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<br />. MAR~28-2000 TUE 10:48 AM <br />E'''''l'''' <br />.~~ ";' - \.~.., A'~ <br />.... , .: ~ "'J "~" , <br /> <br /> <br />F.c.UTUation orthe lIRel LoS.Ii Par.:uuctcJ'S r01" R.outing tho Probable Mllximum Flood <br /> <br />'I ~.I~'O I <br /> <br />I <br /> <br />- SfRTL-'.Oll1cn <br />-- . $ m,TL . U5 inch <br />. SrnTL = D.G inch <br /> <br />(A) <br /> <br />:ijt ~..., <br /> <br /> <br />,: <br />.! <br />,} <br /> <br />;; <br />" <br />~ .I::'~Cy <br />.: <br /> <br />~ ': <br /> <br />CNSTL. 0,1 in~hlhour\ <br />\ <br />~ <br /> <br />.~7:'1oI1' <br /> <br />, <br />,~ <br />" <br /> <br />", <br /> <br /> .tT..lOQ ,_. <br /> 3.00 <br /> i'r./tJO <br /> '"'.:tClOD <br /> L,JIJuO' <br />E 4UOoo . <br />~ 3\"1000 <br />.. <br /> :':uCu,) <br /> 'U"'l.lO <br /> . <br /> . . <br /> <br />. <br /> <br />U!l <br />"1"'" (~.y) <br /> <br />3.50 <br /> <br />,\ <br />i <br />! <br /> <br />STRTL = 1,0 Inch <br /> <br />IB) <br /> <br /> <br />H <br /> <br />\ <br />" <br />I <br />, <br />I <br />r .~ <br />; <br />l <br /> <br />- CNSTL a 0.' IllChlhOLlr <br />.... - CNSTL.a 0.05 InCM10IJr <br />. . .. CNSTL ~ 0.15 inchitlour <br />_.. ODNrt <br /> <br />, <br />': <br /> <br />,j <br />,'I <br />.) <br /> <br />,'. <br /> <br />.,... , -...."", <br />Ii 11 10 12. <br />Time (day) <br /> <br />,i <br />, <br />" <br />I <br />, \ <br />, ~ <br />; <br />.. <br /> <br />l"igul'o a,I~IT..1 orCA) STR'I'L .lId (lIl CNS'!'l, on the PM.' <br />,It lhlt Outlet of the t~nBlcwooll Willillrllheu, 'rhe: valL\c <br />STH'fl.. III: ].0 iueh in (B) dOIJ::l not UJ.lply (11\ tho ODNn curvt!. <br /> <br />'. <br />,,", <br />" <br />, . <br /> <br />III ,'unt.rnst Lo STR'l'I., the pnr:Ulleter CNSTT., great- <br />ly ;'.lfucll'U tho PMF', llH He"o in Figllre Sb, which al.~o <br />.1.,.""" the hydro!!Taph obtained by tho ODNR study. A <br />,.t.d iI,tl"ll ill QNH'I'L hy O,Or. llltltlhuur ro""lto,1 ill ~o <br />11il"""'''' nftho )leak l'MIo' by about 27 percent, which <br />i:, l'!1I>0 to Un' peak PMF obtai nod by the ODNR's <br />SI.II<1)'. 'l'ho incru:Iso in CNS'l'I, by 0.05 inch/hour <br />tallol"l" reduction in th" peak PMF by about 18 per- <br />t,,"l. 'I'ho time-to.peak W,," the same for all hydro- <br />I!I "phs, which iN IJTobnbly due to tho retardation <br />Ull",," Ill' Ibo ro"orvoir noar the dOnI. 1'hc paramoter <br />eN:;'!'!. hau mojor eITects on tbe o\ltflow hydrOb'l'apb <br />\".,'''".,0 the PMP Is a lon~.duration ~torm, and. a" <br /><1i"'II,.,(;('<1 curHer. 8\1eh .torln. arc IItoatl)' ..ffocled by <br />{;H:,'l'l.. <br /> <br />" <br /> <br />t "I <br /> <br />OUl!rtoppilllJ o{the Englewood Dam <br /> <br />The final goal of this study is to estimate the over- <br />l.upplnll of the PMF waters at tho ~rest of the em bank- <br />mcnts of Englewood dam.. ,To determine the effe~t of <br />the parameters STRTL arid CNSTL on the PMF at <br />F.ngJewood.Dam, HEel was.run for 110 pairs of <br />paramcterlvalues"STRTL values ranged from 0,0 to <br />2.0 inches ili'increments of 0,2 inch; CNS'fL values <br />ranged from' 0,02 to 0.20 inchlhour in increments of <br />0.02 inchlhour., '['he resulting maximum depth of flood <br />waters at the erest of the embankment is summarized <br />in Figure 9."Overtopping estimates ranged from a <br />hi gh of nearly: 11 feet abeve the .dam crest to Il. low of <br />2,3 fcet, below 'the' crest: .The horizontal shape of the <br />contours demonstrates that the PMF. is not sensitive' <br />to STR'fL, but'highly sensitive'to CNSTL, Overall, <br />each increaso' of, 0.01 inchlhour In CNSTL produced a <br />decrease of about 0.67,foot in the water level at Engle- <br />wooddam.;~I;,;;:,I...,,1'!."~<<" .', '. ',':' <br />While the ODN-R's lose 'parameters predict an ov~r-' <br />topping height of about,S feet,.. the design parameters' <br />of this study rcsult in an' overtopping of about 3 feet. <br />Figlll'e 9 shows that no overtopping of the dam would <br />OC~llr if CNS'fL ,were . !!Teater or equal to 0,15 "inch/ <br />hQur. ' i.. .' ...., ~.' <br /> <br />, ' <br />, . <br /> <br />" " <br /> <br />':,.:', <br /> <br />, I ~, " " ,;, r. <br /> <br />.' :' <br />" <br /> <br />,', <br /> <br />>, ". <br /> <br />'.' <br /> <br />0,02 <br /> <br />---..-- ~ ---.- ~_..-.- <br />.. "'~"------- ---" <br />-8,0-"-'- ~__--_. <br />--' <br />"7.0--------- <br />,0 _..---~ <br />____-5,0--- <br />.....--- . <br /> <br />0.04 <br /> <br />- <br /> <br />0,08 <br /> <br />'t:' <br />:;l 0,08 <br />o <br />.s;;: <br />- <br />ti <br />g <br /> <br />(0 <br /> <br />--- <br /> <br />0:1 <br /> <br />", '. <br />----.---.- <br /> <br />. ----3.0---- <br /> <br />",---' <br /> <br />...I 0.12 '2,0 <br />I- <br />U) <br />Z <br />o <br /> <br />1.0-- <br />. ~-O.O <br /> <br />0.'4 <br /> <br />0.16 <br /> <br />0,5 <br /> <br />0,18 1.5-'-- <br /> <br />0.20 <br /> <br />" , <br /> <br />0,5 <br /> <br />1 <br />STRTL (Inch) <br /> <br />1,5 <br /> <br />2 <br /> <br />. ~ ,':" <br /> <br />~ .j", ,.; , 'r, .' ,; <br />Fill""' 9. Waier Lovol It tho Bllllllwood Dim It thl pe.l< ' <br />oflbe PMF as . F\lnction .rS"rRTL and CNSTJ... Th. <br />v.lu. O.O,corre,~onda to the ...,t of tl", "'IlbankmoDI.. . <br />1'h".c:irclCl Bod the- Iq~ represont the OONn " <br />~t.1:Idy and the present aLuc!y. rr.spectivaly. <br />! <br /> <br />,. ' <br /> <br /><'.. <br />