中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Rising flux of nutrients (C, N, P and Si) in the lower Mekong River

文献类型:期刊论文

作者Li, Siyue1,2; Bush, Richard T.1
刊名JOURNAL OF HYDROLOGY
出版日期2015-11-01
卷号530页码:447-461
关键词Nutrient flux Anthropogenic activities Nutrient limitation Nutrient stoichiometry Global change
ISSN号0022-1694
DOI10.1016/j.jhydrol.2015.10.005
通讯作者Li, SY (reprint author), So Cross Univ, Southern Cross GeoSci, POB 157, Lismore, NSW 2480, Australia.
英文摘要Changing human land use is accelerating global element cycling and appreciably altering ecosystems in the riverine-estuarine systems. This is evident by dramatic shifts in the supply of nutrients (C, N, P, Si). However, very little is known about the magnitude and rates of these changes. We examine the Mekong, one of the world largest rivers, to assess on a whole-of-system scale, the spatial, monthly and inter-annual flux of nutrients and stoichiometric ratios using a huge data-set (1985-2011). Seasonal and spatial patterns are apparent and linked to hydrology. The estimated mean flux (x10(9) mol/y) of elements from the Mekong at Pakse are 414.5 for DIC, 4.1 for DIN (3.3 for NO3--N and 0.8 for NH4+-N), 10.2 for TN, 0.32 for DIP, 0.46 for TP and 62.8 for DSi, respectively, which are intermediate relative to other large rivers. However, compared to the river reach at Pakse, the total river fluxes are two-fold greater for C, N, P and DSi. Annual flux increases significantly for DIC, NO3--N, DIN, TN and DSi, and is especially pronounced for all N and P species during the recent decade (1998 onward). Distinct shifts of nutrient stoichiometry, with far-reaching changes for phytoplankton productivity in the Mekong estuary are also evident, as the system shifts from potentially N limited to P limited. These notable changes to the exports and ratios of nutrient variables and anthropogenically-driven nutrient concerns are becoming a defining feature of the Mekong Plume to the South China Sea. (C) 2015 Elsevier B.V. All rights reserved.
资助项目Chinese Academy of Sciences, China ; SCU, Australia
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
WOS记录号WOS:000365050600037
出版者ELSEVIER SCIENCE BV
源URL[http://119.78.100.138/handle/2HOD01W0/2039]  
专题生态过程与重建研究中心
通讯作者Li, Siyue
作者单位1.So Cross Univ, Southern Cross GeoSci, Lismore, NSW 2480, Australia
2.Chinese Acad Sci, Key Lab Reservoir Aquat Environm, Chongqing Inst Green & Intelligent Technol, Chongqing 400714, Peoples R China
推荐引用方式
GB/T 7714
Li, Siyue,Bush, Richard T.. Rising flux of nutrients (C, N, P and Si) in the lower Mekong River[J]. JOURNAL OF HYDROLOGY,2015,530:447-461.
APA Li, Siyue,&Bush, Richard T..(2015).Rising flux of nutrients (C, N, P and Si) in the lower Mekong River.JOURNAL OF HYDROLOGY,530,447-461.
MLA Li, Siyue,et al."Rising flux of nutrients (C, N, P and Si) in the lower Mekong River".JOURNAL OF HYDROLOGY 530(2015):447-461.

入库方式: OAI收割

来源:重庆绿色智能技术研究院

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