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Patterns in pCO_2 in boreal streams and rivers of northern Quebec, Canada

机译:加拿大魁北克北部的北方河流和河流中pCO_2的模式

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摘要

Here we examine the patterns in carbon dioxide partial pressure (pCO_2) measured in a number of small boreal streams (<5 km in length) in the northwestern boreal region of Quebec during the ice-free season and compare these to the patterns found in a major river (Eastmain River) and in a tributary in the same region. All systems were consistently supersaturated in CO_2 (range 450 to 5000 μatm) streams having both higher (mean 1850 μatm) and more variable pCO_2 than that of rivers (range 550 to 800 μatm). Stream pCO_2 was positively related to DOC concentration and stream segment length, both suggesting a direct influence of the surrounding landscape. Calculated stream water-air CO_2 fluxes ranged from 700 to over 3000 mg C m~(-2) d~(-1),up to 2 orders of magnitude higher than those measured in large rivers and lakes of the same region. Small streams, despite their extremely reduced areal coverage (1% of the aquatic surface), accounted for 25% of the total aquatic C emissions, and the resulting areal stream fluxes were comparable to those measured in different soils or wetlands in the region.
机译:在这里,我们研究了在无冰季节,在魁北克西北部寒带地区的一些小型寒流(长度<5 km)中测量的二氧化碳分压(pCO_2)的模式,并将这些模式与主要河流(伊斯特曼河)和同一地区的支流。所有系统始终在CO_2(450至5000μatm范围)中过饱和,与河流(550至800μatm范围)相比,pCO_2的含量更高(平均值为1850μatm)并且变量pCO_2的变化更大。流pCO_2与DOC浓度和流段长度呈正相关,都暗示了周围景观的直接影响。计算得出的水-空气流CO_2通量范围为700至3000 mg C m〜(-2)d〜(-1),比同一地区大江湖中的测量值高出2个数量级。尽管小溪的面积被大大减少(占水面的1%),却占水生C排放总量的25%,并且所产生的溪流通量与该地区不同土壤或湿地的通量相当。

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