Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau

Climate warming has significantly changed the hydrological cycle in cold regions, especially in areas with permafrost or seasonal frost. Groundwater flow and its interactions with surface water are essential components of the hydrological process. However, few studies or modeling works have been bas...

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Published in:Earth System Science Data
Main Authors: Z. Pan, R. Ma, Z. Sun, Y. Hu, Q. Chang, M. Ge, S. Wang, J. Bu, X. Long, Y. Pan, L. Zhao
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/essd-14-2147-2022
https://essd.copernicus.org/articles/14/2147/2022/essd-14-2147-2022.pdf
https://doaj.org/article/3380ac94638f4977af5b2e1874776736
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author Z. Pan
R. Ma
Z. Sun
Y. Hu
Q. Chang
M. Ge
S. Wang
J. Bu
X. Long
Y. Pan
L. Zhao
author_facet Z. Pan
R. Ma
Z. Sun
Y. Hu
Q. Chang
M. Ge
S. Wang
J. Bu
X. Long
Y. Pan
L. Zhao
author_sort Z. Pan
collection Unknown
container_issue 5
container_start_page 2147
container_title Earth System Science Data
container_volume 14
description Climate warming has significantly changed the hydrological cycle in cold regions, especially in areas with permafrost or seasonal frost. Groundwater flow and its interactions with surface water are essential components of the hydrological process. However, few studies or modeling works have been based on long-term field observations of groundwater level, temperature, hydrogeochemistry, or isotopic tracers from boreholes due to obstacles such as remote locations, limited infrastructure, and harsh work conditions. In the Hulugou catchment, an alpine catchment in the headwater region of the Heihe River on the northern Qinghai–Tibet Plateau (QTP), we drilled four sets of depth-specific wells and monitored the groundwater levels and temperatures at different depths. Surface water (including river water, glacier meltwater, and snow meltwater), precipitation, groundwater from boreholes, spring water, and soil water were sampled to measure the abundances of major and minor elements, dissolved organic carbon (DOC), and stable and radioactive isotopes at 64 sites. This study provides a dataset of these groundwater parameters spanning 6 consecutive years of monitoring/measurements. These data can be used to investigate groundwater flow processes and groundwater–surface water interactions on the QTP under global climate change. The dataset provided in this paper can be obtained at https://doi.org/10.5281/zenodo.6296057 (Ma et al., 2021b) and will be subject to further updates.
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:3380ac94638f4977af5b2e1874776736 2025-01-17T00:16:48+00:00 Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau Z. Pan R. Ma Z. Sun Y. Hu Q. Chang M. Ge S. Wang J. Bu X. Long Y. Pan L. Zhao 2022-05-01 https://doi.org/10.5194/essd-14-2147-2022 https://essd.copernicus.org/articles/14/2147/2022/essd-14-2147-2022.pdf https://doaj.org/article/3380ac94638f4977af5b2e1874776736 en eng Copernicus Publications doi:10.5194/essd-14-2147-2022 1866-3508 1866-3516 https://essd.copernicus.org/articles/14/2147/2022/essd-14-2147-2022.pdf https://doaj.org/article/3380ac94638f4977af5b2e1874776736 undefined Earth System Science Data, Vol 14, Pp 2147-2165 (2022) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.5194/essd-14-2147-2022 2023-01-22T18:19:44Z Climate warming has significantly changed the hydrological cycle in cold regions, especially in areas with permafrost or seasonal frost. Groundwater flow and its interactions with surface water are essential components of the hydrological process. However, few studies or modeling works have been based on long-term field observations of groundwater level, temperature, hydrogeochemistry, or isotopic tracers from boreholes due to obstacles such as remote locations, limited infrastructure, and harsh work conditions. In the Hulugou catchment, an alpine catchment in the headwater region of the Heihe River on the northern Qinghai–Tibet Plateau (QTP), we drilled four sets of depth-specific wells and monitored the groundwater levels and temperatures at different depths. Surface water (including river water, glacier meltwater, and snow meltwater), precipitation, groundwater from boreholes, spring water, and soil water were sampled to measure the abundances of major and minor elements, dissolved organic carbon (DOC), and stable and radioactive isotopes at 64 sites. This study provides a dataset of these groundwater parameters spanning 6 consecutive years of monitoring/measurements. These data can be used to investigate groundwater flow processes and groundwater–surface water interactions on the QTP under global climate change. The dataset provided in this paper can be obtained at https://doi.org/10.5281/zenodo.6296057 (Ma et al., 2021b) and will be subject to further updates. Article in Journal/Newspaper permafrost Unknown Earth System Science Data 14 5 2147 2165
spellingShingle geo
envir
Z. Pan
R. Ma
Z. Sun
Y. Hu
Q. Chang
M. Ge
S. Wang
J. Bu
X. Long
Y. Pan
L. Zhao
Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title_full Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title_fullStr Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title_full_unstemmed Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title_short Integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern Qinghai–Tibet Plateau
title_sort integrated hydrogeological and hydrogeochemical dataset of an alpine catchment in the northern qinghai–tibet plateau
topic geo
envir
topic_facet geo
envir
url https://doi.org/10.5194/essd-14-2147-2022
https://essd.copernicus.org/articles/14/2147/2022/essd-14-2147-2022.pdf
https://doaj.org/article/3380ac94638f4977af5b2e1874776736