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Land Subsidence Along the Delta‐Mendota Canal, California
This article begins by providing a brief overview of land subsidence and one of its most common causes ‐ overdraft of confined or artesian groundwaters where pumpage exceeds recharge. The Delta‐Mendota Canal in California's San Joaquin Valley is presented as an outstanding example of subsidence, particularly subsidence “lag”, a condition that is created when little or no pumping occurs, thus decreasing the overdraft.
Land Subsidence Along the Delta‐Mendota Canal, California
This article begins by providing a brief overview of land subsidence and one of its most common causes ‐ overdraft of confined or artesian groundwaters where pumpage exceeds recharge. The Delta‐Mendota Canal in California's San Joaquin Valley is presented as an outstanding example of subsidence, particularly subsidence “lag”, a condition that is created when little or no pumping occurs, thus decreasing the overdraft.
Land Subsidence Along the Delta‐Mendota Canal, California
Prokopovich, N. P. (author) / Hebert, D. J. (author)
Journal ‐ American Water Works Association ; 60 ; 915-920
1968-08-01
6 pages
Article (Journal)
Electronic Resource
English
Land subsidence along Delta-Mendota Canal, California
Springer Verlag | 1969
|Sedimentation in the Delta‐Mendota Canal
Wiley | 1965
|