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处理后废水灌溉对以色列土壤中溶解有机碳和土壤有机碳的影响。

Effects of treated wastewater irrigation on the dissolved and soil organic carbon in Israeli soils.

作者信息

Jueschke E, Marschner B, Tarchitzky J, Chen Y

机构信息

Department of Soil Science and Soil Ecology, Ruhr-University Bochum, Universitaetstr. 150, 44780 Bochum, Germany.

出版信息

Water Sci Technol. 2008;57(5):727-33. doi: 10.2166/wst.2008.173.

Abstract

In many arid and semi-arid regions, the demand for drinking water and other domestic uses is constantly growing due to demographic growth and increasing standard of living. Therefore, less freshwater is available for agricultural irrigation and new water sources are needed. Treated wastewater (TWW) already serves as an important water source in Israel since more than 40 years and its usage will further be extended. Related to its high loads with nutrients, salts and organic materials its use as irrigation water can have major effects on the soil physical, chemical and biological properties, in the worst case leading to soil degradation. Additional organic matter reaches the soil with the effluent water and soil microbial activity is stimulated. Soil organic carbon (SOC) seems to accumulate in the topsoil and tends to decrease after long-term irrigation with secondary TWW in the subsoil. The amount of dissolved organic carbon increased and the aromaticity of the organic compounds in the soil percolates decreased over the irrigation period. Priming effects, occurring after stimulation of microbial activity by the addition of easily degradable substances, could be found in the soils and were stronger for subsoil (1 m depth).

摘要

在许多干旱和半干旱地区,由于人口增长和生活水平提高,饮用水及其他生活用水的需求持续增长。因此,可用于农业灌溉的淡水减少,需要新的水源。经过处理的废水(TWW)40多年来一直是以色列的重要水源,其使用范围还将进一步扩大。由于其含有高负荷的养分、盐分和有机物质,用作灌溉水会对土壤的物理、化学和生物学性质产生重大影响,在最坏的情况下会导致土壤退化。额外的有机物质随出水进入土壤,刺激土壤微生物活性。土壤有机碳(SOC)似乎在表层土壤中积累,而在长期用二级处理废水灌溉底土后,土壤有机碳含量趋于下降。在灌溉期间,土壤渗滤液中溶解有机碳的含量增加,有机化合物的芳香性降低。在向土壤中添加易降解物质刺激微生物活性后出现的激发效应在土壤中可以观察到,并且在底土(1米深度)中更为明显。

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