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Foreword
AccordingtotherequirementsofDocumentJIANBIAO[2004]No.67issuedbytheMinistryofConstruction-"NoticeonPrintingandDistributing'theDevelopmentandRevisionPlanofNationalEngineerConstructionStandardsin2004'",thisstandardwasrevisedbyNanjingHydraulicResearch
InstitutebasedonGBJ145-90StandardforClassificationofSoils.
Thisstandardincludesfivechapters.Itsmaintechnicalcontentsinclude:generalprovisions;terms,symbolsanddesignations;basicrequirements;soilclassification;simplifiedsoilidentification,classificationanddescription.Anappendixisalsoprovided.
Themainrevisionsmadeinthisstandardareasfollows:thecontextsrelevanttospecialsoilsareremoved.Terms,symbolsanddesignationsareadded.Appendix1forbasicdesignationsisremoved;onesubgroupfractionsareincreasedforgravel,twosubgroupfraetionsareincreasedforsand;theplasticitychartwiththeliquidlimitscorrespondingto10mmdepthoffall-conepenetrationisremoved,alongwithitsrelatedcontexts;andAppendixA:Systemblockdiagramforengineeringclassificationofsoilsisadded.
TheMinistryofConstructionisinchargeoftheadministrationofthisstandard.GeneralInstituteofWaterResourcesandHydropowerPlanningandDesignofMinistryofWaterResourcesisresponsiblefortheroutinemanagementofthisstandard.ExplanationofthetechnicalconentisundertakenbyNanjingHydraulicResearchInstitute.Alltherelevantorganizationsareencouragedtoobtainexperienceinusingthisstandard,andalsokindlyrequestedtosubmitcommentsandadvices,whenevernecessary,totheNanjingHydraulicResearchInstitute(Address223GuangzhouRoad,Nanjing,210029,China)forfuturerevision.
ChiefDevelopmentOrganizations,Co-DevelopmentOrganizationsandChiefDraftersofthisStardand:
ChiefDevelopmentOrganizations:
NanjingHydraulicResearchInstitute
Co-DeyelopmentOrganizations:
ChinaAcademyofBuildingResearch
ComprehensiveInstituteofGeotechnicalInvestigationandSurveying
BeijingGeotechnicalInstitute
AcademyofRailwaySciences
ResearchInstituteofHighwayofMinistryofCommunications
GeneralBuildingResearchInstituteofChinaMetallurgyGroup
MechanicalIndustrySurveyandDesignInstitute
ChinaInstituteofWaterResourcesandHydropowerResearch
YangtzeRiverScientificResearchInstitute
Xi'anUniversityofTechnology
JilinUniversity
ChiefDrafters:
FANMingqiaoTENGYanjingWUWeiLIUYanhuaLUOMeiyun
WANGYuanXINHongboZHANGWeiWENYanfengGONGBiweiHUZaiqiangWANGQingTIANXichunandWANGFang
Contents
1Generalprovisions (
1)
2Terms,symbolsanddesignations (
2)
2.1Tem (
2)
2.2Symbols (
2)
2.3Designations (
3)
3Basicstipulations (
5)
4Soilclassification (
7)
5Simplifiedidentification,classification,anddescriptionofsoils (
9)
5.1SimplifiedIdentificationmethods (
9)
5.2Identificationandclassifcation (
10)
5.3Soildescription (
10)
AppendixASystemblockdiagramforengineeringclassificationofsoils (
12)
Explanationofwordinginthisstandard (
14)
1Generalprovisions
1.0.1Thisstandardisformulatedtounifytheengineeringclassficationofsoilstofacilitatethequalitative
evaluationofsoilcharacteristics.
1.0.2Thisstandardisapplicabletobasicclassificationofsoils.Aspecializedstandardforsoilclassificationmaybeformulatedincompliancewiththisstandardtomeettheprofessionaldemandsofrelevantindustries.
1.0.3Inadditiontotherequirementsofthisstandard,theindextestingforsoilclassificationshallalsocomplywiththesespecifiedintherelevantcurrentnationalstandards
·2·
2Terms,symbolsanddesignations
2.1Terms
2.1.1grainsize
Theminimumdiameterofsieveopeningthroughwhichsoilgraincouldpass,orthediameterof
equivalentspherewhichhasthesamevelocityofsoilgrainsettleinstillwater.
2.1.2grainsizedistributioncurve
Acurverepresentsthemasspercentageofsoilgrainfinerthanaspecificgrainsize.
2.1.3constrainedgrainsize
Thegrainsizecorrespondingto60%fineronthecumulativegrain-sizedistributioncurveofsoil.2.1.4effectivegrainsize
Thegrainsizecorrespondingto10%fineronthecumulativegrain-sizedistributioncurveofsoil.
2.1.5fraction
Agroupofsoilparticleswithacertainrangeofgrainsizedistribution.
2.1.6coefficientofuniformity
Thecoefficientindicatingthedegreeofuniformityofgrainsizes(
2.1.7coefficientofcurvature
Thecoefficientindicatingtheshapeofgrain-sizedistributioncurve.
2.1.8gradation
Themassproportionofeachspecialgrain-sizegrouptothewhole.
2.1.9liquidlimit
Thewatercontemtboundarybetweenliquidandplasticstatesoffine-grainedsoil.2.1.10plasticlimit
Thewatercontentboundarybetweenplasticandsemi-solidstatesoffine-grainedsoil.2.1.11plasticityindex
Numericaldifferencebetweentheliquidandplasticlimitsoffine-grainedsoil.
2.1.12plasticitychart
Achartforclassifyingfine-grainedsoils,inwhichtheplasticityindexIp(ordinate)isplottedagainsttheliquidlimitw.(abscissa).
2.1.13organicsoil
ClaysorsiltswithcertainorganiccontentOm(5%≤0m<10%),specialodor(smells)andhigh
compressibility.
2.1.14organo-soil
ClaysorsiltswithhighorganiccontentOm(Om≥10%),specialodor(smells)andhigh
compressibility.
2.2Symbols
C.—coefficientofcurvature;
C?—coefficientofuniformity;
·3·
d—grainsize;d—constrained
grainsize;
d?—effectivegrainsize;
Ip—elasticityindex;
wi—liquidlimit;
wp—plasticlimit;
Om—organiccontent.
2.3Designations
2.3.1Basicdesignations:
B—Boulder;
C—Clay;
Cb—Cobble;
F—Finesoil;
G—Gravel;
H—Highliquidlimit;
L—Lowliquidlimit;
M—Silt;
O—Organicsoil;
P—Poorly-graded;
S—Sand;
SI—Mixtureofverycoarsesoils;
W—Well-graded.
2.3.2Groupdesignations
BSI—Boulderswithfinersoils;
CbSI—Cobbleswithfinersoils;
CH—Highliquidlimitclay(Fatclay);
CHG—Gravellyclaywithhighliquidlimit(Gravellyfatclay);
CHO—Organicclaywithhighliquidlimit(Organicfatclay);
CHS—Sandyclaywithhighliquidlimit(Sandyfatclay);
CL—Lowliquidlimitclay(Leanclay);
CLG—Gravellyclaywithlowliquidlimit(Gravellyleanclay);
CLO—Organicclaywithlowliquidlimit(Organicleanclay);
CLS—Sandyclaywithlowliquidlimit(Sandyleanclay);
GC—Clayeygravel;
GF—Gravelwithfines;
GM—Siltygravel;
GP—Poorly-gradedgravel;
GW—Well-gradedgravel;
MH—Highliquidlimitsilt(Elasticsilt);
MHG—Gravellysiltwithhighliquidlimit(Gravellyelasticsilt);
MHO—Organicsiltwithhighliquidlimit(Organicelasticsilt);
MHS—Sandysiltwithhighliquidlimit(Sandyelasticsilt);
ML—Lowliquidlimitsilt(Silt);
MLG—Gravellysiltwithlowliquidlimit(Gravellysilt);
MLO—Organicsiltwithlowliquidlimit(Organicsilt);
MLS—Sandysiltwithlowliquidlimit(Sandysilt);
SC—Clayeysand;
SF—Sandwithfines;
SIB—Mixtureofbouldersandfinersoils;
SICb—Mixtureofcobblesandfinersoils;
SM—Siltysand;
SP—Poorly-gradedsand;
SW—Well-gradedsand.
·5·
3Basicstipulations
3.0.1Classificationofasoilshallbebasedonthefollowingindices:
1Thegrain-sizedistributionandcharacteristicsofthesoil.
2Theconsistencysindicesofthesoil:liquidlimit(wi),plasticlimit(w),andplasticityindex(I?).
3Theorganiccontentofthesoil.
3.0.2ThefractionofasoilshallbedividedaccordingtoitsgrainsizerangeasspecifiedinTable3.0.2.Table3.0.2Divisionoffraction
Fraction
Component
Grain-sizerange(representedbydiameterd,mm)
Verycoarsegrain
Boulder(Blockstone)
d>200
Cobble(Brokenstone)
60<d≤200
Coarsegrain
Gravel
Coarse
20<d≤60
Medium
5<d≤20
Fine
2<d≤5
Sand
Coarse
0.5<d≤2
Medium
0.25<d≤0.5
Fine
0.075<d≤0.25
Finegram
Silt
0.005<d≤0.075
Clay
d≤0.005
3.0.3ThegradationcharacteristicsofsoilshallbedeterminedaccordingtothecoefficientofuniformityCandthecoefficientofcurvatureC.asfollows:
1ThecoefficientofuniformityC.shallbecalculatedbythefollowingequation:
2ThecoefficientofcurvatureCshallbecalculatedbythefollowingequation:
(3.0.3-1)
(3.0.3-2)
wheredoisthegrainsizecorrespondingto30%fineronthecumulativegrain-sizedistributioncurveof
thesoil.
3.0.4Soilscanbeclassifiedintoverycoarse-grained,coarse-grained,andfine-grainedtypesbasedontherelativecontentofdifferentfractionsandshallcomplywiththestipulationsasfollows:
1Verycoarse-grainedsoilsshallbeclassifiedbasedonfraction.
2Coarse-grainedsoilsshallbeclassifiedbasedonfraction,gradation,contentoffine-grainedsoil.
3Fine-grainedsoilsshallbeclassifiedbasedontheplasticitychart,typeofcoarse-grainedcomponentandorganiccontentcontained.
3.0.5Fine-grainedsoilsshallbeclassifiedwiththeplasticitychart(Figure3.0.5).
plasticityindex,Ip
Liquidlimit,wr(%)
Figure3.0.5Plasricitychart
Note:1TheabscissaofFigure3.0.5denotestheliquidlimit(cr)andtheordinatedenotestheplasticityindex(Ip)ofthesoil.
2TheliquidlimitinFigure3.0.5isthewatercontentmeasuredwithCasagrandepercussion-cupapparatus,orthewatercontent
correspondingtoa17mmpenetrationofafallingconewithamassof76gandatipangleof30°.
3TheareabetweenthedottedlinesinFigure3ta.5fthefransionzonefromclaytosit.
·6·
·7·
4Soilclassification
4.0.1Classificationofverycoarse-grainedsoilsshallmeetthestipulationsspecifiedinTable4.0.1.Table4.0.1Classificationofverycoarse-grainedsoils
Soilcategory
Fractioncontent
Groupdesignation
Name
Verycoarse-grainedsoils
Verycoarsefractioncontent>75%
Bouldercontent>cobblecontent
B
Boulder(Blockstone)
Bouldercontent≤cobblecontent
Cb
Cobble(Rubble)
Verycoarsesoils
mixedwithfiner
soils
50%<Verycoarse
ractioncontent≤75%
Bouldercontentcobblecontent
BSI
Boulder(Blockstone)withfinersoil
Bouldereontent
cobblecontent
CbSI
Cobble(Rubble)withfinersoils
Finersoilsmixed
withverycoarse
soils
15%<Verycoarse
fractioncontent≤50%
Bouldercontent>cobblecontent
SIB
Mixtureoffinersoilsandboulders(Blockstones)
Bouldercontent≤cobblecontent
SICb
Mixtureoffinersoilsand
cobbles(Rubbles)
Note:Finersoilsmixedwithyerycoarsesoilsmaybefurthersubdividedbasedonthecontentofcoarsegrainsorfines.
4.0.2Ifthecontentofverycoarse-grainedfractionis15%orless,thesoilsamplemaybeclassifiedbasedonthecorrespondingstipulationsforcoarsegrainsorfineswithoutconsiderationofverycoarse-grainedfraction.Whenverycoarse-grainedfractionhasaninfluenceontheoverallpropertiesofsoil,itshouldbetreatedasgravelfraction.
4.0.3Classifythesoilascoarse-grainedsoils,ifthecoarse-grainedfractioncontentisgreaterthan50%,anditsclassificationshallmeetthefollowingstipulations:
1Classifythesoilasgravel,ifgravelfractioncontentisgreaterthansandcontent;
2Classifythesoilassand,ifgravelfractioncontentisequaltoorlessthansandcontent.4.0.4TheclassificationofgravelsshallmeetthestipulationsspecifiedinTable4.0.4.
Table4.0.4Classificationofgravelsoils
Soilcategory
Fractionconten
Groupdesignation
Name
Gravel
Finesfraction<5%
C≥5and1≤C≤3
GW
Well-gradedgravel
C<5or(C<lorC>3)
GP
Poorly-gradedgravel
Gravelwithfines
5%≤Finesfraction<15%
GF
Gravelwithfines
Finesgravel
15%≤Finesfraction<50%
Finesclassifiedasclay*
GC
Clayeygravel
Finesclassifiedassilt**
GM
Siltygravel
Note:*Thesiltgrainedcontentoffinegrainedfractionis50%orless;
**Thesiltgrainedcontentoffinegrainedfractionisgreaterthan50%.
·8·
4.0.5ClassificationofsandsshallmeetthestipulationsspecifiedinTable4.0.5.
Table4.0.5Classificationofsandsoils
Soilcategory
Fractioncontent
Groupsymbol
Name
Sand
Finesfraction<5%
C≥5and1≤C≤3
C<5or(C<1orC>3)
SW
Well-gradedsand
SP
Poorly-gradedsand
Sandwithfines
5%≤Finesfraction<15%
SF
Sandwithfines
Finessand
15%≤Fines
fraction<50%
Finesclassifiedasclay*
SC
Clayeysand
Finesclassifiedassilt**
SM
Siltysand
Note:*Thesiltgrainedcontentoffinegrainedfractionis50%orless;
**Thesiltgrainedcontentoffinegrainedfractionisgreaterthan50%.
4.0.6Classifythesoilasfine-grainedsoils,ifthefinesfraetioncontentisgreaterthan50%.4.0.7Fine-grainedsoilshallbeclassifiedaccordingtothefollowingstipulations.
1Classifythesoilasfines,ifthecoarse-grainedfractuioncontentis25%orless.
2Classifythesoilassandyorgravellyfines,ifthecoarse-grainedfractioncontentisgreaterthan
25%but50%orless.
3Classifythesoilasorganicsoil,iftheorganiccontentislessthan10%but5%ormore.4.0.8TheclassificationoffinesshallmeeithestipulationsspecifiedinTable4.0.8.
Table4.0.8Classificationoffines
PositionofplasticindicesofsoilinplasticitychartFigure3.0.5
Groupdesignation
Name
I≥0.73(w?.-20)
andIp≥7
w?≥50%
CH
Highliquidlimitclay(Fatclay)
w?<50%
CL
Lowliquidlimitclay
(Leanclay)
1<0.73[w,-20
orl4
w?≥50%
MH
Highliquidlimitsilt
(Elasticsilt)
wi<50%
ML
Lowliquidlimitsilt
(Slit)
Note:Soilsinthetransitionzonefromclaytosilt(CL-ML)maybefurthersubdividedinaccordancewiththetypesofadjacentsoillayers.4.0.9Fineswithcoarsegrainsshallbeclassifiedaccordingtothepositionofplasticindicesofsoilinplasticitychartandtypesofcoarsegrains,andtheirclassificationshallmeetthefollowingstipulations:
1ClassifythesoilasgravellyfinesandaddsymbolGattheendofthedesignationoffines,ifthecontentofgravelincoarsegrainsisgreaterthanthatofsand.
2ClassifythesoilassandyfinesandaddsymbolSattheendofthedesignationoffines,ifthecontentofgravelincoarsegrainsislessthanorequaltothatofsand.
4.0.10TheclassificationoforganicsoilsshallmeetthestipulationsspecifiedinTable4.0.8,andaddsymbolOattheendofthecorrespondingsoildesignation.
4.0.11Ifthesoilindexequalsthecorrespondinglimitvalueasdefined,thesoilmaybeclassifiedbasedonasafetyprincipleforpracticaluse.
4.0.12SoilsmaybeclassifiedaccordingtoAppendixA.
·9·
5Simplifiedidentification,classificationanddescriptionofsoils
5.1Simplifiedidentificationmethods
5.1.1Visualidentification:spreadadispersedair-driedsampleintoathinlayer,andclassifythesoilaccordingtotheproportionofverycoarse,coarse,andfinegrains.
5.1.2Drystrengthtest:pinchasmallpieceofsoilintoapat.Afterdryinginair,crumb,breakoff,andtwistitwithfingers.Thefollowingdistinctionsshallbemadebasedonthefingerpressure:
1Highdrystrength:difficulttocrumborbreakoff.
2Mediumdrystrength:slightforcetocrumborbreakoff.
3Lowdrystrength:easytocrumbortwistintopowder,
Note:Whenthesoilcontainscarbonates,ironoxides,andotherconnponentsthatmayincreasesoildrystrength,wetsamplesshouldbeusedforhand-twisttesttoassessandcheckitsdrystrength.
5.1.3Hand-twisttest:pinchasmallpieceofslightly-wetorhard-plasticsoilinhand,andpinchitintosliceswiththumbandindexfingers.Thefollowingdistinctionsshallbemadebasedonhandfeelingand
smoothnessofsoilslices:
1Highplasticity:creamyfeeling,nosandyfeeling,andsmoothSurface,
2Mediumplasticity:slightlycreamyfeeling,sandyfeeling,andstightlysmoothsurface.3Lowplasticity:slightlyyiseousfeeling,strongsandyfeeling,androughsurface.
5.1.4Thread-rollingtest:evenlykneadapieceofsoilwithwatercontentslightlyhigherthantheplasticlimitinhands,thenrollitintoathreadonpalm.Thefollowingdistinctionsshallbemadebasedontheminimumdiameterthatthesoilthreadcouldbeformedwithoutcrumbling:
1Highplasticity:thediameterlessthan1mm.
2Mediumplasticity:thediameterbetween1mmand3mm.
3Lowplasticity:thediametergreaterthan3mm.
5.1.5Toughnesstest:evenlykneadapieceofsoilwithawatercontentslightlyhigherthantheplasticlimitinhandsevenly,thenrollitintoathreadwithadiameterof3mmonpalm.Thefollowing
distinctionsshallbemadebasedonwhetherthethreadcanberefoldedandrerolled:
1Hightoughness:beingshapedintoapat,rolledintoathread,andrefoldedintoapatwithoutcrumblingpieces.
2Mediumtoughness:beingshapedintoapatandnoteasilycrumbled.
3Lowtoughness:beinghardlyornottobeshapedintoapat,andpronetocrumblingbyslightor
nopinching.
5.1.6Dilatancytest:moldthesoilinsoftorliquidplasticstateintoaball,shakeitrepeatedlyonthepalm,andstrikethesideofthepalmagainstbytheotherpalmseveraltimes.Freewaterseepsoutfromthesoil,andtheballsurfaceshowsluster.Pinchthesoilballwithtwofingers.Afterreleasing,thewaterisreabsorbedandthelusterdisappears.Thefollowingdistinctionsshallbemadebasedonthereactionspeedsofwaterseepageandabsorption:
1Rapidreaction:quickwaterseepageandabsorption.
2Mediumreaction:medium-speedwaterseepageandabsorption.
·10·
3Slowreaction:slowwaterseepageandabsorption.
4Noreaction:nowaterseepageandabsorption.
5.2Identificationandclassification
5.2.1Verycoarse-grainedandcoarse-grainedsoilsmaybeclassifiedandnamedaccordingtostipulationssetoutin4.0.1to4.0.6basedonvisualresults.
5.2.2Fine-grainedsoilsmaybeclassifiedandnamedbasedonresultsofdrystrength,hand-twist,thread-rolling,toughness,anddilatancytestsaccordingtostipulationssetoutinTable5.2.2.
Table5.2.2Simplifiedclassificationoffine-grainedsoils
Drystrength
Hand-twisttest
Thread-rollingtest
Dilatancytest
Designation
Minimum
diameterofsoil
thread(mm)
Toughness
Low-medium
Mainlysilt,sandyfeeling,
slightlyviscous,medium
roughsurface,andnoluster
32
Low-medium
Quick-mediun
ML
Medium-high
Containingsandgraing
viscous,slightlycreamy
feeling;mediumsmooth
surface,slighulylustrous
2-1
Medium
Slow-no
CL
Medium-high
Richsilr,viscous,slightly
creamy/feeling,medium
smoothsurface,slightly
lustrous
2-1
Medium-high
slow-no
MH
High-veryhigh
Nosandyfeelings,highly
viscous,stronglycreamy
feeling,smoothsurface,
lustrous
<1
High
No
CH
Note:Foralltypesofsoilslistedinthetablethataregrayordarkincolorandhaveaspecialsmell,thesymbolOshallbeaddedattheendofcorrespondingsoildesignation,e.g.,MLO,CLO,MHO,andCHO.
5.2.3Organicmattersinsoilsareincompletelydecomposedanimalorplantremainsandamorphoussubstance.Theymaybeidentifiedbyvisualobservation,handtouchingorsmelling.Generally,organicmattersaregreyordark,withspecialodor,elasticityandspongefeeling.
5.3Soildescription
5.3.1Thedescriptionofsoilsshouldincludethefollowingitems:
1Verycoarse-grainedandcoarse-grainedsoils:popularnameandlocalname;maximumgrainsize;degreeofweatheringofparticles;masspercentageofverycoarsegrains,gravelgrains,andsandgrains;shapesofverycoarseorcoarsegrains(round,sub-round,angularorsub-angular);mineralcompositionofsoilparticles;colorandorganicmatter;naturaldensity;typesoffines(clayorsilt)contained;symbolandnameofasoilorsoillayer.
·11·
2Fine-grainedsoils:popularnameandlocalname;maximumgrainsize;masspercentageofvery
coarsegrains,gravelgrains,andsandgrains;naturaldensity;colorandorganicmatterofthesoilinwetstate;humidityofthesoil(dry,wet,verywetorsaturated);consistencyofthesoil(liquidplastic,soft
plastic,plastic,hard
soils.
plastic,hard);plasticity
ofthesoil(high,medium,orlow);symbolandnameof
·12·
AppendixASystemblockdiagramforengineeringclassificationofsoils
Very-coarsefractioncontent>75%
Boulder(B)
Bouldercontent>cobblecontent
Cobble(Cb)
Bouldercontent≤cobblecontent
Verycoarse-grainedsoils
Very-coarsefraction
content>15%
50%<Verycoarsefraction
content≤75%
Boulderwithfinersoils(BSI)
Boulderc
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