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官厅水库自1956年投入正式运用以来,水库沿岸周围某些地区产生了浸没现象,部分库岸发生了坍岸,与水库回水的上游部分发生了淤积三角洲,其中以浸没影响较为严重。如有些村庄由于地下水上升,房基沉陷,墙壁裂缝甚至倒塌;土地沼泽化和果树枯萎、雕谢甚而淹死等。由于这些现象的发生,引起了相当的反应。不少人也担心三门峡水库将来是否也会出现这些问题。
Since the official use of the Guanting Reservoir in 1956, submergence has occurred in some areas along the banks of the reservoir. Some of the banks have been collapsed and silt delta has formed in the upstream part of the backwater of the reservoir, of which the submergence is more serious. If some villages due to the rise of groundwater, housing subsidence, wall cracks or even collapsed; land swamp and withered fruit trees, carving Xie and even drowned. As a result of these phenomena, a considerable response has elicited. Many people are also worried about Sanmenxia reservoir in the future whether these problems will occur.