Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China
Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characte...
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| Veröffentlicht in: | Hydrogeology journal 2018-08, Vol.26 (5), p.1693-1704 |
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| creator | Chen, Li Wang, Wenke Zhang, Zaiyong Wang, Zhoufeng Wang, Qiangmin Zhao, Ming Gong, Chengcheng |
| description | Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characteristics in arid regions, a field experiment was conducted in the Ordos Basin, central China, and high accuracy sensors of soil moisture, moisture potential and temperature were installed in three field soil profiles with water-table depths (WTDs) of about 0.4, 1.4 and 2.2 m. Soil-surface-evaporation values were estimated by observed data combined with Darcy’s law. Results showed that: (1) soil-surface-evaporation rate is linked to moisture content and it is also affected by air temperature. When there is sufficient moisture in the soil profile, soil evaporation increases with rising air temperature. For a WTD larger than the height of capillary rise, the soil evaporation is related to soil moisture content, and when air temperature is above 25 °C, the soil moisture content reduces quickly and the evaporation rate lowers; (2) phreatic water contributes to soil surface evaporation under conditions in which the WTD is within the capillary fringe. This indicates that phreatic water would not participate in soil evaporation for a WTD larger than the height of capillary rise. This finding developed further the understanding of phreatic evaporation, and this study provides valuable information on recognized soil evaporation processes in the arid environment. |
| doi_str_mv | 10.1007/s10040-018-1774-6 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_osti_</sourceid><recordid>TN_cdi_osti_scitechconnect_22780862</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2031621250</sourcerecordid><originalsourceid>FETCH-LOGICAL-a367t-578b79f1b6be7d7247f9684a8a5148164450191c75c5a105cbb56f3f670fb6753</originalsourceid><addsrcrecordid>eNp1kUtPAyEUhSdGE-vjB7gjcesol-ExXWpTH0mTbnRNYAYsTYUK1MaF_13GMXHl5nLD_c7JhVNVF4CvAWNxk0qluMbQ1iAErflBNQHasHLDxOFPDzUBQY-rk5TWuNAgmkn1NU_ZvansgkfBIq2iQSm4DTIfahviOLAhot5Za6LxGfVmm1dpoPcqm4iy0huDnEd5ZdDe-b7Wm7D3KCnfo-KnBnSYLWMfErpTyfkrNFs5r86qI6s2yZz_nqfVy_38efZYL5YPT7PbRa0aLnLNRKvF1ILm2oheECrslLdUtYoBbYFTyjBMoROsYwow67Rm3DaWC2w1F6w5rS5H31BeK1PnsulWXfDedFkSIlrccvJHbWN435mU5Trsoi-LSYIb4AQIw4WCkepiSCkaK7ex_GD8lIDlkIUcs5AlCzlkIXnRkFGTCutfTfxz_l_0DRhAisE</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2031621250</pqid></control><display><type>article</type><title>Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China</title><source>Springer Nature - Complete Springer Journals</source><creator>Chen, Li ; Wang, Wenke ; Zhang, Zaiyong ; Wang, Zhoufeng ; Wang, Qiangmin ; Zhao, Ming ; Gong, Chengcheng</creator><creatorcontrib>Chen, Li ; Wang, Wenke ; Zhang, Zaiyong ; Wang, Zhoufeng ; Wang, Qiangmin ; Zhao, Ming ; Gong, Chengcheng</creatorcontrib><description>Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characteristics in arid regions, a field experiment was conducted in the Ordos Basin, central China, and high accuracy sensors of soil moisture, moisture potential and temperature were installed in three field soil profiles with water-table depths (WTDs) of about 0.4, 1.4 and 2.2 m. Soil-surface-evaporation values were estimated by observed data combined with Darcy’s law. Results showed that: (1) soil-surface-evaporation rate is linked to moisture content and it is also affected by air temperature. When there is sufficient moisture in the soil profile, soil evaporation increases with rising air temperature. For a WTD larger than the height of capillary rise, the soil evaporation is related to soil moisture content, and when air temperature is above 25 °C, the soil moisture content reduces quickly and the evaporation rate lowers; (2) phreatic water contributes to soil surface evaporation under conditions in which the WTD is within the capillary fringe. This indicates that phreatic water would not participate in soil evaporation for a WTD larger than the height of capillary rise. This finding developed further the understanding of phreatic evaporation, and this study provides valuable information on recognized soil evaporation processes in the arid environment.</description><identifier>ISSN: 1431-2174</identifier><identifier>EISSN: 1435-0157</identifier><identifier>DOI: 10.1007/s10040-018-1774-6</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>ACCURACY ; AIR ; Air temperature ; Aquatic Pollution ; Arid environments ; Arid regions ; Arid zones ; CAPILLARIES ; CHINA ; Earth and Environmental Science ; Earth Sciences ; ECONOMICS ; EVAPORATION ; Evaporation rate ; Geology ; Geophysics/Geodesy ; GEOSCIENCES ; GROUND WATER ; Groundwater ; Groundwater levels ; Groundwater table ; Hydrogeology ; Hydrologic cycle ; Hydrological cycle ; HYDROLOGY ; Hydrology/Water Resources ; MOISTURE ; Moisture content ; MOISTURE GAGES ; Profiles ; SAND ; Soil ; Soil conditions ; Soil moisture ; Soil moisture content ; Soil profiles ; Soil properties ; Soil surfaces ; Soil temperature ; Soil water ; SOILS ; SOLAR RADIATION ; Surface temperature ; Temperature effects ; Vadose water ; Waste Water Technology ; Water content ; Water Management ; Water Pollution Control ; Water Quality/Water Pollution ; Water table ; WATER TABLES ; WIND</subject><ispartof>Hydrogeology journal, 2018-08, Vol.26 (5), p.1693-1704</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2018</rights><rights>Hydrogeology Journal is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a367t-578b79f1b6be7d7247f9684a8a5148164450191c75c5a105cbb56f3f670fb6753</citedby><cites>FETCH-LOGICAL-a367t-578b79f1b6be7d7247f9684a8a5148164450191c75c5a105cbb56f3f670fb6753</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10040-018-1774-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10040-018-1774-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>230,314,776,780,881,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/22780862$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Chen, Li</creatorcontrib><creatorcontrib>Wang, Wenke</creatorcontrib><creatorcontrib>Zhang, Zaiyong</creatorcontrib><creatorcontrib>Wang, Zhoufeng</creatorcontrib><creatorcontrib>Wang, Qiangmin</creatorcontrib><creatorcontrib>Zhao, Ming</creatorcontrib><creatorcontrib>Gong, Chengcheng</creatorcontrib><title>Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China</title><title>Hydrogeology journal</title><addtitle>Hydrogeol J</addtitle><description>Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characteristics in arid regions, a field experiment was conducted in the Ordos Basin, central China, and high accuracy sensors of soil moisture, moisture potential and temperature were installed in three field soil profiles with water-table depths (WTDs) of about 0.4, 1.4 and 2.2 m. Soil-surface-evaporation values were estimated by observed data combined with Darcy’s law. Results showed that: (1) soil-surface-evaporation rate is linked to moisture content and it is also affected by air temperature. When there is sufficient moisture in the soil profile, soil evaporation increases with rising air temperature. For a WTD larger than the height of capillary rise, the soil evaporation is related to soil moisture content, and when air temperature is above 25 °C, the soil moisture content reduces quickly and the evaporation rate lowers; (2) phreatic water contributes to soil surface evaporation under conditions in which the WTD is within the capillary fringe. This indicates that phreatic water would not participate in soil evaporation for a WTD larger than the height of capillary rise. This finding developed further the understanding of phreatic evaporation, and this study provides valuable information on recognized soil evaporation processes in the arid environment.</description><subject>ACCURACY</subject><subject>AIR</subject><subject>Air temperature</subject><subject>Aquatic Pollution</subject><subject>Arid environments</subject><subject>Arid regions</subject><subject>Arid zones</subject><subject>CAPILLARIES</subject><subject>CHINA</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>ECONOMICS</subject><subject>EVAPORATION</subject><subject>Evaporation rate</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>GEOSCIENCES</subject><subject>GROUND WATER</subject><subject>Groundwater</subject><subject>Groundwater levels</subject><subject>Groundwater table</subject><subject>Hydrogeology</subject><subject>Hydrologic cycle</subject><subject>Hydrological cycle</subject><subject>HYDROLOGY</subject><subject>Hydrology/Water Resources</subject><subject>MOISTURE</subject><subject>Moisture content</subject><subject>MOISTURE GAGES</subject><subject>Profiles</subject><subject>SAND</subject><subject>Soil</subject><subject>Soil conditions</subject><subject>Soil moisture</subject><subject>Soil moisture content</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>Soil surfaces</subject><subject>Soil temperature</subject><subject>Soil water</subject><subject>SOILS</subject><subject>SOLAR RADIATION</subject><subject>Surface temperature</subject><subject>Temperature effects</subject><subject>Vadose water</subject><subject>Waste Water Technology</subject><subject>Water content</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>Water Quality/Water Pollution</subject><subject>Water table</subject><subject>WATER 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evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China</title><author>Chen, Li ; Wang, Wenke ; Zhang, Zaiyong ; Wang, Zhoufeng ; Wang, Qiangmin ; Zhao, Ming ; Gong, Chengcheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a367t-578b79f1b6be7d7247f9684a8a5148164450191c75c5a105cbb56f3f670fb6753</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>ACCURACY</topic><topic>AIR</topic><topic>Air temperature</topic><topic>Aquatic Pollution</topic><topic>Arid environments</topic><topic>Arid regions</topic><topic>Arid zones</topic><topic>CAPILLARIES</topic><topic>CHINA</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>ECONOMICS</topic><topic>EVAPORATION</topic><topic>Evaporation rate</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>GEOSCIENCES</topic><topic>GROUND 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Basic</collection><collection>Environment Abstracts</collection><collection>OSTI.GOV</collection><jtitle>Hydrogeology journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Li</au><au>Wang, Wenke</au><au>Zhang, Zaiyong</au><au>Wang, Zhoufeng</au><au>Wang, Qiangmin</au><au>Zhao, Ming</au><au>Gong, Chengcheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China</atitle><jtitle>Hydrogeology journal</jtitle><stitle>Hydrogeol J</stitle><date>2018-08-01</date><risdate>2018</risdate><volume>26</volume><issue>5</issue><spage>1693</spage><epage>1704</epage><pages>1693-1704</pages><issn>1431-2174</issn><eissn>1435-0157</eissn><abstract>Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characteristics in arid regions, a field experiment was conducted in the Ordos Basin, central China, and high accuracy sensors of soil moisture, moisture potential and temperature were installed in three field soil profiles with water-table depths (WTDs) of about 0.4, 1.4 and 2.2 m. Soil-surface-evaporation values were estimated by observed data combined with Darcy’s law. Results showed that: (1) soil-surface-evaporation rate is linked to moisture content and it is also affected by air temperature. When there is sufficient moisture in the soil profile, soil evaporation increases with rising air temperature. For a WTD larger than the height of capillary rise, the soil evaporation is related to soil moisture content, and when air temperature is above 25 °C, the soil moisture content reduces quickly and the evaporation rate lowers; (2) phreatic water contributes to soil surface evaporation under conditions in which the WTD is within the capillary fringe. This indicates that phreatic water would not participate in soil evaporation for a WTD larger than the height of capillary rise. This finding developed further the understanding of phreatic evaporation, and this study provides valuable information on recognized soil evaporation processes in the arid environment.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10040-018-1774-6</doi><tpages>12</tpages></addata></record> |
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| subjects | ACCURACY AIR Air temperature Aquatic Pollution Arid environments Arid regions Arid zones CAPILLARIES CHINA Earth and Environmental Science Earth Sciences ECONOMICS EVAPORATION Evaporation rate Geology Geophysics/Geodesy GEOSCIENCES GROUND WATER Groundwater Groundwater levels Groundwater table Hydrogeology Hydrologic cycle Hydrological cycle HYDROLOGY Hydrology/Water Resources MOISTURE Moisture content MOISTURE GAGES Profiles SAND Soil Soil conditions Soil moisture Soil moisture content Soil profiles Soil properties Soil surfaces Soil temperature Soil water SOILS SOLAR RADIATION Surface temperature Temperature effects Vadose water Waste Water Technology Water content Water Management Water Pollution Control Water Quality/Water Pollution Water table WATER TABLES WIND |
| title | Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China |
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