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Extrapolation of Leaf Measurements to Obtain the Whole-Canopy Transpiration of C 3 and C 4 Xerophytic Shrubs

机译:外推叶片测量值以获得C 3和C 4旱生灌木的全冠层蒸腾作用。

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Quantifying the water balance within areas with sparse vegetation requires frequent measurement of transpiration in water-limited, arid, desert ecosystems. Field experiments were conducted in Shapotou, northwestern China, to examine the feasibility of up-scaling the transpiration of C 3 and C 4 xerophytic shrubs ( Reaumuria soongorica and Salsola passerina , respectively) from the leaf to the canopy level throughout the growing season in 2015. The large weighing lysimeter method and LI-6400XT portable photosynthesis system were used to make relatively long-term measurements of transpiration. The results indicated that meteorological factors coupled with stomatal conductance affected the transpiration rate of the two shrubs at the leaf level, and that the vapor pressure deficit other than net radiation and the air temperature affected the transpiration rate of S. passerina at the canopy level. Precipitation and vegetation characteristics determined the transpiration amount of the C 3 and C 4 xerophytic shrubs. The leaf gas exchange measurements were arithmetically scaled up to the canopy level based on the leaf area. The validity of the extrapolation was evaluated by comparing the upscale values of transpiration with the calculated values obtained from lysimeter measurement. The up-scaling approach accurately (±0.005 mm h ?1 , RMSE = 35%) obtained canopy transpiration from the leaf measurements. Our study suggests that the up-scaling method based on leaf area can be adopted to determine the canopy transpiration of C 3 and C 4 xerophytic shrubs in arid desert environments.
机译:要量化植被稀疏区域内的水平衡,就需要经常测量缺水,干旱,沙漠生态系统中的蒸腾作用。在中国西北部的沙坡头进行了田间试验,以研究将C 3和C 4旱生灌木(分别为Reaumuria wongorica和Salsola passerina)的蒸腾作用从叶扩展到冠层水平于2015年的可行性。 。使用大重量溶渗仪和LI-6400XT便携式光合作用系统对蒸腾作用进行相对长期的测量。结果表明,气象因素与气孔导度一起影响了两种灌木在叶片水平上的蒸腾速率,除净辐射外的蒸气压亏空和气温在冠层水平上影响过客链霉菌的蒸腾速率。降水和植被特征决定了C 3和C 4旱生灌木的蒸腾量。根据叶片面积算术地将叶片气体交换测量结果按比例放大到顶篷水平。通过将蒸腾作用的高档值与从溶渗仪测量获得的计算值进行比较,评估外推法的有效性。精确的放大方法(±0.005 mm h?1,RMSE = 35%)从叶片测量中获得了冠层蒸腾作用。我们的研究表明,可以采用基于叶面积的放大方法来确定干旱沙漠环境中C 3和C 4旱生灌木的冠层蒸腾作用。

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