CED
Geotechnical
- Jul 31, 2002
- 4
Hello. I've got an interesting slope issue dealing with a bank along a reservoir. Here's the background:
Our firm has a client who is proposing to develop a flat plateau that overlooks a reservoir to one side and a ravine to the other. The slope along the reservoir ranges from 20 to 30 meters in height. The reservoir is located within a wide mountain valley. The dam associated with the reservoir became operational in 1978.
The valley is very wide, with a very gentle slope from the toe of the bank to the center of the valley where the river is located. Prior to the construction of the dam and flooding of the reservoir, the valley floor was used as an airstrip.
Topographic maps of the region, a recent survey of the toe of the slope (at low water levels) and info from the operators of the reservoir show that the high water level within the reservoir only comes up to about the toe of the slope, where a small bench/beach is located (about 3 meters wide) before the very gentle grading toward the center of the valley/reservoir. The face of the bank in question is vegetated by mosses, grasses and an occasional tree. There was no visible indication of creep of the slope.
The bank is at a constant slope of about 24 degrees, except for a small region that juts out toward the center of the reservoir that has a slightly steeper slope angle of 30 degrees.
A review of air photos dating back to 1971 show that the bank in question has not changed since that time. A site inspection did show some minor surface slumping located just above the high water mark in the region with the steeper slope, likely due to wave action from the reservoir when full.
From the air photos and reviewing other slopes in and around the site, I feel that the bank below the proposed development site is likely already at its stable angle of repose in the locations with the shallower angle.
Now for my question:
Time constraints and client funding limit a full-scale, long-term slope stability analysis. As such, I'm wondering whether or not there are other methods for determining a safe top-of-bank setback guideline for a development in this location, without actually accessing the stability of the slope itself. I'm familiar with the setback guideline formula developed by Dave Cruden for valley slopes, but it may not be applicable in this case.
Thanks,
CED
Our firm has a client who is proposing to develop a flat plateau that overlooks a reservoir to one side and a ravine to the other. The slope along the reservoir ranges from 20 to 30 meters in height. The reservoir is located within a wide mountain valley. The dam associated with the reservoir became operational in 1978.
The valley is very wide, with a very gentle slope from the toe of the bank to the center of the valley where the river is located. Prior to the construction of the dam and flooding of the reservoir, the valley floor was used as an airstrip.
Topographic maps of the region, a recent survey of the toe of the slope (at low water levels) and info from the operators of the reservoir show that the high water level within the reservoir only comes up to about the toe of the slope, where a small bench/beach is located (about 3 meters wide) before the very gentle grading toward the center of the valley/reservoir. The face of the bank in question is vegetated by mosses, grasses and an occasional tree. There was no visible indication of creep of the slope.
The bank is at a constant slope of about 24 degrees, except for a small region that juts out toward the center of the reservoir that has a slightly steeper slope angle of 30 degrees.
A review of air photos dating back to 1971 show that the bank in question has not changed since that time. A site inspection did show some minor surface slumping located just above the high water mark in the region with the steeper slope, likely due to wave action from the reservoir when full.
From the air photos and reviewing other slopes in and around the site, I feel that the bank below the proposed development site is likely already at its stable angle of repose in the locations with the shallower angle.
Now for my question:
Time constraints and client funding limit a full-scale, long-term slope stability analysis. As such, I'm wondering whether or not there are other methods for determining a safe top-of-bank setback guideline for a development in this location, without actually accessing the stability of the slope itself. I'm familiar with the setback guideline formula developed by Dave Cruden for valley slopes, but it may not be applicable in this case.
Thanks,
CED