长江流域资源与环境 >> 2025, Vol. 34 >> Issue (4): 757-768.doi: 10.11870/cjlyzyyhj202504005

• 自然资源 • 上一篇    下一篇

苏南小流域不同类型湿地土壤碳含量及生态化学计量特征

郝社锋1,张楠2,3,李文博1,任静华1,刘玲1,王兆德2,刘成2,张雷2*   

  1. (1. 自然资源部国土(耕地)生态监测与修复工程技术创新中心,江苏省地质调查研究院,江苏 南京 210018; 2. 中国科学院南京地理与湖泊研究所,湖泊与环境国家重点实验室,江苏 南京 210008;3.湖北省生态环境监测中心站,湖北 武汉 430072)
  • 出版日期:2025-04-20 发布日期:2025-04-29

Soil Organic Carbon and Ecological Stoichiometry of Wetlands Within A Sub-Basin In Southern Jiangsu Province

HAO She-feng1, ZHANG Nan2,3, LI Wen-bo1, REN Jing-hua1, LIU Ling1, WANG Zhao-de2, LIU Cheng2, ZHANG Lei2   

  1. (1. Technology Innovation Center for Ecological Monitoring & Restoration Project on Land (Arable), Ministry of Natural Resources, Geological Survey of Jiangsu Province, Nanjing 210018,China; 2. State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008,China;3.Monitoring Center of Ecology and Environment of Hubei Province,Wuhan 430072,China)
  • Online:2025-04-20 Published:2025-04-29

摘要: 数量众多、分布广泛的小微湿地面临土壤碳储量及生态化学计量特征研究不足的问题,制约着对湿地碳储量的精确核算及对碳汇潜力的认识。以苏南地区塘马水库流域河流、水库消落带、水库敞水区、淡水养殖场、农用池塘、稻田等不同类型湿地土壤为研究对象,采集0~1 m湿地土壤剖面样品,分析了土壤有机碳(SOC)、总氮(TN)、总磷(TP)含量及其生态化学计量比值。各类型湿地SOC为3.65±3.60~8.17±6.26 mg/g,C/N为7.7±4.6~10. 8±2.5,C/P为18.0±6.2~34.4±16.4, N/P为1.9±0.5~3.1±1.4;不同类型湿地土壤SOC、TN、TP、C/N、C/P、N/P之间差异显著(p < 0.01),整体而言,其在水库消落带、稻田较高,在河流、水库敞水区与淡水养殖塘较低。经核算,各类型湿地土壤碳密度为4.41±3.94~9.37±5.81 kg/m2,低于全国平均水平,与我国海岸湿地、及东部湖泊湿地处于同一水平,而同时较高的氮磷含量表明该区域有良好的碳汇潜力。

Abstract: Small wetlands are distributed widely. However, the soil carbon stock and ecological stoichiometric characteristics of the wetlands have received little attention, which may restrict the accurate calculation of the budget of wetland carbon stock. In this study, six types of wetlands in the Tangma Reservoir watershed in southern Jiangsu Province were selected, which included river, water-level-fluctuating zone of reservoir, open-water zone of reservoir, freshwater farm, agricultural pond, and paddy field. Specifically, soil profiles of 1 m depth were collected and analyzed for soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), and the ecological stoichiometric ratio. Soil SOC, C/N, C/P and N/P were measured as 3.65±3.60~8.17±6.26 mg/g, 7.7±4.6~10.8±2.5, 18.0±6.2~34.4±16.4 and 1.9±0.5~3.1±1.4, respectively. Significant differences of soil SOC, TN, TP, C/N, C/P, and N/P among different wetlands were identified (p < 0.01). These elements were generally higher in the water-level-fluctuating zone of reservoir and paddy field, and lower in the open-water zone of reservoir, river, and freshwater farm. The soil carbon density of the six types of wetlands ranged 4.41±3.94~9.37±5.81 kg/m2, which was lower than the average of national wetlands, but at a close level to the results of coastal wetlands and eastern lake wetlands in China. The relatively higher TN and TP indicated that the wetlands had a great potential for carbon sinks.

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