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首页> 外文期刊>Journal of Hydrology >Variation of lake-river-aquifer interactions induced by human activity and climatic condition in Poyang Lake Basin, China
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Variation of lake-river-aquifer interactions induced by human activity and climatic condition in Poyang Lake Basin, China

机译:鄱阳湖盆地人类活动和气候条件诱导的湖泊 - 河流腹水互动的变异

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摘要

In low-lying fluvial-lacustrine plain, anthropogenic activities and climatic variation could have a comprehensive influence on the interactions between surface water and groundwater (SW-GW) involving lake-river-aquifer. Quantification of the changes in SW-GW interaction in spatial and temporal scale causing by the two driving sources could help to the understanding of the regional water cycle mechanism and the adjustment of the decision making. However, it is usually difficult to distinguish the impact of anthropogenic activities from the climatic variation on a regional scale. Here, by using a regional three-dimensional groundwater numerical model with long term monitoring of the hydrological dynamic in Poyang Lake Basin (PLB), China, we found that groundwater storage variation in the bank storage districts can be used as an indicator to quantify each source and sink in the process of SW-GW interactions. And surface water infiltration plays a more dominant role in constructing bank storage which is meant to preserve groundwater storage. Our research in PLB demonstrates that the hydrological change caused by the operation of the Three Gorges Dam (TGD) since 2003 is mainly responsible for the autumn drought in PLB. The surface water recession due to the impoundment in TGD from September to October has an impact about 7 times stronger than the rainfall reduction. Moreover, the groundwater storage deficit caused by the insufficient recharge from the surface water infiltration would maintain the whole year, unlike the surface water system which would easily recover at the end of the year. The results demonstrate the chain interactions among lake-river-aquifer. Failing to distinguish the magnitude of each influence factor may lead to underestimating the impact on the whole water system. The results also highlight the function and the vulnerability of the groundwater system which might be vital to the riparian and estuarinewetl and ecosystem.
机译:在低洼的河流-湖泊平原,人类活动和气候变化可能对涉及湖泊-河流含水层的地表水和地下水(SW-GW)之间的相互作用产生综合影响。量化这两个驱动源在时空尺度上引起的SW-GW相互作用的变化,有助于理解区域水循环机制和调整决策。然而,在区域范围内,通常很难区分人为活动的影响和气候变化。在这里,通过对中国鄱阳湖流域(PLB)水文动态进行长期监测的区域三维地下水数值模型,我们发现河岸蓄水区的地下水蓄水量变化可作为量化SW-GW相互作用过程中每个源和汇的指标。而地表水渗透在建造堤坝蓄水中起着更为主导的作用,堤坝蓄水旨在保护地下水蓄水。我们对PLB的研究表明,2003年以来三峡大坝运行引起的水文变化是造成PLB秋季干旱的主要原因。TGD 9月至10月蓄水造成的地表水衰退的影响约为降雨量减少的7倍。此外,由于地表水渗透补给不足而导致的地下水储存不足将维持全年,而地表水系统在年底很容易恢复。结果表明,湖泊-河流含水层之间存在链式相互作用。未能区分每个影响因素的大小可能会导致低估对整个水系统的影响。研究结果还强调了地下水系统的功能和脆弱性,这可能对河岸和河口湿地以及生态系统至关重要。

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