Li Yue, Wang Chun-Xia, He Xin-Lin, Wu Chen-Tao, Niu Jing-Ran
College of Water & Architectural Engineering, Shihezi University, Shihezi 832000, Xinjiang, China.
Xinjang Surveying & Designing Institute of Ministry of Agriculture/Xinjiang Production and Construction Corps Surveying & Designing Institute (Group) Co., Ltd., Urumqi 830000, China.
Ying Yong Sheng Tai Xue Bao. 2022 Apr;33(4):894-900. doi: 10.13287/j.1001-9332.202204.023.
With continuous increases in the amount and duration of plastic film used, the residual film in farmland soil is accumulated and tended to be fragmented, which affects soil water infiltration. We carried out an experiment of one-dimensional vertical infiltration of soil moisture. We examined the effects of different residual film density and area on soil water cumulative infiltration under 21 experimental treatments with 5 residual film area levels (0.25, 0.5, 1, 2, 8 cm) and 5 residual film density levels (0, 60, 180, 300, 420 kg·hm). The results showed that soil water infiltration rate was accelerated and the total infiltration amount was increased by adding a certain amount of residual film into the clay loam soil with bulk density of 1.53 g·cm. The total infiltration amount of different residual film area always appeared mutation or turning point when the single residual film area was 1 cm. When the residual film area and density were larger or smaller than that, the cumulative infiltration amount would be significantly affected, with the treatment of 0.5 cm residual film area and 200 kg·hm residual film density being obvious demarcation. When the residual film area was 0.25 cm, the cumulative infiltration reached the maximum. When the residual film with a single area ≤0.25 cm was uniformly mixed into the soil, the slope of soil water cumulative infiltration curve was significantly different from that of other residual film treatments, forming a "new structure" soil with unique water infiltration characteristics.
随着塑料薄膜使用量和使用时间的不断增加,农田土壤中的残留薄膜不断累积并趋于破碎,这影响了土壤水分入渗。我们进行了土壤水分一维垂直入渗试验。在5个残留薄膜面积水平(0.25、0.5、1、2、8平方厘米)和5个残留薄膜密度水平(0、60、180、300、420千克·公顷)的21种试验处理下,研究了不同残留薄膜密度和面积对土壤水分累积入渗的影响。结果表明,在容重为1.53克·立方厘米的黏壤土中添加一定量的残留薄膜,可加快土壤水分入渗速率并增加总入渗量。当单个残留薄膜面积为1平方厘米时,不同残留薄膜面积的总入渗量总是出现突变或转折点。当残留薄膜面积和密度大于或小于该值时,累积入渗量会受到显著影响,残留薄膜面积为0.5平方厘米、残留薄膜密度为200千克·公顷的处理是明显的分界线。当残留薄膜面积为0.25平方厘米时,累积入渗量达到最大。当单个面积≤0.25平方厘米的残留薄膜均匀混入土壤中时,土壤水分累积入渗曲线的斜率与其他残留薄膜处理显著不同,形成了具有独特水分入渗特征的“新结构”土壤。