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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Controls on the stable carbon isotopic composition of biogenic methane produced in a tidal freshwater estaurine sediment
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Controls on the stable carbon isotopic composition of biogenic methane produced in a tidal freshwater estaurine sediment

机译:控制潮汐淡水河口沉积物中生物甲烷的稳定碳同位素组成

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摘要

The #delta#~(13)C value of methane in sediments from a tidal freshwater site in the White Oak River Estuary, North Carolina, exhibited a relatively small, but consistent, seasonal variation (approx 3 per thousand) with isotopically heavier values occurring during the warmer months (-66.1 per thousand summer, -69.2 per thousand winter). These isotopic shifts could have resulted from changes in: (1) isotopic compositions of precursor molecules; (2) kinetic isotope effects associated with methane production; or (3) pathways of methane production. Methane production rate and isotopic data from sediment incubation experiments and field measurements were used to determine the relative contributions of these factors to the observed seasonal variations. Although changes in #delta#~(13)C values of biogenic methane are typically thought to result from changes in pathways of methane production, this study showed that a significant amount (36 +- 22%) of the seasonal variations between the #delta#~(13) value of methane produced in sediment incubation experiments could be attributed to changes in the #delta#~(13)C value of the #SIGMA#CO_2 pool. This was due to increased methane production rates and removal of ~(12)CO_2 with increasing temperature, a prevalent feature of methanogenic systems that may account for some of the frequently observed ~(13)C enrichment in methane during warmer months. Combining the change in the ~(13)C value of the #SIGMA#CO_2 pool with temperature-controlled changes in fractionation (#alpha#) resulting from kinetic isotope effects accounted for (53 +- 22%) of the ~(13)C enrichment observed during summer sediment incubation experiments. Although large pathway changes were not observed in sediment incubation experiments, the remaining differences in #delta#~(13)C values could have resulted from smaller, undetectable changes in the percentage of methane production from acetate (approx 14%) and/or a shift in the #delta#~(13)C values of methane produced from acetate (approx 4 per thousand).
机译:来自北卡罗来纳州白橡树河河口潮汐淡水站点沉积物中甲烷的δ-(13)C值表现出相对较小但稳定的季节性变化(约千分之三),且同位素值更重在较暖和的月份(夏季每千人-66.1,冬季每千人-69.2)。这些同位素变化可能是由于以下方面的变化引起的:(1)前体分子的同位素组成; (2)与甲烷产生有关的动力学同位素效应;或(3)甲烷生产途径。来自沉积物培养实验和现场测量的甲烷生产率和同位素数据用于确定这些因素对观测到的季节性变化的相对贡献。虽然通常认为生物甲烷的#delta#〜(13)C值变化是由甲烷生成途径的变化引起的,但这项研究表明,#delta之间有相当大的季节性变化(36±22%)沉积物孵育实验中产生的甲烷的#〜(13)值可归因于#SIGMA#CO_2池的#delta#〜(13)C值的变化。这是由于甲烷产生速率增加和温度升高而去除〜(12)CO_2所致,而甲烷化是甲烷生成系统的普遍特征,可能解释了在较暖的月份中甲烷中经常观察到的〜(13)C富集。将#SIGMA#CO_2库的〜(13)C值的变化与温度控制的由动态同位素效应引起的分馏(#alpha#)的变化相结合,占〜(13)的(53 +-22%)在夏季沉积物温育实验中观察到C富集。尽管在沉积物温育实验中未观察到较大的途径变化,但#delta#〜(13)C值的其余差异可能是由醋酸盐产生的甲烷百分比(约14%)和/或由醋酸盐产生的甲烷的δ(13)C值发生变化(约每千个4个)。

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