坎特伯雷北部土壤的风蚀

G. G. Hunter, I. Lynn
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引用次数: 8

摘要

摘要:1981年4月17日和18日,在坎特伯雷北部的格拉斯内温土壤上,测量了一个过度钻孔和沉重滚动的围场在强烈的西北风下的土壤流失量。70吨/公顷的表土被运输并沉积在源围场下风侧的防风林的背风处。土壤在防风林迎风侧呈3 ×树高、背风侧呈7 ×树高的带状沉积。沙子大小的聚集体和颗粒构成了这种物质的大部分。风吹土壤含有高水平的植物养分,包括相当于73公斤过磷酸钙/公顷的有效磷。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wind erosion of a soil in north Canterbury
Abstract Measurements were made of soil loss from an overdrilled and heavy-rolled paddock supporting lucerne on a Glasnevin soil in north Canterbury during strong north-westerly winds on 17 and 18 April 1981. Seventy t/ha of topsoil was transported and deposited in the lee of a windbreak on the downwind side of the source paddock. Soil was deposited in a band extending 3 ✖ tree height on the windward side of the windbreak and 7 × tree height on the leeward side. Sand-sized aggregates and particles made up the bulk of this material. The wind-blown soil contained high levels of plant nutrients including available P equivalent to 73 kg of superphosphate/ha.
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