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AVIS
ihh:
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lng . Everyefforthubeenmade 10ensurethehighest qualityof ree ecoueuen possible. .
...,
II p~~Ds
are~jSSin~:'contact ttie'uni';er~jly,Whl¢h
gran ledltlo"degree. .
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.' .
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Some pages mayhave'ind iSl!nC!printespecially .ll
•theoriJllnal pageaweretypedwithapoortypewriter 'fib,bo nor~tIh~univen;ilysentusapoorph,Oloc op y
Previousl ycopyrigh ted'mate~jals(iournaia:rticl~!.
publishedleslS, etc .jarenotfHmed.
.~
ReplOdu ct lonin futlOf inpart ofthisfilm tsgoverr\ed by the Canadian Copy right Act,"R.S.C.1970. c. C..30 Pleaseread thaauthoriza tionform swhi chaccompa ny this,thesis.
THIS DISSERTATION HAS BEEN MICROFILMED
EXACTLYASRECEIVED
Laqualitil de cetta micro l iche dilpend grandementdela queli tilqelalhesesoumlsea umicrolllmage.Nousavona lout lailpour. assurerun equallt i!socene cre de repro-
eucucn. I ~
.S'i!manq ue d es-pag es;veuilIe zco mmuniqu ll r a\lec. .. -
. '
l"univer sjUrq u la conlilrelegrade;
La q\:al:lte'
tnm·~fesa;o'n· de C:~rj'aines pa~~s_:
peullai~511rIIdeslrer,surtou t611esp.agesorilli n,alesonti11l!
da ct~l~glaPhlilesa l"alde~ 'unrubanuse o us!~' u nlve rsltll nousalaltparVenlrunepliolOcopled amauvalaequalltll·
Lesdo~uments~ul lonldejlJi·~bjel d;~n'_drOiid'~u,
~~r~~~~~:~derevue, ekarriens publi es,: ! c:t ne scm
P :
Lareproduc ncn.marne perllell e,de cernicrolli m eat soumisealaLoi canadiennesur le drolldauteur,SRC 1970,e.C30.vecuteeprendreconnatssa ncedesfor- mulesd:aulo ri SatiOnql1lacco~p ag nerit' ce ltethese
LA THESE AETE MICROFILMEETELLE QUE
NOUS L'AVONSREQUE
I '
s." .
. :
" . 1 ' . :;
I
i i L
" . \
-'\ ..
.St.John's
FREEFALLl""ACTPOlETRATIatTESTS
'*
SOILSsaurendranath!ChaUdhUri.B.E. (C1vl1> @
I;
The ~ts su~tttedin pa~~ al ·fU1ff1tt.
of.thetqui reJrents forthe degT'e.eof MasterofEngi ne ering .
.Facul!yof Englneerin9 Memorlal
Ur;l ~~~i ty Of'N~folllld1and
- .
" - . _ . , " - c·
~
• .._.' .~
l'leyerhO((196.1).IIt'''~s ob~~rve dth~t resll~ts.of-f~e.fillp~netr~":,"
.. y:~n ~sts~_ShM~
a"9~ater~.~~ration I"1!st"sta.~~; C~"r~~d ~to;the ~
'. ,.'sta.ndardJo151-stat1c,tes t s.H~VI!r•.when~~I! ~slll t.swe.ret~anSl~ted
<, lnt otcJIC)ut~tfon.o ftileangleof:shear.resistance .~e'~f(ferencew.a$·~. ·
' ..~ns~gnlflca~t:
v
!'
"
-
.ACKNOWLEDGEMENTS
TIl'"'ctsser te t tenw esccnotetedat the FaclIlty of EnQ1neer1ng.\
ABSTRACT•••;•• ••'••••.•••••• •••• ••• •
'Pa~.
.~ 7. S~nd~r~p';pc to rCompaction Tes tforI'bde ll1ng Clay•• 8 •.
EqU1pme~
MixingClaySamples.~.. . .
• •9al Grain
she
Di"stri bJ,.ati Oll forSl1lca-~a
Sand.9b•.-Gtai n.SizeDistribution
ft
Iobdelli'¥lC1~y•. lOa. TriaxialTes~.
Resu}ts forsi"l ica-70Sa~'d
. .. (51Type Soil).
lOb. r;lax 1alTestResolts-for
Sl1lca-~
SandJ •
" "\ , ---"
...-<"."
-U STOFF1GURES FIGURE
1" Assum2!dFailure Pa tternby1"eyerhOf(1961)~.
2. Dynamit:Free"'"BodY'Oia gram of aPene troflll1te~
...3. Photograph·'ShowingDifferentTypes-of ConeShape.. 4. }ircu1t
Djag~aDl
ofSt,r~l;t /nCa:ngeme~ts
{0a,Y'al, 1974):••- ,' "
. " ' "1 · · · ·
,Sa. Cetal1s of loan
Cell 'Art'ang~~t:~
ss. Phot ographS~owing~tall$.pf-!;Da~ce11
'1,"~::J::::"::o~"; ;,;';i~;iF~,;'~i; " :
6b.
Ta~~;'
gobson~.
4 laljs lJr{ Machin e..:..'# JS2Typeseru -', '
... . .
lOc. Tri axialTest 1iesQltsforSil i ca-70 sand (S3.TypeSoil) _..,,. .lOd.
~J1iaxial
rest gasuttsforItldejlin gClay.lO~ Tr.h.xi.ill,T~~t.
Rfsultsf~r
Jobdel1irig.Cl ay...,'.'(
,. "
"
Page
15 26
27
es
29 -33 J4
"41 42 43 44
48 I
I
·-49'
I
50• .51
\52.
) .
,"
.FIGURE Page
11. ConstantRateofStrai nShearBox - WF 25000. 53 12a. Varia tionof~with e for Silica70 Sandas
Datermlned by DIrectSneer andTri axi"alTe s ts 54 12b; Variationof,.w1thIO,f or Sil i ca, 70 Sandas
Det e r mine d by DirectSheara~dTr1~xialTests 54 13. Typ;calOutplltfroma Free Fall penet ra t i on Test. 57 14a. Comparison ofPredictedan.d Experlf111:!ntalVelocity'Of
penetr~tfonfor3".56,emseta.~neyqmeter(51. 52 and"53 types ofSoil") " .". • 65 14b. Comparis6'nofPredtc ted andExperiment alVeloc ityof
Pene tra tionfor7.62ems.dt a Pe'netromete r($1, 52
and 53Types of Soil) 66
14c. 'Comparisonof Pred1ct e'dand Exper111J'!n tal Velocityof
"pene~ration
for'3. 56ces etaPenetrtll'lleter(D."15°. '.~OGand 90° )14d. Compar iso n
of ~red1cted
andExpert mentalVllloc1tyof Penetrationfor7.62 emsdiaPene trome te r(a" 15', 30Dand90D) •• ••15a. Comparisonof PIlalyticaland!leas uredlhltrowe Resistancefor 3.56 ems dia Penetrometer
67
"
(Wa ng,1971) ",. ..• '.' 69
~'. 15b. Compar is on'ofPIla1yt;caland !leas uredlnitCone seststercefor 3.56emsdl a Penet rometer
(Orrje&~roms,1970) ••. . ", 70
FIGURE
15c. Comparison of Analyt i cala.i'Id 1"eas u.redl.htt Cone Resi stancefor 1.62ensdiaPenetrometer (Or r j e&Broms ,1910 ) .
lSd. Compari sonof~a1yticaland'l'easu redl.fJitCone Resistance for 3.56emsdfePenetrometer
xiii
P'9'
71
82
8'
(Meyerhof,1961 ) '," 72
16 . Protcr teceterat tonvs .PenetrationDept h . 16 17. Plo t ofltl1t ConeReSistance, vs . /ene.tra ti ori'-~Pt~.. ,77
\8. Plot of~latlveIDen s i ty vs.·Ma.xi mufllPenetration
Dept h 78
.19a . Plo toftecet e eart on vs, Penet rat i onIepth ... . 79
19b . Plot oftecete-aetc n.vs ,Penet rat i on Depth ..•. 80
.20a. PlotoflktttCOneResista ncevs:'~enet-;'ati onDepth
for3.56 ens dfa pere tr onetr =15°, 30°&90~). 81 20b. p'iotoflkltt Cone:Res;sta nce s.Penet r ati onDept h
for7,'62 cesdiciPenllt rometer (a=15°,30°,.&90°) .
20e. Plotofqc!YOvs',ConeSemi-apexAngle (a)._..".".
21a . P1.otof ltll t ConeRes ijtancevs.Penet r ati onDepth . for 3.56ems dla Penet rometer,({jf~=0.5, 0.6&0.75) 86
. ' . .
21 b.Plotof lktl tCone~s is t~cevs.pe~pth for'7.62 ems'dillPenet rceete r-
u w .. ~.5 .
0.6'&0.75) 81.21e . P~ ~tofq/ yOvs.Roughnes s(61,)Of.~ne Mat~,r1alfO:
3.56 cms dia Penet romete r(51,52 &53Types·ofSoil) . 88 21d. Plotpf~e/YOvs.Ro:ughnes s,(li/, l'ofCon7Ma~;rialfor
7.6 2 cms-dlaPenet ronete r(51, 52&53Typesof Soi l ). 89
FIGURE Page ZZa. Plotoftecete eatten'is . PenetrationCepthfor
3.56cll'6dtaPen!trt)lleter 9)
22b. Plotof teeete-ettcnvs,Pl!!net ra t1ontepth.for
7.62emsdia P1lnetrollete; .. . •. . • • ..• ... 94
23a.\plot of l.l1ltCon~Resistance'is.Penetra t ion.Depth.
t ) forJ';56emsdfaPenetroseter: " 95
23b..Plot.of.lklit ConeRes1~tance'is.Penetretton.tepth
~for
J.6?
cmS"diaPene'trcmeter".•..,..•". . ',' .~ 96 24. Plot ofq i .... c~vs~ ~gle.
ofShear Resistance'(4)'" '.... '97- 25a "-Pl oto.tlhHcOneRes istance vs.Penet r ati on cepth'for3.56emsdl apenet romet er (WetSand"Ta rge t ).•••.• 98 25b; Plotof!.hitConeI!es"1stance'is.Pene tra tio n Dept "for
7. 62emdlarener reee te- (Wet-SandTa r get).••." . 99 .26a. Plo t of Cecel era t 10nYS.Penetrationr:epthVar yi ng
Soil Proper t ie sandPenet ro. t er db :- "~f,103 26b. Plot of rece1@ratlonvs.Penetrationlepthfor3.56 ces
diasenetroeeter(0''''15'-.30' &90'),•• • •. .:. 104 26e, Plot of'(:«el@rationvs',:--Pf!net ra ti onC2pthfor.7",62CfIlS .
dia-senet rc eeter (a"
·t~·, . ~~ i:
90')••'•;.•:'.:.• 10527a, Compar1s'onof Analyticaland~as u redU'litCaneandlKl1t ste eve
Resh~ance,
for 3,56ems dia Pen et ro meter.,.', , 106.27b, Plat ofU1itCol1eReshta nce and U11t SleeveResistance .vs:Fe.~etrlt1oh.Iepth.tor3.56~dhPenet i"Ol'ieler.".'. 107 '21e, Comparisonof~alyUcal-and~asuredUnitrenegeststence
andUnitSleeveResis tan cefor_7,62 ems db Penet ro mete r. . 108
27d.
fIGURE
Plot.oflkJitConeResista nceandLflttSleeve Resistancevs.Penet r ati cnIepth for 7.62 ems dta
Penetromet er .:'.. 109
1\1', TlIlysurf'Ik:lughness~as ur~mentsforCone(0.=15° ) • • • 124
A2,. Tal ysurf
.
-Rou.
-ghness1'\'!as urements- , -for Cone(0.= 30°)• .•~ 125 A3. TlI.l '/ sur f Roughness~asuremen ts-'f~rCOne.( a,'" ,.9.0')•",-:'., '126 A4. ilil!SUrf-~~?hne;S' ."e~~,ur.emen~ :~~~_ Pla~
__.:.l ~' . :
81'. Typi calOutput"fortense'Sand-
.
.Target...-" - ,.,".'"._82. Typ1calOutput forloled1 iJln'-():>n,se,Sand Tar ge:.
83."'TypicalOutputfor Loose
Sa~d Ta~~.et
84. TypicalOut put for-qayTarget •.
.<
J
consta nt . NOTATION
Pil et iparea;cross-sect 1oNalareaof penetrometer;
.
'" :',,-.'," I
!
~.F ••G.!Ige.facto~•.
<tenstent.. M.m,~ •Jlbs sof proje ctile.
"
,v
xv1.1
V(tj Velocity attimet.
'Vn Velod'tyat ti me
tn·
Weightof~rojecti l e;wei ght"ofpenetrometer.
xvU i
....
;CHAPTERI.
INTRODUCTION
I
1
f .' '. ,,",0''''' ;,,"', <;"c~, ;0... .
t""" ott;, ,;.,i " ""'0' '" L
. ~!
.an ne~o·1~s . '
till!staill:la~d
(ASTM03«1-75T)electric cOnepere t rceet er~asbeen~del1l1$e-d1~ the-statlc_~e:".elther':"'t't:ha5eabed rig .
<.
'cill edthe·5eacal 'i~(O!Ruiter,1975;It,r1cf1e"rg,·1.975) or withabOre:
:",
~Oh; ll~ta~~'~t' [~n.ed ~e :· slfngray~ (~e~~son·
e't~1.;~
..19m.
Ii l.s est11l;t~dthata
typi6als'itefnve$t1~iat1onhicl ud1ng dr111lng'bore netes-~~d 1n
..\~t·tu test1ng'·.'II~th
a~t~ndan:l penet~ome~r
costsUPw~~d'
0,"$1"
~'11 i~~" {H1tCh1~9S
.et.al.:,J 976).':Sucha'deta·l1e~" 1n·Y~st1gatfon.
~y.
not'~ ~'eces;'\J;"
fn, geot~ch~tcal '~urveY$'
orf~~ InYe~t~gat1~n' ~'f
'a'rge tracts.for
1~cai1ng
'pi pe'1-1n~:, ~'ut~5
.etc.T'h~: c~n~ePt ~r·
a'f~e ,'f~;1 ,pen~ trW.et;~
"'~a$'
-tnit1at~d' .
at Me- morial,Urih~;S
.,itY" ..
"(Dayal ,"·1914)witb}he1nun tionof
'~'n!l:1t
'.as_a~too~_ !or
..I:qU1d: liid;.econ~lca~
~. s
. Activltjesrele ted tothedesign'andecnst wcttcnofoffshore
':si~~ctu~s h~~e
' 9ai ned.great:~n~~-
.' in t'her··:l~~t·,de cade.: ' " pe~~tled
' .~ . '
·~nf~o;:m.at.!()~ t~,t.~e.s:t~~t~th.'pr.o~.t~.t~~s,:,ofSet.f1.~r:SO't l;:f~ ~_s:~e.~tiaJ,.
'.::~orsafe a~~ec~nom_1~a1~esIgn,of'fo.un~_a ~f.o~~.~n·:~he oce~nfloo r..
·
~n~e~t1ona1 'S~1I1~~'1ng--'p~cedures ~sed
'on'l~'nd 'a~' ~e~~~all;:~ot
.::.·ttv'e
'1~' t~ oce'I~~' ~c~~s'e ~./~h~· p;~s~~~ - 'iif' 'i~e' ~"te~ ~llm:
andthe·
_hi~h deg~
'O·f.d1siur~ance If
fJle SilfIIlles.':ll~rat~ry tes~1ng'
of~uch
.'
5aq11~S _~re
there'foretobe'lSubstan,thJt:.by
\ ther.met hods. rn-stt«testingUlus'fo....s anintegralpartofany'
OffshO~
5011'investigation.. ". '?
.:".
) 2' ("
. . testi ngof marin esol1lrnoed1at ely belowthe mud line.
Afreefallpenet ron;eter is a cone tippe d rfght,circular . cylindr icalprojec~ilewhfchts allowedtofal lon,soil"target.froma preadjusted~e1ghtof freefan. It is lnstrur:'Ented"\JjfthIcadcejls for measur ing the conetip resistance andfri cti on onthe sidesleeve
d~rlng ~enetration .
Anaccel~erometer
isalsorro~nted
lflithi n the.. ' ....' . . , , ' l
.J. ", ' .,.,.penetrometer for,recording eeceteraetcn,proJ il eJ,~ptothe,run.dept,h
0;' _penetrat~~;
,"I~te~?t~,~_n\~~~:~~.:~e~~;e,r~tl~~~ti~ :'~ford' :rov~des . "
ve_~,Dei~.Y"~~:S.US:~f:~,~~,rv~,whi~~_c~n:_th~n:b~llSe~-':~Ob~r:::,~~
.:
~ts~r:
Ipl.~.~~~~~~_
'versu'su~: ,cu~;e~ c \" ·B~>'t:~O.~~ ,~lottin.~ .-~_~e: re~.':d ;~f ~~r~~r,~,:
t10,n~s1stance,.ve~u,~·dePth~ro.file,i sobta1n~d~'Th~:data thus .. ~ obhined is usedforthefinal aniilyslsofthesot'l..st nlllgt h properties.
, . J ' ..
I~itt,alatt~Ptswfth.~afield.penetr~ter'Jones,,1 97~)showed·
that thes.tandar dpenetrometer (cress sectional,area•10.00 sq.·emS.)
I . ' . . ., .
wasst r uct urall y inadequatein thefree.fallmode. Aco"".1etE!'lY
. . .' . ""
ft .redes1,gnedversten of thefre~:fall,:penetrometert(~r.oss.Sfcti_~n"a'rea,;, 45.62sq',c.ms:)was
succes,~ fUllY te~.t~d du~.t ng.'sea· tr1a1s' 1nPl~\centia
Bay,-off
Newfoundland,dn'Hay,-':197S: (Chad e't':aL,1978):.la~rat~ry' test'~'~i~h':,ihis.re~~~i~~~d·'~enet~te~,and
ananalysis'of'the
'~~ult~;,are pr~sent~i1 n. th<s
d'isse.rtat1on. Freefall penetrattcntes t s'Wen!condLicte~using'the shndard~,Fugro"type-,! , " ,'I',. .I,•._ I." :
penet~meter.,and ~he,r;edesfg ned, "Memor i alUnhers1ty ~pene,tro.me,~e~._
T~(l-types~fsoilta',rgets,Wt! re
Used. .
~Q~~.,.Gawad,r~979rcondll:t~d 'a par al.h:!l',pn;j ect,1~.carr~f~g outq~as1~st.rti'ctests'with thetwo
\ I
. ...
.. s
I \
i
.-,~'
the penetrometer.
2," To
st~d~
;t lle penet rationPIl~)-~~~on -1ri 'dfffereot' S~-1 '
types'.3.' Tocompare'
~he ~SU.ltS o~tii~e,~ fro~
freefall- :t~sts
'wi th-thoseforquas1-stllt1ctests .
4. To-prop'oseappro priat e;reth~d's'of.1nt~rpreti~g.tb~'resuU s.
inthe light-O'f.theor;~ scurrently ava11abl e-fn the.
ttt eret uee ,- dissertation.
.
.
.deqre e ofsatura~10n.,etc.) . ),"_~.e~ase,',ofthefreef~~l'penet ro~ter.' itsweight ts
a~addlt1onal ·1~f·~uenc1~g fattor.·· ,~~
impor tan ceof .~h~S~ ;
factors',, are ' ~~Ud1e~":
1n\.h1:i::~~p~~'~~~t~l:·_fnve,stig~.ti~ri::c- , "
,
The._~as,lC
;almS"of,t~iS'
st&dyare ; ' . .
1;: >J:ci~t:uilY':t"he,'i_nftue~ce;'of:.th.e: ':di f.fe,r·~~ t_c~_a·ra.cte·~i s ~ f.C:~of ..
Themajor factors which influence,the penetrationr-esist anca .1n any cone
penl!t;atio~
test:1\.e
(1)cone apexang ~e'~
(ii)conedhmE!ter;(ii'1)roughness
~f
"theicone material ;'(fv) rateof'pe~el1-a·
.rtc ni(v )'s011properties (angle'of~hearlng're s jsee nce ,cohesion~
....
Q
SMOOTHBASE ROUGH BASE
la) FOR FLAT TIPPI~E
(b I FOR WEOOE OR CONICAL TIp·PILE
fIG1.ASSUME D'fAILUREPATIERH BYHE~ERHIlF(i961 )
. ,
For conestontess soils: q," vn Nq . .(6) ForColles:v~solls: qc~-o+eN, . ... ... . • (7) Conversely,i fq,"a ndfsCarlbemeasured,theul~ jmate 'bearin9 cepecttye no hencethesoilshear proper t.tescan be detemined.
2.2 . DynamicPenetra-ticnTe st .
Atypeofdynaatc penetrationtest that hasb~enpart cr- any boreholeinves t .fgat";onis. the Stand a r.dPenetrationTe st (SPT) , wh~rei\spll~.-spoons~'ertsdrivenbyrepeated blows ofa freely fa1.11ng.standardw.ei ght. I~the recentpast,the useful ness of this testhasbeenquest ioned(Schmertmann.1975). "Itappearstobe the consensusthattheint erpre t ati On of.thistypeof testrequires'not 0II1ya lot ofeeer-tence ,.put 1s to be donewithceut fon. Theot he r typeofdyn~;Gpenetration test whichis discussedtntht sthesis uses apenetromete r which hasthe sameorsimila r conf i9urationto that~scribedunoer the conepen test,
2.2. 1. HighVelocity a,nd lowVelocity-Pe net ration
\ . . • J •
In co nnectionwiththestudyof projectt l epenetrat 10ninto
a .
earth(Young , 1972) atmedi a , reseercntheSandiahasbeen 901ng onLaborat~riessinceinAlbuquerque ,the early 1960 rsNewMexico.
.
Projectiles ofdif fer:-e nt shapes, inst rument edwith.an acce l ero meter have been tes ted with~e1 ocitiesofpene trett onup to 790 III/sec (2570 f t/ se .
In -suchdynamic tess,pl!net ratton15caus ed by vtrtueof theene rgyat'thet me oflmp.a~t. Up~"-~~c~onasoil'mas s
the
project il epus hes agai nsttheso11 particles,rupt uresthe so il
\
.)1
1
structu reand ee-sto restwtlen the projecqhenergy istot all y ctlss1pate d. Depend ing0tIthe l.., a ct veloc ity with lIIllch the projectil e strike sthesoiltar'getthepenetra tionphen~ onhnbeencla s s Hled aslow'I'elo c1tyor1'119/1veloci ty. Thebas isforthisdeNteationis the typeof 5011failure. Thet~nn'lowve locit y'isusedtodescribe tne events for willensoil fai l ure pattern issimilar to'the quasi- stettc ceses (Wang.1971;HurffandCoyle,1912;Day, l ,,1974).
Wang(1971)hnsugge S,ed,that the soil Sl'lear, zone 'tsstmllar. Q'} to_statlec~sefor\IeJoc{t1esup to152m/se,c(500.fps)but hascon-
ductedstudi~sonly~,toaIMxlmurn.impactveloc.ltyof7.~wsec(25:(ps) .. HuHfand Coyl e(19'72) In'l'est1gat ed'tJrojec t11e penetration'Inve locity range of9.1Il/ser."to 91~sec(30 to 300(ps)and ciass ifledthese tes:s aslowvelocitytest s. AlthO~ra dis cuss ionoftheexactHlllit for the1011I'vel ocit y IIlI!dlanismIs outo'f,contut•.ltcanbe seenfnJII the publisll ed re:forts that velocit ie sfn theorderof 9.1-Isec {30
fps~
are~learl1
alow·~elOtity PherlOllll!~.
The'ft'lOCit;ob~aine~
forthef1ft fall conej)l!llI!t ra tlo n test.sreporte d.in tills thesisis In theorderof1. 15II/s ecan.d isclass i fied IS low veloci.tlpene t ratl on.
2.2.2. Dynami cPenetration Theory
_Tile basicas s uqltf onsforderiving tileexpress l onsf<!r proje ctfll!pe ne traHonare (Young.1972;Dayal , 1974):
.). Tlleso tlta rget1s.hOlrogeneous and isotrop1c...
,
2. Tile penetrometer is anuhpoweredpro j ectile of~si~l e configuratlonhavi ngacyli ndri cal bollYand nos.e.1
3. There isno significantangl ebetween'tilea~1sof the• penetrometerand ItsYt'loci ty
.
vecto r.. '
....
:.'(..
~
A(4ay_l )·'ls .'.. . ..(11.)10
(8)
(9)'
_(10) for Vo>,V>V
c v
_*"-,
"'e_vZ+yAll en et a1. (1957) conduct eda se-t esof penetret tontes t s onsenewithdi ff eren t nose shapes. They qrcposedthe (01101;1n 9 theory :
where n.t sthe I!!'lss of th'eprojectile,V Is theproj ec t ll e veloc ity, and a,II,yarec Oflstants ,
Dependingupon.therelat i ve magnitudeof~,.aand'r,the sol uti ons.ofequat ionOCl are:
{l)'.for~hecasewhere62<4cay
yV~ '~
+BVo+"X "'~
1nyy2 +BV" + ."
an Impac tatavel ocitygreater thanV
c15largely1ne hs t 1.c andat a velocityless thanV
cthe projectilesimplypushes the sand elasti cally.
Schmid(l969) es sueadthe\penetrati onequationas
for" Vc>V>0
where ' V
o15the 11lll.dCt veloci t y a,t.-ze ro penetrationand Vc 15the crf tie;.,1 velocity.
Base d on exper 1JJJ:!nta lresu'lt s," thecriticalvelocityIVc (defin edlat er) was calc ula te d tobe'96.5m/se c. Th eyconclu ded't hat
\
\
\
I
\
\
I-
I
\
\
\
\ f
I i
I i
\ b~"~"="~~:c-:====~
(12) whereX is the 1nstafltane.ouspenetrationattimetand velocity \/:
VO1.Stheveloc 1tyo"f.impact.
A=tan- I(ZYVo+8)( 4",r-sz (!l • tan-l (2yV+8){ 4ar-
a2)·~
.. •.• (13)
(;oj 1) fortheca s e wherea2~4",y
where
.(14)
. ,
B..
1.
In'{2yV.+8.+(62·.4"'y )}{2YV o+ a2 . ~
{hV+B·(6.2
-4ew) )fzYVo+a
.
·(a+(a22.4ay) }-.·4IlY) \'12 Startingfrom Newton'sequatio nofectr on , Thompsonet al{ (1969) de rivedthe hllowing"relat ions hipsfor acceleration(Al.velocity(V) andpenetratfoo dept h(Z)
A-
Mtr
+ 9p , .. • .•. 1201
." ', F '··".·' ;,,' ",/.'
v_~,'.J{~.~.9)dt
.
..''.,:....hereF ts tile soilrestsreace ,~i,Smas~ofproje'~tfl e .Me ts mass of~
s~n ..
m.1ving with'the. project1 1ean'd.gi~:the accelerat~on
.due~Q
.gr avity:.,',';
'I/II~ '9ldtl" ,< . :IW
. -.
-. ' , " -- , ';~:;,:_~..
Theyconductedlabo rator y experiments,w1ththeO~iectiveof
,dt!mi:Kl- st~ating the'1~fluence '~f PhySfC~ l
soilpa~t:mete~~mpact' ~eJ-o~fty
"
- ' ..
andtheproj ect 11e,prope rty. Tho~sonet al.-(1969)concludedthat thesoil
' ~trength 'Pi!lra~ters
haveast;.ringinfluence OJ).the~Pth
.f?fpenetration.
Young (1969)p~sen.ted_t~.~~et.ratf.on.~ redi.ct.1.~· e~lItiones".
~x :;. '530'SH(W/A)~ 10~3 ln (J~·ioX10~6.v~)
• • •••(23)fol" Vo.<' 200.ft/S~~·
.' ••.•. • •. ••(24) Vo>WOft/ sec ·
-
for
L~~~~ i
13
wherex..ax fs'theNili lUllpenetra tl~depth,'Sisthe soilcons tant. II is ~enos eperf ormancecG-eff1~ 1ent.WIst~eweight of proj edll e and AIsthecross-sectiona l areaof theprojecti le.
.ValuesofSliewithfn awiderange(roll0.2to50. For solving.tll~aboveequati ons,Itisnecessa~toassl,lllle-thatS.is cons t!lnt fO:"'Igi venta~ge~: TIIus .~~j.pen:trl ttonI,"',a .layt.re?.
lIe,~fU~. O~, W~de,lY, dff~e~li~ .:p~pert~ e$,
' "_~~ ci.
Y:lue.~f -~_ '_w~,fT,
_.~P7n:d:-O~
__th.et~.t~J.·~ePt~ , p:netr:ai~~·., _ :"B_aS;d,',~ ~~ ··dita1,r~d:a~~~~.s:ts:, . . . .
.of'
o~~r'
500'f~'Tl - ~ca l~ t;s~s.
_.YOUng"( 1~72)'
'cOncludedth"atp;ed1'C~f~n~'
\~~~~curat~'- Wli'~t~O:.i~proxf~~lY._·±2~i.':
"'.
' -"'" :.!
',' ". ':
':" '.,." ' :
.•....,'.J, .. '" ..
;
!
". f.:,
,-;-..
:
....
..
;..
~'..
,~.;..
14
C'f'Oss-sectiOflalarea oftilepene trometer.
", --MurffandCOyl e(1913) also conducte d peMtratlontest s by
.
. . ,
vary1'!9 soil par ameters.penetroaetercharacteristics udimpact velocity. Predic tl on e q uatlons
were
sugl}este dinwhtththesoH .re s tsteecewas ISsumedtobeII linea'rfunct i onof the~l<idty
and·de ~th. Goodftt'IlUreportep'botllforchyandund.'.
.
Tur ~~9'e, .~,n.d ~~et ia{(1 969~·,a~:d.,'Tlr~.na9~ .P~~~:~. '_c~n.d~cte~.
_, -.. ..e)(~:efj~n.t.~,..,t~.~~xllm.l.ne.~~eV1,~COUS.:ef~~C~.~.',~,~~:,~.~.~~.1.a.~,fo~.c~s.o_~""...
pelle~ratfQI1.r~s fstllnce:,:ora,W:1 ~v~~.jetyof,pro~,s,tzes.-'.shape~,and.
·.·pe net~a't__fcnvel oc l t'les•
.' ne t' '':'
da~'s~ow, ~Il tthe : 'cone " P!h e:tra tfbrJ
.
re~1st~n~e
0"f;~; __ ~ra~n;; ;~i h wa~ ~roport~o~l} '~.~·lOCfl=Y
and1nY~"rselYproportionaltocane diollleter . AnelponentUlequatipnwas
~~veroped
tod~rlbl! ··th~·
interrelati onship; ..'. 'Yaryf"
~he
sat\prope~tjes. penttrome~e
..cha racter ist1csand 1lllJlact;ve locity•.oi"
yh
(1914),perfo~laboratQI')'s.tudtnforl!~ier.,mini ngge-otetll!li calpropertiesofsoilsusing aninstr~ntedi ....ac t .,
.·: con~.~~~t~te;.a ~rnI.~h~ .~~J~ S~ed good ."g~n.twi~
- . ...'the~l'l! ti ~ a1fIOde1-·.Theiq:~veloctttesofthosetestswe rein the
: ran~e'Clf .i. ~5~~·
.g.f·1l/·~ec
(15'to,30'"f t/S!C) " . . 2.3.~AnalyslsDur fng'·""fr!!fal"lptn; t ; ati0n.,.the
pene~~l!lE!ter ·eIPerjence~
~S1-~tan~~ · bY '~h~··so1'1 f.~·om th~. fris~nt ot'e~t;'y~~tf1' ~e toncl~s1on of'
Penetration.'even~. T~·e
'dynamicfre~ bod~
dta'gr';"~f
'4peneir~~er
•durl ~g penetrat1~n
15shoWn Inr'i9.'2: 'Theanalyt ic ;l:ftlat i·onsbip of'~i!ferent
,parmetel"'S'.(·1·,R. · ' .,:e,:',
."
soilp~~p~:;'ties'
' ",.. . ,J.;~~t vel~c~tY.
.' • ,(Tp~cont 1nue·d~QE!,16)
... ..
15
DRIVING
I
FORCE :
;
;
.... ...
< 'H
... . r
SlOE'ADHE SION
FORCE "
,;
..
':_;'. J
W,' WEIGHT SF·THE PENETRONETER
BEAillNG,PRESSURE.
FOR!lE ' .
'I
.i
\
"
i i i
: i -I i ",
I~t J
pene tromet ercha r acteris tics ,e tc.]gove rningthe dynamicsoil propert iesatlowvetcctty penetrat ionaredlscussed be low.
2:3.1. Mode~fSoilSlIea l"Fail u re
Asdescr ib e d earl ie r,tnt!behav iourof 5011Lmderlow veloeft.¥;penetrat ion\loul<1 besi~l1.rtc.tnequasi-stat icca se.
.
. -' . .
Accordingly ,thefa i l ui'emodedllri-"g ~hefree fal l,pe net ration,isassumed tobethatprcpcsed
bYMe~~rhof (l95i)
fordeep'cone.tiP;P~d
pi le,
f~und~~'jo~,' "(h~:.reason~':f~~ ad~-Ptiri~ M~yerh~fIS ~~ilLl;e ~att'ern
we r es~mniarl~~d bYOay~"
(l9.74 )":'a.s".foll,OWS:(i )".
H~yer~of~
s,t~ellry
tak'es'1~tQ
'accountthe
shapea~d 'surf~ce
roughness.of thepenet romete r.
,, '
(11) Fail ure patternas' observed exp.er iment a llyfor plene-stratn' mode l1mp 8ctp!ne t rat ion test s coutcbeapproxi mat! d .to that'
I ' , . ' •
of Meyerho f 'sfailurepathm.
.(111 ) hperllJlent al resultswerefoundto bein 9:'lld,apreement wIt h. thea~alyti ~al, val ueobta 1ne~byMe.yerhOf ' s.me t hod,
>~l thOU91ldHferent.theori.esare'avlll1able·fromre·l:li~·t ", pUblications(Dllr 9un09l uandMitche ll,',1973)wtdch.a-lsota~~into'.
accciunt ,the" pe~ti"Omet~r
,;hape,sizeark!roughriess . ~Ye~~~f's
theory"is"
p~ferre dby vi r tUeofUs eesecrapPlicail?nan~itsetdeacce p~ nce .
-
-
.Fromthe r-es ultsofa se-tesoflOw'vel ocitY'penet rat ion' .tests.on'
sa~'~s;:'w~ng , (19 '7 '1,),
eXpr es sedt.h~ f~li~ 1~9,;re'1 a~10ns.h.fp
',;or',,theu1tima~ be~rln,g,capaCit y: \
,, ' . ;
•• •• c(!5)
wheNOu •ultimatebear1nQcapaci ty AandC,,-,const ants,dependingon son
proper ty,penetrometershape and
:$h e._ '.. r
. . . -x· depth ofJ)!net rat1on•." .
~ ActO~ 1'~
to'theprinc~pl~ ;f
.cons e.rvat\ono~ ~~er'iY"_'wari:9
':...
1 I
I 1
- /" ---r-
Knowingtilemaxfrrum penetrationdepth1(1!)fora certainlmpact velocity(Yo) '
'c ; c, jut"
be~alculated. f~-eq~tf ~
(ZB). ;"'5 the'~O~~ri bU~IOn
of~
15 very$mal~ (~ang, 1971q_n·c~;t~,,- .to
Cp •A
lls"-,negl rttl! d"~f~e /J@te~m~ng! ~ nl~1I!! o~ ~~.:
.A~ajn
•.eqaat1o~
.'.."' ,
.<.261
'.!'
, s,
'.','. ...) '...
. - '-.
B·~ld (f.,i)
~.I . .. ~mass~fthepenet.l'Qliet e r.
~olu t i onof equation(Zli)was givenas:
. - . I '
. '2 · '" C1' ZA .~ 1<'
-'1
""' Cl'ZA.It.",'i((Va_-n~}T -ll»)e M -(T)~+m·IT·MH-. .(2: r
where Vais the.bipllct
veTOC.'~.
_....,.¥ -r. ~."
'P'I!pefletratl.OI\dep.t h.Isa1lliU1. .ra~1I1!~projectile ROp S;".
.he~ev·pe~et~te!vel ocity
' . . ' : ! 1911: d"j~:dt::~:~:n?:~:tt~ht~,i')d' . ' :..
.
-
,"
. ,
..
: . ...
" ."
-.~
18
(25) coul,dbe r-e -srft.te n as,lNeg l ectingAl.
.. Ou='ell (29)
)
Consideri ng.
equat ,.ion(6 ).asvalidfor. lowve'Iccttyperet ra.
-tton,itcan he re-er fxt en as :
y"
;am~~.-
i- i
Wh!re'
;~
.•avera~e
contact'preisurei ·
acceleratio n19
(321
ofsa tura t~dc14y s. WtlltNn(l9571has fur th r shown thattM strength Is considerably increasedunderveryrapi dratesOfload111g.
';ihl tman (1960) suggestedthat the rate effectuponst rength.ightbe caused by a changein excess poreere sse-egeneratedduringtheShear process. Datareport edbyO'Nel1 l' (962) Indicated that hishypothe s i s was substanti a ll ycorrect .
Inc.onnectt ori withtee ts onbulldozerbladeS,\jismerand luth>O?7'l1att~tedtoquantifYth estrairirateeffectsandused .th'~ecuat ten ofTurnag~and.Freitag (1969 ).andsU~gested :
CIx•('
(~)
x I K..~
•. . • •• .•,••,(35)Ci1
til)s.f1e~CIx'";~one tnde~at penetration
. · rilte rx",1th'cone•dlamete'r. " dx . CI\.••.ccnei.index of astanda~cone
"'ith.penetrati~~rat er s and
"
](=exponent ofsfn!ar rate·fa<:lo r.
v•
"
... . .••(e9".1) "
.e- , \
'
BaseddneXPrrt1ll!nUl'results,Wi~lIi!randL~thsuggesteda .valueofO.1'forthee~ponentta lK.
', ' Frt)lfI
eq~aqon ~ i.~l,··theo'retic~l
vetueof~~ne're.sl$til.nce
fordtffe,renti~act~e'oc 1ty..and'cOne dlllme~rcal!beca !~uhtedwiththe ql.i'asi -s.ta : k~~.etr~,t1.~~'testas theref.er:nce~rvtce- veese.'
Aga inforpure'!cchest ve-sutls"
v.
"
:
.:. ;,
I , .
I t'
, I I
'1
22
I'!ey!rhof (1976)hasghen Ne valuesfor d"lff~ti"nt; ;11types and relativedepthof foundat)on"'
Knowing~ ,
cohesion(eicouldbecal ~·
cut etee.
In sUII'IIIIry,itmay be statedtha
.
tfree fall proJec.tt le.pere tre- tlon at lowve loc ityis influencedby variousfacto rs. ~he5e.a red1f ·. fel"t'ntfor cOheslonlus and,COhes iv e so11S". D1ffu ent~thOdsc,urrentl .(avetiebtecanbeusl!dtoevaluat e the5011propert~esandcompa red wHh
. - : . • 1
eachother.andalsowlth·the·trhx~alanddlre~tshear'test res ult s.;;
.
. ~. ~\
./
I
I I '
I I
he, 1
CHAPTERIII
LABORATORY~X PE RI HE NTALPROGRAM
3.1. ~
Theexperi ment al~rogramwas desi gned with tneobjec~i veof'"
st~dyi ngthe mechanic s of
.fre€
fallpenetrationres tstance ofsofls \ andits cor re lati ontothe st atic.pe~e trat i onmechanis m. Theinflu- ence of cone,
angie . cone'roughnessandthe 'typeo..f.~~n
tar get.
onstatlcpenet retaonresistanceis recogniz edand reporte din l.iter at ur'e;
The~vadables"areexaminedin'the fr ee,fa ll.penetra tion tests con- ducted. The freefall penet rometer that"wds designedandsuccessf ul Iy usedatseais 7.6 2 cmsd.iameterwhil ethestandard.penetr~~ r used tn IOOststatic'.penet rationtestsis 3.56emsdf emet.er. In thfs wor k, tests weredOn~'Nlthbothtypes ofpenetr~etersso tha'tappropria te compar is ons
an~correlations c~uld
be made.. 3.2:
APparatus - Penet rOme t erAdetatledPhys1cal·descr.1~lonofthe-twotypes of penet~-
. .
...
-,setersused.is.given in reb'le 1. Tipsfor~thpenetr omeyrswer,e detachablefrom theshaf tand hadvariousapexangle and rl?ughne,ss.'A compl~telfsting ofthepen'etrometer tips.used inuil s~investigati onis giv entn Iable2. Shapesandsizes ofOdfffe rentcones\together with the noseasselrblpforthe 't woperer rceetersareshawfl1hFig.3.
. , .
13.
-.
24 3..2, 1. Instrumentation
The penetrometerswert!ins t rume nted\<I1 th·th~ esensor s:
accejercnetar,coneload cell and frictionsl eeve load cell . ,Theacceleromete rees mounted1n~idethepene t rometerand alignedinthe direction ofthepenet romet e r axis, The accelerometer useein th
,
t sinvestiga tio nhad thefollowin gspeclficati ons:ENDEVCO: Model2262-25 Type: Fullbridgepie zores 1s t h e Rated range: t25 g
Useful range : 150g ' Sensitivity: 16.7 IllV/g'(atlOY
~excl ta F onl I'\axm,transverse
sensitivity: ,1.2$
St rain gages wer e usedfo~measuringconeandsleeve friction
,
,
loads . Eachloadce ll cont a insfour pa1rs of stra1jl gages arranged
r
in sucha rranne rthatcompensationis made for bending st res s and only theaxialload isme asur ed. Fo urstrai ngages'were arrangedin the axialdi re ct i on andthe remai ningfourinthe circlBl1ferentlaldf rec- tton, equi dis t ant., on theperiphery ofthe tube. The c1n:uit,d1agram is shown1nFfig.4.Con~ "and
frict 40nloadcells;recalib ratedonan'Ins~ron'
i i . .
j
i'
"
I I
i
tes t ing mach1ne. For thecallbratl on(/f loa dcellsspeci al ji gs were designed andfabrl cated sothat onlyaxi alload was appl1ed duri ng compres s i00 of the tube. Thecells we reloaded upt~635, Kg (1400lbr:.)for coneand 2,72Kg(~OO"lbs ), fpr'f ri c Uon'S leeveat 22. 68 Kg(50lbs)increment. Thereslll;:softheca) i br at iontests.
(!extcon'tinlledpage 30)
\
25 TABLEl. DESCRIPTI ONOFTI1EPENETROMETERS
"Fugro" type Memorial
I I
penetromet er penet r dinet e r
~.56ems(1.4{n.} 7.62 ems (3.0in.)
I
\
10.00cm2 (1. 55 In.2) 45.62 an2(7.07 1n,2 i
" i
'JJj0 .60°and1600 300•60°andlailD
\
3.5 6.cms-(l.4 i n.l. "7.62cm~(3 .'0in.)
150 rln2·(23.25tn.2)
'64~u(cm2 ( 1~ ~n;2) /
\ ~ TAB LE 2. DETAILS OF PENETROME TERTIPS
l
rometer Penetrometer Rcaqhness of aeseseet-ter t1pmate r1al cone seteetet apexangl ~
(61. )1 (0)
' f
I '
i 3.56 Sta inless stee lPol1 shedal umlnlum' 0.50.6
~~:' ~g~ :~i :g~
'Sandedaluminium' 0.75 15° . 300end 900
Stai nlessst eel 0. 5 lSD,'300 and'gOo 7.62 Poltshedaluml nl um 0.6 lSD, J0 0<1iid900 SandedallJ111infulil 0.75 150,300and'~Oo
t.:·
..;
26
zr
-- -- -- -
- ---- --- - ---'--- -- - - - -- -'---,.
I :
I
,
-
~FIG .~~ Ci~I~' -D,l~G,~ 'O(~~.~~.-'G.,~ ,~GEMOO'·S, ( -,~.1 .i9~~' )
.FIGSa.'DETAllS,O~LOAD CElL ARRNlGEM£'lri
WATERPROOF BUS..ING O-RING
FRICTiON- STRAIN GAGE E- AIH'GAGE
28
..W TH ROD
:;,",., .~'. '0 - RING
..
\. . ...
/ ..
.-'
1lO.T .TO'SCALEr _' r
I
I I
I
I
29
~~plot ted an<! tileloadver s ~sstrainindicato r teadfngcurveswere
'--'"
.
obta i ned forthe10a ~cell s. The lstraingage bridgesulfibf tedexcel- lent l1n·earity. rjesecalfbratfon curves ,"ere~~e<Itoreducethe data
·frollpenetrceeter tests. Detailsofload cell arrangellll!nts'isshown
"i nF~.gs.Sa'andSb.'The following are the sped fica t i onsof cone and
fr1'c'tfon sleevel oad ~lls:
Gage resista nce: 120Ohms
.Gage.f~ctor(G.Fl
Z .'
1. I
1
,I f,'
.Sensl t.1Yi ty: 200kg/mV (3.56cmsdfa.penet rOlile t er) .
and 329 Kg/mV(7.62cmsdia ;penet~/neter) 3.3. Recordin g Sys t em·
.The output'signal s of th.e·ecct erceete - ,conelo·ad
Cell
and fr icti onsl e~veload cellswere recol"(ledon a hi.ghspeedchart recprder(GOUl D 2000).and alsoatape recorder(HP3968 A).'.The stgnal~wereilIlllllf ie d.byselecting suitablegainon the aqIltfler before feedfng intoth~ \reco"n:ler.
'The char treco~·er
isaself-COntaineduni tho,ed.·~n250mlM~n-fralN!chassistoacc~date three isolatedrecord tn9channels. Thfj,cha rtspeed used.1nthis investigatio n was 200 IlII/sec: Therecorded diU. onthe tapes wi ll be~se dforper1Mnen t r:ecordandfurth erreferencewhenrequi red .
. . '
3.4. Exoer1ll1entaJMeth),d
,... 'sererestarting,:a;htest...tIlefOllowfn.~Ubr'at10n.
checksweremade:
1. The actual gafnofa" amplff fer 1nc1udfngthat ofthe
·tape recorder. 2. Balancing ofthe4.q,l1 f1en.
cells.
I
L
I '
I
I '
31
.3. Thecalibrati onof theac~ le rtllleterby turnoVf!r llethod,i.e., byllr1entl~gttssensitiveuls inve-ueetdirection'and thenturnlng over180~resulting'ina change of'2g', ,4, Ba h nc~ ngthe bridge ofthecone and frl ctionsleeveload
,
.T~penetromete r was at tached toa releu ln g'rnechanismwh1clTwa~
fnturnattachedtil,anylon rope. Thus the penet rometercanbe,pulled
"uPto
~, ce;taln
fhl!dhe1gh'tand released by~ q~.fCk
rel ease;'chanls .l~~te~ lt~~t h.!1 ~~.
. ..
T~ he,1g~; Q.~'
rreefall ...a~
kept constantlit.3.06Ht-~s
forthis.Investigationand'correspondi ng,veloc1ty oftlllPlCt was7. 15wsec.
care'was
tal:.e~· ~Q ~ 'nta1n
thevert1~al1'ty
of.'the~net~ter
befol"'!-, every'experiment. ~h ecanPleteset-up(frame,n!leas l ng mechants m, pul ltes,etc. )for free fallimpactpenetrationtests Is shownin Fig. 5a·.·.
3.5. Roughness oftheCOneMaterial
Surface~~ghnessof the,penet~terhlS's1gnificanteffect on the penetratfonreststenee(Meyerhof.1961;laraf h th, 19n).''
Ca~flll consideni1~n
wlS!l'.Ye~
·.h i le dete!""1n1ri9,the..:oU9hness of.the cone....tert al. L
For
'~st~,in
sOils'r ou9hness.tsgener~lly,expressed
as~
rattooftheIngleof frictionbetweentile penetreeeter-material(a) ....
, , ' ',, '11
andth~SO!lfrictionangle(.Li e.•relative roughness(6/.) . In
Ithislnn stlgat l on absoluteroughness values were a1$o dete,l'1IIlnedin
terms
of the centrelineaverage (a.A). Tayl or-HobSon 1+0.4Talys urf.'
. 1
31
(Fig.Bb}anditrect ilinear recorder were'used to evalu atesurface roughn ess ofthree dIfferentconetips~sedin thisinves t igati on.
Tlie res u lts areshOlininAppendhA. Theroughne~~(CSA895;1962 ) isexpre ssed Intermsofcent relineaverage(CLA(1nmicrons.overa cut -offle ngthof 0.2541IIlI. Themeas ur edroughnes s values are presentedtnTable3a. F:om"these,resu1t~.itisseenth~tthereis
S~~.d tfference,if\.the,.Cl~ V~~~Sof~:~E!pl at es andco~es,.T~U.S.tbe
\(al ueo f 6 obte tnedfort~epfatesfro~direct sheartes,ts~ouldbe 'S'119htlY:differentf~r-th~'cones_actuallyusedl'n,t~-penetration
-.
'~t~'s.:~~: " ':-'1 ~~'~';ectfO~: ~~_ct?_~_ ~~~_ t,here;;ri, ~_PP'li~'~ ·t~·',dlc'u~a.te ~he-.
f1 n~1
,v"Ilu es'of., rou~hri'~:~~for ~ifferent',~one'
materfa;s,.3.6;.TargetPrepara tfon'.
Twotypes,of~D1 l't argetmat er-f al s were,'sele ctedfor thts 1n,ves tf ga tf on:
(l)Sil ica- 70sand '(il)MOd~ni ng'C1a,y
Themateria.l~"!ere readily,available and'.' - .sa~ies'. ." could'
.
~'p'repaf'1!d.
easi1y. sestcee,~these were'chosen as.re-Presen,tat1ve'ofp~relYnon- tiirge'ts.
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FIGsa, PHOTOGRAPH SHOWI1lG EXPERIMENTAL FACILITY
33
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to 1IliL1nta'na cons ta ntdensityatall de pt hsforloosesand.
COlourmarkingswereIWdeina woodenboll.(0.9l 4.ll.0.685II ll.
8.914 .,
at2Semintervalsand sandwasc~refull)'pla ce d upto therequi ; edheight. Coq:lac~i on"as~(joe'witnthe help ofanelectri- callyoper ate d vi brator: As soonas the top layerofsandreachedthe 2~mar k-ing . a furthe rquant ity ofsandwasplaced and...tbreteein. the samemanne rtJ'It l1thedes iredvoll11lewas obtained. Tnis was ecnte ...edbyco"t roll1 ngthe tfmeofvi bl-a tfon'foreachlaye r . Aft e r compactionwas'completedup to the topmos t layer, tota lweightofsand wasd·e~enn1ned.
TIlus , knowing't he volume.tI1effna1unftwe f ght was ca-l.- culated, Ra1 n1Agtecbntquew.asusedfor cons truct i on of loose ta r gets..
'..
.Send "as pouredin ...hthimaint aini nga consta nthei ghtofdrop frDllt
.
"the exist ingta~etsu r f~ ce.:Assoonas.thedes ~redheightofthe sa~lew~sob t ained .thebOiwas ",,?i ghed care fullJ. Thusthe firia l unitwightwas
Cll ~ulated.
Thre ediff e re ntdensit ies'ofsandurge.t·.prepa.recI:
1. Ile1Isesand(51type) : 16.18W.J 2. Hedl1Jllldens e.~and(52type ): 15.05
rJt/,,J
.J. loose sand (53 type): 14.09KN/m3 Forsatu r at edsaqlle s,thesa~rprocedurewas adopte das p.rll:!v10usl,yde s cr i bed fordrysaql1es. After thetar !ltt was co'n- structed,wa terlJla~addedtn the fomof11.9htspr ay.·Thecont a iner .that he ldthe soilwasnotperfect ly wat e r tightresultinginsome:
drai nage ofwaterfr om the.s ample. Saturatedsampl estes~din.this investigationere.not fullysaturatedin thest.rietsense .
3.6.2 . ModellingClay
Before prep arat i onof thetargetmater i al ,St andard Proctor compactio ntests were done toobtaintherelat i onshi pbetween dry unitweight andwatercontentfor thistypeof soil. The results areshowninF 1g.7 .
rhesete-tetvesthoroughl y pulverized and dried. a pre-
dete~l n\!d qua~t1 ty.
ofwat erwasadded to'the sou
andplacedin a large concrete m1xingmachi ne {f i g.8) . When themixturewashoneq- eneous then1twas taken out frtlm t rmac~ine. The volumeofa, 'cy lindr ic alcont a iner (0 . 9144 of xO.4572'}l1)~asaccurate lycalF~lated.Thesol1 mixture was placedinsi de the containerandcompactedwft h a Modif ied AASKTO hand hanmer, The desiredbUl~densl1;ywas'ob:tained using precalculatednumberofblows per hye;' of soil,
Re present a ti vesa~leswere taken at randomand at different' depthsduringthe targetpreparatio nto calculatethe exactwater contentand bulk, densi tyof the target mat eri al. Cylindri cal steel tubeswer eused to coll e ctsampl es forcal c.ulatin gthe'uni tweight ofsoil anB alsotoper formtriaxia l shear tests. Vane sheartest s
,wer e'also conductedbefo reandaftereachsetofexce-teents
~t
diff -..erent depths.,Twd.d1fferent typesofclay samples were usedas follows:
(1) Mediumstiffcl ay(Cltype) :.()ry density ~14.51KJl/m3I
\iater content'"29.61'l (it)··Softclay (e2tyPe) •
Drydensity =13.50K~/m3 WaterCDnte nt=34. 15%
39
3.6.3 . Targe-tprolllJrties
In additiontotargetpreparati on, se veralte s tswereco'll-
)~
ducte dto det ennine thephysicalprope r t i es of soil. Thes einclu de specificgra~itY Igrain sizedistributi on,Atte rberg limi t s(clay) andmaximum andmini mum voidratio(san d).,These.test swerepe rfonned .,. immediate lyafterpre ~ rati onoftheta rget.Classification dataforstttce-zosand are:
Meandiameter '"O~11 5 nrn~
CoooW"ficientofuniformity ..,;95 spect rt cgravltyof9rain~ E2.60
Maxi fl1.lmvoi,drert o ·0.95
Minimumvoidratio : 0.42
•The gra dati oncur ve~orthissot!is sh~wn.in Fig. 9aand is cl ass ified as medi umto ffnesandsh e.
The gr ainsIzedlstr'lbutf onofmodellingcl ayisshownin fig.~b. Ithas thefol 1owingpro~erties:
l.l :3n
'P.l "21%
Plas ti cityInde x ..l6~
spect ttcgravity ..2.80
Ac~'eteset"of propertlesof..t~etargetsare tabulat;d:ln
, "Tables4a.4b andac,
1
1 36
tr:l ax:l a.l compression4 . :::':h:::':,,,ng'h'f,"10,-70
tests anddi r e ct shear"" ."
testsdete...teed
. whl1e" "'J
fur. .
. \ ,
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,r:""-~'_o;A"'-;:;:,t:'~~i~~rt:t,!;,.,,?:,,,_
..,..~,~ '..,
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40
roodel1ing cl ay, thest rengthpr;;p~r{1~weredetemtnedusing triaxial compressiontests and vaneshear tests. Triaxia ltests wereconductedw;-thconfining press ures103'.4 KPa(15 psi),l37.9KPa (20 psi)and206. 8 KPa (30psi) . The resultsare showninFi gs. lOa, lOb.lac,10d andlOe.
A ser iesofdi rectsheartest s were conducted onsilica-70 sandto determi ne the valuesoftheangle,of shearresistance(+) andrelatIve roughnes sof differentcone mat;;;;al(6/" ). Thetest s. wereconduct ed Ina constant ratey( strain shear,bo~,WF25QOO'(Fig.
,l
"'~;' 11)" Thevalueofangle'sh ea'rresista nce-(~)as obt ained fromdirect s~ea rtestsare compared withtr iaxialtest res ul tsIn~l gs .12a and 12b.
A similar met hod was adoptedtodet ennineadhesi on(ca) betwee n oodelling cl ayand steel. Theresultsare showninTable 4c.
comparison
o f
vaneshea"rte stresultswi t hthat cotat nec from trfaxf al testsfO~delH n!lclayis shownin Table4b. Thefinal val ue ofc~hes; on~)
aas takenasthe a;era geofthe twotestresults.3.6.4.1.Penetr OlTM! t ert~SoilFr1ctlo~Angle
Todetennfne thefrict ion angl ebetween thepene t rometer material andsoil .tes tswere conducted1nthe WF25000 shearbox, Theupperhalf was fill edwith
Si1iC~70
sand atadesiredinitialdensit y andthe lower half,oftheshearbox 15 replaced ,by asolid plat e ofthe penetrometermaterial. The resul ts areShO~in Table 3b.Thethree differen t penetraJ t e rcone mater ials tes te d are:
'(l extcont1nue'dPage:55)
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FIG 8. EQUIPllftlTFOR MIXING CLAY SAHPLES
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FIG 12••VAlUATIONOFI/>WITHl!FORSILICA 70SAN aASIHE Rt-IINED .8Y DIRECTS.HEAR.AND TRIAXIAl-·TESTS
.. / .,/.,
/ / .. ..
7 ..
o ' . .
/,
·1 I .
ss
1. Stainl ess Steel
•2. PolishedAlumfniln J. SandedAluml n!~m
The valuespfdlrectshear testeere corrected for theactual cone roughness. The eorre ctto nfact O,f Swen! obta inedfromtheresults of
"Ielysur-f" tests onDothplat esand coneasshown inTabl e3a. Correct i on factor sof 1.125,1.2and1.1~6we reappl ted forst ai nlesssteel , pol is hed alum.fn1umandsandeda.1umfnll1ll,respectively. The cor- rectedvaluesofrel at iverou9hnes~ (~/.lare:
Stai lflessSteel 6/' 0.;5
Pol h hedA lumlnlum' SandedAlumi nium
6i• •
0.6 6/ . . . 0.75 Inthe next chapte r, these valueswillbeused 1nthecal- cvts ttons,3.7.~
The met hodsof preparingthesoil.terc ets
and
thephY,sical prepertf es ofthesoils and thepe~eti-ornetersare ghenf~this chepter-. Resultsofconventionallaborator y tfsts have beenpre sent ed andthese resultswtllbe used forccepaet scnand correlati on withthe penet romet ertests.)
~'-'.'"
i
f
CHAPTERIY
'illLYSIS OFRESULTS ANDDISCUSSION
4.1. General
Freehllpenet rationtestsas-descr ibed1nthe previous chapter wereconductedand the output frOllthepelletrometer'was recordedon"a)-channelchartrecorder.endalsoanl~ strlllllenta tio n taperecorder. Typicalraw dat a fromthechar t record er is shown in fig.13.'The recordobtai nedisavoltageoutput , fromthe .accelerometer ,theconeload celland theIsleeve
ro~d
ce"l, as afunction'of realtlme.·Represent atiYe Nwdata for differenttypes ofsollIs given InAppendlx B.
(alAccelerati on/decel er a t ionrecord'
As soonas the penetrometerisreleased,itisunder a constantaccelera tton 'g' duetogravitytillitst r ike s thesoil
.c·
tal"get. Thiseoe-respcndstothe initi alhorizontal str aightlineof the decel erationrecord. Upon'l11Pact,thepenet roo'eterdecelerat es,
'. "" . ,
the IIilgn1t udl!ofwhichincreaseswiththe depthofpenetra tion , as shownintherangeab of therecord. At.b,'thed~cele~ationisa
. . .
.,maxlmumanafttapersoff1nthe"rangebe.
"tc, therefsanaccelerat ion,pulseatthe endof penetration eyent ."At
~;~\1l1le
thepene.tromete~
haspassedthrough'll1Il xfmWll" '
. ,
penet gat.tu n andiseltp:erfenc.ing,.averysmall.upwardmoverent . The so11res istance'woul d thusbenegat ive. SCot t andPearce(1975)
56 (Te~t~t1nUed.pa ge58)
57
., .
CDNE RESISTANCE
. . '
.
~,DE'CELERA-r:IDN
C2 TYPE SOIL PENETRDMETER 3. 56 em. DIA. CONE 30·
STAINL E SS STEEL
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