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首页> 外文期刊>Soil & Tillage Research >Effects of soil water content during primary tillage - laser measurements of soil surface changes.
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Effects of soil water content during primary tillage - laser measurements of soil surface changes.

机译:初级耕作过程中土壤水分的影响-激光测量土壤表面变化。

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摘要

Soil water content during tillage can have a large impact on soil properties and tillage outcome. Measurement of soil relief in relation to fixed elevation points provides a non-destructive method of monitoring loosening/compacting processes during the year. The main objective of this study was to determine the effect of soil water content during primary tillage on soil physical properties. The treatments included mouldboard and chisel ploughing of a clay soil on three occasions in the autumn, with gradually increasing water content (0.76, 0.91 and 1.01 x plastic limit). Soil surface height was measured by laser within a 0.64 m2 area from fixed steel plates after each tillage occasion, and before and after seedbed preparation in the following spring. The measurements of surface height were compared with measurements of other soil physical properties, such as bulk density, saturated hydraulic conductivity and seedbed properties. Tillage at the lowest water content (0.76 x plastic limit) produced the greatest proportion of small aggregates, and generally the most favourable soil conditions for crop growth. Soil loosening, as measured by increase in soil height during primary tillage, was highest for mouldboard ploughing and for tillage at the lowest water content. Differences between tillage treatments decreased with time, but were still significant after sowing in the spring. Natural consolidation during winter was smaller than the compaction during seedbed preparation in the spring. No significant differences in bulk density were found between treatments, and thus soil surface height was a more sensitive parameter than bulk density determined by core sampling to detect differences between treatments. Late tillage under wet conditions caused a greater roughness of the soil surface and the seedbed base, which was also found in the traditional seedbed investigation. The effect of tillage time on seedbed properties also resulted in a lower number of emerged plants in later tillage treatments. The laser measurements were effective for studying changes in soil structure over time. The results emphasize the need to determine changes in soil physical properties for different tillage systems over time in order to model soil processes..
机译:耕作过程中的土壤水分会对土壤性质和耕作结果产生很大影响。与固定海拔高度相关的土壤释放量的测量提供了一种非破坏性的方法,用于监测一年中的松动/压实过程。这项研究的主要目的是确定初次耕作期间土壤含水量对土壤物理性质的影响。这些处理方法包括在秋季秋季三遍用粘土板和凿子犁土,并逐渐增加水分含量(0.76、0.91和1.01 x塑性极限)。在每次耕作之后,第二年春季的苗床准备前后,用激光在距固定钢板0.64 m2的区域内测量土壤表面高度。将表面高度的测量值与其他土壤物理特性(例如堆积密度,饱和水力传导率和苗床特性)的测量值进行了比较。在最低含水量(0.76 x塑性极限)下的耕作产生了最大比例的小集料,并且通常是最有利于作物生长的土壤条件。用一次耕作时土壤高度的增加来衡量,松土的最高程度是土壤松动,而在最低含水量的耕作中,其土壤松动程度最高。耕作处理之间的差异随着时间的推移而减小,但在春季播种后仍显着。冬季的自然固结要小于春季的苗床准备过程中的压实。在处理之间没有发现体积密度的显着差异,因此,土壤表面高度是比通过岩心采样确定以检测处理之间差异的体积密度更敏感的参数。在潮湿条件下的后期耕作会导致土壤表面和苗床基部更大的粗糙度,这在传统的苗床调查中也发现。耕作时间对苗床特性的影响还导致后期耕作处理中出苗的植物数量减少。激光测量对于研究土壤结构随时间的变化是有效的。结果强调需要确定不同耕作系统的土壤物理性质随时间的变化,以便对土壤过程进行建模。

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