Construction Methods - Chapter06.pdf
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RockExcavation
6–1INTRODUCTION
RockCharacteristics
Rockmaybeclassifiedasigneous,sedimentary,ormetamorphic,accordingtoitsorigin.
Igneousrock
formedwhentheearth’smoltenmaterialcooled.Becauseofitsorigin,itis
quitehomogeneousandisthereforethemostdifficulttypeofrocktoexcavate.Examples
ofigneousrockaregraniteandbasalt.
Sedimentaryrock
wasformedbytheprecipitationof
materialfromwaterorair.Asaresult,itishighlystratifiedandhasmanyplanesofweak-
ness.Thusitisthemosteasilyexcavatedtypeofrock.Examplesincludesandstone,shale,
andlimestone.
Metamorphicrock
originatedasigneousorsedimentaryrockbuthasbeen
changedbyheat,pressure,orchemicalactionintoadifferenttypeofrock.Metamorphic
rockisintermediatebetweenigneousrockandsedimentaryrockinitsdifficultyofexca-
vation.Examplesofmetamorphicrockincludeslate,marble,andschist.
Thedifficultyinvolvedinexcavatingrockdependsonanumberoffactorsinaddi-
tiontotherocktype.Someofthesefactorsincludetheextentoffracturesandotherplanes
ofweakness,theamountofweatheringthathasoccurred,thepredominantgrainsize,
whethertherockhasacrystallinestructure,rockbrittleness,androckhardness.
RockInvestigation
Relativehardnessismeasuredon
Moh’sscale
from1(talc)to10(diamond).Asarule,any
rockthatcanbescratchedbyaknifeblade(hardnessabout5)canbeeasilyexcavatedby
rippingorothermechanicalmethods.Forharderrock,additionalinvestigationisrequired
toevaluatetherockcharacteristicsdescribedabove.Theprincipalmethodsforinvestigat-
ingsubsurfaceconditionsincludedrilling,excavatingtestpits,andmakingseismicmeas-
urements.Drillingmaybeusedtoremovecoresamplesfromtherockortopermitvisual
observationofrockconditions.Coresamplesmaybevisuallyinspectedaswellastestedin
thelaboratory.ObservationinatestpitorinspectionbyTVcamerasplacedintodrilled
holeswillreveallayerthickness,theextentoffracturingandweathering,andthepresence
155
156
CHAPTER6
Figure6–1
Schematicrepresentationofseismicrefractiontest.
Figure6–2
Graphofrefractiontestdata.
ofwater.Useoftherefractionseismographpermitsarapiddeterminationofrocksound-
nessbymeasuringthevelocityatwhichsoundtravelsthroughtherock.
Inperformingaseismicrefractiontest,asoundsourceandanumberofreceivers(geo-
phones)aresetup,asillustratedinFigure6–1.Thetimerequiredforasoundwavetotravel
fromthesoundsourcetoeachreceiverismeasuredandplottedagainstthedistancefromthe
soundsource,asillustratedinFigure6–2.Inthisplottheslopeofeachsegmentofthecurve
representsthesoundvelocityinthecorrespondingsubsurfacelayer.Thisvelocityhasbeen
foundtorangefromabout1000ft/s(305m/s)inloosesoiltoabout20,000ft/s(6100m/s)
insoundrock.Sincetherelationshipbetweentheangleofincidenceandtheangleofre-
fractionofasoundwavecrossingtheinterfaceoftworocklayersisafunctionoftheirre-
spectivesoundvelocities,theseismicrefractiontestmethodmayalsobeusedtodetermine
157
ROCKEXCAVATION
thethicknessofrocklayers.Equation6–1maybeusedtodeterminethethicknessofthe
upperlayerwhenthesoundvelocityincreaseswithlayerdepth,thatis,whenthevelocity
inthetoplayerislessthanthevelocityinthesecondlayer,whichistheusualcaseinthe
field.
(6–1)
where
H
1
%
thicknessofupperlayer(ftorm)
D
1
%
distancefromsoundsourcetofirstintersectionoflinesontime-distance
graph(ftorm)(pointA,Figure6–2)
V
1
%
velocityinupperlayer(ft/sorm/s)
V
2
%
velocityinsecondlayer(ft/sorm/s)
EXAMPLE6–1
Findtheseismicwavevelocityanddepthoftheuppersoillayerbasedonthefollowingre-
fractionseismographdata:
DistancefromSound
SourcetoGeophone
ft
m
T ime(ms)
10 3.05 5
20 6.10 10
30 9.15 15
40 12.20 20
50 15.25 22
60 18.30 24
70 21.35 26
80 24.40 28
SOLUTION
PlottimeoftravelagainstdistancefromsoundsourcetogeophoneasshowninFigure6–3.
%
40
#
%
2000ft
>
0.020
#
B %
12.2
#
%
610m
0.020
#
%
80
#
40
0.028
#
0.020
%
5000ft
>
B %
24.4
#
12.2
0.028
#
0.020
%
1525m
158
CHAPTER6
Figure6–3
Graphofrefractiontestdata,Example6–1.
1
%
40
¢
5000
#
2000
5000
"
2000
≤
%
13.1ft
B %
12.2
2
¢
1525
#
610
1525
"
610
≤
%
4.0m
Rock-HandlingSystems
Theprocessofrockmovingmaybeconsideredinfourphases:loosening,loading,hauling,
andcompacting.ThemethodsemployedforrockcompactingarediscussedinChapter5.
Therefore,thisdiscussionofrock-handlingsystemswillbelimitedtothephasesofloos-
ening,loading,andhauling.Theprincipalmethodsandequipmentavailableforaccom-
plishingeachofthesephasesarelistedinTable6–1.
Thetraditionalmethodforexcavatingrockinvolvesdrillingblastholesintherock,
loadingtheholeswithexplosives,detonatingtheexplosives,loadingthefracturedrock
intohaulunitswithpowershovels,andhaulingtherockawayintrucksorwagons.Newer
alternativesincludetheuseoftractor-mountedripperstoloosenrock,theuseofwheel
Table6–1
Principalrock-handlingsystems
Operation EquipmentandProcess
Loosen Drillandblast
Rip
Load Shovel
Wheelloader
Haul Truck
Wagon
Loadandhaul Reinforcedscraper
159
ROCKEXCAVATION
Figure6–4
Largetunnelingmachine.(CourtesyofTheRobbinsCompany)
loaderstoloadfracturedrockintohaulunits,andtheuseofreinforced(or“specialappli-
cation”)scraperstobothloadandhaulfracturedrock.Theequipmentandproceduresuti-
lizedareexplainedinSections6–2to6–4.Theselectionoftherock-handlingsystemtobe
employedinaparticularsituationshouldbebasedonmaximizingthecontractor’sprofit
fromtheoperation.
Tunneling
Tunnelinginrockisaspecializedformofrockexcavationthathastraditionallybeenac-
complishedbydrillingandblasting.Recently,however,
tunnelingmachines
ormechanical
moles
equippedwithmultiplecutterheadsandcapableofexcavatingtofulltunneldiameter
havecomeintoincreasinguse.ThetunnelingmachineshowninFigure6–4weighs285tons
(258t),producesathrustof1,850,000lb(8229kN),anddrillsa19-ft(5.8-m)–diameterhole.
Someofthespecializedtermsusedintunnelingincludejumbos,hydraulicjumbos,and
muckingmachines. A
jumbo
isalargemobileframeequippedwithplatformsatseveral
elevationstoenabledrillsandworkerstoworkonthefulltunnelfaceatonetime.The
hydraulicjumbo
illustratedinFigure6–5isaself-propelledmachineequippedwithanum-
berofhydraulicdrills,eachmountedonitsownhydraulicboom.Suchamachineiscapable
ofdrillingblastholesacrossthefulltunnelfaceatonetime.A
muckingmachine
isaformof
shovelespeciallydesignedforloadingfracturedrockintohaulunitsduringtunnelexcavation.
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