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[中国泉州湾滨海湿地沉积物中碳和氮的空间变化]

[Spatial variations of carbon and nitrogen in coastal wetland sediments of Quanzhou Bay in China].

作者信息

Wang Ai-jun, Chen Jian, Li Dong-yi, Zhuo Zhi-qiang

机构信息

Open Laboratory of Ocean & Coast Environmental Geology, Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China.

出版信息

Huan Jing Ke Xue. 2007 Oct;28(10):2361-8.

Abstract

Six short sediment cores were collected from different coastal wetlands of Quanzhou Bay in order to obtain the particle size distribution and median grain size by laser particle size analyzer, and the contents of total organic carbon (TOC), total nitrogen (TN) and total inorganic carbon (TIC) by element analyzer. Analysis results show that sediment in coastal wetlands of Quanzhou Bay can be classified as silt and clayey-silt, and the median grain size varies from 9.2 microm to 18.5 microm. The TIC content in bare flat sediments of Shuitou area is about 0.137%, which is higher than that in coastal wetland covered by Spartina alterniflora (0.014%-0.038%). TIC content decreases when grain size decreases in these sediments. Contents of TOC and TN vary from 0.939% to 2.057% and from 0.163% to 0.260% respectively. Spartina alterniflora has a strong absorption ability of carbon and nitrogen while mangrove has a weak one, and sewage discharge increases the TOC content in the sediments of Shuitou area which is higher than that of Luoyangjiang River estuary. Weak correlations occur between the contents of TOC and TN and median grain size; a typical strong positive relationship is observed between TOC and TN contents; and significant positive relationships of TN content with C/N ratio in Spartina alterniflora wetland and TOC content with C/N ratio in Spartina alterniflora wetland and bare flat are also observed. All these data indicate that the sources of TOC and TN in the coastal wetland sediments of Quanzhou Bay originate from sewage discharge and biogenic production.

摘要

为了通过激光粒度分析仪获得粒度分布和中值粒径,并通过元素分析仪获得总有机碳(TOC)、总氮(TN)和总无机碳(TIC)的含量,从泉州湾不同的沿海湿地采集了6个短沉积岩芯。分析结果表明,泉州湾沿海湿地的沉积物可分为粉砂和黏土质粉砂,中值粒径在9.2微米至18.5微米之间变化。水头地区裸滩沉积物中的TIC含量约为0.137%,高于互花米草覆盖的沿海湿地(0.014%-0.038%)。在这些沉积物中,TIC含量随粒度减小而降低。TOC和TN的含量分别在0.939%至2.057%和0.163%至0.260%之间变化。互花米草对碳和氮具有较强的吸收能力,而红树林的吸收能力较弱,污水排放增加了水头地区沉积物中的TOC含量,该地区高于洛阳江河口。TOC和TN含量与中值粒径之间存在弱相关性;TOC和TN含量之间观察到典型的强正相关关系;还观察到互花米草湿地中TN含量与C/N比以及互花米草湿地和裸滩中TOC含量与C/N比之间存在显著正相关关系。所有这些数据表明,泉州湾沿海湿地沉积物中TOC和TN的来源源于污水排放和生物源生产。

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