globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6441045
论文题名:
基于面积-高程积分的地下水动态分析以泾惠渠灌区为例
其他题名: Groundwater dynamic analysis based on hypsometric integral: a case study of Jinghuiqu irrigation district, China
作者: 徐斌1; 王金凤1; 张艳2; 金岚2; 李换换2; 熊玉晴2
刊名: 地球环境学报
ISSN: 1674-9901
出版年: 2019
卷: 10, 期:1, 页码:809-818
语种: 中文
中文关键词: 面积-高程积分 ; 地下水 ; 动态 ; 分析 ; 泾惠渠灌区
英文关键词: hypsometric integral ; groundwater ; dynamic ; analysis ; Jinghuiqu irrigation district
WOS学科分类: MINERALOGY
WOS研究方向: Mineralogy
中文摘要: 为了研究泾惠渠灌区的地下水动态特征,探讨面积-高程积分在地下水动态分析中的可行性,利用ArcGIS空间分析工具计算了灌区地下水面积-高程积分数据,绘制了不同时期的地下水面积-高程积分曲线,分析了灌区地下水水位与储存量动态特征。结果显示:1978 2012年,泾惠渠灌区地下水面积-高程积分值为0.46、0.44、0.38、0.39,表明地下水水位与储存量整体呈下降趋势;1991 2012年, 410.00 446.19 m水位区间面积由1978年的2.54下降为0,342.51 360.00 m水位区间面积多年持续增加,中等水位区间存在演化差异性,反映出不同时期地下水开发强度具有空间变异性;以1978年为基准,至2012年地下水储存量减少约7.08*10~8 m~3;降水、地表水引水量、人工开采是影响泾惠渠灌区地下水动态的重要因素,补排失衡是引起灌区地下水储存量下降的主要原因。研究表明:面积-高程积分曲线可以表征地下水水位空间结构特征和储存量的变化情况,利用面积-高程积分值能够近似估算地下水储存量变化量,证明了面积-高程积分在地下水动态研究中具有一定的实用性。
英文摘要: Background, aim, and scope Groundwater is an important water resources and a significant factor in maintaining regional environmental health and ecological balance. The combined effect of human activities and climate change has led to changes in the groundwater environment that inevitably have a corresponding impact on groundwater dependent ecosystems. Therefore, an accurate analysis of the dynamic characteristics of groundwater has important practical significance for making rational strategies of groundwater exploitation, the protection of ecological balance and the sustainable development of society and economy. The hypsometric integral is a quantitative index to study the relationship between the horizontal cross-sectional area and its elevation, which is a kind of the quantitative analysis to reflect the status and erosion trend of the geomorphology. It is widely used in the research of geomorphic evolution, evaluation of lithology and tectonics, hydrological characteristics analysis of drainage basin. From the perspective of spatial data model representation of ground objects, both the shallow groundwater surface and the drainage basin topography surface can be described by digital elevation model and have the same mathematical basis for the hypsometric integral analysis. By analyzing the variation characteristics of groundwater surface, the hypsometric integral analysis provides an applicable method for studying groundwater dynamics. Jinghuiqu irrigation district is an important food and vegetable production base in Shaanxi Province where residents mainly rely on groundwater. In recent years, the groundwater level and storage in the region has been impacted by industrial and agricultural activities.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/155578
Appears in Collections:气候变化事实与影响

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作者单位: 1.长安大学环境科学与工程学院
2.长安大学水与发展研究院
3.长安大学,
4.旱区地下水文与生态效应教育部重点实验室, 西安
5.西安
6.西安,
7.710054
8.710054
9.710054
10.长安大学地球科学与资源学院, 西安, 陕西 710054, 中国

Recommended Citation:
徐斌,王金凤,张艳,等. 基于面积-高程积分的地下水动态分析以泾惠渠灌区为例[J]. 地球环境学报,2019-01-01,10(1):809-818
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