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Temporal Changes in Soil Water Content and Penetration Resistance under Three Tillage Systems

机译:三种耕作制度下土壤水分和抗渗透性的时空变化

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摘要

This study aims to evaluate the impact of different tillage systems on water conservation and penetration resistance in Stagnosols on slopes. Three tillage systems were evaluated during a long-term experiment in Central Croatia in a period from 2011 to 2014, in order to identify sustainable land management practices: control treatment (CT), ploughing and other seedbed layer preparation up and down the slope; ploughing across the slope (PA) – to 30 cm, other operations depending on the crop, also across the slope; and ploughing across the slope (30 cm) with subsoiling (SUB) to 50 cm. Penetration resistance and soil water content were measured each investigated season during five terms to a depth of 60 cm. Tillage systems significantly influence soil water content and penetration resistance, but the results showed great temporal and vertical variation in each investigated season. The results also showed that in low quality Pseudogley deep loosening is required because of the inability of these soils to recover naturally. The hardness of these soils decreases after tillage, or when the moisture content increases, so the period with potentially limiting soil impedance is shorter in systems with subsoiling than in conventionally tilled soils. Fallow has been effective in reducing soil strength in non-traffic areas and increasing soil moisture content. When comparing cropping variants it was established that only a system including subsoiling ensures higher moisture content. Results indicate that since soil water content and penetration resistance were adversely affected, subsoiling should be applied continuously in Pseudogley sites in the hills. Generally, soil resistance increased with time from the date of primary tillage. Although penetration resistance values increase after tillage, the differences were attributed to temporal variation of soil water content. In this study soil moisture condition is presented as a more important factor for soil resistance than the time between primary tillage and measurements.
机译:这项研究的目的是评估不同耕作制度对坡地土壤中的节水和防渗性能的影响。为了确定可持续的土地管理实践,在克罗地亚中部从2011年至2014年进行的一项长期实验中,对三种耕作系统进行了评估:控制处理(CT),耕作和坡地上其他耕作层的准备;在坡度(PA)上耕种– 30厘米,根据作物的不同,也要在坡度上耕作;然后在30厘米的斜坡上进行深耕(SUB),直至50厘米。在五个学期至60 cm的深度中,每个调查季节测量了抗渗透性和土壤含水量。耕作制度对土壤含水量和抗渗透性有显着影响,但结果表明每个调查季节的时间和垂直变化都很大。结果还表明,由于这些土壤无法自然恢复,因此在劣质Pseudogley中需要深度疏松。耕作后或水分含量增加时,这些土壤的硬度会降低,因此,在带深层耕作的土壤中,具有潜在限制的土壤阻抗的时间要短于传统耕作的土壤。小食已有效降低非交通区的土壤强度并增加了土壤水分。在比较种植变量时,可以确定只有包括深松的系统才能确保较高的水分含量。结果表明,由于土壤含水量和抗渗透性受到不利影响,因此应在丘陵的Pseudogley场地连续进行深耕。通常,从初次耕作之日起,土壤抗性随时间增加。尽管耕作后的穿透阻力值增加,但差异是由于土壤含水量随时间变化而引起的。在这项研究中,土壤湿度条件是比主要耕作和测量之间的时间更重要的土壤抗力因素。

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