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长江流域不同地质生态环境土壤碳酸酐酶活性、有机碳含量及其相关性

潘伟志 Sila Onesmus Nzung’a 申泰铭 李 为 王晨玮 余龙江

潘伟志, Sila Onesmus Nzung’a, 申泰铭, 李 为, 王晨玮, 余龙江. 长江流域不同地质生态环境土壤碳酸酐酶活性、有机碳含量及其相关性[J]. 中国岩溶, 2016, 35(2): 173-178. doi: 10.11932/karst20160206
引用本文: 潘伟志, Sila Onesmus Nzung’a, 申泰铭, 李 为, 王晨玮, 余龙江. 长江流域不同地质生态环境土壤碳酸酐酶活性、有机碳含量及其相关性[J]. 中国岩溶, 2016, 35(2): 173-178. doi: 10.11932/karst20160206
PAN Wei-zhi, SILA Onesmus Nzung'a, SHEN Tai-ming, LI Wei, WANG Chen-wei, YU Long-jiang. Soil carbonic anhydrase activity, soil organic carbon and their relationships in different geological eco-environments of the Changjiang River basin[J]. CARSOLOGICA SINICA, 2016, 35(2): 173-178. doi: 10.11932/karst20160206
Citation: PAN Wei-zhi, SILA Onesmus Nzung'a, SHEN Tai-ming, LI Wei, WANG Chen-wei, YU Long-jiang. Soil carbonic anhydrase activity, soil organic carbon and their relationships in different geological eco-environments of the Changjiang River basin[J]. CARSOLOGICA SINICA, 2016, 35(2): 173-178. doi: 10.11932/karst20160206

长江流域不同地质生态环境土壤碳酸酐酶活性、有机碳含量及其相关性

doi: 10.11932/karst20160206
基金项目: 中国地质调查局地质调查工作项目子项目(12120113005200)子课题

Soil carbonic anhydrase activity, soil organic carbon and their relationships in different geological eco-environments of the Changjiang River basin

  • 摘要: 为了探讨流域岩溶生态系统土壤碳酸酐酶(CA)活性、有机碳含量及CA固碳之间的潜在关系,选取长江流域干流及支流沿岸不同地质生态环境下的10个样地,比较长江流域不同地质生态环境下表层土壤(0~20 cm)中的碳酸酐酶(CA)活性与土壤有机碳(SOC)含量,并分析二者之间的关系。结果表明:(1)长江流域岩溶区的表层土壤CA活性要高于非岩溶区(P<0.01),土壤CA活性的差异与样地的地质类型及植被类型不同有关;(2)位于岩溶区高场(GC)样地的年平均SOC含量最高(1.09%),而位于非岩溶区外洲(WZ)样地的年平均SOC含量最低(0.29%),而且总体比较而言,长江流域冬季表层土壤的平均SOC含量显著高于夏季(P<0.01);(3)相关性分析结果显示,不同季节长江流域岩溶区表层土壤CA活性与SOC含量呈一定的正相关。研究结果为进一步研究流域岩溶生态系统土壤CA与土壤固碳能力之间的关系奠定了基础。

     

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  • 发布日期:  2016-04-25

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