活性地膜覆盖甘薯田土壤导水率的变化

IF 2.3 4区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY
Junko Nishiwaki, Takuya Koseki, Naomi Asagi, Hirotaka Saito, Roy C. Sidle
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引用次数: 0

摘要

活覆盖物(LM)用于农田中抑制杂草、控制疾病和减轻侵蚀。它还增加了生长季节根系死亡和腐烂阶段的土壤养分供应。然而,LM对与土壤孔隙结构相关的土壤水力特性的益处在此尚未详细阐述。我们重点研究了在种植和不种植LM(大麦,Hordeum vulgare L.)的红薯的田地中土壤导水率(K)的时间变化。K是在三个不同的压头下使用迷你盘式渗透计在田地中测量的。在有LM的地块中,与没有LM的地块相比,K在8月份显著下降,然后在10月份增加(在–0.5 cm压头下)。由于根系生长或死亡和腐烂导致的土壤孔隙结构变化可能会改变土壤的导水性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Changes in soil hydraulic conductivity in sweet potato field with living mulch

Changes in soil hydraulic conductivity in sweet potato field with living mulch

Living mulch (LM) is used in agricultural fields to suppress weeds, control diseases, and mitigate erosion. It also enhances soil nutrient supply at the root death and decay stage during the growing season. However, benefits of LM to soil hydraulic properties related to soil pore structure have not been elaborated here. We focus on temporal changes in soil hydraulic conductivity (K) in a field where sweet potato was grown with and without LM (barley, Hordeum vulgare L.). K was measured in the field using a mini-disk infiltrometer at three different pressure heads. In the plots with LM, K decreased significantly in August and then increased in October compared to plots without LM (at –0.5 cm pressure head). Changes in soil pore structure due to root growth or death and decay may alter soil hydraulic conductivity.

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来源期刊
CiteScore
3.70
自引率
3.80%
发文量
28
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