Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China
Purpose Understanding the characteristics of soil infiltration response to rainfall is critical for soil water transport processes and hydrologic modeling. However, little is known about how they vary with forest conversion at different temporal stages (
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| Veröffentlicht in: | Journal of soils and sediments 2024, Vol.24 (1), p.1-16 |
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| creator | Lu, Shiguo Liu, Muxing Yi, Jun Zhang, Hailin Wang, Weijie Wan, Jinhong |
| description | Purpose
Understanding the characteristics of soil infiltration response to rainfall is critical for soil water transport processes and hydrologic modeling. However, little is known about how they vary with forest conversion at different temporal stages ( |
| doi_str_mv | 10.1007/s11368-023-03599-4 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2913296727</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3153549921</sourcerecordid><originalsourceid>FETCH-LOGICAL-c352t-b55d4e4774e6eb8bd2ad8e2ed5fd7ca4ede0554cd55236c57b389313fb36bb523</originalsourceid><addsrcrecordid>eNp9kc1q3TAQhU1JoEmaF8hK0E02TvVr2ctySZNCoJt2LWRpnKugSO5IDuQd-tDV7Q0UuuhqhpnvnBk4XXfF6A2jVH8qjIlh7CkXPRVqmnr5rjtjA5O9liM9ab0UU08ZHd9356U8USp0W591v3Z7i9ZVwFBqcIXkhZQcIglpCbGirSEnglDWnAqQmgnatrLxQBAflgUQUo2vxOX0AljBkyU3vpJ9iLHEvEI5oLbZbnUPmEjZ5op5Dc5GYhHs4eZuH5L90J025wKXb_Wi-_Hl9vvuvn_4dvd19_mhd0Lx2s9KeQlSawkDzOPsufUjcPBq8dpZCR6oUtJ5pbgYnNKzGCfBxDKLYZ7b7KK7PvqumH9u7VfzHIqDGG2CvBUjmBJKThNnDf34D_qUN0ztO8MnJvg0aK4bxY-Uw1wKwmJWDM8WXw2j5hCQOQZkWkDmT0BGNpE4ikqD0yPgX-v_qH4DfRyXEw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2913296727</pqid></control><display><type>article</type><title>Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China</title><source>Springer Nature - Complete Springer Journals</source><creator>Lu, Shiguo ; Liu, Muxing ; Yi, Jun ; Zhang, Hailin ; Wang, Weijie ; Wan, Jinhong</creator><creatorcontrib>Lu, Shiguo ; Liu, Muxing ; Yi, Jun ; Zhang, Hailin ; Wang, Weijie ; Wan, Jinhong</creatorcontrib><description>Purpose
Understanding the characteristics of soil infiltration response to rainfall is critical for soil water transport processes and hydrologic modeling. However, little is known about how they vary with forest conversion at different temporal stages (< 20 years) below the rooting zone. Therefore, this study aims to investigate soil infiltration response patterns in different subtropical forest conversion hillslopes, including mature original forest (thick root), young secondary forest (middle root), and very young secondary grassland (fine root), and analyzed the effects of environmental factors on the dynamics of soil infiltration.
Materials and methods
Several metrics were evaluated to characterize and quantify the nature of these responses by estimating changes in the soil water content, the response time difference between two adjacent soil depths, and infiltration velocities for 1144 infiltration events at 6 locations on the three hillslopes.
Results and discussion
Soil infiltration responses were similar on both forestland hillslopes, yet significantly different from those on the grassland hillslope. The preferential flow was more evident in the profile of thick-rooted vegetation, and the velocity of the wetting front was faster in the profiles of middle- and fine-rooted vegetation. Topography and root characteristics interact to influence soil infiltration response at the hillslope scale.
Conclusions
Conversion from thick-rooted forests into fine-rooted grasslands altered the rainfall-related soil infiltration dynamics below the rooting zone. In particular, the occurrence of preferential flow and infiltration rates varied, which helps enhance our understanding of ecohydrological processes in the context of changing land use and hydroclimatic conditions.</description><identifier>ISSN: 1439-0108</identifier><identifier>EISSN: 1614-7480</identifier><identifier>DOI: 10.1007/s11368-023-03599-4</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>China ; deforestation ; Earth and Environmental Science ; Ecohydrology ; Environment ; Environmental effects ; Environmental factors ; Environmental Physics ; fine roots ; forest land ; Forests ; Grasslands ; hydrologic cycle ; Hydrologic models ; Infiltration ; Infiltration rate ; Land use ; Moisture content ; Precipitation ; Preferential flow ; rain ; Rainfall ; Response time ; Rooting ; Sec 1 • Soil Organic Matter Dynamics and Nutrient Cycling • Research Article ; secondary forests ; Soil ; Soil depth ; Soil dynamics ; Soil infiltration ; Soil investigations ; Soil Science & Conservation ; Soil water ; soil water content ; soil water movement ; Soils ; topographic slope ; Transport processes ; Tropical forests ; Vegetation ; Water content ; Water transport ; Wetting front</subject><ispartof>Journal of soils and sediments, 2024, Vol.24 (1), p.1-16</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c352t-b55d4e4774e6eb8bd2ad8e2ed5fd7ca4ede0554cd55236c57b389313fb36bb523</citedby><cites>FETCH-LOGICAL-c352t-b55d4e4774e6eb8bd2ad8e2ed5fd7ca4ede0554cd55236c57b389313fb36bb523</cites><orcidid>0000-0003-0363-0692</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11368-023-03599-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11368-023-03599-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,777,781,27905,27906,41469,42538,51300</link.rule.ids></links><search><creatorcontrib>Lu, Shiguo</creatorcontrib><creatorcontrib>Liu, Muxing</creatorcontrib><creatorcontrib>Yi, Jun</creatorcontrib><creatorcontrib>Zhang, Hailin</creatorcontrib><creatorcontrib>Wang, Weijie</creatorcontrib><creatorcontrib>Wan, Jinhong</creatorcontrib><title>Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China</title><title>Journal of soils and sediments</title><addtitle>J Soils Sediments</addtitle><description>Purpose
Understanding the characteristics of soil infiltration response to rainfall is critical for soil water transport processes and hydrologic modeling. However, little is known about how they vary with forest conversion at different temporal stages (< 20 years) below the rooting zone. Therefore, this study aims to investigate soil infiltration response patterns in different subtropical forest conversion hillslopes, including mature original forest (thick root), young secondary forest (middle root), and very young secondary grassland (fine root), and analyzed the effects of environmental factors on the dynamics of soil infiltration.
Materials and methods
Several metrics were evaluated to characterize and quantify the nature of these responses by estimating changes in the soil water content, the response time difference between two adjacent soil depths, and infiltration velocities for 1144 infiltration events at 6 locations on the three hillslopes.
Results and discussion
Soil infiltration responses were similar on both forestland hillslopes, yet significantly different from those on the grassland hillslope. The preferential flow was more evident in the profile of thick-rooted vegetation, and the velocity of the wetting front was faster in the profiles of middle- and fine-rooted vegetation. Topography and root characteristics interact to influence soil infiltration response at the hillslope scale.
Conclusions
Conversion from thick-rooted forests into fine-rooted grasslands altered the rainfall-related soil infiltration dynamics below the rooting zone. In particular, the occurrence of preferential flow and infiltration rates varied, which helps enhance our understanding of ecohydrological processes in the context of changing land use and hydroclimatic conditions.</description><subject>China</subject><subject>deforestation</subject><subject>Earth and Environmental Science</subject><subject>Ecohydrology</subject><subject>Environment</subject><subject>Environmental effects</subject><subject>Environmental factors</subject><subject>Environmental Physics</subject><subject>fine roots</subject><subject>forest land</subject><subject>Forests</subject><subject>Grasslands</subject><subject>hydrologic cycle</subject><subject>Hydrologic models</subject><subject>Infiltration</subject><subject>Infiltration rate</subject><subject>Land use</subject><subject>Moisture content</subject><subject>Precipitation</subject><subject>Preferential flow</subject><subject>rain</subject><subject>Rainfall</subject><subject>Response time</subject><subject>Rooting</subject><subject>Sec 1 • Soil Organic Matter Dynamics and Nutrient Cycling • Research Article</subject><subject>secondary forests</subject><subject>Soil</subject><subject>Soil depth</subject><subject>Soil dynamics</subject><subject>Soil infiltration</subject><subject>Soil investigations</subject><subject>Soil Science & Conservation</subject><subject>Soil water</subject><subject>soil water content</subject><subject>soil water movement</subject><subject>Soils</subject><subject>topographic slope</subject><subject>Transport processes</subject><subject>Tropical forests</subject><subject>Vegetation</subject><subject>Water content</subject><subject>Water transport</subject><subject>Wetting front</subject><issn>1439-0108</issn><issn>1614-7480</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kc1q3TAQhU1JoEmaF8hK0E02TvVr2ctySZNCoJt2LWRpnKugSO5IDuQd-tDV7Q0UuuhqhpnvnBk4XXfF6A2jVH8qjIlh7CkXPRVqmnr5rjtjA5O9liM9ab0UU08ZHd9356U8USp0W591v3Z7i9ZVwFBqcIXkhZQcIglpCbGirSEnglDWnAqQmgnatrLxQBAflgUQUo2vxOX0AljBkyU3vpJ9iLHEvEI5oLbZbnUPmEjZ5op5Dc5GYhHs4eZuH5L90J025wKXb_Wi-_Hl9vvuvn_4dvd19_mhd0Lx2s9KeQlSawkDzOPsufUjcPBq8dpZCR6oUtJ5pbgYnNKzGCfBxDKLYZ7b7KK7PvqumH9u7VfzHIqDGG2CvBUjmBJKThNnDf34D_qUN0ztO8MnJvg0aK4bxY-Uw1wKwmJWDM8WXw2j5hCQOQZkWkDmT0BGNpE4ikqD0yPgX-v_qH4DfRyXEw</recordid><startdate>2024</startdate><enddate>2024</enddate><creator>Lu, Shiguo</creator><creator>Liu, Muxing</creator><creator>Yi, Jun</creator><creator>Zhang, Hailin</creator><creator>Wang, Weijie</creator><creator>Wan, Jinhong</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>H97</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M0K</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7S9</scope><scope>L.6</scope><orcidid>https://orcid.org/0000-0003-0363-0692</orcidid></search><sort><creationdate>2024</creationdate><title>Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China</title><author>Lu, Shiguo ; Liu, Muxing ; Yi, Jun ; Zhang, Hailin ; Wang, Weijie ; Wan, Jinhong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c352t-b55d4e4774e6eb8bd2ad8e2ed5fd7ca4ede0554cd55236c57b389313fb36bb523</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>China</topic><topic>deforestation</topic><topic>Earth and Environmental Science</topic><topic>Ecohydrology</topic><topic>Environment</topic><topic>Environmental effects</topic><topic>Environmental factors</topic><topic>Environmental Physics</topic><topic>fine roots</topic><topic>forest land</topic><topic>Forests</topic><topic>Grasslands</topic><topic>hydrologic cycle</topic><topic>Hydrologic models</topic><topic>Infiltration</topic><topic>Infiltration rate</topic><topic>Land use</topic><topic>Moisture content</topic><topic>Precipitation</topic><topic>Preferential flow</topic><topic>rain</topic><topic>Rainfall</topic><topic>Response time</topic><topic>Rooting</topic><topic>Sec 1 • Soil Organic Matter Dynamics and Nutrient Cycling • Research Article</topic><topic>secondary forests</topic><topic>Soil</topic><topic>Soil depth</topic><topic>Soil dynamics</topic><topic>Soil infiltration</topic><topic>Soil investigations</topic><topic>Soil Science & Conservation</topic><topic>Soil water</topic><topic>soil water content</topic><topic>soil water movement</topic><topic>Soils</topic><topic>topographic slope</topic><topic>Transport processes</topic><topic>Tropical forests</topic><topic>Vegetation</topic><topic>Water content</topic><topic>Water transport</topic><topic>Wetting front</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lu, Shiguo</creatorcontrib><creatorcontrib>Liu, Muxing</creatorcontrib><creatorcontrib>Yi, Jun</creatorcontrib><creatorcontrib>Zhang, Hailin</creatorcontrib><creatorcontrib>Wang, 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Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Journal of soils and sediments</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lu, Shiguo</au><au>Liu, Muxing</au><au>Yi, Jun</au><au>Zhang, Hailin</au><au>Wang, Weijie</au><au>Wan, Jinhong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China</atitle><jtitle>Journal of soils and sediments</jtitle><stitle>J Soils Sediments</stitle><date>2024</date><risdate>2024</risdate><volume>24</volume><issue>1</issue><spage>1</spage><epage>16</epage><pages>1-16</pages><issn>1439-0108</issn><eissn>1614-7480</eissn><abstract>Purpose
Understanding the characteristics of soil infiltration response to rainfall is critical for soil water transport processes and hydrologic modeling. However, little is known about how they vary with forest conversion at different temporal stages (< 20 years) below the rooting zone. Therefore, this study aims to investigate soil infiltration response patterns in different subtropical forest conversion hillslopes, including mature original forest (thick root), young secondary forest (middle root), and very young secondary grassland (fine root), and analyzed the effects of environmental factors on the dynamics of soil infiltration.
Materials and methods
Several metrics were evaluated to characterize and quantify the nature of these responses by estimating changes in the soil water content, the response time difference between two adjacent soil depths, and infiltration velocities for 1144 infiltration events at 6 locations on the three hillslopes.
Results and discussion
Soil infiltration responses were similar on both forestland hillslopes, yet significantly different from those on the grassland hillslope. The preferential flow was more evident in the profile of thick-rooted vegetation, and the velocity of the wetting front was faster in the profiles of middle- and fine-rooted vegetation. Topography and root characteristics interact to influence soil infiltration response at the hillslope scale.
Conclusions
Conversion from thick-rooted forests into fine-rooted grasslands altered the rainfall-related soil infiltration dynamics below the rooting zone. In particular, the occurrence of preferential flow and infiltration rates varied, which helps enhance our understanding of ecohydrological processes in the context of changing land use and hydroclimatic conditions.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11368-023-03599-4</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0003-0363-0692</orcidid></addata></record> |
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| subjects | China deforestation Earth and Environmental Science Ecohydrology Environment Environmental effects Environmental factors Environmental Physics fine roots forest land Forests Grasslands hydrologic cycle Hydrologic models Infiltration Infiltration rate Land use Moisture content Precipitation Preferential flow rain Rainfall Response time Rooting Sec 1 • Soil Organic Matter Dynamics and Nutrient Cycling • Research Article secondary forests Soil Soil depth Soil dynamics Soil infiltration Soil investigations Soil Science & Conservation Soil water soil water content soil water movement Soils topographic slope Transport processes Tropical forests Vegetation Water content Water transport Wetting front |
| title | Characteristics of soil infiltration response to rainfall in differently converted forest hillslopes in a southern subtropical area of China |
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