文伟, 彭友贵, 谭一凡, 史正军. 深圳市森林土壤主要类型有机碳分布特征[J]. 西南林业大学学报, 2018, 38(6): 106-113. DOI: 10.11929/j.issn.2095-1914.2018.06.014
引用本文: 文伟, 彭友贵, 谭一凡, 史正军. 深圳市森林土壤主要类型有机碳分布特征[J]. 西南林业大学学报, 2018, 38(6): 106-113. DOI: 10.11929/j.issn.2095-1914.2018.06.014
Wei Wen, Yougui Peng, Yifan Tan, Zhengjun Shi. Distribution Characteristics of Organic Carbon in Main Forest Soil Types in Shenzhen City[J]. Journal of Southwest Forestry University, 2018, 38(6): 106-113. DOI: 10.11929/j.issn.2095-1914.2018.06.014
Citation: Wei Wen, Yougui Peng, Yifan Tan, Zhengjun Shi. Distribution Characteristics of Organic Carbon in Main Forest Soil Types in Shenzhen City[J]. Journal of Southwest Forestry University, 2018, 38(6): 106-113. DOI: 10.11929/j.issn.2095-1914.2018.06.014

深圳市森林土壤主要类型有机碳分布特征

Distribution Characteristics of Organic Carbon in Main Forest Soil Types in Shenzhen City

  • 摘要: 通过对深圳市森林土壤主要类型91个调查样点土样的有机碳含量、有机碳密度和有机碳储量进行测算,分析各土壤类型的有机碳分布特征。结果表明:不同土壤类型的有机碳含量差异大,表现为盐渍沼泽土>黄壤>红壤>赤红壤>滨海沙土,平均有机碳含量7.15g/kg;不同土壤类型有机碳密度为盐渍沼泽土>红壤>赤红壤>黄壤>滨海沙土,平均有机碳密度8.00kg/m2;有机碳含量和密度随土层深度的增加而降低。全市森林土壤有机碳储量为581.01×104 Mg C,其中赤红壤有机碳储量最高,占88.77%,其后依次为红壤(11.45%)、黄壤(0.43%)、盐渍沼泽土(0.33%)和滨海沙土(0.02%);土壤表层(0~30cm)有机碳储量占55.95%。土壤有机碳含量与pH值呈显著负相关性(P < 0.05),与土壤容重呈极显著负相关性(P < 0.01)。

     

    Abstract: Through forest soil survey in 91 sample plots, soil organic carbon content, density and storage of all forest soil types were assessed and their distribution characteristics were therefore analyzed in Shenzhen City. The organic carbon contents among soil types were vastly different, and the order of content was salt swamp soil>yellow soil>red soil>latored soil>seashore sandy soil. The average content of forest soil organic carbon was 7.15g/kg. The soil organic carbon density was salt swamp soil>red soil>latored soil>yellow soil>seashore sandy soil; the average organic carbon density of forest soil was 8.00kg/m2. Forest soil carbon content and density declined with the increase of soil depth. The total organic carbon storage of forest soil was 581.01×104 Mg C in which the organic carbon storage of latored soil, red soil, yellow soil, salt swamp soil and seashore sandy soil accounted for 88.77%, 11.45%, 0.43%, 0.33% and 0.02%, respectively; the organic carbon storage in surface soil (0-30cm) accounted for 55.95%. Soil organic carbon content of forest soil was significantly negative correlated with pH value (P < 0.05) and very significantly negative correlated with soil volume weight (P < 0.01).

     

/

返回文章
返回