LR11
Structural
- Sep 13, 2001
- 166
I never paid much attention to this before.
So far my understanding was that if you have a saturated soil, the lateral pressure was based on the modified (reduced) density of soil and the additional hydrostatic pressure, see image.
The lateral pressure coefficient, I thought was unchanged.
Yesterday I read on a forum, possibly this one, that when soil is saturated, it loses it's shear strength and the lateral coefficient was equal to 1. I did not pay too much attention to it. I can't remember the type of soil, or whether there was a potential difference allowing water to flow, such as retaining walls subject to tides, I don't know if this is relevant.
Today I came across a Table from California Trenching and Shoring Manual, which shows a much different Ko value for clays, depending on the level of saturation.
Firstly, my question is: Is this relevant for clays only?
Secondly, is there a good reference with tabulated values, showing how Ko changes based on the level of saturation.
So far my understanding was that if you have a saturated soil, the lateral pressure was based on the modified (reduced) density of soil and the additional hydrostatic pressure, see image.
The lateral pressure coefficient, I thought was unchanged.
Yesterday I read on a forum, possibly this one, that when soil is saturated, it loses it's shear strength and the lateral coefficient was equal to 1. I did not pay too much attention to it. I can't remember the type of soil, or whether there was a potential difference allowing water to flow, such as retaining walls subject to tides, I don't know if this is relevant.
Today I came across a Table from California Trenching and Shoring Manual, which shows a much different Ko value for clays, depending on the level of saturation.
Firstly, my question is: Is this relevant for clays only?
Secondly, is there a good reference with tabulated values, showing how Ko changes based on the level of saturation.