Biophysical control of whole tree transpiration under an urban environment in Northern China
► VPD was the major environmental influence on diurnal and nocturnal transpiration. ► Urban trees adopted a stronger stomatal control over transpiration. ► Deep water, time lag and nocturnal water uptake served to survive the water stress. ► Urban trees maintained stable transpiration across years o...
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description | ► VPD was the major environmental influence on diurnal and nocturnal transpiration. ► Urban trees adopted a stronger stomatal control over transpiration. ► Deep water, time lag and nocturnal water uptake served to survive the water stress. ► Urban trees maintained stable transpiration across years of contrasting rainfalls.
Urban reforestation in China has led to increasing debate about the impact of urban trees and forests on water resources. Although transpiration is the largest water flux leaving terrestrial ecosystems, little is known regarding whole tree transpiration in urban environments. In this study, we quantified urban tree transpiration at various temporal scales and examined the biophysical control of the transpiration pattern under different water conditions to understand how trees survive in an urban environment. Concurrent with microclimate and soil moisture measurements, transpiration from C
edrus deodara(Roxb)Loud
.,
Zelkova schneideriana Hend.-Mazz.,
Euonymus bungeanus Maxim., and
Metasequoia glyptostroboides Hu et cheng was measured over a 2-year period using thermal dissipation probe (TDP) techniques. The average monthly transpiration rates reached 12.78
±
0.73 (S.E.) mm, 1.79
±
0.16
mm, 10.18
±
0.55
mm and 19.28
±
2.24
mm for
C. deodara,
Z.schneideriana,
E. bungeanus and
M. glyptostroboides, respectively. Transpiration rates from
M. glyptostroboides reported here may need further study as this species showed much higher sap flows and greater transpiration fluctuation under different environmental conditions than other species. Because of deep soil moisture supply, summer dry spells did not reduce transpiration rates even when tree transpiration exceeded rainfall. While vapor pressure deficit (
VPD) was the dominant environmental factor on transpiration, trees controlled canopy conductance effectively to limit transpiration in times of water stress. Our results provide evidence that urban trees could adopt strong physiological control over transpiration under high evaporative demands to avoid dehydration and can make use of water in deeper soil layers to survive summer dry spells. Moreover, urban trees have the ability to make the best use of precipitation when it is limited, and are sensitive to soil and air dryness. |
doi_str_mv | 10.1016/j.jhydrol.2011.03.034 |
format | Article |
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Urban reforestation in China has led to increasing debate about the impact of urban trees and forests on water resources. Although transpiration is the largest water flux leaving terrestrial ecosystems, little is known regarding whole tree transpiration in urban environments. In this study, we quantified urban tree transpiration at various temporal scales and examined the biophysical control of the transpiration pattern under different water conditions to understand how trees survive in an urban environment. Concurrent with microclimate and soil moisture measurements, transpiration from C
edrus deodara(Roxb)Loud
.,
Zelkova schneideriana Hend.-Mazz.,
Euonymus bungeanus Maxim., and
Metasequoia glyptostroboides Hu et cheng was measured over a 2-year period using thermal dissipation probe (TDP) techniques. The average monthly transpiration rates reached 12.78
±
0.73 (S.E.) mm, 1.79
±
0.16
mm, 10.18
±
0.55
mm and 19.28
±
2.24
mm for
C. deodara,
Z.schneideriana,
E. bungeanus and
M. glyptostroboides, respectively. Transpiration rates from
M. glyptostroboides reported here may need further study as this species showed much higher sap flows and greater transpiration fluctuation under different environmental conditions than other species. Because of deep soil moisture supply, summer dry spells did not reduce transpiration rates even when tree transpiration exceeded rainfall. While vapor pressure deficit (
VPD) was the dominant environmental factor on transpiration, trees controlled canopy conductance effectively to limit transpiration in times of water stress. Our results provide evidence that urban trees could adopt strong physiological control over transpiration under high evaporative demands to avoid dehydration and can make use of water in deeper soil layers to survive summer dry spells. Moreover, urban trees have the ability to make the best use of precipitation when it is limited, and are sensitive to soil and air dryness.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2011.03.034</identifier><identifier>CODEN: JHYDA7</identifier><language>eng</language><publisher>Kidlington: Elsevier B.V</publisher><subject>canopy ; Canopy conductance ; Cedrus deodara ; China ; Decoupling coefficient ; Drying ; Earth sciences ; Earth, ocean, space ; environmental factors ; Environmental variables ; Euonymus hamiltonianus var. maackii ; Exact sciences and technology ; forest trees ; Hydrology. Hydrogeology ; Metasequoia glyptostroboides ; microclimate ; rain ; reforestation ; sap flow ; Soil (material) ; soil air ; Soil moisture ; soil water ; Summer ; Transpiration ; Trees ; Urban environments ; Urban tree ; vapor pressure ; water stress ; Zelkova</subject><ispartof>Journal of hydrology (Amsterdam), 2011-05, Vol.402 (3), p.388-400</ispartof><rights>2011 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a418t-a9c125e4c8538ba5913b8c376a762c94394f152000825dc586e525bb6c480dae3</citedby><cites>FETCH-LOGICAL-a418t-a9c125e4c8538ba5913b8c376a762c94394f152000825dc586e525bb6c480dae3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhydrol.2011.03.034$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>315,781,785,3551,27929,27930,46000</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24223335$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Chen, Lixin</creatorcontrib><creatorcontrib>Zhang, Zhiqiang</creatorcontrib><creatorcontrib>Li, Zhandong</creatorcontrib><creatorcontrib>Tang, Jianwu</creatorcontrib><creatorcontrib>Caldwell, Peter</creatorcontrib><creatorcontrib>Zhang, Wenjuan</creatorcontrib><title>Biophysical control of whole tree transpiration under an urban environment in Northern China</title><title>Journal of hydrology (Amsterdam)</title><description>► VPD was the major environmental influence on diurnal and nocturnal transpiration. ► Urban trees adopted a stronger stomatal control over transpiration. ► Deep water, time lag and nocturnal water uptake served to survive the water stress. ► Urban trees maintained stable transpiration across years of contrasting rainfalls.
Urban reforestation in China has led to increasing debate about the impact of urban trees and forests on water resources. Although transpiration is the largest water flux leaving terrestrial ecosystems, little is known regarding whole tree transpiration in urban environments. In this study, we quantified urban tree transpiration at various temporal scales and examined the biophysical control of the transpiration pattern under different water conditions to understand how trees survive in an urban environment. Concurrent with microclimate and soil moisture measurements, transpiration from C
edrus deodara(Roxb)Loud
.,
Zelkova schneideriana Hend.-Mazz.,
Euonymus bungeanus Maxim., and
Metasequoia glyptostroboides Hu et cheng was measured over a 2-year period using thermal dissipation probe (TDP) techniques. The average monthly transpiration rates reached 12.78
±
0.73 (S.E.) mm, 1.79
±
0.16
mm, 10.18
±
0.55
mm and 19.28
±
2.24
mm for
C. deodara,
Z.schneideriana,
E. bungeanus and
M. glyptostroboides, respectively. Transpiration rates from
M. glyptostroboides reported here may need further study as this species showed much higher sap flows and greater transpiration fluctuation under different environmental conditions than other species. Because of deep soil moisture supply, summer dry spells did not reduce transpiration rates even when tree transpiration exceeded rainfall. While vapor pressure deficit (
VPD) was the dominant environmental factor on transpiration, trees controlled canopy conductance effectively to limit transpiration in times of water stress. Our results provide evidence that urban trees could adopt strong physiological control over transpiration under high evaporative demands to avoid dehydration and can make use of water in deeper soil layers to survive summer dry spells. Moreover, urban trees have the ability to make the best use of precipitation when it is limited, and are sensitive to soil and air dryness.</description><subject>canopy</subject><subject>Canopy conductance</subject><subject>Cedrus deodara</subject><subject>China</subject><subject>Decoupling coefficient</subject><subject>Drying</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>environmental factors</subject><subject>Environmental variables</subject><subject>Euonymus hamiltonianus var. maackii</subject><subject>Exact sciences and technology</subject><subject>forest trees</subject><subject>Hydrology. Hydrogeology</subject><subject>Metasequoia glyptostroboides</subject><subject>microclimate</subject><subject>rain</subject><subject>reforestation</subject><subject>sap flow</subject><subject>Soil (material)</subject><subject>soil air</subject><subject>Soil moisture</subject><subject>soil water</subject><subject>Summer</subject><subject>Transpiration</subject><subject>Trees</subject><subject>Urban environments</subject><subject>Urban tree</subject><subject>vapor pressure</subject><subject>water stress</subject><subject>Zelkova</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LKzEUhoMoWD9-gpiNuJrefM5kVqJFvRfKdaHuhJDJnHFSpklNpkr_vSktbg2Hkyye8-bwIHRByZQSWv5ZTBf9po1hmDJC6ZTwXOIATaiq6oJVpDpEE0IYK2hZi2N0ktKC5MO5mKC3OxdW_SY5awZsgx9zDA4d_urDAHiMsG3Gp5WLZnTB47VvIWKTH7HJHfyni8EvwY_Yefw_xLGH6PGsd96coaPODAnO9_cpen24f5n9LeZPj_9mt_PCCKrGwtSWMgnCKslVY2RNeaMsr0pTlczWgteio5LllRWTrZWqBMlk05RWKNIa4Kfoepe7iuFjDWnUS5csDIPxENZJq5zDaaWqTModaWNIKUKnV9EtTdxoSvRWpl7ovUy9lakJzyXy3NX-B5OyqS4rsS79DDPBGOdcZu5yx3UmaPMeM_P6nIMEIbQqidgm3ewIyEI-HUSdrANvoXUR7Kjb4H7Z5RsKjpbX</recordid><startdate>20110525</startdate><enddate>20110525</enddate><creator>Chen, Lixin</creator><creator>Zhang, Zhiqiang</creator><creator>Li, Zhandong</creator><creator>Tang, Jianwu</creator><creator>Caldwell, Peter</creator><creator>Zhang, Wenjuan</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20110525</creationdate><title>Biophysical control of whole tree transpiration under an urban environment in Northern China</title><author>Chen, Lixin ; Zhang, Zhiqiang ; Li, Zhandong ; Tang, Jianwu ; Caldwell, Peter ; Zhang, Wenjuan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a418t-a9c125e4c8538ba5913b8c376a762c94394f152000825dc586e525bb6c480dae3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>canopy</topic><topic>Canopy conductance</topic><topic>Cedrus deodara</topic><topic>China</topic><topic>Decoupling coefficient</topic><topic>Drying</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>environmental factors</topic><topic>Environmental variables</topic><topic>Euonymus hamiltonianus var. maackii</topic><topic>Exact sciences and technology</topic><topic>forest trees</topic><topic>Hydrology. Hydrogeology</topic><topic>Metasequoia glyptostroboides</topic><topic>microclimate</topic><topic>rain</topic><topic>reforestation</topic><topic>sap flow</topic><topic>Soil (material)</topic><topic>soil air</topic><topic>Soil moisture</topic><topic>soil water</topic><topic>Summer</topic><topic>Transpiration</topic><topic>Trees</topic><topic>Urban environments</topic><topic>Urban tree</topic><topic>vapor pressure</topic><topic>water stress</topic><topic>Zelkova</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chen, Lixin</creatorcontrib><creatorcontrib>Zhang, Zhiqiang</creatorcontrib><creatorcontrib>Li, Zhandong</creatorcontrib><creatorcontrib>Tang, Jianwu</creatorcontrib><creatorcontrib>Caldwell, Peter</creatorcontrib><creatorcontrib>Zhang, Wenjuan</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Lixin</au><au>Zhang, Zhiqiang</au><au>Li, Zhandong</au><au>Tang, Jianwu</au><au>Caldwell, Peter</au><au>Zhang, Wenjuan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Biophysical control of whole tree transpiration under an urban environment in Northern China</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2011-05-25</date><risdate>2011</risdate><volume>402</volume><issue>3</issue><spage>388</spage><epage>400</epage><pages>388-400</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><abstract>► VPD was the major environmental influence on diurnal and nocturnal transpiration. ► Urban trees adopted a stronger stomatal control over transpiration. ► Deep water, time lag and nocturnal water uptake served to survive the water stress. ► Urban trees maintained stable transpiration across years of contrasting rainfalls.
Urban reforestation in China has led to increasing debate about the impact of urban trees and forests on water resources. Although transpiration is the largest water flux leaving terrestrial ecosystems, little is known regarding whole tree transpiration in urban environments. In this study, we quantified urban tree transpiration at various temporal scales and examined the biophysical control of the transpiration pattern under different water conditions to understand how trees survive in an urban environment. Concurrent with microclimate and soil moisture measurements, transpiration from C
edrus deodara(Roxb)Loud
.,
Zelkova schneideriana Hend.-Mazz.,
Euonymus bungeanus Maxim., and
Metasequoia glyptostroboides Hu et cheng was measured over a 2-year period using thermal dissipation probe (TDP) techniques. The average monthly transpiration rates reached 12.78
±
0.73 (S.E.) mm, 1.79
±
0.16
mm, 10.18
±
0.55
mm and 19.28
±
2.24
mm for
C. deodara,
Z.schneideriana,
E. bungeanus and
M. glyptostroboides, respectively. Transpiration rates from
M. glyptostroboides reported here may need further study as this species showed much higher sap flows and greater transpiration fluctuation under different environmental conditions than other species. Because of deep soil moisture supply, summer dry spells did not reduce transpiration rates even when tree transpiration exceeded rainfall. While vapor pressure deficit (
VPD) was the dominant environmental factor on transpiration, trees controlled canopy conductance effectively to limit transpiration in times of water stress. Our results provide evidence that urban trees could adopt strong physiological control over transpiration under high evaporative demands to avoid dehydration and can make use of water in deeper soil layers to survive summer dry spells. Moreover, urban trees have the ability to make the best use of precipitation when it is limited, and are sensitive to soil and air dryness.</abstract><cop>Kidlington</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2011.03.034</doi><tpages>13</tpages></addata></record> |
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subjects | canopy Canopy conductance Cedrus deodara China Decoupling coefficient Drying Earth sciences Earth, ocean, space environmental factors Environmental variables Euonymus hamiltonianus var. maackii Exact sciences and technology forest trees Hydrology. Hydrogeology Metasequoia glyptostroboides microclimate rain reforestation sap flow Soil (material) soil air Soil moisture soil water Summer Transpiration Trees Urban environments Urban tree vapor pressure water stress Zelkova |
title | Biophysical control of whole tree transpiration under an urban environment in Northern China |
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