非饱和土带对区域水平衡的重要性

O. Nestroy
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引用次数: 2

摘要

在两个不同的地点:Marchfeld(维也纳盆地,海拔170 m,降水550 mm,年平均气温9.5°C)和Radstadter Tauern(萨尔茨堡国家,海拔1600 m),研究了土壤水分平衡,特别是非饱和土带的功能,入渗率。降水量1500 - 2000毫米,年平均气温2-5℃)。研究结果表明,人类活动的巨大影响——比如集约化农业或过度建造滑雪道——在积极意义上是指马尔奇菲尔德的可持续土地管理,而在消极意义上是指表土被破坏导致的水量减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The importance of unsaturated soil zone for the regional water balance
Abstract Studies of the soil water balance, especially the function of the unsaturated soil zone, infiltration rate was made on two very different sites: Marchfeld (Vienna basin, 170 m asl, 550 mm precipitation and 9.5°C mean annual temperature), and in the Radstadter Tauern (Country of Salzburg, 1600 m asl. 1500 – 2000 mm precipitation, 2–5°C mean annual temperature). The results demonstrate the big influence of human activity - like intensive agriculture or exaggerated creation of ski slopes - in positive sense: a sustainable land management in the Marchfeld, and negative sense: decrease of the water capacity due the destroying of the topsoil.
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