Estimation of Water Conductivity of Typical Chernozem in the Depressed Zone of the Water-Regulating Forest Belt

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Abstract

The studies aimed to assess the change in the absorbency of the soil with distance from the forest belt, including the depressed zone. The work was carried out in 2018–2022 in a long-term field stationary experience in contour-reclamation agriculture in the Kursk region. The assessment was carried out for erosion-threatening slopes of southern and northern exposures with an agroforest reclamation complex, represented by contour-parallel placed water-regulating two-row forest belts with a water-catching ditch in the row-spacing and a masonry-cum-earth dam along the lower edge. The soil was a typical medium-thick low-humus heavy loamy chernozem. To determine the width of the depressed zone, the yield of crops was studied at 5, 10, and 25 m from the forest belt up and down the slope, the control was the upland. A significant decrease in harvest, regardless of weather conditions, was observed at 5 m; for buckwheat it was 68.8–75.0%, spring barley 40.0–65.7%, winter wheat 24.9–56.9% compared to control. The absorbing capacity of the soil was determined on perennial grasses and spring barley in the depressed zone by the method of small flooded areas and sprinkling of runoff areas. The intensity of pressure absorption in the crops of perennial grasses on the soils of the slope of the northern exposure was higher than in the crops of barley by 55%, of the southern, four times. The intensity of water absorption, estimated by the method of sprinkling of runoff plots, in crops of perennial grasses on the slope of the northern exposure was 0.6 mm/min, of the southern exposure 0.8 mm/min, which was significantly higher than in barley crops. To increase the absorbency of the soil, both during the period of snowmelt and during heavy rains, it is recommended to sow perennial grasses along forest strips more than 5 m wide.

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估算水调节森林带凹陷区典型切尔诺泽姆的导水率
摘要 研究旨在评估土壤吸水性随距离林带(包括郁闭区)的变化情况。这项工作于 2018-2022 年在库尔斯克地区一个具有长期污染开垦农业经验的田间固定点进行。评估针对的是南面和北面有侵蚀威胁的斜坡,斜坡上有一个农林开垦综合体,由等高线平行放置的水调节双行林带代表,林带的行间距上有一条集水沟,下沿有一个砖石土坝。土壤为典型的中厚低腐殖质重壤土。为了确定郁闭带的宽度,研究了坡上和坡下距离林带 5 米、10 米和 25 米处的作物产量,对照为高地。与对照组相比,无论天气条件如何,5 米处的收成都明显减少;荞麦减少了 68.8-75.0%,春大麦减少了 40.0-65.7%,冬小麦减少了 24.9-56.9%。通过小面积漫灌和径流区洒水的方法,测定了郁闭区多年生禾本科植物和春大麦的土壤吸收能力。北坡土壤上多年生禾本科作物的压力吸收强度比大麦作物高 55%,是南坡的四倍。根据径流地块洒水法估算,北部斜坡上多年生禾本科作物的吸水强度为 0.6 毫米/分钟,南部斜坡上多年生禾本科作物的吸水强度为 0.8 毫米/分钟,明显高于大麦作物。为了在融雪期和暴雨期提高土壤的吸收能力,建议在宽度超过 5 米的林带上播种多年生牧草。
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