黄土坡面溶解性碳流失特征及其对水土保持措施的响应
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王璞(1997—),男,硕士研究生,主要从事水土保持与土壤碳循环研究。E-mail:wangpussr@163.com

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S157.2

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国家自然科学基金联合基金重点项目(U2243225)


Characteristics of Dissolved Carbon Loss on Loess Slopes and Its Response to Soil and Water Conservation Measures
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    摘要:

    [目的] 为系统认识不同水土保持措施下土壤碳的流失过程、通量特征及其影响因素。[方法] 采用野外模拟降雨试验,对比分析梯田、草地、上梯下草、上梯下裸等水土保持措施下黄土坡面溶解性有机碳与无机碳随降雨过程的流失特征及影响因素,量化不同水土保持措施对坡面溶解性碳流失的拦蓄效益。[结果] 各水土保持措施下坡面溶解性碳浓度随降雨过程无明显变化规律,但溶解性碳流失通量均较裸地显著降低(p<0.05),且以溶解性无机碳流失为主,其贡献碳流失量的79.5%~83.1%;草地、上梯下草、梯田和上梯下裸措施对坡面溶解性碳的拦蓄效益分别为76.9%、56.3%、47.6%和18.0%;坡面产流量是影响溶解性碳流失通量的决定因素,碳流失量与产流量呈显著正相关。[结论] 研究结果深化对不同水土保持措施减少土壤碳流失过程的认识,为黄土高原坡面水土保持碳汇效益评估提供科学依据。

    Abstract:

    [Objective] The implementation of soil and water conservation measures has led to a notable reduction in the loss of soil carbon pools,while simultaneously facilitating effective control of soil erosion. However,there is a paucity of systematic understanding of the processes of carbon loss,flux characteristics and the factors that influence them under different soil and water conservation measures. [Methods] In this study,a comparative analysis of the characteristics and influencing factors associated with the loss of dissolved organic carbon(DOC) and inorganic carbon(DIC)from loess slopes under different soil and water conservation measures was conducted. These measures included terraces,grasslands,upper terraces and lower grasslands,and the upper terraces and lower bare soil. To this end,a simulated rainfall test in the field was employed to quantify the benefits of the above-mentioned soil and water conservation measures in reducing the loss of dissolved carbon from the slopes. [Results] The dissolved carbon concentration on the slope surface under each soil and water conservation measure remained relatively constant throughout the rainfall process. However,the flux of dissolved carbon loss was significantly lower than that observed on bare ground(p<0.05). Furthermore,the loss of dissolved inorganic carbon contributed to 79.5%—83.1% of the total carbon loss. The retention benefits of grassland,the upper terraces and lower grasslands,the upper terraces and lower bare soil measures for dissolved carbon on slopes were 76.9%,56.3%,47.6% and 18.0%,respectively. The volume of flow production on the slope surface was identified as the determining factor affecting the flux of dissolved carbon loss. Furthermore,the flux of carbon loss was found to be significantly positively correlated with the flow volume. [Conclusion] This study enhances our understanding of the mechanisms through which soil carbon loss is mitigated by diverse soil and water conservation measures. It offers a scientific foundation for evaluating the carbon sink benefits of soil and water conservation on the slopes of the Loess Plateau.

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王璞, 任宗萍, 马晓妮, 王凯博, 董彭蓓, 贺国凯.黄土坡面溶解性碳流失特征及其对水土保持措施的响应[J].水土保持学报,2025,39(2):48~56,64

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  • 收稿日期:2024-10-15
  • 最后修改日期:2024-10-30
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  • 在线发布日期: 2025-05-07
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