Chapter 1
Introduction
Publication: Investigation of Land Subsidence due to Fluid Withdrawal
Abstract
Land subsidence can occur on local and regional scales worldwide and is often discovered only after damage to buildings and important infrastructure occurs. Many mechanisms cause land subsidence; much known subsidence occurs along coasts where subsidence contributes to relatively higher sea levels and coastal flooding, which may be exacerbated by global warming. This book explores problems associated with subsidence caused by aquifer system compaction accompanying subsurface fluid withdrawal, including changes in the natural gradients of streams, as well as the as-built gradients of engineered water conveyance structures, increased riverine and coastal flooding, and damage to wells penetrating the affected lithologic units.
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