Evaluation of Nitrogen Removal in a Soil Trench System after a 10-year Operation

T. Maekawa, Xiaohui Lei, H. Fujimaki, W. Bai
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Abstract

Many studies have confirmed the efficiency of soil trench systems; however, few have systematically studied the distributions of soil temperature, moisture content, and nitrogen in the profile of a soil trench system. In this study, the nitrogen removal in a soil trench system located in Sasagi (Tsukuba, Ibaraki, Japan) was evaluated by incorporating temperature and soil moisture content profile measurements. The results revealed that despite relatively small fluctuations, the soil temperatures at the top layer of soil (depth of 10cm) were greatly affected by air temperature; in comparison, the air temperature had little effect on the soil temperatures of soil layers at deep depth. A similar result was also obtained for soil moisture content, which was mainly affected by precipitation, evapotranspiration, etc. An investigation of the nitrogen distributions revealed a pattern similar to that obtained from the results of a previous simulation. Ammonia can be almost completely removed by using the soil trench system; however, some nitrates still remain in the effluent due to incomplete denitrification that might be caused by an insufficient carbon source.
土壤沟渠系统运行10年后氮去除效果评价
许多研究已经证实了土壤沟渠系统的有效性;然而,很少有人系统地研究土壤温度、水分含量和氮在土壤沟槽系统剖面中的分布。在这项研究中,通过结合温度和土壤含水量剖面测量,评估了位于佐佐木(Tsukuba, Ibaraki, Japan)的土壤沟渠系统的氮去除效果。结果表明:土壤表层(深度10cm)土壤温度受气温影响较大,但波动幅度较小;相比之下,气温对深层土层的土壤温度影响较小。土壤含水量也有类似的结果,主要受降水、蒸散等的影响。对氮分布的调查揭示了一种与先前模拟结果相似的模式。采用土壤沟槽系统可以几乎完全去除氨;然而,由于碳源不足可能导致的反硝化不完全,一些硝酸盐仍然留在流出物中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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