Man-Induced Land Subsidence
How would you feel if your land had sunk 9 m in the past 50 years because of human activity? It happened in the San Joaquin Valley. In fact, land subsidence has been caused by man’s activities in at least 37 of the 50 states of the United States and affects more than 40,000 km2 in this country alone. Data from a few sites where economic impact is documented suggest a total annual cost to the nation of more than $100 million; worldwide, the total economic impact is astounding and growing. These nine papers, dedicated to Joseph Fairfield Poland's life work, constitute a major contribution to measuring and understanding this problem. They are arranged in three categories: (1) fluid withdrawal from porous media; (2) drainage of organic soil; and (3) collapse into man-made and natural cavities.
Subsidence over oil and gas fields
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Published:January 01, 1984
Abstract
Most oil and gas reservoirs experience only small amounts of compaction and surface subsidence. Significant subsidence due to production of hydrocarbons has been observed over some oil and gas fields. This paper presents a review of the fundamentals of reservoir compaction and surface subsidence over oil and gas fields and explains why large-scale subsidence is rare. A new method of estimating maximum potential subsidence is presented and used to analyze the subsidence over oil and gas fields in Louisiana. Large-scale compaction and subsidence are evidently associated with inelastic behavior of the reservoir rock and in some cases of the surrounding rock. No reliable methods have been established for predicting either the transition from elastic to inelastic reservoir rock behavior or large-scale reservoir compaction and subsidence.
The preconsolidation effect evident in some field data introduces an additional difficulty in understanding and predicting subsidence. Various possible causes for the effect include uplift and erosion, temporary pressure drop or an increase in horizontal stresses prior to hydrocarbon production, effects of loading rate on reservoir rock, and changes from elastic to inelastic behavior of the reservoir rock or surrounding formations.