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Transpiration Rates of Carex Meyeriana in Relation to Micrometerological Factors in a Mountain Valley Wetland

Transpiration Rates of Carex Meyeriana in Relation to Micrometerological Factors in a Mountain Valley Wetland
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摘要 In order to reveal transpiration rates of wetland plants and its relationships to micro-meterological factors in a mountain valley wetland, relative humidity, air temperature, leaf temperature, soil temperature, photo flux density and transpiration rates were measured once two hours in a Carex meyeriana wetland of the Changbai Mountain valley in dry (July) and wet (September) of 2003, respectively. Results showed that the tendency of "decreasing after increasing" was obvious in wet season. However, a relatively stable trend was observed for the transpiration in dry season.. Generally, the photon flux density of Carex meyeriana was higher in wet season than that in dry season. However, the variabilities of leaf temperature, air temperature and relative humidity were similar in both seasons. Higher transpiration rates of Carex meyeriana leaves were observed in July (varied from 40 to 150 mol·m-2·s-1) compared to those (varied from 7 to 14 mol·m-2·s-1) in September. Transpiration rates were significantly correlated with air temperature (P<0.01), leaf temperature (P<0.01), and wind speed (P<0.05), but correlationship between relative humidity and photo flux density was not significant (P<0.05). In order to reveal transpiration rates of wetland plants and its relationships to micro- meterological factors in a mountain valley wetland, relative humidity, air temperature, leaf temperature, soil temperature, photo flux density and transpiration rates were measured once two hours in a Carex meyeriana wetland of the Changbai Mountain valley in dry (July) and wet (September) of 2003, respectively. Results showed that the tendency of "decreasing after increasing" was obvious in wet season. However, a relatively stable trend was observed for the transpiration in dry season.. Generally, the photon flux density of Carex meyeriana was higher in wet season than that in dry season. However, the variabilities of leaf temperature, air temperature and relative humidity were similar in both seasons. Higher transpiration rates of Carex meyeriana leaves were observed in July (varied from 40 to 150 mol.m^-2.s^-1) compared to those (varied from 7 to 14 mol.m^-2.s^-1) in September. Transpiration rates were significantly correlated with air temperature (P〈0.01), leaf temperature (P〈0.01), and wind speed (P〈0.05), but correlationship between relative humidity and photo flux density was not significant (P〈0.05).
出处 《Journal of Mountain Science》 SCIE CSCD 2009年第3期293-298,共6页 山地科学学报(英文)
基金 supported by the National Basic Research Program of China (No.2006CB403301) the National Natural Science Foundation Project (4) the Emphasis Project Fund of National Eleventh Five-Year Scientific and Technical Support Plans (No.2006BAB04A08)
关键词 叶片蒸腾速率 乌拉苔草 湿地植物 山谷 相对湿度 空气温度 通量密度 叶片温度 Micrometerological factors transpiretion rates Carex meyeriana mountain valley wetland
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