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首页> 外文期刊>Estuarine Coastal and Shelf Science >Inter-annual variability of CO_(2) exchanges between an emersed tidal flat and the atmosphere
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Inter-annual variability of CO_(2) exchanges between an emersed tidal flat and the atmosphere

机译:涌潮后的潮滩与大气之间CO_(2)交换的年际变化

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Carbon dioxide ( CO_(2)) exchanges between a tidal flat (Wadden Sea, Netherlands) and the atmosphere were measured during a three-year survey. CO_(2) exchanges were monitored during 1-2 days each month between September 2006 and September 2009 using a flux chamber. The flux of CO_(2) was separated into two fluxes: the dark flux and the gross light flux, with the dark flux representing the flux during darkness and the gross light flux the difference between the net CO_(2) flux (measured under light) and the dark flux. It was argued that dark and light fluxes may deviate from respiration and photosynthesis, as the fluxes between wet tidal sediment and the atmosphere are affected by the partial pressure of CO_(2) in pore water, which is only gradually changed by sources and sinks of CO_(2) in the sediment. Light and dark fluxes were empirically related to environmental parameters in order to interpolate between succeeding measure-ments. The dark flux appeared to increase with temperature and the light flux became more intense with increasing irradiance with signs of saturation at high light levels on many but not all measurement days. These relations with environmental parameters showed seasonal and inter-annual variability. Fluxes were negligible just after the site was emersed and it took up to 3 h of emersion until fluxes were adapted to environmental conditions. Dark and light fluxes both showed strong seasonality with high values in summer and low values in winter. The tidal flat appeared as a source of atmospheric CO2 in the first year of measurement (+0.35 mol CO_(2) m~(-2) yr~(-1)) and a sink in the following two years (-1.59 and -0.72 mol CO_(2) m~(-2) yr~(-1)). Since the source of CO_(2) was observed during an extremely warm year, we suggest that climate warming might influence the carbon budget of tidal flats.
机译:在为期三年的调查中,测量了滩涂(荷兰瓦登海)与大气之间的二氧化碳(CO_(2))交换。在2006年9月至2009年9月之间,每月使用通量室监测1-2次CO_(2)交换。 CO_(2)的通量分为两个通量:暗通量和总光通量,其中暗通量代表黑暗期间的通量,总光通量表示净CO_(2)通量之间的差(在光照下测量) )和暗通量。有人认为,由于潮汐沉积物和大气之间的通量受孔隙水中CO_(2)的分压的影响,暗和光通量可能会与呼吸和光合作用相偏离,而孔隙水中的CO_(2)分压会影响该通量。沉积物中的CO_(2)。光和暗通量根据经验与环境参数相关,以便在后续的测量之间进行插值。在许多而非全部测量日中,暗通量似乎随着温度的升高而增加,并且随着辐照度的增加,光通量变得更加强烈,并且在高光照水平下出现饱和迹象。这些与环境参数的关系显示出季节和年际变化。现场被淹没后,通量可以忽略不计,并且要花3个小时才能出现,直到通量适应环境条件为止。暗和光通量都表现出强烈的季节性,夏季高,冬季低。在测量的第一年,潮滩出现为大气CO2的来源(+0.35 mol CO_(2)m〜(-2)yr〜(-1)),而在随后的两年(-1.59和- 0.72 mol CO_(2)m〜(-2)yr〜(-1))。由于在非常温暖的一年中观测到了CO_(2)的来源,因此我们建议气候变暖可能会影响潮滩的碳收支。

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