东北典型厚层黑土区坡耕地侵蚀对土壤质量的影响研究
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西北农林科技大学

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国家重点研发计划项目(2022YFD1500102, 2024YFD1501104)


Effects of Soil Erosion on Soil Quality in Slope Farmland of Typical Thick-layer Mollisol Region of Northeast China
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1.NORTHWEST A&2.F UNIVERSITY

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National Key R&D Program of China (2022YFD1500102, 2024YFD1501104)

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    摘要:

    [目的]阐明东北黑土区土壤侵蚀-沉积对坡耕地土壤质量的影响,可为黑土资源保护和可持续利用提供重要科学依据。[方法]选取黑龙江省克山县的两块厚层黑土区的坡耕地,采用137Cs示踪技术估算土壤侵蚀速率,基于最小数据集方法构建土壤质量评价指标,分析典型厚层黑土区土壤侵蚀-沉积对坡耕地土壤质量的影响。[结果]1)研究区坡耕地土壤侵蚀-沉积速率在-1563.2~7916.1 t/km2/a之间,平均侵蚀速率为2669.0 t/km2/a。且土壤侵蚀速率在坡面空间分布上均表现为坡中下部侵蚀强烈,坡顶和坡上部为轻度-中度侵蚀,坡脚50 m坡段出现沉积,坡面土壤侵蚀最严重部位分布在120~170 m坡段。2)构建了包含土壤粘粒(Clay)、土壤有机碳(SOC)、全磷(TP)、有效氮(AN)、微生物量碳(MBC)和β-1,4-葡萄糖苷酶(BG)的土壤质量评价最小数据集,且基于最小数据集和全数据集计算的土壤质量指数(SQI)之间存在显著的线性正相关关系(p<0.001),说明最小数据集可以替代全数据集,较真实地反映研究区耕地的土壤质量状况。3)研究区在侵蚀区的SQI与土壤侵蚀速率呈显著的负相关关系(p <0.01),而在沉积区的SQI与沉积速率呈不显著的正相关关系,两块样地侵蚀区的SQI较沉积区平均减少了13.3%,且SQI的空间分布与土壤侵蚀速率的空间分布呈现相反的变化趋势。[结论]研究区土壤侵蚀是导致坡耕地土壤质量退化的关键驱动力。

    Abstract:

    [Subjective] Elucidating the effects of soil erosion-deposition on the soil quality of slope farmland in Mollisol region of Northeast China is crucial for protecting black soil resource and maintaining its sustainable utilization. [Methods] This paper, selecting two sloping farmlands located at Keshan county, Heilongjiang province as the study site, utilized the 137Cs tracer technique to estimate soil erosion rates and the minimum data set (MDS) method to calculate soil quality index (SQI) to analyze impacts erosion-deposition of sloping farmland on soil quality in typical thick-layer mollic regions. [Results] 1) The soil erosion-deposition rate of slope farmland in the study area ranges from -1563.2 to 7916.1 t/km2/a, with an average erosion rate of 2669.0 t/km2/a. The spatial distribution of soil erosion rate along the hillslopes was characterized by intensive erosion in the middle and lower slope segment, light-moderate erosion in the top and upper slope segment, deposition at the 50 m slope segment at the foot of the slope, and the most severe slope segment of soil erosion was distributed in 120-170 m slope length. 2) The soil quality evaluation indicators based on the MDS included soil clay, soil organic carbon (SOC), total phosphorus (TP), available nitrogen (AN), soil microbial biomass carbon (MBC) and β-1,4-glucosidase (BG). Moreover, there was a significant linear positive relationship between the MDS-SQI and SQI based on the full data set (p < 0.001), indicating that the MDS could replace the full data set and really reflected the soil quality regime of the slope farmland in the study area. 3) In the study area, there was a significantly negative correlation between SQI and soil erosion rates in the erosion sites (p < 0.01); while the SQI numerally increased with deposition rates without significant difference in the depositional sites. The SQI in the erosion sites reduced by 13.3% on average compared with that in the deposition sites; and the spatial distribution of the SQI along hillslopes was opposite to that of the soil erosion rates. [Conclusion] Soil erosion in the study area is the key driving force to soil quality degradation in sloping farmland.

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  • 收稿日期:2025-04-18
  • 最后修改日期:2025-05-16
  • 录用日期:2025-05-26
  • 在线发布日期: 2025-07-07
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