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    退耕还林前后渭河流域土壤保持功能变化

    Changes in soil conservation function before and after the Grain for Green project in the Weihe River Basin

    • 摘要: 基于InVEST模型的土壤保持模块, 定量评估退耕还林前后渭河流域土壤保持功能的变化, 并统计不同土地利用类型及坡度下的土壤保持量。结果表明: 1)相较于1980年, 2020年实际土壤侵蚀量减少1.40亿t, 平均土壤侵蚀模数减少1 033.51 t/(km2·a), 微度侵蚀的比例由60.75%增加至77.43%, 土壤保持总量由48.60亿t增加到53.73亿t; 2)不同土地利用类型中, 草地的土壤保持量最大, 占土壤保持总量的40%以上; 而单位面积土壤保持量最大的是林地; 3)0~5°的微坡地区土壤保持量最小, 单位面积的土壤保持量也最低; >15°~25°的较陡坡地区土壤保持量最大, 占土壤保持总量的1/3以上。退耕还林工程主要通过减少土壤侵蚀量来提高土壤保持功能, 随着植被恢复, 不同土地利用类型及坡度的土壤保持功能增强。研究结果可为流域植被恢复效果和土壤保持功能的定量评估提供参考。

       

      Abstract:
      Background Soil conservation function plays an important role in soil formation, vegetation fixation and water conservation. Since the implementation of the Grain for Green project (GFGP), soil erosion in China has been effectively controlled. The change of soil conservation function in Weihe River Basin (WRB) before and after the GFGP was quantitatively evaluated in this study.
      Methods Based on the Sediment Delivery Ratio (SDR) module of the InVEST model, the soil conservation function of the WRB in 1980 and 2020 was evaluated using the data of rainfall erosivity (R), soil erodibility (K), vegetation coverage factor (C), DEM, and soil and water conservation measures factor (P). And the soil conservation amount under different land use types and slopes were counted in ArcGIS 10.2.
      Results 1) After the GFGP, the soil erosion of the WRB was significantly improved. Compared with 1980, the actual amount of soil erosion in 2020 decreased by 1.40×108 t, the average soil erosion modulus decreased by 1 033.51 t/(km2·a). The total amount of soil conservation increased from 48.60×108 t to 53.73×108 t. The soil erosion intensity has generally changed from a stronger level to a weaker level. The proportion of slight erosion increased from 60.75% to 77.43%. 2) Among different land use types, grassland had the largest soil conservation amount, accounting for > 40% of the total, while the largest amount of soil conservation per unit area was forestland. The soil conservation function of water area and unused land was relatively low. 3) The amount of soil conservation per unit area increased with the increase of slope within a certain range. The soil conservation amount in 0-5° micro slope area was the lowest. The area with >15°-25° steep slope has the largest amount of soil conservation, accounting for more than one third of the total soil conservation amount.
      Conclusions After the implementation of GFGP, the soil conservation function of the WRB has been significantly improved. Land use and slope were two important factors affecting the soil conservation function. With the progress of vegetation restoration, the soil conservation function of different land use types and different slopes is gradually strengthened. The results provided a reference for quantitative evaluation of vegetation restoration effect and soil conservation function in the basin.

       

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