georam
Geotechnical
- Apr 28, 1999
- 114
I would like to get some comments or input on the selection of c’ and phi’ for cohesive soil<br>
properties in slope stability analyses using effective stress analyses.<br>
<br>
Let us say, that based on a considerable amount of direct shear tests, it was found that the soil has <br>
the following properties (same data, by regression analysis) :<br>
<br>
1. Regression - not forcing result to c’=phi’=0 <br>
c’= 20 kPa<br>
phi’= 18 deg.<br>
<br>
2. Regression - forcing results to c’=phi’=0<br>
c’=0 (forced)<br>
Phi’= 22 deg.<br>
<br>
In the steady state seepage analysis (long term), we usually are reluctant to include any c’ component in the effective stress analyses. Adding a small amount of c’ in the stability analyses would affect the results considerably. However, if we choose the properties based on No. 1 above and dropping the c’ to 0, then we “internally” penalize (over conservative) in just using phi’=18 deg.<br>
<br>
What about using the properties as shown on No.2 above ? (ie., we accept that c’=0, but another rerun on regression analysis will be carried out, forcing the data to include<br>
c’=phi’=0. This way, we will use the strengths of c’= 0 and phi’= 22 deg.<br>
<br>
Of course, if we choose No. 1 above and minimum F.O.S =1.5, it will be too conservative. What about the option of using data from No.2 ? <br>
<br>
Any comments ?<br>
<br>
PS.<br>
Some people tend to analyze using concept of No. 1 above, but then they add a little cohesion in the analyses, such as using minimal value of c’= 4 kPa (0.5 psi), instead of zero. So, which is the right way for effective stress analyses ? <br>
properties in slope stability analyses using effective stress analyses.<br>
<br>
Let us say, that based on a considerable amount of direct shear tests, it was found that the soil has <br>
the following properties (same data, by regression analysis) :<br>
<br>
1. Regression - not forcing result to c’=phi’=0 <br>
c’= 20 kPa<br>
phi’= 18 deg.<br>
<br>
2. Regression - forcing results to c’=phi’=0<br>
c’=0 (forced)<br>
Phi’= 22 deg.<br>
<br>
In the steady state seepage analysis (long term), we usually are reluctant to include any c’ component in the effective stress analyses. Adding a small amount of c’ in the stability analyses would affect the results considerably. However, if we choose the properties based on No. 1 above and dropping the c’ to 0, then we “internally” penalize (over conservative) in just using phi’=18 deg.<br>
<br>
What about using the properties as shown on No.2 above ? (ie., we accept that c’=0, but another rerun on regression analysis will be carried out, forcing the data to include<br>
c’=phi’=0. This way, we will use the strengths of c’= 0 and phi’= 22 deg.<br>
<br>
Of course, if we choose No. 1 above and minimum F.O.S =1.5, it will be too conservative. What about the option of using data from No.2 ? <br>
<br>
Any comments ?<br>
<br>
PS.<br>
Some people tend to analyze using concept of No. 1 above, but then they add a little cohesion in the analyses, such as using minimal value of c’= 4 kPa (0.5 psi), instead of zero. So, which is the right way for effective stress analyses ? <br>