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Geotechnical and Materials Engineering Standards for Bridge ...

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INTACT ROCK STRENGTH - Although rack masses are non-isotropic <strong>and</strong> the<br />

main feature of their weakness 1s the strength along<br />

discontinuities, it is oftcn useful to have some in<strong>for</strong>mation<br />

about tha uniaxial cc~pressive strength of the intact rock.<br />

The tabla below gives seven grades of rock strength <strong>and</strong> simple<br />

methods of identification. These grades have been based on<br />

results of unconfined compressive stkength tests <strong>for</strong> which<br />

st<strong>and</strong>ard methods have been ruggcsted3,<br />

Strength Fleld Rgnge of unconfined<br />

Grsds Classification Identification Compressive strength<br />

Hethad INf a3<br />

RO Extremely vesk Idtnted by thumbnail < 1<br />

R1 Very weak Crumbles under firm 1 - 5<br />

blows of gtologfcal .<br />

hzmtr; can b6 petlcd<br />

with a pocket knifa<br />

R2 Weak rock Can ba peeled by a pocket<br />

knife vith difficuity;<br />

shallov indentations mads<br />

by a fim blow with point<br />

of gcalogical hammer<br />

R3 Hedim strong Cannot be scraped or<br />

peeled vlth a pocket hife;<br />

spechen can be fractured<br />

vith a single firm blow<br />

. of geological hamer.<br />

R4 Strong Specimen requires more SO - 100<br />

than one blow of geolog-<br />

ical h-er to fracture<br />

R5 Very strong Spechen requires many 100 - 250<br />

blows of geological h-er<br />

to fracture:<br />

R6 Extremely strong Specben can only be<br />

chipped by a geological<br />

hammer

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