CAJ | 학술논문

通过研究崇明东滩不同类型天然湿地土壤在不同潮间的有机质(OM)、全氮(TN)、全磷(TP)的含量与分布,进而分析不同类型滨海湿地土壤作为营养盐氮、磷汇与碳沉积的环境效应.结果表明,芦苇型沙质湿地土壤中有机质、全氮、全磷的平均值分别为1.36%、0.1%、0.03%,而芦苇,米草混合型黏质土壤中分别为2.41%、0.27%、0.07%.随着高程的增加(从光滩向高潮滩过渡),芦苇(Phragmites communis)型沙质湿地土壤与芦苇/米草(Phragmites communis/Spartina alterniflora)混合型黏质土壤中有机质、全氮含量平稳上升,但全磷变化并不显著.这表明芦苇,互花米草混合型黏质湿地土壤对造成沿海水域富营养化的氮、磷营养盐以及引起全球气候变化的碳排放具有更好的汇聚效应,同时高潮滩的汇聚功能总体较光滩为高.
통과연구숭명동탄불동류형천연습지토양재불동조간적유궤질(OM)、전담(TN)、전린(TP)적함량여분포,진이분석불동류형빈해습지토양작위영양염담、린회여탄침적적배경효응.결과표명,호위형사질습지토양중유궤질、전담、전린적평균치분별위1.36%、0.1%、0.03%,이호위,미초혼합형점질토양중분별위2.41%、0.27%、0.07%.수착고정적증가(종광탄향고조탄과도),호위(Phragmites communis)형사질습지토양여호위/미초(Phragmites communis/Spartina alterniflora)혼합형점질토양중유궤질、전담함량평은상승,단전린변화병불현저.저표명호위,호화미초혼합형점질습지토양대조성연해수역부영양화적담、린영양염이급인기전구기후변화적탄배방구유경호적회취효응,동시고조탄적회취공능총체교광탄위고.
Based on the analysis of different types and inter-tidal of wetlands about organic matter, TN, TP content and distribution in Chongming Dongtan, environmental effects of different coastal wetlands soil as nutrients meeting and carbon deposition were assessed. Results showed that organic matter, TN and TP on average of Phragmites communis-sandy wetlands soil were 1.36%, 0.1% and 0.03%, while the mixed wetlands soil of Phragmites communis-sandy wetlands soil were 2.41%, 0.27% and 0.07%. With the increase in elevation from low ebb to upsurge beach, organic matter and TN in the Phragmites communis-sandy wetlands soil and the mixed wetlands soil of Phragmites communis/Spartina alterniflora was in a smooth rise while TP change was not significant, which showed that the mixed wetlands soil of Phragmites communis / Spartina alterniflora has better clustering effect about N and P nutrients caused of eutrophication of coastal waters as well as the carbon emissions caused of global climate change, and the upsurge beach has better clustering function than the low ebb.