 15/34 Ramkrishnapur (Clay Dominant) Poor P Areas of low groundwater potential. Bagmara BS12 F (BS) LS TW 60-70 m Low ! b ! Chhota 4 40-50 LPM Not Required D" Derul )" (! (12) Better potential at greater depths. " h D Itasar"an 14/34 " Haidarpur i Bathan a Derul (! r ! " Ghutepukur " E a "Panchanandapur 10/34 ) D w E e Singar ! t N " Jalukhan 4/38 "D n " a " 14/34 Lalbagh a Fakirpur d i ! ! e D Pamla Khekul ª K " / 16/34 " c (! "Rajdharpur Rasulpur " a D! " E 16/34 o Chandpur r D! 15/38 l u o "Garera ! Bhattabati " ! D s Isanpur ( Aimadpur Raghupur H " " Srirampur " " E " n NP Muldanga i " e Alluvial Plain 4/34 Gangarampur 13 / 9 RW Areas with high Arsenic and Iron " t Ratanpur h Hijrol " 4/34 ! ! Talguri Younger TW 100-120 m 400-500 LPM High (As&Fe) 42 "Saidpur D ( ! " (! a Low concentration.Potable water Panchanandpur ! ( Bilbari APY113 C Good LS ! " D " 15 [At shallow / 18/61 L ª Gopgram E " E (APY) available at depth range above 100m. " E Jaykrishnapur Upar h "Gorara depth] o Diha g " t "Rajarampur Lakhanpur " a " " Rainda y " " Pitharpukur b Hajipur Jhulanpur 6/35 "Sibpur " Lakshmanpur Belun l Alluvium N. " " ! r a m rk (! Bichhuti wa DKalianganj " (Sand and Silt) D Mururia a " E a B " r (113) r Bagaripara E "Palsa a ( Srirampur1 A hm"Barkhatpur " Diha a n APO13 " / i (! "Natungram Ramchandrapur N a " a Alluvial Plain 13 / 9 Good Potable water available at shallow Samostapur " d E Mukundapur r i " " LS 200-250 LPM High P Not Required "Alinagar Chetanpur Debidaspur Dangipara APY113 u Younger 25-30 m 49 depth. 16/34 " " 28 TW "Radhanagar Darerdanga 12/34 k ! 16/34 " "Sankuria Khili (APY) D " ! " s Rahimanagar ! ( D! D E n Bagmaria a (! " Rajkhanda P " E "Mahadlpur "Chandnagar "Atbhagia 7 "Achhra ) n H Indrani e " o S 15/34 n " i e 11/35 Banara t ! " NP Amarkunda D c Rabigram " Dafarpur ! Bhimpur a Alluvial Plain Older 18 / 12 Areas with high Arsenic & Iron " 15/34 " D "Fatepur o Moderate to "Santaldanga Bundhalpara " l (As&Fe) RW ! Gramdighi m Moderate to Good 65 D " APO13 o (APO) LS 100-120 m 300-400 LPM concentration. Recharge of r 6 TW High Moderate to Low Sherpur 18/34 H [At shallow " Madhunia o ! " Nialispara shallow aquifer suggested. Gobindpur " y Achhra F D " Gangarampur " " l depth] ! r t ª Chandpur a 14/58 ! " (! a ª Anantapur E " 16/48 E - Alluvium h Amjua e " Daspara Kanakpara r " n " 4/34 "Budharpara (Sand,Silt & Clay) 4/34 u "Sahapara ! e c 15/34 D! D 5/34 p (13) ! o Durgarampur ! " t " D 14/34 16/78 D m Raghunathpur 15/34 MS111" s i " Digari ! (! ! " Nandigram a 18 / 12 ! " D e ª l 15/40 Sadal D R Alluvial Plain Older Moderate to RW Moderate groundwater potential at E / 75 Patna APO13 P Moderate to Good P ! " 54 LS 40-60 m 150-200 LPM ª a (APO) TW Moderate to Low e High intermediate depths. t 16/63 Raninagar u j a " " i ) L "Churigram ! Godapara ( ª Bagor " Sibpur S Maharul " 16/34 " 19/34 Khurd D! ! Bhatkonda " 10/35 D Narayanpur ! ! "Bagrain " 13/34 ( D F F " ! Bhatpara E 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. Jahangirpur Asua D Bhatpara " " " Tentulia Shiyaipa"ra Radharghat " Palasi 20/34 "Charkhadanga " D! 16/34 ! 11 "Shankarpur D D Q P SH D Q P Q Q P P These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. 10/34 D D "Ugura1 "Bardanga "Phophar ! BazDarpara Surkhali " " 16/30 Bogpur D! 12/34 " ! 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. "Bahadurpur "Jamna D 6/45 Gura M2 Polladanga!" Locations of the recharge structures shown in the map are tentative. This map is useful for narrowing down the target zones,and exact location on the ground for wells and recharge structures should be identified based on follow-up ground hydrogeological/geophysical surveys. " " Parbatpur D "Sundarmanik Jibgrrti Udalchandpur " " Moktarpur 12/34 " Panch ! Lakshminarayanpur 15/34 D " "Kethe "Gatla 21/34 ! Balarampur " ! D " D " Haridasmati 16/34 23/34 16/34 " 16/34 15/34 7/22 Liakharda Muraripur Dhala Kandibandha Panthapara ! ! "Mahal ! " " " D ! ! D Benpara D " ! D ª " Jiyadara Jhaudari D " Gosaindor " "Andarmani "Dangapara 14/34 "Basudebkhali Dunigram "Pathal ! " Sundarpur " D 16/34 GROUND WATER PROSPECTS INFORMATION STRUCTURAL INFORMATION BASE MAP INFORMATION "Pushkarni HYDROLOGICAL INFORMATION LOCATION INFORMATION "Mahalandi ! "Belun " D " Natunpara Beliakhali " Durgapur " Kalidaspur " DEPTH RANGE OF WELLS DESCRIPTION SYMBOL SCHISTOSITY/ Salpara "Badtipara DIPS BEDDING SYMBOL DESCRIPTION Margram M14 " YIELD COLOUR o FOLIATION STATE INDEX DISTRICT INDEX "Nisadbagh Dangapara 16/34 " " RANGE SHALLOW MODERATE DEEP CANAL / TANK IRRIGATED AREA A-BIRBHUM Naoda Hatpara CODE GENTLE ( < 15 ) B-BARDDHAMAN " o NH - 2 NATIONAL HIGHWAY ! Nischintapur Pulia i OF WELLS < 30 METERS 30 - 80 METERS > 80 METERS E E E E D " " GROUND WATER