西北黄土高原林草植被蒸散消耗对自然降水的响应研究

Wang Fu, Sha Yan, He Qian, Zhao Qiang, Zhang He, Han Fen
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摘要

本文采用蒸散比(Ea/Q、Ep/Q)、蒸散差(Q-EA、Q-EP)和实际(潜在)供水比(1-Ea/Q、1-Ep/Q)3 类 6 个指标分析了西北黄土高原不同区域林草植被的蒸散平衡状况。它用于根据降水量客观反映不同类型植被在不同生长时期的适宜性。换句话说,这种适宜性反映了在黄土高原特定的气候环境下,自然降水对植被通过蒸腾作用消耗水分的支持能力。结果表明(1)该地区各类植被的实际蒸散耗水量在生长期的前三个月(4-6 月)明显增加,导致植被的水分干燥指数相对较高,平均 k 值为 0.44。主要原因是这一阶段自然降水较少,气温逐渐升高,大部分植被的蒸腾作用增强。森林的压力最大。5 月底 6 月初,随着自然降水量的增加,各类植被的平均 k 值开始下降。7 月至 9 月,由于该地区进入汛期,降水量急剧增加,水分干燥指数处于整个生长期的最低范围,平均 k 值在 0.26 至 0.30 之间变化,最低值为 8 月底 9 月初的 0.26。(2)森林的水分胁迫明显高于灌木和草地。这充分说明,植被类型的不同导致蒸腾作用的差异,从而导致不同植被类型实际蒸腾耗水量的差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Response of Evapotranspiration Consumption of Forest and Grass Vegetation to Natural Precipitation in Northwest Loess Plateau
In this paper, the evapotranspiration balance of forest and grass vegetation in the Loess Plateau of Northwest China in different regions was analyzed using 6 indexes in 3 categoriess, namely, evapotranspiration ratio (Ea/Q, Ep/Q), evapotranspiration difference (Q-EA, Q-EP), and actual (potential) water supply ratio (1-Ea/Q, 1-Ep/Q). It is used to objectively reflect the suitability of different types of vegetation in different periods of growth based on precipitation. In another words this suitability reflects the support capacity of natural rainfall to vegetation consumed water through evapotranspiration under the specific climate environment of the Loess Plateau. The results show that: (1) The actual evapotranspiration water consumption of all types of vegetation in this region increased significantly in the first three months of the growth period from April to June, resulting in a relatively high moisture dryness index of vegetation with an average k value of 0.44. The main reason was that natural precipitation was less at this stage, and the gradually rising temperature strengthened the transpiration of most vegetation. The forest was the most stressed. At the end of May and the beginning of June, with the increase of natural precipitation, the average k value of all types of vegetation began to decline. From July to September, due to the flood season in this region, the precipitation increased sharply, and the moisture dryness index was in the lowest range of the whole growth period, and the average k value varied between 0.26 and 0.30 with the lowest value was 0.26 at the end of August and the beginning of September. (2) It is obvious that the water stress of forest is higher than that of shrub and grassland. It is fully indicated that the difference of transpiration caused by the difference of vegetation types leads to the difference of actual evapotranspiration water consumption of different vegetation types.
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