Carbon biogeochemistry and CO2 emissions in a human impacted and mangrove dominated tropical estuary (Can Gio, Vietnam)

被引:0
|
作者
Frank David
Tarik Meziane
Nhu-Trang Tran-Thi
Vinh Truong Van
Nguyen Thanh-Nho
Pierre Taillardat
Cyril Marchand
机构
[1] Sorbonne Universités,Faculty of Chemistry
[2] MNHN,Department of Geography
[3] UPMC Univ Paris 06,undefined
[4] UNICAEN,undefined
[5] UA,undefined
[6] CNRS,undefined
[7] IRD,undefined
[8] Biologie des Organismes et Ecosystèmes Aquatiques (BOREA),undefined
[9] University of Science Vietnam National University,undefined
[10] IMPMC,undefined
[11] Institut de Recherche pour le Développement (IRD),undefined
[12] UPMC,undefined
[13] CNRS,undefined
[14] MNHN,undefined
[15] Nong Lam University,undefined
[16] National University of Singapore,undefined
来源
Biogeochemistry | 2018年 / 138卷
关键词
Tropical estuary; Carbon speciation; Tidal cycle; Water–air CO; emissions; Vietnam;
D O I
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中图分类号
学科分类号
摘要
The quantitative contribution of tropical estuaries to the atmospheric CO2 budget has large uncertainties, both spatially and seasonally. We investigated the seasonal and spatial variations of carbon biogeochemistry downstream of Ho Chi Minh City (Southern Vietnam). We sampled four sites distributed from downstream of a highly urbanised watershed through mangroves to the South China Sea coast during the dry and wet seasons. Measured partial pressure of CO2 (pCO2) ranged from 660 to 3000 μatm during the dry season, and from 740 to 5000 μatm during the wet season. High organic load, dissolved oxygen saturation down to 17%, and pCO2 up to 5000 μatm at the freshwater endmember of the estuary reflected the intense human pressure on this ecosystem. We show that releases from mangrove soils affect the water column pCO2 in this large tropical estuary (~600 m wide and 10–20 m deep). This study is among the few to report direct measurements of both water pCO2 and CO2 emissions in a Southeast Asian tropical estuary located in a highly urbanised watershed. It shows that the contribution of such estuaries may have been previously underestimated, with CO2 emissions ranging from 74 to 876 mmol m−2 day−1 at low current velocity (< 0.2 m s−1). Corresponding gas transfer velocities k600, ranging from 1.7 to 11.0 m day−1, were about 2 to 4 times of k600 estimated using published literature equations.
引用
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页码:261 / 275
页数:14
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