The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China

Determining the age and sources of stream water is critical for understanding the watershed hydrological processes and biogeochemical cycle. In this study, daily isotope data of rainfall and runoff, as well as continuously monitored conductivity data from June to October in 2019 in-Laoyeling(LYL) wa...

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Published in:Frontiers in Earth Science
Main Authors: Xiao, Xiang, Cai, Tijiu, Duan, Liangliang
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2023
Subjects:
Online Access:http://dx.doi.org/10.3389/feart.2023.1225291
https://www.frontiersin.org/articles/10.3389/feart.2023.1225291/full
id crfrontiers:10.3389/feart.2023.1225291
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spelling crfrontiers:10.3389/feart.2023.1225291 2024-02-11T10:07:51+01:00 The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China Xiao, Xiang Cai, Tijiu Duan, Liangliang 2023 http://dx.doi.org/10.3389/feart.2023.1225291 https://www.frontiersin.org/articles/10.3389/feart.2023.1225291/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Earth Science volume 11 ISSN 2296-6463 General Earth and Planetary Sciences journal-article 2023 crfrontiers https://doi.org/10.3389/feart.2023.1225291 2024-01-26T10:02:29Z Determining the age and sources of stream water is critical for understanding the watershed hydrological processes and biogeochemical cycle. In this study, daily isotope data of rainfall and runoff, as well as continuously monitored conductivity data from June to October in 2019 in-Laoyeling(LYL) watershed located in permafrost region of northeastern China were used to separate streamflow components through the application of two independent methods: isotope-based hydrograph separations (IHS) and the conductivity mass balance (CMB) methods. The results showed that stream water in a boreal forest watershed with permafrost of the Daxing’an Mountains is mainly composed of pre-event water. Although the IHS method is more sensitive and provides more details than the CMB method, the results of both methods show a similar trend. The average value of the young water fractions (F yw ) for those aged less than 65 days is 5.6%, while the mean transit time (MTT) was calculated to be 3.33 years. These findings enhance our understanding of the fundamental characteristics of runoff generation mechanisms and changes in runoff components in permafrost regions. Such knowledge is crucial for effective regional water resource management under the context of climate change, such as construction of water conservancy facilities and prediction of flood and drought disasters. Article in Journal/Newspaper permafrost Frontiers (Publisher) Frontiers in Earth Science 11
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Xiao, Xiang
Cai, Tijiu
Duan, Liangliang
The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
topic_facet General Earth and Planetary Sciences
description Determining the age and sources of stream water is critical for understanding the watershed hydrological processes and biogeochemical cycle. In this study, daily isotope data of rainfall and runoff, as well as continuously monitored conductivity data from June to October in 2019 in-Laoyeling(LYL) watershed located in permafrost region of northeastern China were used to separate streamflow components through the application of two independent methods: isotope-based hydrograph separations (IHS) and the conductivity mass balance (CMB) methods. The results showed that stream water in a boreal forest watershed with permafrost of the Daxing’an Mountains is mainly composed of pre-event water. Although the IHS method is more sensitive and provides more details than the CMB method, the results of both methods show a similar trend. The average value of the young water fractions (F yw ) for those aged less than 65 days is 5.6%, while the mean transit time (MTT) was calculated to be 3.33 years. These findings enhance our understanding of the fundamental characteristics of runoff generation mechanisms and changes in runoff components in permafrost regions. Such knowledge is crucial for effective regional water resource management under the context of climate change, such as construction of water conservancy facilities and prediction of flood and drought disasters.
format Article in Journal/Newspaper
author Xiao, Xiang
Cai, Tijiu
Duan, Liangliang
author_facet Xiao, Xiang
Cai, Tijiu
Duan, Liangliang
author_sort Xiao, Xiang
title The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
title_short The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
title_full The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
title_fullStr The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
title_full_unstemmed The age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast China
title_sort age and sources of stream water in a boreal forest watershed in the permafrost region: a case study of a watershed in northeast china
publisher Frontiers Media SA
publishDate 2023
url http://dx.doi.org/10.3389/feart.2023.1225291
https://www.frontiersin.org/articles/10.3389/feart.2023.1225291/full
genre permafrost
genre_facet permafrost
op_source Frontiers in Earth Science
volume 11
ISSN 2296-6463
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/feart.2023.1225291
container_title Frontiers in Earth Science
container_volume 11
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