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Extension of RMR and Q-system in Taiwan

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Table 3-1 Criteria for rat<strong>in</strong>g Rock Type A <strong>and</strong> B<br />

Rock mass class <strong>of</strong><br />

Rock Type A<br />

<strong>RMR</strong> range <strong>of</strong><br />

Rock Type A<br />

<strong>RMR</strong> range <strong>of</strong><br />

Rock Type B<br />

Rock mass class <strong>of</strong><br />

Rock Type B<br />

AⅠ <strong>RMR</strong>≧81 ---- ----<br />

AⅡ <strong>RMR</strong>80~61 <strong>RMR</strong>≧81 BⅡ<br />

AⅢ <strong>RMR</strong>60~41 <strong>RMR</strong>80~61 BⅢ<br />

AⅣ <strong>RMR</strong>40~21 <strong>RMR</strong>60~41 BⅣ<br />

AⅤ <strong>RMR</strong>20~11 <strong>RMR</strong>40~21 BⅤ<br />

AⅥ <strong>RMR</strong>≦10 <strong>RMR</strong>≦20 BⅥ<br />

Table 3-2 Criteria for rat<strong>in</strong>g Rock Type C <strong>and</strong> D<br />

Rock mass class<br />

Cementation<br />

St<strong>and</strong>ards <strong>of</strong> rat<strong>in</strong>g<br />

Geologic material composition<br />

Rock<br />

Type<br />

CⅠ(C)<br />

CⅠ(MIX)<br />

CⅠ(S)<br />

Fair or good cementation<br />

(can’t be dented by the thumb)<br />

The content <strong>of</strong> silt <strong>and</strong> clay is greater than 50%<br />

The content <strong>of</strong> s<strong>and</strong>, silt, clay or gravel<br />

<strong>in</strong>dividually isn’t greater than 50%<br />

The content <strong>of</strong> s<strong>and</strong> is greater than 50%<br />

C<br />

CⅡ(C)<br />

Poor or loose cementation<br />

CⅡ(MIX)<br />

(can be dented by the thumb)<br />

The content <strong>of</strong> silt <strong>and</strong> clay is greater than 50%<br />

The content <strong>of</strong> s<strong>and</strong>, silt, clay or gravel<br />

<strong>in</strong>dividually isn’t greater than 50%<br />

CⅡ(S)<br />

The content <strong>of</strong> s<strong>and</strong> is greater than 50%<br />

The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

DⅠ(G) Extremely good cementation size greater than sieve #4) is greater than 75 %;<br />

(boulders or gravel need to be contact with each other<br />

knocked <strong>of</strong>f by geologic hammer The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

DⅠ(M) with great power)<br />

size greater than sieve #4) is between 50% ~<br />

75%; don’t contact with each other<br />

The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

Rock<br />

Type<br />

D<br />

DⅡ(G)<br />

DⅡ(M)<br />

size greater than sieve #4) is greater than 75 %;<br />

Fair or good cementation<br />

contact with each other<br />

(boulders or gravel need to be<br />

knocked <strong>of</strong>f by geologic hammer)<br />

The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

size greater than sieve #4) is between 50% ~<br />

75%; don’t contact with each other<br />

The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

DⅢ(G)<br />

DⅢ(M)<br />

Poor or loose cementation<br />

(boulders or gravel need to be<br />

knocked <strong>of</strong>f by h<strong>and</strong>)<br />

size greater than sieve #4) is greater than 75 %;<br />

contact with each other<br />

The content <strong>of</strong> boulders <strong>and</strong> coarse gra<strong>in</strong>s (gra<strong>in</strong><br />

size greater than sieve #4) is between 50% ~<br />

75%; don’t contact with each other<br />

Notes: 1.Because the amount <strong>of</strong> water content affects the tunnel construction <strong>of</strong> Rock Type C <strong>and</strong> D<br />

considerably, this table must be adopted based on dra<strong>in</strong>age <strong>in</strong> advance.<br />

2.S<strong>and</strong> layers <strong>and</strong> gravel layers possibly appear simultaneously on the excavation face. The<br />

location <strong>of</strong> s<strong>and</strong> layers on the excavation face has a determ<strong>in</strong>ate <strong>in</strong>fluence on the stability <strong>of</strong><br />

tunnels, <strong>and</strong> it should be considered carefully while design<strong>in</strong>g tunnel supports.<br />

D7 - 6

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