南非一些灌溉土壤有机质和养分含量的变化

C. D. Preez, G. Wiltshire
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引用次数: 17

摘要

耕种导致南非中部旱地土壤有机质含量无一例外地下降。问题是耕作如何影响这些地区灌溉土壤的有机质含量。因此,主要目的是量化耕作对三种灌溉方案土壤有机质含量的影响,以原始土壤为参考。从Riet河的7个地点、Ramah的8个地点和Vaalharts的6个地点取样了原始和耕作表土(0-200毫米)。每个灌溉方案的地点代表不同的耕种时期。土壤样品的粒径分布、pH、交换性Na、K、Mg和Ca、可提取P和Zn、CEC、有机C和全n含量在未开垦土壤和栽培土壤之间存在显著差异:随着栽培和灌溉,K、P和Zn含量降低,P和Zn含量增加。有机碳和全氮在7个站点显著增加,在6个站点显著降低。
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Changes in the organic matter and nutrient contents of some South African irrigated soils
Cultivation caused, without exception, a decline in the organic matter content of dryland soils in the central regions of South Africa. The question arose as to how cultivation affects the organic matter content of irrigated soils from these regions. The main aim, therefore, was to quantify the effect of cultivation on the organic matter content of soils from three irrigation schemes with virgin soils serving as reference. Virgin and cultivated topsoils (0–200 mm) were sampled from seven sites at Riet River, eight sites at Ramah and six sites at Vaalharts. The sites at each irrigation scheme represented varying periods of cultivation. Soil samples were analysed for particle size distribution, pH, exchangeable Na, K, Mg and Ca, extractable P and Zn, CEC, organic C and total N. The K, P and Zn contents differed significantly between virgin and cultivated soils: K decreased, while P and Zn increased with cultivation and irrigation. Organic C and total N significantly increased at seven sites and decreased at...
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