黄河口不同生境下翅碱蓬湿地土壤碳、氮储量与垂直分布特征
其他题名Storage and Vertical Distribution Characteristics of Carbon and Nitrogen in Different Suaeda salsa Marsh Soils of the Yellow River Estuary
牟晓杰 ; 孙志高 ; 刘兴土
发表期刊土壤通报
ISSN0564-3945  
2012-12-06
卷号43期号:6页码:1444-1449
关键词黄河口 潮滩湿地 垂直分布
产权排序中国科学院东北地理与农业生态研究所;中国科学院烟台海岸带研究所;中国科学院研究生院;
通讯作者孙志高 zgsun@yic.ac.cn
作者部门中科院海岸带环境过程与生态修复重点实验室
英文摘要选择位于黄河口滨岸中潮滩和低潮滩上的翅碱蓬湿地为研究对象,对比研究了湿地土壤碳、氮在不同时期的垂直分布特征。结果表明,两种湿地土壤的TC、TN、NO3--N、NH4+-N和C/N在不同时期的垂直分布特征均存在不同程度差异,TC、TN的垂直分布特征主要受制于土壤有机质的分布和潮汐影响状况,NO3--N、NH4+-N主要与不同时期土壤水分条件差异及其引起的不同土层硝态氮的垂直淋失和对铵态氮的吸附程度有关,C/N的差异主要与其受陆源影响程度有关;两种湿地土壤TC、TN、NO3--N、NH4+-N和C/N在不同时期均存在较高的垂直变异性,原因主要与上下层土壤影响碳、氮分布的主导因素差异有关;两种湿地土...
中文摘要The Suaeda salsa marshes in middle tidal flat (MTF) and low tidal flat (LTF) of the Yellow River estuary, were selected as study objects, and the profile distribution characteristics of carbon (C) and nitrogen (N) in different periods were contrastively studied. Results showed that the vertical distribution characteristics of TC, TN, NO3 -- N, NH4 +- N and C/N in the two types of soil in different periods had some differences. The vertical distribution characteristics of TC and TN were mainly controlled by the distribution of soil organic matter and the effects of tide, while those of NO3 -- N and NH4 +- N were mainly correlated with the differences of soil water condition in different periods. The NO3 -- N vertical leaching and soil NH4 +- N adsorption were the direct reasons for the distribution of NO3 -- N and NH4 +- N in different periods. The C/N in different soils was related to the effects of terrestrial sources. The TC, TN, NO3 -- N, NH4 +- N and C/N in the two types of soil in different periods had significantly vertical variability, which were mainly correlated with the differences of dominant factors affecting the C and N distributions in topsoil and subsoil. The C and N stocks and their distribution statuses in MTF and LTF soils had significantly differences, and the C and N stocks of the latter (3.9413 kg m- 2 and 0.4041 kgm- 2) were much higher than those of the former (3.5964 kg m- 2 and 0.3639 kg m- 2). Except for the 40 - 50 cm and 50 - 60 cm layers, the C and N stocks in LTF soil in different layers were separately 2.87% - 51.01% and 2.52% - 3.89% higher than those in MTF soil.
资助机构国家海洋局海洋公益性行业科研专项经费项目(2012418008-3);; 国家自然科学基金(41171424,40803023);; 中国科学院战略性先导科技专项(XDA05030404);; 山东省自然科学基金重点项目(ZR2010DZ001);; 中国科学院人才专项(青年创新促进会)基金(Y129091041);; 国家重大科学研究计划项目(2012CD956100)资助
收录类别CSCD
语种中文
CSCD记录号CSCD:4691705
引用统计
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/5800
专题中国科学院海岸带环境过程与生态修复重点实验室
推荐引用方式
GB/T 7714
牟晓杰,孙志高,刘兴土. 黄河口不同生境下翅碱蓬湿地土壤碳、氮储量与垂直分布特征[J]. 土壤通报,2012,43(6):1444-1449.
APA 牟晓杰,孙志高,&刘兴土.(2012).黄河口不同生境下翅碱蓬湿地土壤碳、氮储量与垂直分布特征.土壤通报,43(6),1444-1449.
MLA 牟晓杰,et al."黄河口不同生境下翅碱蓬湿地土壤碳、氮储量与垂直分布特征".土壤通报 43.6(2012):1444-1449.
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