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Distribution, flux and biological consumption of carbon monoxide in the Southern Yellow Sea and the East China Sea

机译:一氧化碳在南黄海和东海的分布,通量和生物消耗

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摘要

Carbon monoxide (CO) concentration distribution and microbial consumption rate constants, along with atmospheric CO mixing ratios, were measured in the Southern Yellow Sea (SYS) and the East China Sea (ECS) in November 2007. The surface water CO concentrations in the investigated area ranged from 0.13 to 2.30 nmol L~(-1), with an average of 0.68 nmol L~(-1). Vertical profiles showed that CO concentrations declined with depth, with the maximum values appearing in the surface water (0-1 m). The diurnal variations of seawater CO concentrations were investigated at two anchor stations and the results showed that CO concentrations varied by a factor of 6-8 in the diurnal cycle, with maximum values appearing in the surface water (0-1 m). Atmospheric CO mixing ratios varied from 165 to 671 ppbv, with an average of 297 ppbv; these ratios decreased from 380 to 253 ppbv in the seaward direction and increased from 239 to 345 ppbv from south to north in the studied areas. Undersaturation was observed at eight of the 55 stations measured (15%) and the saturation factors ranged from 0.58 to 15.42, with an average of 3.34 ± 2.95. The sea-to-air fluxes of CO in the SYS and the ECS ranged from 0.50 to 4.20 umol m~(-2) d~(-1), with an average of 1.82 ± 1.43 pmol m~(-2)d~(-1). In the incubation experiments, the microbial CO consumption rate constants in the surface water (K_(co)) ranged from 0.15 to 2.14 h~(-1). A negative correlation between K_(co) and salinity was observed in the present study.
机译:2007年11月,在南黄海(SYS)和东海(ECS)中测量了一氧化碳(CO)的浓度分布和微生物消耗率常数,以及大气中的CO混合比。面积范围为0.13至2.30nmol L〜(-1),平均为0.68nmol L〜(-1)。垂直剖面表明,CO浓度随深度下降,最大值出现在地表水(0-1 m)中。在两个锚定站研究了海水中CO浓度的日变化,结果表明,CO浓度在日循环中变化了6-8倍,最大值出现在地表水(0-1 m)中。大气中的CO混合比从165到671 ppbv不等,平均为297 ppbv。在研究区域中,这些比例在朝海方向上从380 ppbv下降到253 ppbv,从南到北从239 ppbv上升到345 ppbv。在所测量的55个站点中有8个站点观测到了欠饱和(15%),其饱和因子范围为0.58至15.42,平均值为3.34±2.95。 SYS和ECS中CO的海气通量范围为0.50至4.20 umol m〜(-2)d〜(-1),平均为1.82±1.43 pmol m〜(-2)d〜 (-1)。在温育实验中,地表水中微生物CO的消耗速率常数K_(co)为0.15〜2.14 h〜(-1)。在本研究中观察到K_(co)与盐度之间呈负相关。

著录项

  • 来源
    《Marine Chemistry》 |2010年第4期|p.74-82|共9页
  • 作者单位

    Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China,College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    carbon monoxide; distribution; biological consumption; diurnal variation; southern yellow sea; east china sea;

    机译:一氧化碳;分配;生物消耗;日变化南部黄海;东海;

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