Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China

Abstract The oxygen and hydrogen isotopic compositions (δ18O and δ2H) were measured on river water and precipitation collected from four sub-catchments within the upper Tuojiang River catchment. δ18O values of river water and precipitation exhibit significant seasonal variations. These seasonal vari...

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Main Authors: Jing Zhou, Guodong Liu, Yuchuan Meng, ChengCheng Xia, Ke Chen, Yu Chen
Format: Article
Language:English
Published: Nature Publishing Group 2021-02-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-82349-3
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spelling doaj-d808c9d52a054c9eabb9cbc1eb204d9c2021-02-07T12:33:30ZengNature Publishing GroupScientific Reports2045-23222021-02-0111111210.1038/s41598-021-82349-3Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, ChinaJing Zhou0Guodong Liu1Yuchuan Meng2ChengCheng Xia3Ke Chen4Yu Chen5State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan UniversityAbstract The oxygen and hydrogen isotopic compositions (δ18O and δ2H) were measured on river water and precipitation collected from four sub-catchments within the upper Tuojiang River catchment. δ18O values of river water and precipitation exhibit significant seasonal variations. These seasonal variations are used for estimating the mean residence time (MRT) for four sub-catchments by an exponential model, ranging from 346 to 493 days. The correlation between catchment MRT and mean slope of the catchment (r2 = 0.29) is weak, while the correlations between catchment MRT, catchment area (r2 = 0.79) and topographic index (r2 = 0.98) are strong. These results indicate that topography and catchment area, both control the catchment MRT and the topographic index may be a reliable parameter for estimating the catchment MRT. Moreover, the relationship between land use types and MRT was investigated. The results show that paddy fields (r2 = 0.95) compared to the other land use types may have a greater impact on the MRT of the irrigation-dominated catchment. This study provides a preliminary exploration of the factors affecting MRT in the plain region and a basis for simulating MRT in the future.https://doi.org/10.1038/s41598-021-82349-3
collection DOAJ
language English
format Article
sources DOAJ
author Jing Zhou
Guodong Liu
Yuchuan Meng
ChengCheng Xia
Ke Chen
Yu Chen
spellingShingle Jing Zhou
Guodong Liu
Yuchuan Meng
ChengCheng Xia
Ke Chen
Yu Chen
Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
Scientific Reports
author_facet Jing Zhou
Guodong Liu
Yuchuan Meng
ChengCheng Xia
Ke Chen
Yu Chen
author_sort Jing Zhou
title Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
title_short Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
title_full Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
title_fullStr Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
title_full_unstemmed Using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, Chengdu, China
title_sort using stable isotopes as tracer to investigate hydrological condition and estimate water residence time in a plain region, chengdu, china
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-02-01
description Abstract The oxygen and hydrogen isotopic compositions (δ18O and δ2H) were measured on river water and precipitation collected from four sub-catchments within the upper Tuojiang River catchment. δ18O values of river water and precipitation exhibit significant seasonal variations. These seasonal variations are used for estimating the mean residence time (MRT) for four sub-catchments by an exponential model, ranging from 346 to 493 days. The correlation between catchment MRT and mean slope of the catchment (r2 = 0.29) is weak, while the correlations between catchment MRT, catchment area (r2 = 0.79) and topographic index (r2 = 0.98) are strong. These results indicate that topography and catchment area, both control the catchment MRT and the topographic index may be a reliable parameter for estimating the catchment MRT. Moreover, the relationship between land use types and MRT was investigated. The results show that paddy fields (r2 = 0.95) compared to the other land use types may have a greater impact on the MRT of the irrigation-dominated catchment. This study provides a preliminary exploration of the factors affecting MRT in the plain region and a basis for simulating MRT in the future.
url https://doi.org/10.1038/s41598-021-82349-3
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