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

机译:碳生物地球化学和人类受影响的二氧化碳排放和红树林主导的热带河口(Can Gio,越南)

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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 (pCO(2)) ranged from 660 to 3000 mu atm during the dry season, and from 740 to 5000 mu atm during the wet season. High organic load, dissolved oxygen saturation down to 17%, and pCO(2) up to 5000 mu atm 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 pCO(2) in this large tropical estuary (similar to 600 m wide and 10-20 m deep). This study is among the few to report direct measurements of both water pCO(2) 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 k(600), ranging from 1.7 to 11.0 m day(-1), were about 2 to 4 times of k(600) estimated using published literature equations.
机译:热带河口对大气CO2收支的定量贡献在空间和季节上都有很大的不确定性。我们调查了越南南部胡志明市下游碳生物地球化学的季节和空间变化。在旱季和雨季,我们对从高度城市化的流域下游穿过红树林到南海海岸的四个地点进行了采样。在旱季测得的二氧化碳分压(pCO(2))范围为660至3000μatm,在雨季测得的分压范围为740至5000μatm。河口淡水端的高有机负荷、低至17%的溶解氧饱和度和高达5000亩atm的pCO(2)反映了人类对该生态系统的巨大压力。我们发现,红树林土壤的释放会影响这个大型热带河口(类似于600米宽和10-20米深)的水柱pCO(2)。这项研究是为数不多的直接测量位于高度城市化流域的东南亚热带河口水域pCO(2)和CO2排放量的报告之一。它表明,这些河口的贡献以前可能被低估了,在低流速(;0.2 m s(-1))下,二氧化碳排放量在74到876 mmol m(-2)天(-1)之间。相应的气体传输速度k(600),范围为1.7至11.0 m day(-1),约为使用已发表文献方程式估算的k(600)的2至4倍。

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