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1 <br />'CWO 5L11 V{-L111Ce[Inll I,~•I'W~•.~I,i ilk I•" d~•r.• I~~.r "r'n~ t 1'1 i',I lu' dal 1 :Ind <br />y results Cron tests ncrl uria••~I i~t tli~: f.n~l; :•.nu~., in I{i,:~ .li '.I:~I'..' noa '::i lli:u•i:; Urnw <br /> <br />are Div^_n in nttachn_~I Pi;•~Ir~• ~', tiln,; ~. ••.c 112;;-:;I-l' :~n~1 I'iy,iu-~: ~;, Sln;; 'rest <br />028-81-25, respectively. fh.: ~Inr.l from Li,o.;~• ~:.t Ir.t :; w•rc ptnttcd :Ind found <br />to Eit the type curves, and nre ihcn:lurc I~~Ir.::i~L_r^ i repr•_~u;ntatLve of the <br />permeability of the Sudd.ltln so:un i.n ch_ fnl.lt zo,:eti. l'i•,,, nrr-,;c:bilicy derived <br />Erom the test nn wall. 1)28-91-32 i.n Ilu~;h Dr:lw ~.a:c; 5. 7 ,;pd/:;q. fc. The pcr- <br />meabiLi[y derived Ernm the test un well 112;1-SL-25 i n '::I LI i..~ms Dr:r/ was 5.1 <br />gpd/sq. Et, These numbers cuiop;uv with pr~:;:,•,1!li I ir.i~r; r.ln•;inf; from 3.8 [0 25.4 <br />gpd/sq. Et. derived Cron pump tcstr; ..n nc~ Snd~lnth ;c. ~:n l:cc h,;hibit SL nE the <br />permit, Aquifer Test Data). From [hu dn[n cu!luc[~_d, [he Sud~lutll Senn does not <br />appear to he more permeabLc. is the faill.t ::nne-; than cl:;cwhcrc. These tests <br />confirm that the faults Flu nu[ .u.[ n:; .:nml~li[•: fnr ;;ru nnel w.lrrr flow, ns :;rated <br />in the permit In Sectiu^ 779.11. <br />Kerr ;tine .1raa - Al.l.uvinl r;ruund '.!:I t~tr <br />Water Levels have 6ccn nu,ls~lred and sn~npl~•:; r.ulLcr[~td nt ;u1cr[.:J nLLuvlal <br />wells on a mun[hly basis, liatn un w.ltcr Lcvcl, L.~mp~n'nture, p!1 una eLuctrical <br />conductivity are Lis [ad in at[nr_h~d 'ra61e 3, :~:crr Stine .11 Iuvi:Il Ground '.;a[er <br />°ield Data. Seasonal ELuctu:+t Lon; in w.lcc:r Lew:•Lc du~a ru r.ochargu fro:a enowmeLt <br />and discharge from evapotranspir:I[ion nre rrudily nppnren[ in [he data. <br />Analyses of samples take;, from four LLuvi,IL wclLs at the Kerr 14ine are <br />listed in attached Table 4, Kcrr Mina .\LluvinL Gruund hater l2uaLity Data. Al- <br />luvial groundwater [ends [o be more saline than rnnfined groundwater at the !Corr <br />Hine, because of exposure uE the water tablo to cvapo[ranspiration. <br />Kerr Mine Area - Surface Writer <br /> There was practicul.Ly nu nl:cumnlatiun uE ;now and Littlr_ ,;i,^,niEicant rain- <br />fall in North Park in 1931. Iloncc, the ru wn•; ,Ilm„sr nu ntnnff n[ [he Karr Fiine. <br />No d ischarge from sed Lmentnt Lon po nds; qr epile~.ne r•I 1. drel inm•e~; was reported. At <br />one monitoring station, Sttu 108, flow wag rrruni~•rl nn,l n s.xnplc taken. These <br />data are listed in attached 'r a'n 1e 5, 1981 :iurf rice ~'atcr Site 303 Flow and Qua- <br />lity Da[a. A perennl.aL sprinh at SLtu X011 w:IS respunoihLc Enr the disChaCgC. <br />