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Air-water CO2 flux in an algae bloom year for Lake Hongfeng,Southwest China: implications for the carbon cycle of global inland waters

机译:中国西南地区红枫湖藻类开花年的空气-水CO2通量:对全球内陆水域碳循环的影响

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摘要

The carbon cycle of global inland waters is quantitatively comparable to other components in the global carbon budget.Among inland waters,a significant part is man-made lakes formed by damming rivers.Manmade lakes are undergoing a rapid increase in number and size.Human impacts and frequent algae blooms lead to it necessary to make a better constraint on their carbon cycles.Here,we make a primary estimation on the airwater CO2 transfer flux through an algae bloom year for a subtropical man-made lake-Hongfeng Lake,Southwest China.To do this a new type of glass bottles was designed for content and isotopic analysis of DIC and other environmental parameters.At the early stage of algae bloom,CO2 was transferred from the atmosphere to the lake with a net flux of 1.770 g.C.m-2.Later,the partial pressure (pCO2) of the aqueous CO2 increased rapidly and the lake outgassed to the atmosphere with a net flux of 95.727 g.C.m-2.In the remaining days,the lake again took up CO2 from the atmosphere with a net flux of 14.804 g.C.m-2.As a whole,Lake Hongfeng released 4527 t C to the atmosphere,accounting for one-third of the atmosphere/soil CO2 sequestered by chemical weathering in the whole drainage.With an empirical mode decomposition method,we found air temperature plays a major role in controlling water temperature,aqueous pCO2 and hence CO2 flux.This work indicates a necessity to make detailed and comprehensive carbon budgets in man-made lakes.
机译:全球内陆水域的碳循环在数量上可与全球碳预算中的其他组成部分相提并论。在内陆水域中,很大一部分是由堰塞河流形成的人造湖,人造湖的数量和规模都在迅速增加。在此,我们初步估算了亚热带人造湖-红峰湖通过藻类开花年的空气CO2传递通量。为此,设计了一种新型玻璃瓶,用于DIC的含量和同位素分析以及其他环境参数。在藻类开花初期,CO2以1.770 gCm-2的净通量从大气中转移到湖泊中。后来,二氧化碳水溶液的分压(pCO2)迅速增加,湖泊以净通量95.727 gCm-2排入大气。在剩余的日子里,湖泊又从大气中吸收了二氧化碳。 ha净通量为14.804 gCm-2。总体上,洪峰湖向大气释放了4527 t C,占整个排水过程中化学风化作用所隔离的大气/土壤CO2的三分之一。采用经验模式分解方法,我们发现空气温度在控制水温,pCO2水溶液并进而控制CO2通量中起着重要作用。这项工作表明有必要对人造湖进行详细而全面的碳预算。

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  • 来源
    《中国地球化学学报(英文版)》 |2017年第4期|658-666|共9页
  • 作者

    Faxiang Tao;

  • 作者单位

    State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry, Chinese Academy of Sciences, 99 Lincheng West Road, Guanshanhu District,Guiyang 550081, Guizhou, China;

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