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Age-hardening phenomena in an oxisol from the subtropical region of Brazil

机译:巴西亚热带地区的oxisol年龄硬化现象

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Soil strength is not only affected by water content and bulk density, but also by the age-hardening phenomena, which plays a key role in increasing the soil strength as a function of time. It has been demonstrated that soil penetration resistance in no-tillage is higher when compared with other tillage systems at the same bulk density and water content. The objectives of this study was to investigate the effects of the age-hardening phenomena on soil penetration resistance in a long-term soil management system, running since 1988 in a very clayey Oxisol, in southern Brazil. Soil samples were collected from three soil layers (0.0-0.10 m; 0.10-0.20 m and 0.20-0.30 m) and five soil tillage systems: conventional tillage; minimum tillage with chiselling performed every year or every three years; and no-tillage for 11 or 24 years. Age-hardening was investigated using soil penetration resistance analysis and modelling. We used the area under the soil resistance to penetration curve to compare the age-hardening phenomena under the different tillage systems. For the same bulk density and water content, the soil resistance to penetration increased with time under no-tillage or without soil chiselling. For the same bulk density, no differences were found for macroporosity and microporosity Among the tillage systems. Higher soil penetration resistance values in long-term no-tillage at the same soil bulk density and water content were attributed to the age-hardening phenomena, which increased the number and strength of bonds among soil particles, leading to higher soil cohesion. It is necessary to establish critical limits of soil penetration resistance as a function of the soil tillage system, and the time without soil chiselling or under no-tillage system. (C) 2017 Elsevier B.V. All rights reserved.
机译:土壤强度不仅受水含量和散装密度的影响,而且由年龄硬化现象的影响,这在增加土壤强度作为时间的函数时起着关键作用。已经证明,与相同堆积密度和含水量的其他耕作系统相比,无耕作中的土壤渗透性较高。本研究的目的是调查长期土壤管理系统中硬化现象对长期土壤管理系统中的土壤渗透性的影响,自1988年在巴西南部的一个非常粘土的oxisol中运行。从三层土壤层收集土壤样品(0.0-0.10米; 0.10-0.20米和0.20-0.30米)和五种土壤耕作系统:常规耕作;每年或每三年进行烟道素的最小耕作;和耕作11或24年。使用土壤渗透性分析和建模研究了年龄硬化。我们在土壤抵抗下使用该地区渗透曲线,以比较不同耕作系统下的年龄硬化现象。对于相同的堆积密度和含水量,土壤抗性随着空中的时间而增加,或没有土壤烟道。对于相同的堆积密度,在耕作系统中没有发现巨孔率和微孔的差异。在相同的土壤堆积密度和水含量的长期无耕作中的土壤穿透性值较高,归因于硬化现象,这增加了土壤颗粒之间键的数量和强度,导致土壤粘合更高。必须根据土壤耕作系统的函数建立土壤渗透性抗性的关键限制,以及没有土壤烟道的时间或无耕作系统。 (c)2017 Elsevier B.v.保留所有权利。

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