近20年气候和土地利用变化对白洋淀流域土壤保持功能的影响
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作者单位:

1.河北农业大学 城乡建设学院;2.中国地质调查局水文地质环境地质调查中心

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中图分类号:

TV212.4

基金项目:

河北省自然科学基金资助项目(E2024204017);河北省省属高等学校基本科研业务费研究项目(KY2021001); 中国地质调查项目(DD20240081,DD20242735)


Impacts of climate and land use change on soil conservation function in the Baiyangdian Basin in the past two decades
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College of Urban and Rural Construction,Hebei Agricultural University

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    摘要:

    摘要:[目的]对白洋淀流域的土壤保持功能进行评估,量化气候和土地利用变化对土壤保持量变化的影响,可为推进白洋淀流域生态环境保护提供科学依据。[方法]本文基于2000-2020年气象、土地利用、土壤等数据,应用InVEST模型模拟分析白洋淀流域土壤保持量的时空变化特征,并基于情景模拟与趋势分析法识别了土地利用与气候变化对土壤保持量变化的相对贡献。[结果](1)2000-2020年白洋淀流域降水量多年平均值为445mm,整体呈现增加趋势,流域范围内北京市和保定市东北部降水量均高于流域多年平均值。(2)2000-2020年,白洋淀流域的主要土地利用类型为耕地和林地,面积占比分别为40.16%-44.13%和24.71%-27.72%。耕地和草地面积显著减少,林地和建设用地面积显著增加,耕地主要转化为建设用地,草地主要转化为林地。(3)2000年、2005年、2010年、2015年和2020年,白洋淀流域的土壤保持强度分别为9.50×10^3 t?km^(-2),9.38×10^3 t?km^(-2),1.10×10^4 t?km^(-2),1.07×10^4 t?km^(-2),1.25×10^4 t?km^(-2)。年际变化整体呈波动增加趋势,空间分布上呈西北高东南低的格局。林地和草地的土壤保持强度远远大于其他土地利用类型。(4)气候变化主导土壤保持量变化的面积占比为93.07%,土地利用变化主导土壤保持量变化的面积占比为6.93%。[结论]白洋淀流域土壤保持量变化受气候和土地利用变化共同主导,气候变化为主因。

    Abstract:

    Abstract: [Objective] Evaluating the soil conservation function of Baiyangdian Basin and quantifying the impact of climate and land use changes on soil conservation changes can provide a scientific basis for promoting the ecological environmental protection of Baiyangdian Basin. [Methods] Based on meteorological, land use and soil data from 2000 to 2020, the InVEST model was used to simulate and analyze the spatial and temporal variation characteristics of soil conservation in Baiyangdian Basin, and the relative contributions of land use and climate change to soil conservation changes were identified based on scenario simulation and trend analysis. [Results] (1) The annual average precipitation in the Baiyangdian Basin was 445 mm from 2000 to 2020, with an overall increasing trend. And the precipitation in Beijing and northeastern Baoding within the basin was higher than the annual average precipitation. (2) From 2000 to 2020, the main land use types in the Baiyangdian Basin were cropland and forest, with the proportion of area ranging from 40.16% to 44.13% and from 24.71% to 27.72%, respectively. The area of cropland and grassland decreased significantly, and the area of forest land and construction land increased significantly. The cropland was mainly transformed into construction land, and grassland was mainly transformed into forest land. (3) In 2000, 2005, 2010, 2015 and 2020, the soil conservation intensity in the Baiyangdian watershed were separately 9.50×10^3 t?km^(-2),9.38×10^3 t?km^(-2),1.10×10^4 t?km^(-2),1.07×10^4 t?km^(-2),1.25×10^4 t?km^(-2). The overall interannual variation of soil conservation showed a fluctuating upward trend, and the spatial distribution of soil conservation showed a pattern of high in the northwest and low in the southeast. The soil conservation intensity of forest land and grassland was much higher than that of other land use types. (4) The climate change dominated 93.07% area of the soil conservation change, and land use change dominated 6.93% area of the soil conservation change. [Conclusion] Changes in soil conservation in Baiyangdian Basin are attributed to the combination effects of climate and land use changes, with climate change as the main cause.

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  • 收稿日期:2024-09-18
  • 最后修改日期:2025-01-21
  • 录用日期:2025-01-22
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