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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Veröffentlicht in:Journal of hydrology (Amsterdam) 2011-05, Vol.402 (3), p.388-400
Hauptverfasser: Chen, Lixin, Zhang, Zhiqiang, Li, Zhandong, Tang, Jianwu, Caldwell, Peter, Zhang, Wenjuan
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container_issue 3
container_start_page 388
container_title Journal of hydrology (Amsterdam)
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creator Chen, Lixin
Zhang, Zhiqiang
Li, Zhandong
Tang, Jianwu
Caldwell, Peter
Zhang, Wenjuan
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
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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. 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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. 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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.</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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