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Effects of conservation tillage on soil porosity in maize-wheat cropping system

机译:保护性耕作对玉米-小麦种植系统土壤孔隙度的影响

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A study was conducted on the effect of two single practices, including soil tillage and returning straw to soil, and their interaction on soil porosity of maize-wheat cropping system. Field experiments involved four tillage practices, including conventional tillage (C), zero-tillage (Z), harrow-tillage (H) and subsoil-tillage (S), with straw absent (A) or straw present (P). Total porosity, capillary porosity and non-capillary porosity of soil were investigated. The results showed that the soil total porosity of 0–10 soil layer was mostly affected; conventional tillage can increase the capillary porosity of soil, but the non-capillary porosity of S was the highest. Returning of straw can increase the porosity of soil. Through the analysis of affecting force, it can be concluded that interaction of soil tillage and straw is the most important factor to soil porosity, while the controlling factor to non-capillary porosity was soil tillage treatment.
机译:研究了两种耕作方式的影响,包括土壤耕作和秸秆还田以及它们对玉米-小麦种植系统土壤孔隙度的相互作用。田间试验涉及四种耕作实践,包括常规耕作(C),零耕作(Z),耙耕(H)和地下耕作(S),其中不存在稻草(A)或存在稻草(P)。研究了土壤的总孔隙度,毛细管孔隙度和非毛细管孔隙度。结果表明,0-10土层的土壤总孔隙度受到最大影响;常规耕作可增加土壤的毛细孔隙度,但S的非毛细孔隙度最高。秸秆还田会增加土壤的孔隙度。通过对影响力的分析,可以得出结论认为,耕作与秸秆的相互作用是影响土壤孔隙度的最重要因素,而对非毛管孔隙度的控制因素则是耕作处理。

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