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首页> 外文期刊>Journal of Hydrology >Determining the independent impact of soil water on forest transpiration: A case study of a black locust plantation in the Loess Plateau, China
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Determining the independent impact of soil water on forest transpiration: A case study of a black locust plantation in the Loess Plateau, China

机译:确定土壤水对森林蒸腾的独立影响 - 以黄土高原黑蝗种植案例研究

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摘要

Transpiration (Tr) is influenced by environmental factors, vegetation properties, and anthropogenic management. The effect of environmental factors on Tr are taking place from two aspects: evaporative demand (i.e., potential evapotranspiration, PET) and water supply (i.e., soil water). Soil water is one of the most important factors that limit plant transpiration in terrestrial ecosystems, especially in semi-arid and arid regions. Investigating the relationship between Tr and soil water is crucial for an improved understanding of plant survival strategies and predicting hydrological cycles and water resources under climate change. Although the relationships of soil water and Tr have been widely studied, the independent effects of soil water on Tr are difficult to separate because soil water and PET occur concurrently under natural conditions. This study carried out field observations of sapflow density, meteorological factors and soil water in a black locust (Roblin:a pseudoacacia) plantation in the semi-arid Loess Plateau of China. This information was used to develop a model integrating the daily PET and relative extractable soil water (REW, an index that represents the available soil water): Tr = (0.27 x PET - 0.02 x PET2 - 0.32) x (1 - e(-5.70 x) (REW)). The model fitted the measured data well (R-2 = 0.65 and RMSE = 0.06 mm day(-1)). We found that the daily Tr increased as the REW increased under varying PET levels. Additionally, the independent effects of soil water on Tr were analysed using the factorial experiment analysis method. The REW was manipulated and PET varied naturally during the measurements to separate the independent effects of the REW on Tr. The results showed that Tr increased with the REW during the study period at a rate of 0.53 mm day(-1) per 0.1 REW when the REW < 0.4 and 0.09 mm day(-1) per 0.1 REW beyond the threshold (REW = 0.4). Tr increased by 27.3 mm (43.7%) compared to the controlled Tr (observed PET and lowest REW) due to the effect
机译:蒸腾(TR)受环境因素,植被性质和人体管理的影响。环境因素对TR的影响是从两个方面进行的:蒸发需求(即潜在的蒸散,宠物)和供水(即土壤水)。土壤水是限制陆地生态系统植物蒸腾的最重要因素之一,特别是在半干旱和干旱地区。调查TR和土壤水之间的关系对于改善对植物生存策略和预测气候变化下的水文循环和水资源的理解至关重要。虽然土壤水和TR的关系已被广泛研究,但土壤水对TR的独立影响难以分离,因为土壤水和PET在自然条件下同时发生。本研究在中国半干旱黄土高原中的黑色蝗虫(roblin:伪曲线)种植园中的露珠密度,气象因素和土壤水域进行了现场观察。这些信息用于开发一体化,整合日常宠物和相对可提取的土壤水(REW,代表可用土壤水的指数):TR =(0.27 x PET - 0.02 x PET2 - 0.32)x(1 - E( - 5.70 x)(REW))。该模型拟合测量数据阱(R-2 = 0.65和RMSE = 0.06mm(-1))。我们发现,随着REW在不同的宠物水平下增加,每日TR增加。另外,使用阶乘实验分析方法分析了土壤水对TR的独立影响。在测量期间,REW被操纵并宠物自然而然地改变,以分离REW对TR的独立效果。结果表明,当REW <0.09毫米(-1)每0.1 REW超出阈值时,每0.1 rew时,在研究时期的速率下,在研究时期以0.13mm的速度(-1)的速度,TR的速度增加了TR的速度(REW = 0.4 )。由于效果,TR增加27.3毫米(43.7%)(观察到的PET和最低REW)

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