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Impacts of radiation, temperature and soil moisture on hidden heat of transpiration and leaf temperature of Quercus variabilis seedlings |
CHEN Jingling1, WANG Peishu1, LIU Linqi1, WANG Qian1, WANG Xu1, YANG Xitian1, ZHANG Jinsong2 |
1. College of Forestry, Henan Agricultural University, 450002, Zhengzhou, China; 2. Research Institute of Forestry, Chinese Academy of Forestry, 100091, Beijing, China |
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Abstract [Background] Drought threats plants' survival and in the same time it causes variation of their leaf temperature (TL), which provides people an efficient path to diagnose soil moisture. Many scholars have been using crop leaf-air temperature deficit (LATD) to calculate crop water stress index (CWSI). However, there are few studies on leaf-air temperature of Quercus variabilis, and no works on diagnose of soil moisture. The transpiration (Tr) of Q. variabilis is less than that of crops, and its LATD is larger than agricultural crop, thus the water stress index (WSI) of Q. variabilis should be different to CWSI. The key that uses LATD to evaluate water stress is to analyze the energy factors of leaf temperature. [Methods] Watering the pots then soil moisture decreased through natural evaporation, we controlled soil moisture in 3 levels: light drought, 12.5%-14.5% (W1); moderate drought, 9.5%-11.5% (W2), and severe drought, 5.5%-7.5% (W3). Selecting clear and cloudy days, from 8:00 to 18:00, we measured Tr and TL as well as air temperature (t) and solar radiation (R). We also measured Tr in artificial chamber controlling temperature at 25-43℃, at every 2℃interval of treating temperature. According to the ratio of net radiation ΔR, convection Φc, latent heat of transpiration LE, and leaf area density ρ, heat capacity Cp:ΔR/ρCp,Φc/ρCp,LE/ρCp ,we calculated the contribution of each energy item to TL. [Results] 1) The Tr of W1 was close to of normal soil moisture, the maximum Tr was 2.5 mmol/(m2·s). The Tr of W2 and W3 reduced to be <1.5 mmol/(m2·s). 2) In clear day, Tr positively related to solar radiation, which indicated that solar radiation was main factor of Tr. The slopes of the regression line between Tr and solar radiation were different with different soil moistures, the dryer the soil was, and the greater the slope was. 3) In cloudy day, the relation coefficient between Tr and solar radiation decreased clearly, which meant Tr did not decline with short time interval of radiation reducing, once transpiration started in the morning. 4) On any case of soil moisture, air temperature was not main factor of Tr. Though in artificial chamber the linear relation of Tr and temperature was clear, Tr was lower than natural clear day. [Conclusions] 1) Light drought did not impact Tr of Q. variabilis. 2) When wind speed was zero, solar radiation was main factor of leaf temperature variation. Net radiation accounted for 50%-70% of energy budget, and provided approximately 7℃ of leaf temperature variation. 3) The latent heat of Tr and convection heat exchange had an equal effect on energy budget, which accounted for 10%-20% respectively. Each of two factors caused approximately 1-2℃ of leaf temperature variation respectively.
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Received: 04 August 2016
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