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Land Subsidence,also occur, but in a lesser amount. The flow and stress-strain fields, which develop because of fluid withdrawals, are intimately connected and theoretically coupled. However, coupling is weak in most real hydrogeological settings, and uncoupled prediction models can be used. Furthermore, in large a
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查看完整版本: Titlebook: Hydrology of Disasters; Vijay P. Singh Book 1996 Springer Science+Business Media Dordrecht 1996 climate.climate change.hydrology.natural d