黄土丘陵沟壑区梯田碳汇作用及其特征
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1.西北农林科技大学水土保持科学与工程学院;2.中国科学院教育部水土保持与生态环境研究中心;3.水利部水土保持监测中心;4.黄河流域水土保持生态环境监测中心;5.延安市吴起县吴起镇林业站

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S157.3+1

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中欧典型农业系统退化土壤修复管理创新研究平台(2022YFE0115300)


The Functions and Characteristics of Terrace Carbon Sink in the hilly and gully areas of the Loess Plateau
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    摘要:

    [目的]定量分析和探讨梯田碳汇作用与其特征,对进一步明确梯田的碳汇作用、巩固和提升生态系统碳汇能力、研编梯田碳汇方法学等具有重要意义。[方法]选取黄土丘陵沟壑区吴起县1—7 a (T5)、8—12 a(T10)、13—17 a(T15)、18—22 a(T20)、23—27 a(T25)等5个年份区间的梯田作为研究对象,以未实施水土保持措施的坡耕地为对照,研究不同年份梯田保碳、减排、增汇等能力与其变化规律。[结果]①坡耕地修建为梯田后可发挥保碳、减排、增汇等碳汇作用,梯田年均保碳量、减排量、增汇量(0—100 cm)分别为0.26、0.05和1.36 t/(hm2?a)。②梯田各土层均发挥了一定的增汇效益,表层土壤(0—40 cm)和深层土壤(40—100 cm)增汇效益分别占0—100 cm整个土层的61.50%和38.50%。③随着运行年份的增加,梯田表层土壤增汇效益显著增加,深层土壤的增汇效益稍有提升但总体上保持平稳。表层土壤增汇率从T5的16.30%提升至T25的51.34%,深层土壤从T5的14.00%提升至T25的23.66%。[结论]黄土丘陵沟壑区梯田发挥着良好的保土保碳、减蚀减排和土壤增汇等碳汇作用。在修建27 a内,梯田增汇作用的占比最大,且表层土壤增汇更为显著;随着运行年份增加,梯田保碳作用的占比将逐渐增大。

    Abstract:

    [Objective] Quantitative analysis and understanding the role of terrace carbon sink and its characteristics are significant for further giving play to the role of terrace carbon sink, consolidating and enhancing the carbon sink capacity of the ecosystem, and aiding in the development of methods for assessing the carbon sequestration capacity of terraces. [Methods] In Wuqi County of the loess hilly and gully region, we selected terraces with operational ages between 1-7 years (T5), 8-12 years (T10), 13-17 years (T15), 18-22 years (T20) and 23-27 years (T25) for our research objects. For baseline comparison, we chose slope cropland without soil and water conservation measures, studying the capabilities of terraces in terms of carbon preservation, emission reduction and carbon sequestration across different years. [Results] ① After the transformation of slope cropland into terraces, we observed an increase in carbon preservation, emission reduction, and carbon sequestration. The annual carbon preservation, emission reduction, and carbon sequestration (0-100 cm) are 0.26, 0.05 and 1.36 t/hm2 respectively. ② Each soil layer of the terraces contributes certain benefits, the carbon sequestration benefits of the surface (0-40 cm) and deep (40-100 cm) soil layers account for 61.50% and 38.50% of the entire soil layer, respectively. ③ With the increase in the operation year of the terrace, the benefits of the terrace surface soil increased significantly, while the benefits of deep soil were slightly improved but remained stable on the whole. The rate of carbon sequestration in surface soil increased from 16.30% of T5 to 51.34% of T25, and that in deep soil increased from 14.00% in T5 to 23.66% of T25. [Conclusion] The terrace in the loess hilly and gully region exhibits significant carbon sink functions, including carbon preservation, emission reduction, and carbon sequestration. Within 27 years of the operation of the terraces, the proportion of the carbon sequestration capacity is the largest, and the increase of the surface soil is more significant. With the increase of terrace operation year, the proportion of carbon preservation in the carbon sink capacity of terrace will gradually increase.

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  • 收稿日期:2024-06-24
  • 最后修改日期:2024-08-20
  • 录用日期:2024-08-22
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