1990—2020年中国东北地区土地利用变化对SOC储量的影响
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秦祝元(1999-),男,硕士研究生,主要从事土地利用与土壤有机碳相互作用研究。E-mail:zhuyuanqing@myyahoo.com

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X825

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国家重点研发计划项目(2021YFD1500100)


Impact of Land-Use Changes on SOC Stocks in Northeast China from 1990 to 2020
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    摘要:

    [目的] 旨在探讨土地利用和覆盖变化(land use and cover change,LUCC)对东北地区特定土壤类型碳储量的影响。[方法] 依据获取的土壤有机碳(soil organic carbon,SOC)储量数据和1990—2020年土地覆盖数据,采用ArcGis软件进行空间分析,提取长期耕地和地类转化期,分析LUCC动态及其对SOC储量的影响机制。[结果] 1)1990—2020年,研究区总体为碳源状态,SOC储量减少0.046 Pg。具体来看,耕地和湿地的SOC储量分别减少0.111、0.007 Pg,其他土地利用类型的SOC储量下降0.313 Pg,而草地和林地的SOC储量分别增加0.102、0.283 Pg。2)长期耕作导致SOC储量损失0.341 Pg;天然土地(林地和草地)开垦使得SOC分别损失5.79%和4.32%。3)土地利用变化主要表现为耕地面积减少(11 917 km2),林地和草地面积增加(1 535~4 213 km2);湿地面积减少(1 185 km2),且主要分布在内蒙古和黑龙江(89.00%)。4)耕地面积的减少主要转化为草地(64.00%)和其他用地(29.00%),其中草甸土、暗棕壤和黑钙土是主要的土壤类型。湿地减少的区域主要分布在黑土和草甸土地区,其他土地利用类型转化为林地和草地时,主要涉及的土壤类型为暗棕壤(15.00%~41.00%)和草甸土。[结论] 东北地区SOC的储量变化主要由天然土地开垦及长期耕作驱动,受退耕还林还草政策和生态修复需求推动。未来应加强黑龙江地区的耕地与湿地恢复及林地、草地保护,以提升SOC储量。

    Abstract:

    [Objective] To investigate the effects of land use and cover change(LUCC)on carbon stocks of specific soil types in northeast China. [Methods] Based on the obtained soil organic carbon(SOC)stock data and land cover data from 1990 to 2020,ArcGis was used for spatial analysis to extract long-term cropland and land type conversion periods. LUCC dynamics and their influencing mechanism on SOC stocks were analyzed. [Results] 1)From 1990 to 2020,the study area generally maintained as a carbon source,with SOC stocks decreasing by 0.046 Pg. Specifically,SOC stocks in croplands and wetlands decreased by 0.111 Pg and 0.007 Pg, respectively,while those of other land-use types declined by 0.313 Pg. In contrast,SOC stocks in grasslands and forests increased by 0.102 and 0.283 Pg,respectively. 2)Long-term cultivation resulted in a loss of 0.341 Pg of SOC stocks. Reclamation of natural lands(forests and grasslands)led to SOC losses of 5.79% and 4.32%,respectively. 3)Land-use changes were mainly reflected in a decrease in cropland area(11 917 km2 )and an increase in forest and grassland areas(1 535-4 213 km2 ). Wetlands decreased by 1 185 km2,primarily occurring in Inner Mongolia and Heilongjiang(89.00%). 4)The decreased cropland area was mainly converted into grasslands(64.00%) and other land types(29.00%),with meadow soil,dark brown soil,and chernozem being the main soil types. Wetland loss mainly occurred in black soil and meadow soil regions,while the conversion of other land-use types into forests and grasslands primarily involved dark brown soil(15.00%-41.00%)and meadow soil. [Conclusion] Changes in SOC stocks in northeast China are mainly driven by natural land reclamation and long-term cultivation,as well as the policies of returning croplands to forests and grasslands and the demand for ecological restoration. In the future, efforts should be strengthened to restore croplands and wetlands and to protect forests and grasslands in Heilongjiang,so as to enhance SOC stocks.

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秦祝元, 刘焕军, 孟祥添, 王翔, 于云飞.1990—2020年中国东北地区土地利用变化对SOC储量的影响[J].水土保持学报,2025,39(5):421~428

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  • 收稿日期:2025-04-07
  • 最后修改日期:2025-05-16
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  • 在线发布日期: 2025-10-20
  • 出版日期: 2025-10-28
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