Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China

Study region: The Urumqi River, nourished by glaciers in arid regions of northwest China, plays a crucial role in the economic, ecological, and social development of the region. Study focus: Water resource management in arid regions is a perennial concern, compounded by the complex interplay of fact...

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Main Authors: Siqi Wu, Fang Feng, Shuang Jin, Zhongqin Li, Michael A. Urban, Qiaohua Huang, Qiannian Shi
Format: Article
Language:English
Published: Elsevier 2025-02-01
Series:Journal of Hydrology: Regional Studies
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Online Access:http://www.sciencedirect.com/science/article/pii/S2214581824005238
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author Siqi Wu
Fang Feng
Shuang Jin
Zhongqin Li
Michael A. Urban
Qiaohua Huang
Qiannian Shi
author_facet Siqi Wu
Fang Feng
Shuang Jin
Zhongqin Li
Michael A. Urban
Qiaohua Huang
Qiannian Shi
author_sort Siqi Wu
collection DOAJ
description Study region: The Urumqi River, nourished by glaciers in arid regions of northwest China, plays a crucial role in the economic, ecological, and social development of the region. Study focus: Water resource management in arid regions is a perennial concern, compounded by the complex interplay of factors such as global warming and glacial response dynamics. Based on stable isotope and hydrochemistry data of 725 water samples, this study conducts a comprehensive analysis of the hydrochemical characteristics, runoff composition, and mean residence time of the Urumqi River Basin to enhance understanding of the hydrological processes of the river. New hydrological insights for the region: The hydrochemical type of river water is Calcium-Sulphate, with rock weathering as the main influence factor. Using the end-member mixing analysis (EMMA), it was calculated that the contribution ratios of ice and snow meltwater, atmospheric precipitation and groundwater to runoff were as follows: 3.81 %, 60.45 %, 35.75 % in spring; 28.99 %, 15.42 %, and 55.59 % in summer; and 22.72 %, 3.34 %, and 73.94 % in autumn. Based on the convolution integration method, the mean residence time (MRT) of water in the basin was calculated, and the result was 86 weeks (21.5months).
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publishDate 2025-02-01
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series Journal of Hydrology: Regional Studies
spelling doaj-art-6e2084386a9b42d4b0fd61e456e0058b2025-01-22T05:42:20ZengElsevierJournal of Hydrology: Regional Studies2214-58182025-02-0157102174Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest ChinaSiqi Wu0Fang Feng1Shuang Jin2Zhongqin Li3Michael A. Urban4Qiaohua Huang5Qiannian Shi6School of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, ChinaSchool of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, China; Correspondence to: Jiangsu Normal University, No. 101 Shanghai Road, Xuzhou, Jiangsu 221116, China.School of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, China; State Key Laboratory of Cryosphere Sciences/Tianshan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaState Key Laboratory of Cryosphere Sciences/Tianshan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaCollege of Arts and Science, Department of Geography, University of Missouri, Columbia, MO 65201, USASchool of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, ChinaSchool of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, China; State Key Laboratory of Cryosphere Sciences/Tianshan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaStudy region: The Urumqi River, nourished by glaciers in arid regions of northwest China, plays a crucial role in the economic, ecological, and social development of the region. Study focus: Water resource management in arid regions is a perennial concern, compounded by the complex interplay of factors such as global warming and glacial response dynamics. Based on stable isotope and hydrochemistry data of 725 water samples, this study conducts a comprehensive analysis of the hydrochemical characteristics, runoff composition, and mean residence time of the Urumqi River Basin to enhance understanding of the hydrological processes of the river. New hydrological insights for the region: The hydrochemical type of river water is Calcium-Sulphate, with rock weathering as the main influence factor. Using the end-member mixing analysis (EMMA), it was calculated that the contribution ratios of ice and snow meltwater, atmospheric precipitation and groundwater to runoff were as follows: 3.81 %, 60.45 %, 35.75 % in spring; 28.99 %, 15.42 %, and 55.59 % in summer; and 22.72 %, 3.34 %, and 73.94 % in autumn. Based on the convolution integration method, the mean residence time (MRT) of water in the basin was calculated, and the result was 86 weeks (21.5months).http://www.sciencedirect.com/science/article/pii/S2214581824005238The Urumqi RiverHydrochemistryStable isotopesRunoff compositionMean residence time
spellingShingle Siqi Wu
Fang Feng
Shuang Jin
Zhongqin Li
Michael A. Urban
Qiaohua Huang
Qiannian Shi
Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
Journal of Hydrology: Regional Studies
The Urumqi River
Hydrochemistry
Stable isotopes
Runoff composition
Mean residence time
title Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
title_full Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
title_fullStr Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
title_full_unstemmed Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
title_short Assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in Urumqi River Basin, northwest China
title_sort assessment of runoff composition and residence time using stable isotopes and hydrochemical characteristics in urumqi river basin northwest china
topic The Urumqi River
Hydrochemistry
Stable isotopes
Runoff composition
Mean residence time
url http://www.sciencedirect.com/science/article/pii/S2214581824005238
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