中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial and Seasonal Variations of Nutrients in Sediment Profiles and Their Sediment-Water Fluxes in the Pearl River Estuary, Southern China

文献类型:期刊论文

作者Zhang, L ; Wang, L ; Yin, KD ; Lu, Y ; Yang, YQ ; Huang, XP
刊名JOURNAL OF EARTH SCIENCE
出版日期2014
卷号25期号:1页码:197-206
关键词nutrient pore water sediment-water flux Pearl River Estuary
ISSN号1674-487X
通讯作者lzhang@scsio.ac.cn ; yinkd@mail.sysu.edu.cn
中文摘要Three cruises were launched in the Pearl River Estuary (PRE) in 2005 to investigate the biogeochemical cycling of nutrients associated with early diagenesis related to degradation of organic matter. Seasonal and spatial variations of pore water nutrient concentrations and profile patterns in sediments were studied. Nutrient fluxes at the sediment-water interface (SWI) were measured by incubation experiments, and we here discussed the accumulation and transformation processes of nutrients at the SWI. The nutrients generally decreased from the Pearl River outlets downstream, indicating anthropogenic influences on the nutrient inputs in the estuary. NO3-N concentration was the highest of the three forms of DIN (dissolved inorganic nitrogen, the sum of NH4-N, NO3-N and NO2-N) in the overlying water, and NH4-N was the main component of DIN in pore water. The gradual increase of NH4-N and the rapid decrease of NO3-N with sediment depth provided the evidence for anaerobic conditions below the SWI. Negative fluxes of NO3-N and positive fluxes of NH4-N were commonly observed, suggesting the denitrification of NO3-N at the SWI. The DIN flux direction suggested that the sediment was the sink of DIN in spring, however, the sediment was generally the source of DIN in summer and winter. PO4-P distribution patterns were distinct while SiO4-Si inconspicuously varied in sediment profiles in different seasons. The flux results indicated that PO4-P mainly diffused from the water column to the sediment while SiO4-Si mainly diffused from the sediment to the water column. Generally, the incubated fluxes were the coupling of diffusion, bioturbation and biochemical reactions, and were relatively accurate in this study.
学科主题Geology
收录类别SCI
资助信息National Natural Science Foundation of China [91328203, 41306110]
原文出处CHINA UNIV GEOSCIENCES
WOS记录号WOS:000330554900016
公开日期2014-12-11
源URL[http://ir.scsio.ac.cn/handle/344004/10476]  
专题南海海洋研究所_中科院海洋生物资源可持续利用重点实验室
推荐引用方式
GB/T 7714
Zhang, L,Wang, L,Yin, KD,et al. Spatial and Seasonal Variations of Nutrients in Sediment Profiles and Their Sediment-Water Fluxes in the Pearl River Estuary, Southern China[J]. JOURNAL OF EARTH SCIENCE,2014,25(1):197-206.
APA Zhang, L,Wang, L,Yin, KD,Lu, Y,Yang, YQ,&Huang, XP.(2014).Spatial and Seasonal Variations of Nutrients in Sediment Profiles and Their Sediment-Water Fluxes in the Pearl River Estuary, Southern China.JOURNAL OF EARTH SCIENCE,25(1),197-206.
MLA Zhang, L,et al."Spatial and Seasonal Variations of Nutrients in Sediment Profiles and Their Sediment-Water Fluxes in the Pearl River Estuary, Southern China".JOURNAL OF EARTH SCIENCE 25.1(2014):197-206.

入库方式: OAI收割

来源:南海海洋研究所

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