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1956年以来洞庭湖盆的演变

Evolution of Dongting Lake Basin Since 1956

  • 摘要: 1956年以来洞庭湖盆经历了萎缩和扩容的历史过程,为分析各历史阶段变化原因和预测变化趋势,根据1956-2019年洞庭湖水系水沙和湖盆水面面积、湖容实测资料开展研究,基于分离变量法重点识别泥沙淤积、湖盆沉降、湖区围垦及洞庭湖水系采沙对湖容变化的贡献比例。结果表明:1956-2019年洞庭湖水面面积减小1 247.59 km2,其中东洞庭湖水面面积萎缩最为严重,1956-1980年湖区围垦是洞庭湖水面面积减小的主要因素,1980年以后洞庭湖水面面积趋于稳定。三峡水库蓄水前(1956-2002年)入湖沙量及出湖沙量均持续减少,泥沙淤积率约为70%;三峡水库蓄水后(2003-2019年),入湖沙量大幅减少,泥沙淤积率降至14%。湖盆沉降、湖区采沙与泥沙淤积对湖容的影响存在抵消效应,洞庭湖盆目前仍处于缓慢的构造沉降中,平均沉降速率约3 mm/a;2003年以后随着采沙活动进行,洞庭湖萎缩速率有所减缓。1980年以前湖容减小,湖区围垦、泥沙淤积和湖盆沉降对湖容增大的贡献比例分别为-92.7%、-13.2%和5.9%;1980年以后湖容经历了由减小至变大的过程,整体为减小,1981-2002年泥沙淤积、湖盆沉降的贡献比例分别为-107.6%和7.6%,2003-2019年泥沙淤积、湖盆沉降及采沙的贡献比例分别为-11%,24.8%和86.2%。三峡水库蓄水后湖盆沉降速率大于泥沙淤积速率,同时湖区采沙为三峡水库蓄水后湖容变化控导因素,随着新一轮采沙规划(2023-2027年)实施,洞庭湖将呈现扩张趋势。

     

    Abstract: Since 1956, the Dongting lake basin has experienced a historical process from shrinkage to development. To investigate the reason behind its evolution during each historical stage and predict its evolution trend, we work out this study based on data of water-sediment discharge, lake-basin water surface area and lake capacity during 1956-2019, in which contribution ratios of sedimentation, lake basin subsidence, reclamation and sand mining on lake-capacity variation are identified using the variable separation method. Results show that the lake-basin water surface area decreased by 1 247.59 km2 during 1956-2019, in which the shrinkage of the east lake basin was the most severe, and reclamation within the lake basin was the major driving factor during 1956-1980, whereas the lake-basin water surface area became stable after 1980. Both sediment input and output continuously declined before the impoundment of the Three Gorges Dam(1956-2002), with a rough sedimentation ratio of 70% in the lake. However, sediment input experienced a remarkable reduction after the impoundment(2003-2019), with the sedimentation ratio falling to 14%. There was an offset effect among lake-basin subsidence, sand mining and sedimentation when they altered the lake capacity. At present, the lake basin is still in a slow tectonic subsidence, with an average rate of 3mm/a. As sand minning proceeds, the lake shrinkage slows down. Before 1980, the lake capacity decreased, with contribution ratios of reclamation, sedimentation and tectonic subsidence were-92.7%,-13.2% and 5.9%. However, after 1980, the lake capacity witnessed a shift from declination during 1981-2002 to augment during 2003-2019 and a net declination, with contribution ratios of sedimentation and tectonic subsidence were-107.6% and 7.6% during 1981-2002 and those of sedimentation, tectonic subsidence and sand mining were-11%, 24.8% and 86.2% during 2003-2019. Considering the higher rate of tectonic subsidence than sedimentation after the impoundment of the Three Gorges Dam and the dominance of sand mining in the lake capacity change, the Dongting lake will continuously develop as the new sand mining planning(2023-2027) implements.

     

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