Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake

This paper aims to calculate and analyze the spatial and temporal variations in the groundwater flow quantity in Nam Co Lake based on the water balance principle. The results show that a large amount of groundwater was gradually lost and that, groundwater loss decreased from 1.9 billion m3 to 1.5 bi...

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Main Authors: Yan Du, Zhide Huang, Mowen Xie, Asim Farooq, Chen Chen
Format: Article
Language:English
Published: MDPI AG 2018-07-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/10/7/941
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spelling doaj-5aac326baff64e91a4eeeffed4ca33982020-11-24T23:05:54ZengMDPI AGWater2073-44412018-07-0110794110.3390/w10070941w10070941Temporal Variations in the Quantity of Groundwater Flow in Nam Co LakeYan Du0Zhide Huang1Mowen Xie2Asim Farooq3Chen Chen4School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, ChinaSchool of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, ChinaSchool of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, ChinaSchool of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, ChinaSchool of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, ChinaThis paper aims to calculate and analyze the spatial and temporal variations in the groundwater flow quantity in Nam Co Lake based on the water balance principle. The results show that a large amount of groundwater was gradually lost and that, groundwater loss decreased from 1.9 billion m3 to 1.5 billion m3 from the period of 1980–1984 to 1995–2009. The comparative analysis in the current study indicates that the decrease in the groundwater index has a strong linear relationship with the temperature of the ground surface on the Tibetan Plateau, with a correlation coefficient as high as 0.92. Moreover, environmental variations such as large-scale engineering construction projects and increases in water storage may have played dominant roles in the sudden changes in the water quantities of plateau lakes (e.g., Nam Co Lake) during the periods of 1990–1995 and 2000–2009. The increased water levels resulted in reduced groundwater losses, which may lead to the substantial expansion or gradual shrinkage of the Qinghai–Tibet Plateau lakes over short periods of time. The results of this study provide an important reference for studying the mechanisms of lake water level changes on the Qinghai–Tibet Plateau.http://www.mdpi.com/2073-4441/10/7/941Nam Co Lakegroundwater lossenvironmental variationwater level change mechanismQinghai–Tibet Plateau
collection DOAJ
language English
format Article
sources DOAJ
author Yan Du
Zhide Huang
Mowen Xie
Asim Farooq
Chen Chen
spellingShingle Yan Du
Zhide Huang
Mowen Xie
Asim Farooq
Chen Chen
Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
Water
Nam Co Lake
groundwater loss
environmental variation
water level change mechanism
Qinghai–Tibet Plateau
author_facet Yan Du
Zhide Huang
Mowen Xie
Asim Farooq
Chen Chen
author_sort Yan Du
title Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
title_short Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
title_full Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
title_fullStr Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
title_full_unstemmed Temporal Variations in the Quantity of Groundwater Flow in Nam Co Lake
title_sort temporal variations in the quantity of groundwater flow in nam co lake
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-07-01
description This paper aims to calculate and analyze the spatial and temporal variations in the groundwater flow quantity in Nam Co Lake based on the water balance principle. The results show that a large amount of groundwater was gradually lost and that, groundwater loss decreased from 1.9 billion m3 to 1.5 billion m3 from the period of 1980–1984 to 1995–2009. The comparative analysis in the current study indicates that the decrease in the groundwater index has a strong linear relationship with the temperature of the ground surface on the Tibetan Plateau, with a correlation coefficient as high as 0.92. Moreover, environmental variations such as large-scale engineering construction projects and increases in water storage may have played dominant roles in the sudden changes in the water quantities of plateau lakes (e.g., Nam Co Lake) during the periods of 1990–1995 and 2000–2009. The increased water levels resulted in reduced groundwater losses, which may lead to the substantial expansion or gradual shrinkage of the Qinghai–Tibet Plateau lakes over short periods of time. The results of this study provide an important reference for studying the mechanisms of lake water level changes on the Qinghai–Tibet Plateau.
topic Nam Co Lake
groundwater loss
environmental variation
water level change mechanism
Qinghai–Tibet Plateau
url http://www.mdpi.com/2073-4441/10/7/941
work_keys_str_mv AT yandu temporalvariationsinthequantityofgroundwaterflowinnamcolake
AT zhidehuang temporalvariationsinthequantityofgroundwaterflowinnamcolake
AT mowenxie temporalvariationsinthequantityofgroundwaterflowinnamcolake
AT asimfarooq temporalvariationsinthequantityofgroundwaterflowinnamcolake
AT chenchen temporalvariationsinthequantityofgroundwaterflowinnamcolake
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