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[inamshy 4 SOURCE of LJaterR SOURCE i Sur face Subsurface (qmund wate). — > Rain/ precipdation « : 1p With negent aie) eo xtvaction [presence of wot in a OA i | Soll ow ee Aloe Zone . Zone of Trheamediate Wates Kone poe K fractuTe >mediem pomhcle i, { ( ; “seb ? “= Cop’ takly alder Ron i > é H Ge a . 00rd wole, Zone Free watey/ | + of mau of wile SH Zone > =. om AMpteanat Watér zone. 7 ape ae a Md eT medice hth = ya _ eee iat fo" whee tae 1S prepent 7 Dee ce ne eae te piasie shress. SOGV sai toga io exif rye 988 SSP CN SED ere 7. 69°F se + toner epeneh GS \ ee “Totes preove tt — Ws Yo . bAw X75 hati 2b ; Cort taht fact 2. = Yale eon > bypoatadc PA 5 Pressute Se te ee 9 ESENOTES.COM 1odeh> @ye0/ Properly of caPilav\y wwe 37 « Vigcos ty ‘s bigher a ° Wigeh bail 2 Lower foVeZ1 3 ighss density ” ww 4 Si) ; K Wwores tom (rvoUNA ig possible af meciom Wy Extachon so! oe : Wy possess foo perticr: " wiki ; fe ; | % = WOL Inodi capa ( foovsi a) WwW ¢ J = Nv_ seo Vv Au Vy &X $i Feat volunne of Void = Wy 20 ESENOTES.COM AWE WA we Now choice to extooct esate, pom capil ony - ond then vx first Choice grould be ground wal fe ean this wok) is fee but in capitlaaly, Zone bec aus yone water ig held by soll So mme energy is reqs @ 4p ex teact woler pom this gone a : ‘a paeccn » oO FOL wif we have the choice ™) ‘Bie Intamectiote o yee and capiialy zone then ous first choice | i be Capillary because thee more wale S$ available € inleamediale Zone vols one ai preety here will be lack of water: oi ll eohare oN Ged with waier 30 Conducdios (4) . iS Y ofe che meckum +0 pamt jntesconnect yg avavlic slit H @& Fesmece y/ ee ofeill > Peameatillty 5 ME Guid though ME the flow of voids Me 6 pores [avo i moy be dejnet 0” pew Ke {eked yoids ayn contact CFE: ys face axeo z pPorrrregeae DDO COL DD 22 ESENOTES.COM S : Site fine Sand. mm X Water is only exbacted from COPE’ NS “ Doxcys law = ee ‘ -{lovo. woni- Get and jamimnon =) Assompro _ he e Pa Vv Ox t f 5c. nce te Nest, 3 1a hydaavlic «pod enty ee sot] =.) _ wead os ne ie) = hydsuis gee ~) — vengih of Flow: <3 - | Hy dpaviic head = << bn OB. fe? me) me u fy 2: e——_ ‘2 Sseate samy i = 8 _ mobilen -t LoD: = ° (2+h) - (z+he) _ hohe C anwans' A LE 7 C | ee) _ drodiewt ENG, / Hyddadhic F im) acaurydsadic § ayaa o Z ie LB sume - 4 arek 2 oe a , ye Ki ad bai 23 ESENOTES.COM : : ate Cs we Fravomissi ili ly > Kote of pus tnroug'e mecion rape os} eo m?/n [sex oudg vwt - hydraulic sadn pa ot codth. 7 Aes o| | . © : 1 d = K— 2m A ds ta neo eke Hime of teavel = Gs | | ; op == nowt ae ; | — n = zoso kN “i — 2aso% 0:35 bo dene | ict Ki | = 2orsoKo8> q23+2 days | FUVVORDETTOOOHSFOB0050404556604066%6 [ 25 ESENOTES.COM sPecihes (pet? gwe nt or G > IB Even CAN cwwithyaot all wader. Wecavse cestain ame e Ovex soxsface of “Poaticte pene @ erween coo meet? ¢ if the mecttum is posus an ex meable a wate wil be selaimed of physical force of crt sackoN ib and poicle. and this coarey cetaine A inside’ es She mMedivm particle this Coates ig called od sorbed ale Ayo quanhly ist Wd Specific Yield (Ye) soy yo Armout of oat asoined by SE = { ium dane! $ - Amoonl of mediv Y= Me me: : Vv wae * ial copaci\: . sestic engny re fad dete adhoro > The W A oont of water we laine Aa aga Ye = FN rad amOUne OF ais — NR y\00 Vv Vy . YR Upt Va _ Nw Ye Ya= = eet ma Vv if S =A 4 \ 26 ESENOTES.COM TTrrerent “TYPES OF MEOLOBICAL Fopmario’ a » AQuiter: Aqu' fe, are Wose ja ological format @ eonich are ; h\y peiooun ond ‘perme e@. oe hence, -Ihey Gr high yield: “ e4- fine sand, Coorse cand: « SAgueee Fowenity * Ray Yield exomble « AS vVIFE _—s ee 2 - oe ? uy nh ae 2 AQUICLUDE ATT NANG mx cloy « $) AGHITAES watt x -sandy cloy o- (see page _ 5 AQDIFUSE K . a “? (wide 2210) x x Gwe sto ge Types of Aqui fen - ’) uncomined Aguifa/ Nor orks uy confined aquifer f Axtesion- (iy Pesched aquifer. sian [woos sable aquier. ron colich Qe 2 of geolo cod qoomok eae OF ee oases cant be dwained Arrovgh proppneee @ Aqeiyds Thes se pose fou} impettneable tk eg: clay. @ Aquitas a: These ave type of fosmoatiod vorich, One Poses ae : (but less oo compare to aguic\ode) an less permeable hence wore cloes not fjous thasy ‘them put instead — tt scePps: (seeIe9e) eq. samy clays @ Aquijese é- These ave 4osmatio® re) CSOUS nov peinteable . : ‘ eae si woele + 28 ESENOTES.COM | hich are ne! soar oe 1D) Dacomined/ Water Table Aquifer, /NON-oB 1140: 2 No oi press ove - : > No artifice pressors: > Top zene or satus ation > These ave type of satuvation aquifer maaks dhe upper limit of satuxation - > IAlater in “hese aqujor is gubyec tect Jo pressure no ‘ch Anak hydleostalic pressure - ja water table level. in. eahich Grtast, i Wy Confined Artesian Aqui: 3 ail a paessure. | > Thesewore the type of aquifer which’ ore fosmed when | a peaviors medium 1's {yund +o ent in beiween ! Jwo compercreable laya- > wate, in these aquifer ave sub Hydao statce pressurve. ecled 70 Pz ssuve grea than Popched agu {eg . Sometimes an impesmea ble ‘ periows medivm, abeve qe Gwe: COB*VIKF snot can Jolso be uged oD somce O layer is found 4o exist 11a Hhe sotvsased £ water cD) Sol mass and 1s koamed co YP Semi: eonjined 4> Confined aq TN do ARH aquirord 3" M21 i eyched agquiles. : Lifer. & Giall AW cqutsel Axa water leak al ee | woboevv>UUDUEEGEUGEBE4O5459 4460660 9'9 \.. m.29 ESENOTES.COM ee Hence in “this case storage co-efficient js Aefined ap volume af water geleane from dhe aquiler from fowl aquile, heign! and ynil c7oss- sectimal qveq when Prometsic Surface clecline bY ortity. " Stoxege of Cortiedent dow comfined aguilas = = @hn(+ne) = YwH fas Yeo = Unt i of watel H = contined aquifer sthicknees ™- K= Compress i billy of pe aquifa -e EC, = Slaoticily of aquile. B = Compressibilily of waty = = , ly of Water. Gor elevtic! avast : ESENOTES.COM Diffexeni yosms of exiwection of Ground Wode: \D Infilbation Golleny _ ogiee'e! fitsakion galiesy ae enesally legit at shallow depth of 3-6mt along the bon th hich nN Water beawieg stuciure ene “ eohich 18 is utilized by Seqpoys from Sv srace | 0] oe made up of brick mowan’y [Se no - sonnel! ce of the wer che vwooreh genvory eames te &—— . 4 LLL / RA impermeab\e \oyeh H qa } H = Height of the coatey in the viver/ oo heh of pigir cooler table. hoe hejant of wates tn AID BEAGWAY = R= godivs of infivence ~ SY0™: 132 ESENOTES.COM mo tice RRR 1 GRIN ©) In Gi rasion Wwoll. in G : ee nGilPation wells ave hallow cligcoutinouy Cc Qhor \ the banls of she awe vhooudh wonich the gocties is Utilised by Seepage fom bottom, on oveted miilbaliog wells are connectect ~yreoug > Sevejal Sveh Known ad Jack well: from where was Qa Common ell beg pomPed who the twealment plant ee (a+ dt ds). _.&n) 3 Spay ahe gourd Nokvrel out of Siow of around paler GP Ove’ _ ausface js Feomed qo span: ; - p.6Kk asiepian sping awe co iderd as ihe potenk al SQUsce fo) grond poodgn Qince roalies Keo onder preoorel, J v OPEN TUBE ! \ SHALLOW peer cAuny Screen STRAINER aravel PACK OUIesy THD Cos Dia - “ Nv clepth — wv ~ Disehoor ~ ve av cohics dese OOd fom yvppa evr Spattow well - are hose pearing stata. ; gases Wales pearing Sots - peer well+ leave wale: fort (gaee booles a — TT oT ESENOTES.COM es bats 38] Vevelody, Gy verre dime depen: V, = Xo GQ 7 Q> =ihw ; Q, = AKt = A, Peas ; RK “Rh Gh CA Se Oe / : Shmnt{mn / sec le fe copay of open wort (nis or see prone: Not 036 Fo ynsread y otal, . nk ? Dis MONE cake 37 ESENOTES.COM W) Kecureran0N vest As it is difficolt to marntatn constant level (sk State) of waters in well wecupmateon ost {S ot paxjoarn® in oxdes to find 4the speaific Capacity of dhe level of wale, vecoPAaled in-the well well In & ger as nolect $1 Osclex to find us yield, eady e Sntme ak. Volume of wore? pecubetated ‘in well 0 siete olume incseosi's) « dv =7Q dt =tA ds Geers) 7 As chapel” Ss 38 ESENOTES.COM 
