(1991 Duncan & Wright) Slope stability during rapid drawdown
Short Description
(1991 Duncan & Wright) Slope stability during rapid drawdown...
Description
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INTRODTION The wters had he gea plesur of wong th Pofessor Seed on the eseh erd n ths a. He plyd n cive le in te sudies sud ies whih we gun in the ey 1980s (Wong, Duncn ad Seed 83 d contnued late unde a ntat fo the S Ay Cps of Engnees Wgh nd Duncan 187 e gt nuence on d onbutin to leased t akwedge rofes Seed's gt ths work ad to dedate ths pa o his memo
AID DRADON LOP BILIT PROBL hen the wate leve outsde so dops, th sablzing nuence of the water ressue ressue n the slope slope s los If he we eve subsdes pdy th the e ressues withn the slo do no hv tme chnge n equibum wth the drop n exel wte evel the slo s de less sble Many filures of dm slopes n nu sopes hve cued dung d don don hese hes e ncude fo eple eple Pilos D u of of S Fncisco Fncisco A We & Ass 7 Wle Bouldn D n (Witeside, 176 d num of e k sos ong Ro ono n Pe ee d uncn, 75 Rpd ddon imss ve ve odng on slos nd is ondio cs c s seepss of upsm slos of uenly te desgn ondio ams Anlysis of pd ddon s heefoe m consdeon fr esgn of dms, nd fo desgn of he slos t wll submeged d subject t dwdwn
UniverslY Dinguh ofe. Vgn Poyhc In In d S Unrty Bakb, VA Ashley Pidy Cnnnl Pro C Engr. Unvrt Txa, Ausn A Poe o C Enn n Ny Tnonsu ng
Dun�n W&h a W n
at of hgh aby can dring pid drado but teas clay cnten ca T aalyze sably during pid radow it s ecss di whch teal ll drain an hich will no. In doubtful c it mu b a tat dina eihr ill or ill nt cu whhver ill reslt in low n withn h picul o th lowest facto of fety f th lo s an imprabe i mprabe evet evet F da d aOn rom a high or lvel s n nt ee loing ca h da it i aroat to lo f f y f h rapid drawn drawn con For other da da otabl t jtS, epi of pid down c quntly, and he to rui n ul oti oti conditio conditio In h h ca i i i hih of fty factor fo th dawdown conition a othr dsig c c hih pbilie cc
MTHOD OF
AAY
ili dn pid aon has e analy in o bcally fferen wa: I usin effctiv sress mhs, ad (2) usng totl ses s hch h unind h sreh of he soil relaed o th conolato presures in l t adon Boh mehs at f f inig marials in he sa trnghs aed of efeiv sreses a s ssum way. that e prssurs hn hm hrosc
o ffctiv sress analyes s th it is latively e to vluat te q h sngth pt ffcv s s sh sngth pter pterss fo rdily dtind b mans of ioopicaly coldatd ndri (C-U t with reur rnt Thi ty of te i wl wlll t o chnc chnc la wit e f ctiv e aly is that i i dicult to esimat wit
y ru tha will exit withi one drang tels d dn T ressur change urin rawdown end on th change in ss tha ul fm th changin waer loads on th slo ad th unai r f t il within th lo o h chgs in load Whil he chane chane in c b simae wit aablaccucy aicully a shallo de nat t ue of the slo th undain s of th sol is much haer to t. t . T chaes chae s i re presure oud xcted to to cosieral diffren fo teils tei ls h tend o date ui shear an os h o o Whie Whie n cipl it i ssie o esime hse r pssures us kmpo's prss ts po 9 p s s u
f
dug rpd ao have In st caes efe used he sumpo por su h r sue y shp 195 and ler us b Mo 1963 hee asumpos hav e
SS
justi on e i of e f t t cve cs y hve n foud to ult vu of f of fet f d tht uffer pid dwwn pid dwwn flu W e 183) f vs of set fctor lculted using Mrgnste ui w F 1.2 f Pilito D F : 10 fo Wter Bouldn D of whh fl t sms liy th Bisop nd Morgenses supions for pore pressures own my b re ur urte te for sil sil h not tend te nd o dil dil durng uring dw uring dwown sh th for hos th do e t dilte u, ug sumptions my coe e wt fl of lo n mtis mti s e not ho how w rle coee co ct d dl dung s te te lkel o b nl coct t to dlte dung ndu conve fo he he s of eff ef fii v e o e Bs d Morgenst u wou l w s p esu dung u wdn gdl of w we w ngly he gt gt d dt dung gh nd P (1967) suggs resse dung wdown in wll co compcted sily snds snds could b et e t ung ow nt everl invesigtors rowzin, 1961 Brhm d H H 1963; Newlin nd Rossier, 196; Desi nd han, 19 sa, 2 1977) u htcl ths to nlyz th onsad onsad low conditions following follo wing drwdown ik ik the ishop ish op and orgnstern re pressure ssutions tese meths o not consider he hvior of the ol wit gd o diltnc, nd e tu not caple of presentng all of te n fctors t conrl the re pressures during rawdown ano nd Nord (197) nd Wg nd Duncn (1987) used prurs for sng p pss ss dg dwdwn t t t ue ue of dily re pressu pressu changs changs vo vo nd No u wo-stage sility anlys irat to hiee nsistey bwn t clcul ftor of set e es f he pssures nd Du us nie elent nyses to sme ketons r pressure pmers o e sess chnge durng lcul lcule te re ressure e te te indce indce t it i ssile to estim estim alistic pressures for ecv s , ut it cubo icult t using tot sss s s de in te followng secons rghi d Pk (196) sumz the prolems in estiming re prssurs urng drwdown in tse words " in i n order to determin deter min the pore pressure conditions fr te t e drwdown stte all he following factor fac torss nd o b known the lation f te undies btwen mterials with signicanly di d iff eren er entt prop pr oper ertitis s;; he pe perm rme ei iiiy y nd c onso on sollda da ion io n chara ch aract ctri risi sics cs o ch of hese materi mat erials als nd the anticipa anti cipa mximm mximm ra ra drwdown n dition he pore prssurs inc y e chngs in h sheing sss thmsels n o n ino considetion considetion ngineng practice, fw o cn b relily deteined The gps n he vaila thse facors cn
c, Wieht d We
By , e anale a ei i the folloing io p etive s y f pb iat iat with tabity aals y av te o( v by imp
t Cos o( gn 1970) a ttage e ( age, hih azs s fo awn i u p e deee dee e ves ve s of onoliatio pre aon aon e i p fa fae e The The d ps a to e he g value e s wh the w w T nt vae ( he d e a eteined t -U g eve how F 1 At w s, whe enve ie ae the eeve n n gh envelope i to etene engths (r the y
Either drained or U enelope s used. whiheer ges lor strength
,
:
Normal stress effect e str n bae of slie before drawdown
Normal Stess F
Srh Evelop Used in Cops of Er Mtod
T j ( di engh evel alow e i o avoi
y h tha negave p u, hih oul
Rapid Dro
cause the effectve al sess us to determe te she sength is the fctive sess foe rawdw. which is wer tha the effective sess after awdow eve when it is ssud that e re pressres after dawdown ydrosttic ydrosttic As a result the Corps Corps f Engieers metho meth o is unnecess unnecessly ly nseatve e os nees meth avds the pblems f pblems f estimating estimating changes n esse d dwdwn by usng urin stregths t aayze stabty after adwn adwn By sng sn g ndrained stegths this predure pre dure accuts accuts fr the ndecy f e eal to dlate compss dug sh While the of the ttal sss IC-U evelo is quitively cot. it cot jstie in detail Te cirles f se u to eel te total sess evelo mbie te efftive s ng colio wit devi se a filure filure d nt pret state of sss i e e il t y gien r e ay that the sesses o e sli se a relat to e ICU eveo is sistent sistent wit te wy the eelo is lo lough e ers resutg tese icnsistecies re ot exemey ge in os cses te se o an icosistent a illogical met lg se s to lo pressu is undesirable undesirable As dscusse dscusse i sube ios tter tter pes fr relag shear stength t consolitio pressre ve e develpe by Lowe a araath (19)
ike the Crps Egineers meth Lowe an araaths meth uses a two sge alysis rere. and ses uae sregs or alysis o stability urng rawdw rawdw s shw in Fig, 2, we and Karafaths meth us eves that are mre gcal than the tta stess C-U envelo for eang unin shear sengths t ndation pressures The hortal ais ais is the effetive sess sess on the failure lane urng cosoliati ( fc ) the veic axis is te shea sess o the
ailu lane at failure ( ff ) we and Karaath shwe tht the ndained seng of soils when ptted as vs 0'fc vaes with the efie pcil sess tio dung conlidatin c
l c "3 c The value o this ratio ca vay rm uity (fr cosolidatio under istropic stresses t K f the vaue of 0'1/0'3 at failue As the value of K c ncreases. the ndraine ndrained d strengt increases increases Fr ay materl there is a amly o ndane ndane strength strength envelos coesnding to dfferent dfferent values of c varying t Kf
e maner f repeseting uai sength suggested by Lwe and Kafath, hih is shwn in Fg 2. is lgica ad accute e testing ruire o establish envepes however is diffcult diffc ult Test specin hese strength envepes
S
Dc. Wriehl Won
us onderble t d carful tteto cu the ree mut wll l durg nc slwy t vod the poblt tht the . vue K c. th e m re t s pu a e t t wl l dn cld Fe exenc orn l , nd t o empl Lw K t o l
u .
-
+u
C -
� +
0 u
C O
Effecive ess on the Fue Plne Dng Consoldn-
C;c
Srh Elop Usd Low ad Krfh' Meth
U Eer Eerss t te Lwe d Krt Kr t th u the the ni sn evelopes t low tree ere he udred treth vel l ave e enelo T th tu ot ll O b sb to blz ll ndre tth n w w cv e VALUATIG TT FO PD DWDOW LE
A
e t reptn ure ure ent p s c d ccrte, bu eblsn the vto Lw & wt coldton ure ole dcult d enve
re
Rad Dawown
Bau o dfi ivv ng ACU ail s a num of have suggstd esmang rl o ACU tesS rsus o ICU es o n abe his e o y un I- e a T s cD d, au y D bj T s pp i a snge n li r.
c,,y o en, ACU sg ul o IU Tay (18) (1) Ny T s by W, (1983) wi t - eby Tay (18) rl o te AC l c u it �irs ph ng ur f y sgs dung - the the met meth h sugg sugges esed ed m o
we and Kaaiath (96) esults nh envels f vs of
t sue by y rsu n able
AU sngh enve
sties d by g e 983) s is al ssibe e AC-U ng enve CU sn rul rul ntelaon ntelaon e envel envel cosng c l 1. n F, 2 is ICU nvelo an bhed plOn ' c enve sndin to c Kf siy he e sss sngh envel tlis plg val o 1 V C ll o ru ( 1 1 Cf c n n ompu omp udd m h rsus o IC-U axil tes ith e Envel f val of inae ae n . ur sun Envel K estals y ing l t envels ( 10 K K . is ur es t of AC ngs mh ease l u i lies e sy o in& in& cut A· Aon s rth AC-U nels of t ty swn n 2 etlh lin nce sig he sul o C-U tes T
EW MTHOD FOR VALUATIG STABILTY DURG PID A WDO A WDO h un stte of o anazn stabiliy un d dwwn it is
Duc, Wrht d Wg
Lke he he C o ngnee ngnee h a e n Kth' ew t us unned he ngths to aod the oml ccces invlve n etimtn uaned reue ur dww Lke e a Karh' met t e moe ue v ene th AC-U ngth ng th te al o K c Fw t s W e (13) the AC-U trengts emd ilan u sus o ICU s uned sn hJ her her n snth hi o v f cvi e e di sength u weeve ey e sme nde p i de fm vv e C Ei . o E Me eve s wi he eecve sts dww eteie s. new pred he eecve ss w s u w i Ue o eve ss e dww ru I yss ys s e rs w w staes staes re he s s s he he Lwe meh h h thrd ae draied sh sd of the l sue where the draed sen sller tha nh. e ew s e t the t ee o e t I ha vsy lyss rd wdw tabl tabl I dtio ce ew ew eas ea s:: I) I) t smle sm le he he ask esm es mn n AC- S by usn e ntelation ad 2) t us crate a le f cn ible ruon of uane engts t ps d vain o dinge
sc eps ivole te mt he Dteie or eah i te cton hethe drange ll (1) d dwdw. T s ll ans f mn tis etenato is t e v he dmesoe or gve by he ollw ex
(1) wc • ccie f oldton t ro n lengt p the ccuate cc uatedd vlue v lue of T s reate reat e tha tha r equa equa to 0 ds o excs ssue durin wn ll ee e a te mtia a lly i V o c lculated i dta he t rte o ontio ri pxe vaues or vaous s omed ls e lted 1
pd rwdow
al 1 Apoxie Valus o o Vous Soils Ty o Soil
socv
Co sand
> 10 2 /day
Fine snd
1 to 10 /day
Sily sand Silt
10 to Xt /day 05 to 1 /dY
Cpt clay
005 t 5 /day
Sot clay
< 02 t2 /day
I the vale o T cacuat using quaio I is ess than 30. the undran trength should should b consiee The ollowing ses ssure t t the undraned ngth ngth used in e e staiity staiity ays w b ge t e de sngth is thus conative to assu th he mtei is unin in tho cases where u e is dot whet ot c dge w u nveos qued o the analyses or (2) Estaish the sength nveos ateas that ain dun awdown. oy the ane strength enveope is quired or mteals tha a undrined ing drawdow. th te drained ndrined nvelop nvelop (f f vs 'fc) re re quired. Th e en env el op (tf f el o f) an d the ndrined f s a'f f
qu nlops or alus o K c bwen 1 and K can een y
sly ly.. vios ed p vio cuss ed p d cuss n, as d tion, latio ner la lin lin ner
(3) For a lete sip sip sfe ccuate e actor o ety ar drwdown y a 3ste u: (i) Pero ysis ysi s of sity bo drwdown usng in sengt paraters or l mes o deteine he eve no sss c) slice Values o K c on he ae of ach slice. nd the value o K c o each slice re deeine re deeine n the mner sggest y Lowe and rath. aed on duing drwdown the assumption of no eieto of prncip sess duing drwdown These values e sed t deemne undrained sength vaues or he y dung wdown wdown marials marials that tha t do n dn y (ii) Pero an anaysis of staility ae dwdown using undrand sengths o mates ha do not ain reey. draind drain d sengths seng ths or
\V
i mi th drJned sngh r any s is lowr an th ai str nh ud in (i. Th i n i icd ung th tt ese n the be f the lice fm te i) and oe pue f th din ii f o y li the nd s ng th ta the undine ength. o the naly i usng drned ath n unin tnth li wh th ain ln e lo
w
(4) Ret th 3-te e f the li u to lte th wi the lwet act f f Y f lo in aw
Th cmuttn nvlve in h me h a quite engthy, n omput gm pactc ecty t d al f the cmuttn e t eh f tcl lip uace u ace The nly iu i t fllwg etn wee e t th cmut pg UEXAS3 hch ncte th e mt p aw t bilty aay
EXME nysis desrixd rviuly hv en ued 10 nlyze the a a a cu cu i th ectn ectn he ft to th dm Pilct Wat Bul uff lde due t api dwdw T thd hthtic l dm pumpd tag pject Th am cnde t ujt 1 l ddo a a l patg ctn f th um tg et Aordigly lib tmt th tlty dui a spec ally
Th mt f
mt t makmt an t u ct aet i hg th mt c p a a lat ulel cuec
Pilito Dm Dm hw hw n n Fg Fg 3 a homoou olld tfi mbakmnt e ct t dm aut ft v t upm t upsm lo i 2.5 t lower 58 ft t El d t 3 1 m pt to t r (l W t t vl a l m El t El t Ot d ovmb 19 199 lid ou Dui t twO
698 7
78
9 eoe eoe adon adon EI 692
678
EI 698
AteE1657
Say Cy CL L: 45 P RC: 94% Ca Method - Y m 135 p eed s sfae
:
Fi Picis m ssci
22
Rapd Dawdown
t the faure t wwn rae was e ct at aut 7 r da. Te axiate n of flure sue fnd i expato h hw In ig 3
A. Wahle & Assies P l lifi s C by e n cio Wter n el invesigons larato tests nases t re su. e infotio info tio regin iios Dam pent in ts bi fom e Wale a siaes A Wl As T eri cpsng us s is cls s y ca wi g n to 0 y 4 x 1* e iqi li is 45 t lt lim is 23 n. e eage eld w y t of l siy sng ·t' ve ve lif Me) T bin fl envel u f Engpu wn n u of Fig. 4 e evel in L Kth' the t-tae -tae pu a in Fig. 4. hw i . S the fact of sfey cacuat b the s f i ue was 082 Te ctr afet clcuated we ad aaaths u ad the ew ure ure a th 0 Te tic cie a e e f a ts as c b i ig S Baue it us ed snths h ey e ower than uai se w t alwas sl f of o f sey a as or o r or th ft of e c by t Le p e ca of itos D he slie he te sngs e� owe ta unined stgth, n e fto of fety calculate usin we ad ahs t e ew f t lter lin D is emn o a fl ply f hi l f of cl s vel; e derying k s his A sn in , le ion io n f e e n clayey cla yey y vel volv in t se Overlig o f s cy z o s s cayey si vel a l of layer t blnke sl T n of e pm i s ete pra pra e psm psm s s 2 ve Elev E lev 4 4 5 n S on on w Elev4 cu o o Fe 19 du an exly ri dow f ide cu fai e in 5S u t a sult of T slie exte f len of f l e slo T sip exe t 0 l o n ges o y n of t w eva, y
Du l and l
0 5 � Q
S9ent
Envelope
ece
Age
()
Drained
4 5 0
2
IC-U
60ps
2 0
f Egee' Meh
05
10
Nmal tss - (ksf)
_ � : . . �
05
0 � : " Q �c UQ C �
0. 5
1.0
Eetive Stress on the Failue Plane Dung Consolidation f (ks)
Fig.
Strngh Envlop for Pllarcos Dam
rwdown
" Bere o
C ps f Eiers Crtcol CrcJ.FaO82
" Afer
-- "L erd Sp Surfoce
" Bere rown
Kooh
Aer
Crco Crc05 erve Sp Surfce
Befo rown
Afer
-. Pig.
Ne Met Cr Crce 105
F
Oseved Sp Sufoce
Reul of Sably Calculaon fo llaco Dam
•
ncn, Wgh and Wng Unifed ss
Matrol
Zn
< @
R MS Clyy Slty Sand ML Mccu Sl Caus Cly H layy Sandy Gvl
Q Bo Dawdon - E
PL
39 31 43 33 52 28
RCMod. o c t or
Ym(p)
8 8 88
128 123 124
r
252
Obs Sl Sufocs
® Fg
Wlr Bouldn Dam Cro-Son
eding a t Bdi Dam pre st d in hi iteside (hieid, 1976)
pa as btand frm th
nvv in s Tab 2 Sng f e as nvv fo an enh v o o u in e Cs f ni e (y dnition) h sam as h pates fo he = f nl we and Kaa's and h new h
•
Strength Parameters fr Walter Budin Dam
Matera
Cayey Slty Sand
Crps Engneers Me Draned
IC·U
c' 40 ps
c
.' 327 Mcaceous St
• 13 d
c 220 ps . - 5 5 g g
etaceos Cay
6 ps
c' 180 ps
' • 19d 19d
c 450 ps
• 11 d c 2 0 s 3
Lwe and Kraat and New Mets
Ke. K to 2 3 t o 22 22
- 13 g
o 180 psf
o 2 ps
19d
155
Ke. 10 to 750 ps 5 g to 480 f
•
Rapid Drawdon
7, he fact of afey cacula A hown in te Co of Eninrs' edure wa Lwe d Kaath T facor o ety ccuat t new pu wa 1.0 w 1.0, d t v cc T cc t s y b en n c c cle cle f U t w i 7.
e dam f i exampe i hown in Fig. Fi g. 8. Te emb knt a a a wide, nly cpted ilty cay c cay c T ower i of t upm lo i a m zn with t s ngt pe the c T upr i of down so i a f-ainng f-ainng k upsam lo a of t down Befoe Cps o EnQies EnQies Ctol Cic., &0.93
Bere Le od Korooth Crtol Crc F 109 =
Observed Slip SUoc"
v
Beoe
Oserved Sp Suoces
Duncan, Wrighl nd Wog
Zon
C ® G
Q
Materl
Ym(pf )
ompcted Rokf Rokf Siy Cy o
1 14
Sy Cy Rd o
1
545 Befr Drwd E 545
Fig. 8 Hypohical Pumpd Sorage Pojt Dam Cross-Scon Stngth pamts fo te mateias t dam lst Tble 3. sct (20 ps oeso teet o te IC-U nvlp s dcatve dcatve a hhy tnt mtal mt al he dne segt o th th e th t un sength te ag of sesses ow te t to evel c, n ctv ctv consodton stes o ppxt ppxt 50 ps crn n mtly t dpt 4 et n slo n 0 et . l n d zos a dn nd hv t h dy n tute unt h 128 nd 142 l Dy un h usd o pon mts nd u u un ht u on l Tbl 3 trngh Paramrs r Hypical Pumpd Sge rjt Da Meri
Crps Engnrs' Mhd
Lwe & Kath nd Nw hds
Dand
IC-U (R)
K· K ,
K. .0
Compced Rck;I
c' • 0
N
to • 0
NA
and Fls
" 37 de
y Cly Coe
c • 0
c
•
&
6
•
Sl Cla Ranom
c·
0
c
•
Zn
•
6 g
• 1
'
8
- 37 g
2000 ps t • 0
t
8 Og
9 3 g
9 - 2 0 Og
2000 ps
to •
Og
220 s
t - 220 psI
0
93
•
d
9 2 0 O
• Rd Dwdown T stbility of the embnkn was anz f a dition of dawdown fm va S4S (5 fee w t rs a) o li 380, whic s t a a -J T d n pl pl waten waten o ups t a m fl lay b ll.
culat b y te Cps e ccula Cps of Engin rs' ft s e Fig . 9, h e ft ow i i Fig . ow arath's Lw e ad Karath's Y calcul calculat b y Lw e ft o fe Y pu was 1.37 T ft wa 158. a t a cu w w h s. a my b i � m W� circles fo aU t m W c ritc ritc circles F, .9 As
C ps o Eis F-1.37
Low an Korofioh r Ctco. Ccle
Befor·
FJ
Mt Ca Crcl F-156
•
Fig. 9 suls f Slit Cmputatis r he Hyhec Pump rag -
()
J)unt'an, Wri�h nd W(I1�
he ew meth lzg l lt g pd awd e the peious pges e ht e leed to h st fetue o t es t he n s el t aods the ples td wth ettg poe preue n mtea for th fe-dwdown ondon b usn undrined tength orrt rees the stnghs of eia h d dae urng her t the mos accuat represettion of na ngh (vas o f th v w the vs f ' ad )' bu i avois th ncssi dic ACU sent tesng b us ie terJlin of sength vau o o IU ts. B ug died egth le whee these e smar ha urad stegt the meh oids rel o stregths du o aiv e essures whi not not moli f aiton aiton r dng dng c for for eimina eimina engths due to gatie poe pessus is mo acr, e onserai thn he redue use n he Corps of Eninee h The e eh s somewh moe onseaive ha L and rfia meh, a ovides a reliabe esime of sabliy ol awdon tha i v ace s ssib t te n a of . Fo h h mples desrd the ftos of safey cacuated using the eh 15 rcen o 30 peren higher ha vaues caca usin he Cor E h, and ro to 5 pren lowe ha a cacu Kaa eh Ahoh he vaus of sfe faor lulat usin th h are ol ihty aer han vaues calcua using e a Kat eh for t xa coie coie it is iant tha he e e aiv cau i o ey senghs un f ea ha ha L a Kaas mh ds rely o hs srnhs s, he e e eth offers the s reliability ith sc o srehs o negav por presses s he Cops of Egeers meth i se a accra vluion of strength nd result in vlue of sfty aco only sitl we nd aths aths meth meth Th meh meh h liably conseai low ha we wih undined strengths, b ds no invv cvly consai approxaions
KNLEMEN he wters wish to epre he ppetion to Hdin awn Asites Nikk Sekei td. who prode up for th ear ph of this std a to h U S A Egees Wtews Eprimen Satio ho sppted t pha es Dk Volpe proided ifoion ifo ion regardin Piaitos m ler phaes an Cough and Stephen Wheside provided ifoao ari al
•
•
Rad n
7
uln D rl o Lul o Dke Power me a numr of epfu suggestins d prided wte wh n opun o su e estcs of t u rcc cdtis. e wters ateful nlge l of the vubl nbuin to stus ta ave l to en o e d M e ex y Jorn df gus.
EFC
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