承德坝上高原东部月亮湖湖面萎缩原因及应对建议

殷志强, 赵磊, 刘文波, 李瑞敏, 邵海, 彭超, 田钰琛. 2020. 承德坝上高原东部月亮湖湖面萎缩原因及应对建议. 水文地质工程地质, 47(6): 57-64. doi: 10.16030/j.cnki.issn.1000-3665.202008039
引用本文: 殷志强, 赵磊, 刘文波, 李瑞敏, 邵海, 彭超, 田钰琛. 2020. 承德坝上高原东部月亮湖湖面萎缩原因及应对建议. 水文地质工程地质, 47(6): 57-64. doi: 10.16030/j.cnki.issn.1000-3665.202008039
YIN Zhiqiang, ZHAO Lei, LIU Wenbo, LI Ruimin, SHAO Hai, PENG Chao, TIAN Yuchen. 2020. Shrinkage reasons and countermeasures of Moon Lake area in the eastern part of Bashang Plateau, Chengde City. Hydrogeology & Engineering Geology, 47(6): 57-64. doi: 10.16030/j.cnki.issn.1000-3665.202008039
Citation: YIN Zhiqiang, ZHAO Lei, LIU Wenbo, LI Ruimin, SHAO Hai, PENG Chao, TIAN Yuchen. 2020. Shrinkage reasons and countermeasures of Moon Lake area in the eastern part of Bashang Plateau, Chengde City. Hydrogeology & Engineering Geology, 47(6): 57-64. doi: 10.16030/j.cnki.issn.1000-3665.202008039

承德坝上高原东部月亮湖湖面萎缩原因及应对建议

  • 基金项目:

    中国地质调查局地质调查项目(DD20190310)

详细信息
    作者简介: 殷志强(1980-),男,高级工程师,主要从事第四纪环境演变研究。E-mail:yinzq@cigem.cn
  • 中图分类号: P931.7

Shrinkage reasons and countermeasures of Moon Lake area in the eastern part of Bashang Plateau, Chengde City

  • 承德坝上高原位于我国北方生态脆弱区,近年来正面临着自然湖泊面积萎缩和局部地下水位下降等问题。为查明坝上高原东部月亮湖萎缩原因,更好服务生态环境支撑区建设,笔者在野外调查和资料收集分析基础上,对坝上高原地区的生态环境变化和月亮湖萎缩原因进行了详细研究,初步认为:(1)1975—1993年为月亮湖水面面积较快增长期,1993年湖面面积最大,为0.43 km2;1993—2013年为缓慢萎缩期,2013年之后为较快萎缩期;(2)年际尺度上月亮湖区降水量和蒸发量都呈增加趋势,但因温度升高和下垫面条件改变引起的蒸发量增加趋势更明显;(3)人类活动对湖泊面积影响作用也不容忽视,人工林面积增加、旅游开发后的道路硬化、地下水开采和牲畜饮水增多可能也是湖泊快速萎缩的重要原因。建议坝上高原地区未来发展节水型生态旅游,同时实施湖区及周边地区地下水禁限采,强化水源涵养保护。
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出版历程
收稿日期:  2020-08-15
修回日期:  2020-09-01

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