【24h】

Dynamic modeling of groundwater spatial distribution in the lower reaches of Tarim River, China

机译:塔里木河下游地下水空间分布动态模拟

获取原文
获取原文并翻译 | 示例

摘要

Tarim River is a typical inland river. Riverbank plants mainly depend on the flood and groundwater to maintain their growth. Groundwater table depth, one of eco-environment factors, determined constitutes distribution and growth of natural plant. Since 2000, it has carried on continuously monitoring of groundwater by Tarim River Management Bureau and Xinjiang Institute of Ecology and Geography, Chinese Academy of Science, through setting cross section and observation wells, and some pertinent researches and analyses have been done. But using limited observation data to inverse groundwater spatial distribution will play a more dominant role in rational evaluation and scientific management ecosystem in the lower reaches of Tarim River. In this paper, the groundwater flowing processes and the water-table fluctuating processes during the past 3 years were simulated to obtain the spatial and temporal distribution of groundwater table by means of the GIS-assisted FEFLOW modeling based on the Digital Elevation Model data (DEM) and hydrogeologic data obtained in the Alagan section, one representative section of 12 groundwater monitoring sections, in the lower reaches of Tarim River. The model can be applied with relatively limited data to reappear the dynamic change of groundwater. Then groundwater table and calculated groundwater table depth can be used to analyze the relationship between groundwater and eco-environment. The results of model showed that groundwater was affected by river leakage, the main effective transverse region was 1.0 km from the river and within this effective region the groundwater depth was below 10 m.
机译:塔里木河是典型的内陆河。河岸植物主要依靠洪水和地下水来维持其生长。地下水位深度是生态环境因素之一,它决定了天然植物的分布和生长。自2000年以来,它通过设置断面和观测井,由塔里木河管理局和中国科学院新疆生态地理研究所连续进行了地下水监测,并进行了相关研究和分析。但是,使用有限的观测数据来反演地下水的空间分布将在塔里木河下游合理评估和科学管理生态系统中发挥更大的作用。本文通过基于数字高程模型数据(DEM)的GIS辅助FEFLOW建模,模拟了过去3年的地下水流动过程和地下水位波动过程,以获取地下水位的时空分布。 )和塔里木河下游12个地下水监测区的一个代表性区Alagan区获得的水文地质数据。该模型可以使用相对有限的数据来重新显示地下水的动态变化。然后可以利用地下水位和计算出的地下水位深度来分析地下水与生态环境之间的关系。模型结果表明,地下水受到河流渗漏的影响,主要有效横向区域距河流1.0 km,在该有效区域内,地下水深度在10 m以下。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号