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Characteristics of the rain water and soil moisture flows in the fields covered with film mulch

机译:覆盖薄膜覆盖覆盖的雨水和土壤水分的特点

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摘要

Film mulch is being used in many farm lands because it improves the environment for cultivation by suppressing water evaporation from soil surface, maintaining a mild soil moisture condition, and maintaining the soil temperature higher than the bare sou surface, in addition to protecting against pests and diseases. Crop cultivation in cool high lands (such as the Shinshu Plateau) can be made possible with the introduction of film mulch. However, as the direct infiltration in the root zone are lower in fields where film mulch is used than in bare soil fields, and this raises fears that droughts would be exacerbated. Experimental comparisons of the soil moisture condition and flow between mulched bed and furrow space using the soil moisture measurement technique at many positions and many depths were carried out in the fall of 1995 in field planted with Chinese cabbage (Brassica pekinensis Rupr.),and in the spring of 1996 in field planted with cabbage (Brassica oleracea L.). The results are summarized as follows; (1) The shallow topsoil of the mulched beds had less soil moisture than furrow space and bare soil even after light rains at low soil moisture condition. The sowed areas (hold of the mulch film) in mulched beds, however, were moisture than the surrouding of sowed area. But one or two days after rainfall, soil moisture condition in mulched bed and furrow space were almost same. (2) As the crops grew, the soil moisture became lower than furrow space due to the water uptake by the crops' root system. In the soil layer below the root zone, i.e. at a depth of more than 0.3 m, soil moisture is moved from the furrow space to the mulched bed by the gradient of soil moisture potential caused by the soil moisture uptake by the root system. These results propose that occasional plowing in the furrow space causes an increase in the infiltration rate of rain water, and facilitates the movement of moisture from the furrow space to root zone of the mulched beds.
机译:在许多农场土地上使用薄膜覆盖物,因为它通过抑制土壤表面的水蒸发来改善培养环境,保持温和的土壤水分状况,并使土壤温度保持高于裸露的表面,除了保护害虫和害虫疾病。随着薄膜覆盖物的引入,可以使凉爽高地(如什南高原)的作物培养。然而,由于根区的直接渗透在胶片覆盖物的领域中低于裸露的土地,因此这引发了害怕干旱会加剧的担忧。用土壤水分测量技术在许多位置和许多深度下使用土壤水分测量技术的土壤水分状况和流量的实验比较,在大白菜(BrassicaPekinensis Rupr)中占地面积的田间和许多深度。 1996年春天在种植卷心菜(Brassica Oleracea L.)的田间。结果总结如下; (1)覆盖的床的浅表层,除了在低土壤水分条件下的下雨之后,覆盖床的土壤水分也比沟槽空间和裸土。然而,在覆盖的床中播出的区域(覆盖胶片)是散热区域的水分。但降雨后的一两天,覆盖床和沟槽空间的土壤水分状况几乎相同。 (2)随着作物的增长,由于作物根系的水吸收,土壤水分变得低于沟槽空间。在根区下方的土壤层中,即在大于0.3米的深度下,通过根系土壤水分吸收引起的土壤水分潜力梯度,土​​壤水分从沟槽空间移动到覆盖的床上。这些结果提出偶尔在沟槽空间中的耕作导致雨水的渗透率增加,并促进水分从犁毛床的根区到覆盖床的根区。

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