高级检索+

黄土坡面苜蓿种植比例对土壤水分的影响

Effects of proportions of Medicago sativa on the loess slope on soil moisture

  • 摘要: 掌握黄土坡面不同苜蓿种植比例下土壤水分状况,可以为坡面紫花苜蓿合理配置提供理论支撑。利用黄土区已建的6个退耕后配置不同比例紫花苜蓿的坡面小区,于2019年6月至10月每月中旬,使用中子仪测量小区不同坡位0~300 cm土壤含水量,研究不同苜蓿种植比例对土壤水分的消耗状况。结果表明:经过雨季的降水补给,各坡位人工苜蓿地降水入渗深度为50~60 cm。不同坡位处苜蓿地储水量变化不同,坡上贮水量增加12.4 mm,坡中贮水量增加8.1 mm,坡下贮水量下降19.4~66.11 mm。受到表层土壤密度影响,撂荒地0~100 cm土层降水入渗量由坡上至坡下逐渐增多。坡上撂荒地降水入渗深度为100~220 cm,贮水量增加24.3~68.3 mm;坡中撂荒地降水入渗深度为60~120 cm,贮水量增加23.9~36.9 mm;坡下撂荒地降水入渗深度为50~100 cm,贮水量增加23.9 mm。随人工苜蓿种植比例的增加,坡面小区土壤总贮水量降低。因此,退耕坡面种植高耗水苜蓿显著消耗土壤水分,坡面植被配置中应减少高耗水植被的种植比例。13:2的撂荒-苜蓿配置模式更有利于黄土高原植被的恢复和土壤水分的积蓄。

     

    Abstract:
    Background Soil and water loss is serious in the Loess Plateau. Returning Farmland to Forest (Grass) and restoring vegetation is an effective measure to prevent soil and water loss. Improper planting will increase soil moisture depletion and even dry soil layer. Alfalfa (Medicago sativa)is an important vegetation for returning farmland to grassland on the Loess Plateau. The comparison of soil moisture in six plots with different alfalfa allocation ratio provides theoretical basis for alfalfa planting rational allocation on the loess slope, and makes the soil moisture on the loess slope to be used reasonably.
    Methods The experimental plots were six slope plots with different ratios of alfalfa in the loess region. From June to mid-October 2019, a neutron meter was used to measure the soil moisture content in the upper, middle and lower parts of the plots at depths of 0-300, 10 cm apart from 0-100 and 20 cm apart from 100-300 cm. Three to five days after the rain, the infiltration degree of precipitation reached the deeper soil layer, and an additional measurement was conducted. A standard rain gauge was set up in the experimental area to measure precipitation with rain gauge after rain. Excel and Origin software for data processing.
    Results 1) The infiltration depth of precipitation in the artificial alfalfa field was 50-60 cm in each slope position after the precipitation was of replenishment in rainy season. 2) The water storage of the alfalfa field varied with different slope positions. The water storage on the upper slope increased by 12.40 mm, in the middle slope increased by 8.10 mm, and in the lower slope decreased by 19.40-66.11 mm. 3) Due to the influence of surface soil density, precipitation infiltration of 0-100 cm soil layer in the abandoned land gradually increased from the upper slope to the lower slope. 3) The precipitation infiltration depth of the abandoned land on the upper slope was 100-220 cm, and the water storage increased by 24.3-68.3 mm. The precipitation infiltration depth of the abandoned land in the slope was 60-120 cm, and the water storage increased by 23.9-36.9 mm. The precipitation infiltration depth of the abandoned land under the middle slope was 50-100 cm, and the water storage increased by 23.9 mm. With the increase of planting proportion of artificial alfalfa, the total soil water storage in slope plot decreased.
    Conculsions With the increase of the proportion of the artificial alfalfa on the sloping land, the total water storage in the plot decreased, and the soil water could not recover under the effect of natural precipitation. Slope vegetation configuration should reduce the proportion of vegetation configuration with high water consumption. When the ratio of abandoned land to alfalfa land was 13:2, soil erosion was controlled and soil moisture was in good situation.

     

/

返回文章
返回