中国地质2024,Vol.51Issue(5) :1501-1512.DOI:10.12029/gc20230505002

重庆市表层土壤有机碳空间分布、影响因素及对碳减排的贡献

Spatial distribution,influencing factors and contribution to carbon emission reduction of topsoil organic carbon in Chongqing,China

鲍丽然 李瑜 张风雷 岳甫均 罗恺 邓海 严明书
中国地质2024,Vol.51Issue(5) :1501-1512.DOI:10.12029/gc20230505002

重庆市表层土壤有机碳空间分布、影响因素及对碳减排的贡献

Spatial distribution,influencing factors and contribution to carbon emission reduction of topsoil organic carbon in Chongqing,China

鲍丽然 1李瑜 1张风雷 2岳甫均 3罗恺 1邓海 1严明书1
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作者信息

  • 1. 重庆市地质矿产勘查开发局川东南地质大队,重庆 400030
  • 2. 重庆市地质矿产勘查开发局川东南地质大队,重庆 400030;重庆大学环境与生态学院,重庆 400044
  • 3. 天津大学地球系统科学学院,天津 300072
  • 折叠

摘要

[研究目的]土壤碳汇和岩溶碳汇共同构成自然地质碳汇,土壤中的碳参与碳循环的主要形式是有机碳.因此,土壤有机碳研究对提升土壤碳汇、实现"双碳"目标具有重要意义.[研究方法]基于多目标区域地球化学调查数据,利用地统计学方法分析了重庆市表层土壤有机碳密度空间分布,应用单因素方差分析及分类回归树法研究了土壤有机碳密度影响因素及其重要性,采用模型法评估了农田土壤固碳减排潜力.[研究结果]研究区表层土壤有机碳平均密度为 2.75 kg/m2,空间分布上具有中等程度空间自相关性,呈现南北两端高、中间低的分布格局.海拔、温度、土壤类型是影响有机碳密度的重要因素,降雨量、土地利用方式次之.农田土壤固碳潜力约为 36.88 Tg C,相当于 2018年重庆市能源消耗碳排放量的 24.10%.[结论]重庆市凉爽湿润的高海拔区表层土壤有机碳密度较大;不同土地利用方式中林草地、水田更利于土壤有机碳的积累.在达到碳平衡之前,农田土壤整体呈"碳汇"效应,吸收着空气中的碳.

Abstract

This paper is the result of environmental geological survey engineering.[Objective]Natural geological carbon sinks mostly consist of soil and karst carbon sinks,and the main form of carbon's participation in the carbon cycle in soil is organic carbon.Therefore,the study of topsoil organic carbon has great significance for increasing soil carbon sink and achieving the"carbon peaking and carbon neutrality"goal.[Methods]Based on the data of a multi-objective regional geochemical survey,this paper analyzed the spatial distribution of topsoil organic carbon density in Chongqing with the geostatistical method,studied the influencing factors and importance of soil organic carbon density by one-way ANOVA and classification regression tree and evaluated the carbon sequestration and emission reduction potential of the farmland soil with the model approach.[Results]The average density of topsoil organic carbon in the study area was 2.75 kg/m2,and the spatial distribution had a moderate degree of spatial autocorrelation,showing a distribution pattern of being high at the north and south ends and low in the middle.Altitude,temperature and soil type were the main factors affecting the organic carbon density,followed by precipitation and land use method.The carbon sequestration potential of farmland topsoil was about 36.88 Tg C,equivalent to 24.10% of Chongqing's carbon emissions from energy consumption in 2018.[Conclusions]The soil organic carbon density was relatively high in cool and humid high-altitude areas,in Chongqing;and forests,grasslands,and paddy fields can help with the accumulation of soil organic carbon among different land use methods.Before the carbon balanceis achieved,the farmland soil,has a"carbon sink"effect as a whole,absorbing carbon from the air.

关键词

土壤有机碳/空间分布/碳减排/地统计学/环境地质调查工程

Key words

soil organic carbon/spatial distribution/carbon emission reduction/geostatistics/environmental geological survey engineering

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基金项目

重庆市地质矿产勘查开发局2022年度科研项目(DKJ-2022-208-B-001)

出版年

2024
中国地质
中国地质调查局

中国地质

CSTPCD北大核心
影响因子:2.317
ISSN:1000-3657
参考文献量46
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