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中国农学通报 ›› 2018, Vol. 34 ›› Issue (21): 121-126.doi: 10.11924/j.issn.1000-6850.casb17060033

所属专题: 资源与环境 农业生态

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

近30年石羊河流域生态环境变化及驱动力分析

蒋菊芳   

  1. 甘肃省武威市气象局
  • 收稿日期:2017-06-06 修回日期:2017-08-08 接受日期:2017-08-24 出版日期:2018-07-26 发布日期:2018-07-26
  • 通讯作者: 蒋菊芳
  • 基金资助:
    公益性行业(气象)科研专项(重大专项)“干旱气象科学研究—我国北方干旱致灾过程及机理”(GYHY201506001-2);国家自然科学基金项 目“半干旱区作物干旱致灾过程特征及其若干阈值研究”(41275118);干旱基金“荒漠植物对干旱环境的适应机理及干旱阈值研究”(IAM201507);甘 肃省气象局科研面上项目“甜高粱在河西的气候适应性研究”(GSMAMs2016-13)。

Ecological Environment Change and Driving Force in Shiyang River Basin in Recent 30 Years

  • Received:2017-06-06 Revised:2017-08-08 Accepted:2017-08-24 Online:2018-07-26 Published:2018-07-26

摘要: 为保护石羊河流域生态环境提供科学依据,笔者以气候变化和人类活动为主要因素,分析了石羊河流域治理前后生态环境的变化趋势。结果表明:1987—2016年石羊河流域气温显著升高,降水略增加,日照时数增加,蒸发量增大。植被覆盖面积增大,2007—2016年与2000—2006年相比,归一化植被指数(NDVI)在0.3~0.5之间的面积增大0.9%。2007年流域治理以来,机井数量和耕地面积较前二十年减少。2000—2016年石羊河年平均流量呈显著增加趋势,尤其蔡旗水文站向下游下泄水量明显增加。2005—2016年石羊河流域中、下游沙丘移动和沙漠边缘进退速度明显减缓,流域地下水位埋深稳步回升。青土湖重现水域以来,水域面积平均每年增加3.59平方公里,地下水位埋深平均每年回升0.12米,流域生态环境明显改善。

关键词: 玉米, 玉米, 马铃薯, 间作, 行比, 生态

Abstract: In order to provide scientific basis for protecting the ecological environment of Shiyang river basin, the author analyzed the change tendency of the ecological environment before and after the treatment of Shiyang river basin, which took the climate change and human activities as the main factors. The results showed that the temperature significantly increased, the precipitation slightly increased, the sunshine hours increased, and the evaporation volume increased in Shiyang river basin from 1987 to 2016. The area of vegetation coverage increased, and the area of NDVI increased by 0.9% from 0.3-0.5 in 2007 to 2016 year compared with 2000-2006 year. Since the 2007 year Shiyang river basin management, the number of machine wells and arable land areas decreased compared the twenty years before. The annual average runoff significantly increased of Shiyang river, and the released water significantly increased from Caiqi flag station to the downstream from 2000 to 2016 year. The movement of sand dunes and the edge of the desert obviously slowed down, and the groundwater depth recovered steadily in shiyang river basin from 2005 to 2016. Since reappeared water of the qingtu lake, the water area increased by an average of 3.59 square kilometers per year, the average depth of groundwater level rose by an average of 0.12 meters per year. The ecological environment had improved significantly of Shiyang river basin.