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IMPACTS OF DIFFERENT MULCHIN G PRACTICES ON SOIL WATER CONSERVATION IN A SEMIARID REGION OF TURKEY

机译:不同地膜G做法对土耳其半干旱地区土壤水分保持的影响

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The use of mulch is an important application in the conservation of water in the soil for a longer period of time. As mulch materials, organic and inorganic materials can be used. The use of mulch in researches was generally evaluated during plant growth season. In this study, it was carried out only in certain soil conditions without any plant growth. The aim of the study was to determine the change in the soil water content under the conditions where an organic mulch (straw), raking and no treatment were applied. Four treatments compared were A) Mulch application with straw (organic mulch material) immediately after the soil was saturated; B) Roughly 3 days after the water was applied, the raking was done; C) When the raking was done, straw (organic mulch material) and mulch application were done; D) Control treatments without any special application. The study was carried out in 16 square borders with soil embankments and 4 treatments and 4 replications. Each square border was formed in 1x1 m dimensions. A distance of 2 m was left between the square borders. Soil water content was measured at 20, 30, 40, 50, 60, 70, 80 and 90 cm depth with neutron meter. Neutron meter tubes were placed in the center of the square borders with soil embankments. In the study, reference measurements were made before applying water to the square borders. Then each square border was filled with water to saturate soil profile. Changes in soil water content were observed at specific time intervals after saturation. At the end of the study, the water content of the soil was calculated as 41.28 mm for A, 48.71 mm for B, 47.35 mm for C and 52.72 mm for D. The loss of soil water content was ranked as A
机译:覆盖物的使用是长期保持土壤水分的重要应用。作为地膜材料,可以使用有机和无机材料。覆盖物在研究中的使用通常在植物生长季节进行评估。在这项研究中,它仅在某些土壤条件下进行,没有任何植物生长。该研究的目的是确定在有机覆盖物(秸秆)、耙地和不进行处理的条件下土壤含水量的变化。比较的四种处理是:A)在土壤饱和后立即用秸秆(有机地膜材料)进行覆盖;B) 施水后大约 3 天,完成耙子;C)耙耙完成后,秸秆(有机覆盖材料)和覆盖物施用完成;D) 无需任何特殊应用即可控制治疗。该研究在 16 个方形边界进行,有土堤和 4 次处理和 4 次重复。每个正方形边框的尺寸为 1x1 m。方形边界之间留有 2 m 的距离。用中子计测量20、30、40、50、60、70、80和90 cm深度的土壤含水量。中子计管被放置在带有土堤的方形边界的中心。在这项研究中,在将水施加到方形边界之前进行了参考测量。然后,每个方形边界都充满水以饱和土壤剖面。在饱和后的特定时间间隔内观察到土壤含水量的变化。在研究结束时,土壤的含水量计算为A为41.28 mm,B为48.71 mm,C为47.35 mm,D为52.72 mm。土壤含水量损失等级为A

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