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

机译:覆膜农田雨水和土壤水分的流动特征。

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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:薄膜覆盖物被用于许多农田,因为它不仅可以防止土壤中的虫害和侵害,还可以通过抑制土壤表面的水分蒸发,保持温和的土壤湿度以及保持土壤温度高于裸露的土壤表面来改善耕种环境。疾病。引入地膜覆盖可以在凉爽的高原地区(例如信州高原)进行农作物种植。但是,由于使用地膜覆盖的田地的根部区域的直接入渗量要比裸土田地的低,因此人们担心干旱会加剧。 1995年秋季,在大白菜(Brassica pekinensis Rupr。)和大白菜种植的田间,利用土壤水分测量技术,在许多位置和深度进行了覆盖床与沟间土壤水分状况和流量的实验比较。 1996年春天,在田间种植了甘蓝(Brassica oleracea L.)。结果总结如下; (1)即使在低土壤湿度条件下小雨后,覆盖床的浅表土的土壤水分也比犁沟空间和裸露土壤少。但是,覆盖床中的播种区域(覆盖膜的保持)比播种区域周围的水分高。但是降雨后的一两天,覆盖床和犁沟的土壤水分状况几乎相同。 (2)随着农作物的生长,由于农作物根系吸收水分,土壤水分低于犁沟空间。在根部区域下方的土壤层中,即深度大于0.3 m,土壤水分会因根系系统吸收土壤水分而引起的土壤水分势能梯度从犁沟空间移至覆盖床。这些结果表明,偶尔在犁沟空间中耕作会增加雨水的渗透率,并有利于水分从犁沟空间移动到覆盖床的根部。

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