近40年沈阳市耕地土壤有机碳变化速率时空特征

Temporal and Spatial Characteristics of Soil Organic Carbon Change Rate in Cultivated Land of Shenyang over the Past 40 Years

  • 摘要:
    目的 探究沈阳市近 40 年耕地土壤有机碳(SOC)含量及其变化速率(SOCr)时空特征,为耕地保护与双碳目标实现提供基础资料。
    方法 应用反距离权重插值法和GIS空间分析方法,结合沈阳市1980年、2008年和2020年土壤数据,对三个时期耕地SOC含量和SOCr时空特征进行分析。
    结果 近40年沈阳市耕地SOC含量及SOCr均呈先降低(1980 ~ 2008年)后增长(2008 ~ 2020年)趋势。1980年、2008年和2020年耕地SOC含量均值依次为10.58、10.09和11.27 g kg−1。其中,2020年最高,较 1980年增长 6.52%,较 2008年增长11.10%。沈阳市耕地SOC含量总体呈东高西低的分布格局,SOCr无明显空间分布特征。前期(1980 ~ 2008年)、后期(2008 ~ 2020年)和近40年整体(1980 ~ 2020年)耕地SOCr均值依次为 −0.02、0.10和0.02 g kg−1 a−1。从各区县来看,于洪区、新民市和康平县耕地SOCr始终为正值,且近40年整体SOCr较前期显著提高(P < 0.05),表明这些区域耕地土壤碳汇功能增强;沈北新区、苏家屯区和辽中区整体耕地SOCr由前期负值转变为正值,表明前期SOC下降趋势逆转,已实现从“碳源”到“碳汇”的转变;法库县耕地SOCr均值虽从近40年整体来看仍为负值,但经后期改良培肥,已较前期显著提升(P < 0.05);仅浑南区耕地SOCr均值较前期下降。
    结论 沈阳市耕地SOC含量和SOCr显著提升(P < 0.05),耕地土壤已从“碳源”转为“碳汇”,表明近年SOC提升和耕地质量培育工程取得了显著效果。未来应针对各区域耕地SOCr时空特征,因地制宜制定耕地SOC保护与提升政策。

     

    Abstract:
    Objective This study aims to explore the spatio-temporal characteristics of soil organic carbon (SOC) content and its change rate (SOCr) in cultivated land in Shenyang City over the past 40 years, thereby to provide basic data for cultivated land protection and the realization of the dual carbon goals.
    Method By means of the methods of Inverse Distance Weight interpolation and GIS spatial analysis, combining with the data from the soil survey in 1980, 2008 and 2020 in Shenyang City, the spatio-temporal characteristics of SOC content and SOCr of cultivated land during these periods were analyzed.
    Result SOC content and SOCr of cultivated land in Shenyang showed a trend of decreasing first (1980–2008) and then increasing (2008–2020) in recent 40 years. The average SOC content of cultivated land in Shenyang in 1980, 2008 and 2020 was 10.58, 10.09 and 11.27 g kg−1, respectively. Among them, it in 2020 was the highest, with an increase of 6.52% compared with 1980 and an increase of 11.10% compared with 2008. The SOCr of cultivated land in Shenyang in the early period (1980–2008), the later period (1980–2008) and the overall past 40 years (1980–2008) was -0.02, 0.10 and 0.02 g kg−1 a−1, respectively. From the perspective of the district and county scale, the SOCr of cultivated land in Yuhong District, Xinmin City and Kangping County in each period was positive, and the overall SOCr was significantly increased compared with the previous period (P < 0.05), indicating that the soil carbon sequestration capacity was further enhanced. The SOCr in Sujiatun District, Shenbei New District and Liaozhong District over the past 40 years was reversed from a negative value to a positive value, indicating that the decline trend of SOC in the previous period was reversed and the transformation from "carbon source" to "carbon sink". Although the SOCr in Faku County over the last 40 years was still negative, after improvement and fertilization, it had significantly increased compared with the previous periods (P < 0.05). Only SOCr in Hunnan District was further decreased.
    Conclusion SOC content and SOCr of cultivated land in Shenyang were significantly increased (P < 0.05), and the cultivated land soil had transformed from a "carbon source" to a "carbon sink", indicating that the input of SOC improvement and cultivated land quality cultivation projects had achieved remarkable results in recent years. In the future, the policies for the protection and improvement of cultivated land SOC should be formulated based on the spatio-temporal characteristics of cultivated land SOCr in each region and local conditions.

     

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