黄土高原植被恢复过程中土壤碳固存变化及其驱动因素
DOI:
作者:
作者单位:

1.生物与食品工程系;2.中国科学院生态环境研究中心;3.西北农林科技大学水土保持科学与工程学院

作者简介:

通讯作者:

中图分类号:

基金项目:

国家重点研发计划项目(2022YFF1300403);国家自然科学基金青年项目(42201099);中央高校科研启动经费(2452024023)


The dynamics and drivers of soil organic carbon sequestration after cropland conversion on the Loess Plateau
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    土壤固碳是缓解全球气候变化的有效方式之一,大规模的植被恢复深刻改变了土壤固碳过程,明确生态脆弱区生态恢复过程中土壤碳固存变化及其驱动因素对生态管理及固碳减排有重要借鉴价值。本研究通过整合1992-2020年期间发表的100篇文献(935条观测数据,55个地区),分析了干旱半干旱黄土高原区域尺度植被恢复(人工乔木、人工灌木和撂荒草地)过程中土壤碳固存变化及其驱动因素。研究表明:(1)人工乔木和灌木固碳速率均为0.30 Mg C / (ha·yr),高于撂荒草地(0.10 Mg C / (ha·yr));常绿人工林固碳速率(0.45 Mg C / (ha·yr))高于落叶人工林(0.33 Mg C / (ha·yr)),但后者具有更高固碳量,恢复约51年后,常绿人工林具有更大固碳效益;(2)土壤固碳速率随降雨量的增加而增加,但变化程度受植被类型和恢复年限影响;(3)区域尺度上,土壤固碳速率先增加(<30yr)后稳定(>30yr),0-10yr, 10-20yr, 20-30yr,>30yr土壤固碳平均速率分别为0.02、0.13、0.19、0.18 Mg C / (ha·yr);(4)在植被恢复过程中,不同恢复阶段土壤碳固存的主要影响因子不同,总体来说,主要受气候因子调控(降雨和温度)。降雨量、温度、恢复年限、植被类型和初始碳储量对土壤碳固存变化的相对重要度分别为31.8%,16.3%,17.7%,15.9%和18.3%。本研究建议,建立基于固碳速率大小及固碳能力可持续性的生态恢复模式,通过可持续的科学管理增加植被数量和质量,将有效增加生态脆弱区土壤固碳量。

    Abstract:

    Soil organic carbon (SOC) sequestration is one of the effective ways to mitigate global climate change, and large-scale vegetation restoration has profoundly changed this process. Clarifying the changes of soil carbon sequestration and its driving factors in the process of ecological restoration in fragile areas has important reference value for ecological management and carbon sequestration and emission reduction.In this study, we analyzed the changes of SOC sequestration and its driving factors during the process of vegetation restoration (planted forest, planted shrub and abandoned grassland) on the arid and semi-arid Loess Plateau by synthesizing 100 peer-reviewed publications (935 observations and 55 sites) published between 1992 and 2020. The results showed that 1) the rate of SOC sequestration for planted forest and shrub was 0.30 Mg C / (ha·yr), which was higher than that of abandoned grassland (0.10 Mg C / (ha·yr)). In addition, the rate of evergreen tree species (0.45 Mg C ha-1yr-1) was higher than that of deciduous tree species (0.33 Mg C / (ha·yr)), but the latter had higher SOC sequestration amount. After 51 years, the evergreen tree species may have greater carbon sequestration benefit; 2) The SOC sequestration rate increased with precipitation, but the change degree was affected by vegetation types and restoration years; 3) Regionally, SOC sequestration rate continued to increase (<30yr) and thereafter stabilized (>30yr). The average SOC sequestration rates in 0-10yr, 10-20yr, 20-30yr and >30yr were 0.02, 0.13, 0.19 and 0.18 Mg C / (ha·yr), respectively; (4) Overall, the main influencing factors of SOC sequestration was different in various restoration stages. Generally speaking, the SOC sequestration is mainly regulated by climatic factors (precipitation and temperature). The relative importance of precipitation, temperature, restoration age, vegetation types and initial SOC stock were 31.8%, 16.3%, 17.7%, 15.9% and 18.3%, respectively. Finally, we suggest that a sustainable ecological restoration model based on SOC sequestration rate and capacity should be established, and the amount and quality of vegetation should be increased through sustainable scientific management, which will effectively increase the amount of SOC sequestration in ecologically fragile areas.

    参考文献
    相似文献
    引证文献
引用本文
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2024-12-11
  • 最后修改日期:2025-01-13
  • 录用日期:2025-01-14
  • 在线发布日期:
  • 出版日期: