基于遥感技术估算藏东南山区地下水径流模数方法

张家森; 许模; 张强; 漆继红; 王杨双; 夏强

doi:10.3799/dqkx.2021.034

Volume 47 Issue 2

Feb. 2022

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Zhang Jiasen, Xu Mo, Zhang Qiang, Qi Jihong, Wang Yangshuang, Xia Qiang, 2022. Estimating Groundwater Runoff Modulus Method Based on Remote Sensing in Mountainous Areas of Southeast Tibet. Earth Science, 47(2): 642-651. doi: 10.3799/dqkx.2021.034

Citation:

Zhang Jiasen, Xu Mo, Zhang Qiang, Qi Jihong, Wang Yangshuang, Xia Qiang, 2022. Estimating Groundwater Runoff Modulus Method Based on Remote Sensing in Mountainous Areas of Southeast Tibet. Earth Science, 47(2): 642-651. doi: 10.3799/dqkx.2021.034

Citation:

Zhang Jiasen, Xu Mo, Zhang Qiang, Qi Jihong, Wang Yangshuang, Xia Qiang, 2022. Estimating Groundwater Runoff Modulus Method Based on Remote Sensing in Mountainous Areas of Southeast Tibet. Earth Science, 47(2): 642-651. doi: 10.3799/dqkx.2021.034

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Estimating Groundwater Runoff Modulus Method Based on Remote Sensing in Mountainous Areas of Southeast Tibet

doi: 10.3799/dqkx.2021.034

State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2021-10-22
Publish Date: 2022-02-25

Abstract

Abstract

How to scientifically evaluate the groundwater runoff modulus under field conditions has important application value to meet the needs of engineering hydrogeology. In this paper, the study of groundwater runoff modulus under site conditions in the Parlung Zangbo watershed is carried out by establishing a linear regression model combined with technical means such as field survey, remote sensing interpretation and meteorological and hydrological observations. The results show that the study area has a typical seasonal snowmelt law. The snow accumulate in winter melt into runoff in summer, which serves as an additional source of groundwater recharge. After removing the influence of snowmelt runoff on the runoff modulus, the groundwater runoff modulus of magmatic aquifer, metamorphic aquifer, clastic aquifer and carbonate-clastic aquifer in the study area are respectively between 1.081-2.792 L/s·km², 1.833-3.225 L/s·km², 1.128-2.889 L/s·km², 3.455-3.879 L/s·km². The estimation results show that the groundwater runoff estimation model established in this paper can be used as a new method for estimating groundwater runoff modulus in southeastern Tibet and similar conditions, providing important hydrogeological parameter support for large-scale infrastructure projects in this area included the cascade development of the lower reaches of the Yarlung Zangbo River.
- remote sense,
- linear regression,
- groundwater runoff modulus,
- southeast Tibet,
- hydrogeology

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References(42)

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Estimating Groundwater Runoff Modulus Method Based on Remote Sensing in Mountainous Areas of Southeast Tibet

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