moe333
Geotechnical
- Jul 31, 2003
- 416
I am looking at a water-banking project and trying to evaluate if there would be subsidence due to the recharge and pumping operations over long periods of time.
Water will be "spread" on surface into a diked recharge basin of about one square mile. The water will recharge an aquifer with the current groundwater level at about 300 feet below surface. The "water spreading" will occur sporadically as excess water is available, and groundwater pumping will occur during times of relative drought.
The subsurface soils consist of sand/silty sand alluvium which probably grades from loose to dense with depth. I'm thinking there will be some ground subsidence as a result of the fluctuating groundwater levels, but I am not really sure how to evaluate what the magnitude may be.
Some adjacent structures such as well pads, pipelines, and weir structures could potentially be affected by the subsidence.
Any ideas on how to evaluate whether there would be significant subsidence, and approximate magnitudes?
Water will be "spread" on surface into a diked recharge basin of about one square mile. The water will recharge an aquifer with the current groundwater level at about 300 feet below surface. The "water spreading" will occur sporadically as excess water is available, and groundwater pumping will occur during times of relative drought.
The subsurface soils consist of sand/silty sand alluvium which probably grades from loose to dense with depth. I'm thinking there will be some ground subsidence as a result of the fluctuating groundwater levels, but I am not really sure how to evaluate what the magnitude may be.
Some adjacent structures such as well pads, pipelines, and weir structures could potentially be affected by the subsidence.
Any ideas on how to evaluate whether there would be significant subsidence, and approximate magnitudes?