Using stable isotopes to investigate differences of plant water sources in subalpine habitats
Located along the northeastern edge of the Qinghai‐Tibet Plateau in China, the Qilian Mountains are an important ecological barrier in Northwest China. Therefore, it is of great significance to study the plant water sources in subalpine habitats for understanding the ecological and hydrological proc...
Gespeichert in:
Veröffentlicht in: | Hydrological processes 2022-02, Vol.36 (2), p.n/a |
---|---|
Hauptverfasser: | , , , , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | n/a |
---|---|
container_issue | 2 |
container_start_page | |
container_title | Hydrological processes |
container_volume | 36 |
creator | Zhang, Fuhua Jia, Wenxiong Zhu, Guofeng Zhang, Zhiyuan Shi, Yang Yang, Le Xiong, Hui Zhang, Miaomiao |
description | Located along the northeastern edge of the Qinghai‐Tibet Plateau in China, the Qilian Mountains are an important ecological barrier in Northwest China. Therefore, it is of great significance to study the plant water sources in subalpine habitats for understanding the ecological and hydrological processes in the Qilian Mountains. Here, based on the samples of precipitation, xylem water, soil water, river water, and spring water collected during May–October 2019 from subalpine habitats on the northern slope of the Qilian Mountains and the measured hydrogen and oxygen stable isotope values (δ2H and δ18O, respectively), the present study gained further insight into plant water sources in this region using the IsoSource model. Water absorption characteristics of shrubs were similar in subalpine habitats. Specifically, plants absorbed water primarily from the topsoil layer (0–30 cm) and rarely from the deep soil layers. Nevertheless, in the dry and growing seasons with high water demand, subalpine shrubs competed for water resources at similar depths. As a result of this competition, the utilization rate of deep soil water improved in some shrubs, expanding the differences in water sources of subalpine shrubs within the same habitat. In addition, in the dry and growing seasons, the water sources of the same subalpine shrub varied across different habitats. Compared with other subalpine shrubs, Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. could alter their water use strategies with variations in water conditions, exhibiting a greater drought tolerance. These findings provide valuable information for understanding the subalpine region's eco‐hydrological processes and contribute to the selection of suitable species for the restoration of the subalpine ecological environment under the background of global change.
Subalpine shrubs absorbed water primarily from the topsoil layer (0–30 cm).
Water use of subalpine shrubs varies with seasons. In the dry and growing seasons with high water demand, the main water source of some subalpine shrubs was switched to soil water at >30 cm.
Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. exhibiting a greater drought tolerance. |
doi_str_mv | 10.1002/hyp.14518 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2632189508</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2632189508</sourcerecordid><originalsourceid>FETCH-LOGICAL-a3208-fa6971fab7f4fe707defa62cad98e6c5a942c0c7d5993d3887566c44c5088da13</originalsourceid><addsrcrecordid>eNp1kE1LAzEQhoMoWD8O_oOAJw_bTvYryVGKWqGgB3vwICGbTdqUdbMmqaX_3tT16mngnWdm3nkRuiEwJQD5bHMYpqSsCDtBEwKcZwRYdYomwFiV1cDoOboIYQsAJTCYoI9VsP0ahyibTmMbXHSDDjg6bPtvHaJdy6hxa43RXvcqtZzBQyf7iPep43FwO3-UbY_DrpHdYHuNN7KxUcZwhc6M7IK-_quXaPX48DZfZMuXp-f5_TKTRQ4sM7LmlBjZUFMaTYG2Okm5ki1nulaV5GWuQNG24rxoC8ZoVdeqLFWV3molKS7R7bh38O5rl2yLbbLVp5Mir4ucMJ7IRN2NlPIuBK-NGLz9lP4gCIhjeiKlJ37TS-xsZPe204f_QbF4fx0nfgBLlHKr</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2632189508</pqid></control><display><type>article</type><title>Using stable isotopes to investigate differences of plant water sources in subalpine habitats</title><source>Wiley Online Library Journals Frontfile Complete</source><creator>Zhang, Fuhua ; Jia, Wenxiong ; Zhu, Guofeng ; Zhang, Zhiyuan ; Shi, Yang ; Yang, Le ; Xiong, Hui ; Zhang, Miaomiao</creator><creatorcontrib>Zhang, Fuhua ; Jia, Wenxiong ; Zhu, Guofeng ; Zhang, Zhiyuan ; Shi, Yang ; Yang, Le ; Xiong, Hui ; Zhang, Miaomiao</creatorcontrib><description>Located along the northeastern edge of the Qinghai‐Tibet Plateau in China, the Qilian Mountains are an important ecological barrier in Northwest China. Therefore, it is of great significance to study the plant water sources in subalpine habitats for understanding the ecological and hydrological processes in the Qilian Mountains. Here, based on the samples of precipitation, xylem water, soil water, river water, and spring water collected during May–October 2019 from subalpine habitats on the northern slope of the Qilian Mountains and the measured hydrogen and oxygen stable isotope values (δ2H and δ18O, respectively), the present study gained further insight into plant water sources in this region using the IsoSource model. Water absorption characteristics of shrubs were similar in subalpine habitats. Specifically, plants absorbed water primarily from the topsoil layer (0–30 cm) and rarely from the deep soil layers. Nevertheless, in the dry and growing seasons with high water demand, subalpine shrubs competed for water resources at similar depths. As a result of this competition, the utilization rate of deep soil water improved in some shrubs, expanding the differences in water sources of subalpine shrubs within the same habitat. In addition, in the dry and growing seasons, the water sources of the same subalpine shrub varied across different habitats. Compared with other subalpine shrubs, Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. could alter their water use strategies with variations in water conditions, exhibiting a greater drought tolerance. These findings provide valuable information for understanding the subalpine region's eco‐hydrological processes and contribute to the selection of suitable species for the restoration of the subalpine ecological environment under the background of global change.
Subalpine shrubs absorbed water primarily from the topsoil layer (0–30 cm).
Water use of subalpine shrubs varies with seasons. In the dry and growing seasons with high water demand, the main water source of some subalpine shrubs was switched to soil water at >30 cm.
Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. exhibiting a greater drought tolerance.</description><identifier>ISSN: 0885-6087</identifier><identifier>EISSN: 1099-1085</identifier><identifier>DOI: 10.1002/hyp.14518</identifier><language>eng</language><publisher>Hoboken, USA: John Wiley & Sons, Inc</publisher><subject>Drought ; Drought resistance ; Ecology ; Growing season ; Habitats ; Hydrogen ; Hydrologic processes ; Hydrology ; Hygroscopic water ; IsoSource model ; Isotopes ; Moisture content ; Mountains ; Oxygen ; Plant water ; plant water source ; Qilian Mountains ; Qinghai‐Tibet Plateau ; Restoration ; Rhododendron ; River water ; Rivers ; Shrubs ; Soil ; Soil improvement ; Soil layers ; Soil water ; Spring water ; stable isotope ; Stable isotopes ; subalpine shrub ; Topsoil ; Water absorption ; Water demand ; Water resources ; Water sources ; Water use ; Willow ; Xylem</subject><ispartof>Hydrological processes, 2022-02, Vol.36 (2), p.n/a</ispartof><rights>2022 John Wiley & Sons Ltd.</rights><rights>2022 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3208-fa6971fab7f4fe707defa62cad98e6c5a942c0c7d5993d3887566c44c5088da13</citedby><cites>FETCH-LOGICAL-a3208-fa6971fab7f4fe707defa62cad98e6c5a942c0c7d5993d3887566c44c5088da13</cites><orcidid>0000-0002-0069-4271</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fhyp.14518$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fhyp.14518$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27903,27904,45553,45554</link.rule.ids></links><search><creatorcontrib>Zhang, Fuhua</creatorcontrib><creatorcontrib>Jia, Wenxiong</creatorcontrib><creatorcontrib>Zhu, Guofeng</creatorcontrib><creatorcontrib>Zhang, Zhiyuan</creatorcontrib><creatorcontrib>Shi, Yang</creatorcontrib><creatorcontrib>Yang, Le</creatorcontrib><creatorcontrib>Xiong, Hui</creatorcontrib><creatorcontrib>Zhang, Miaomiao</creatorcontrib><title>Using stable isotopes to investigate differences of plant water sources in subalpine habitats</title><title>Hydrological processes</title><description>Located along the northeastern edge of the Qinghai‐Tibet Plateau in China, the Qilian Mountains are an important ecological barrier in Northwest China. Therefore, it is of great significance to study the plant water sources in subalpine habitats for understanding the ecological and hydrological processes in the Qilian Mountains. Here, based on the samples of precipitation, xylem water, soil water, river water, and spring water collected during May–October 2019 from subalpine habitats on the northern slope of the Qilian Mountains and the measured hydrogen and oxygen stable isotope values (δ2H and δ18O, respectively), the present study gained further insight into plant water sources in this region using the IsoSource model. Water absorption characteristics of shrubs were similar in subalpine habitats. Specifically, plants absorbed water primarily from the topsoil layer (0–30 cm) and rarely from the deep soil layers. Nevertheless, in the dry and growing seasons with high water demand, subalpine shrubs competed for water resources at similar depths. As a result of this competition, the utilization rate of deep soil water improved in some shrubs, expanding the differences in water sources of subalpine shrubs within the same habitat. In addition, in the dry and growing seasons, the water sources of the same subalpine shrub varied across different habitats. Compared with other subalpine shrubs, Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. could alter their water use strategies with variations in water conditions, exhibiting a greater drought tolerance. These findings provide valuable information for understanding the subalpine region's eco‐hydrological processes and contribute to the selection of suitable species for the restoration of the subalpine ecological environment under the background of global change.
Subalpine shrubs absorbed water primarily from the topsoil layer (0–30 cm).
Water use of subalpine shrubs varies with seasons. In the dry and growing seasons with high water demand, the main water source of some subalpine shrubs was switched to soil water at >30 cm.
Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. exhibiting a greater drought tolerance.</description><subject>Drought</subject><subject>Drought resistance</subject><subject>Ecology</subject><subject>Growing season</subject><subject>Habitats</subject><subject>Hydrogen</subject><subject>Hydrologic processes</subject><subject>Hydrology</subject><subject>Hygroscopic water</subject><subject>IsoSource model</subject><subject>Isotopes</subject><subject>Moisture content</subject><subject>Mountains</subject><subject>Oxygen</subject><subject>Plant water</subject><subject>plant water source</subject><subject>Qilian Mountains</subject><subject>Qinghai‐Tibet Plateau</subject><subject>Restoration</subject><subject>Rhododendron</subject><subject>River water</subject><subject>Rivers</subject><subject>Shrubs</subject><subject>Soil</subject><subject>Soil improvement</subject><subject>Soil layers</subject><subject>Soil water</subject><subject>Spring water</subject><subject>stable isotope</subject><subject>Stable isotopes</subject><subject>subalpine shrub</subject><subject>Topsoil</subject><subject>Water absorption</subject><subject>Water demand</subject><subject>Water resources</subject><subject>Water sources</subject><subject>Water use</subject><subject>Willow</subject><subject>Xylem</subject><issn>0885-6087</issn><issn>1099-1085</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LAzEQhoMoWD8O_oOAJw_bTvYryVGKWqGgB3vwICGbTdqUdbMmqaX_3tT16mngnWdm3nkRuiEwJQD5bHMYpqSsCDtBEwKcZwRYdYomwFiV1cDoOboIYQsAJTCYoI9VsP0ahyibTmMbXHSDDjg6bPtvHaJdy6hxa43RXvcqtZzBQyf7iPep43FwO3-UbY_DrpHdYHuNN7KxUcZwhc6M7IK-_quXaPX48DZfZMuXp-f5_TKTRQ4sM7LmlBjZUFMaTYG2Okm5ki1nulaV5GWuQNG24rxoC8ZoVdeqLFWV3molKS7R7bh38O5rl2yLbbLVp5Mir4ucMJ7IRN2NlPIuBK-NGLz9lP4gCIhjeiKlJ37TS-xsZPe204f_QbF4fx0nfgBLlHKr</recordid><startdate>202202</startdate><enddate>202202</enddate><creator>Zhang, Fuhua</creator><creator>Jia, Wenxiong</creator><creator>Zhu, Guofeng</creator><creator>Zhang, Zhiyuan</creator><creator>Shi, Yang</creator><creator>Yang, Le</creator><creator>Xiong, Hui</creator><creator>Zhang, Miaomiao</creator><general>John Wiley & Sons, Inc</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-0069-4271</orcidid></search><sort><creationdate>202202</creationdate><title>Using stable isotopes to investigate differences of plant water sources in subalpine habitats</title><author>Zhang, Fuhua ; Jia, Wenxiong ; Zhu, Guofeng ; Zhang, Zhiyuan ; Shi, Yang ; Yang, Le ; Xiong, Hui ; Zhang, Miaomiao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3208-fa6971fab7f4fe707defa62cad98e6c5a942c0c7d5993d3887566c44c5088da13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Drought</topic><topic>Drought resistance</topic><topic>Ecology</topic><topic>Growing season</topic><topic>Habitats</topic><topic>Hydrogen</topic><topic>Hydrologic processes</topic><topic>Hydrology</topic><topic>Hygroscopic water</topic><topic>IsoSource model</topic><topic>Isotopes</topic><topic>Moisture content</topic><topic>Mountains</topic><topic>Oxygen</topic><topic>Plant water</topic><topic>plant water source</topic><topic>Qilian Mountains</topic><topic>Qinghai‐Tibet Plateau</topic><topic>Restoration</topic><topic>Rhododendron</topic><topic>River water</topic><topic>Rivers</topic><topic>Shrubs</topic><topic>Soil</topic><topic>Soil improvement</topic><topic>Soil layers</topic><topic>Soil water</topic><topic>Spring water</topic><topic>stable isotope</topic><topic>Stable isotopes</topic><topic>subalpine shrub</topic><topic>Topsoil</topic><topic>Water absorption</topic><topic>Water demand</topic><topic>Water resources</topic><topic>Water sources</topic><topic>Water use</topic><topic>Willow</topic><topic>Xylem</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhang, Fuhua</creatorcontrib><creatorcontrib>Jia, Wenxiong</creatorcontrib><creatorcontrib>Zhu, Guofeng</creatorcontrib><creatorcontrib>Zhang, Zhiyuan</creatorcontrib><creatorcontrib>Shi, Yang</creatorcontrib><creatorcontrib>Yang, Le</creatorcontrib><creatorcontrib>Xiong, Hui</creatorcontrib><creatorcontrib>Zhang, Miaomiao</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Hydrological processes</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, Fuhua</au><au>Jia, Wenxiong</au><au>Zhu, Guofeng</au><au>Zhang, Zhiyuan</au><au>Shi, Yang</au><au>Yang, Le</au><au>Xiong, Hui</au><au>Zhang, Miaomiao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Using stable isotopes to investigate differences of plant water sources in subalpine habitats</atitle><jtitle>Hydrological processes</jtitle><date>2022-02</date><risdate>2022</risdate><volume>36</volume><issue>2</issue><epage>n/a</epage><issn>0885-6087</issn><eissn>1099-1085</eissn><abstract>Located along the northeastern edge of the Qinghai‐Tibet Plateau in China, the Qilian Mountains are an important ecological barrier in Northwest China. Therefore, it is of great significance to study the plant water sources in subalpine habitats for understanding the ecological and hydrological processes in the Qilian Mountains. Here, based on the samples of precipitation, xylem water, soil water, river water, and spring water collected during May–October 2019 from subalpine habitats on the northern slope of the Qilian Mountains and the measured hydrogen and oxygen stable isotope values (δ2H and δ18O, respectively), the present study gained further insight into plant water sources in this region using the IsoSource model. Water absorption characteristics of shrubs were similar in subalpine habitats. Specifically, plants absorbed water primarily from the topsoil layer (0–30 cm) and rarely from the deep soil layers. Nevertheless, in the dry and growing seasons with high water demand, subalpine shrubs competed for water resources at similar depths. As a result of this competition, the utilization rate of deep soil water improved in some shrubs, expanding the differences in water sources of subalpine shrubs within the same habitat. In addition, in the dry and growing seasons, the water sources of the same subalpine shrub varied across different habitats. Compared with other subalpine shrubs, Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. could alter their water use strategies with variations in water conditions, exhibiting a greater drought tolerance. These findings provide valuable information for understanding the subalpine region's eco‐hydrological processes and contribute to the selection of suitable species for the restoration of the subalpine ecological environment under the background of global change.
Subalpine shrubs absorbed water primarily from the topsoil layer (0–30 cm).
Water use of subalpine shrubs varies with seasons. In the dry and growing seasons with high water demand, the main water source of some subalpine shrubs was switched to soil water at >30 cm.
Salix cupularis Rehder, Salix oritrepha Schneid., Potentilla fruticosa L., Salix sclerophylla Anderss., Rhododendron anthopogonoides Maxim., and Rhododendron przewalskii Maxim. exhibiting a greater drought tolerance.</abstract><cop>Hoboken, USA</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1002/hyp.14518</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0002-0069-4271</orcidid></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0885-6087 |
ispartof | Hydrological processes, 2022-02, Vol.36 (2), p.n/a |
issn | 0885-6087 1099-1085 |
language | eng |
recordid | cdi_proquest_journals_2632189508 |
source | Wiley Online Library Journals Frontfile Complete |
subjects | Drought Drought resistance Ecology Growing season Habitats Hydrogen Hydrologic processes Hydrology Hygroscopic water IsoSource model Isotopes Moisture content Mountains Oxygen Plant water plant water source Qilian Mountains Qinghai‐Tibet Plateau Restoration Rhododendron River water Rivers Shrubs Soil Soil improvement Soil layers Soil water Spring water stable isotope Stable isotopes subalpine shrub Topsoil Water absorption Water demand Water resources Water sources Water use Willow Xylem |
title | Using stable isotopes to investigate differences of plant water sources in subalpine habitats |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T03%3A05%3A11IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Using%20stable%20isotopes%20to%20investigate%20differences%20of%20plant%20water%20sources%20in%20subalpine%20habitats&rft.jtitle=Hydrological%20processes&rft.au=Zhang,%20Fuhua&rft.date=2022-02&rft.volume=36&rft.issue=2&rft.epage=n/a&rft.issn=0885-6087&rft.eissn=1099-1085&rft_id=info:doi/10.1002/hyp.14518&rft_dat=%3Cproquest_cross%3E2632189508%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2632189508&rft_id=info:pmid/&rfr_iscdi=true |