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Distribution and Rate of Methane Oxidation in Sediments of the Florida Everglades

机译:佛罗里达大沼泽地沉积物中甲烷氧化的分布和速率

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摘要

Rates of methane emission from intact cores were measured during anoxic dark and oxic light and dark incubations. Rates of methane oxidation were calculated on the basis of oxic incubations by using the anoxic emissions as an estimate of the maximum potential flux. This technique indicated that methane oxidation consumed up to 91% of the maximum potential flux in peat sediments but that oxidation was negligible in marl sediments. Oxygen microprofiles determined for intact cores were comparable to profiles measured in situ. Thus, the laboratory incubations appeared to provide a reasonable approximation of in situ activities. This was further supported by the agreement between measured methane fluxes and fluxes predicted on the basis of methane profiles determined by in situ sampling of pore water. Methane emissions from peat sediments, oxygen concentrations and penetration depths, and methane concentration profiles were all sensitive to light-dark shifts as determined by a combination of field and laboratory analyses. Methane emissions were lower and oxygen concentrations and penetration depths were higher under illuminated than under dark conditions; the profiles of methane concentration changed in correspondence to the changes in oxygen profiles, but the estimated flux of methane into the oxic zone changed negligibly. Sediment-free, root-associated methane oxidation showed a pattern similar to that for methane oxidation in the core analyses: no oxidation was detected for roots growing in marl sediment, even for roots of Cladium jamaicense, which had the highest activity for samples from peat sediments. The magnitude of the root-associated oxidation rates indicated that belowground plant surfaces may not markedly increase the total capacity for methane consumption. However, the data collectively support the notion that the distribution and activity of methane oxidation have a major impact on the magnitude of atmospheric fluxes from the Everglades.
机译:在缺氧的黑暗和有氧的光照以及黑暗的温育过程中,测量了来自完整岩心的甲烷排放速率。甲烷的氧化速率是在有氧的培养基础上通过使用缺氧排放量作为最大潜在通量的估算值来计算的。这项技术表明,甲烷氧化消耗了泥炭沉积物中最大潜在通量的91%,但在泥灰沉积物中氧化可忽略不计。确定完整芯的氧气微轮廓与就地测量的轮廓相当。因此,实验室培养似乎提供了原位活性的合理近似值。测量的甲烷通量与基于通过孔隙水原位采样确定的甲烷剖面预测的通量之间的一致性进一步证明了这一点。泥炭沉积物中的甲烷排放量,氧气浓度和渗透深度以及甲烷浓度曲线均对明暗变化敏感,这是通过现场分析和实验室分析确定的。与光照条件相比,光照条件下甲烷排放更低,氧气浓度和渗透深度更高;甲烷浓度曲线与氧气曲线的变化相对应,但估计的进入氧气区的甲烷通量变化很小。无沉淀物,与根相关的甲烷氧化显示出与核心分析中的甲烷氧化相似的模式:在泥灰沉积物中生长的根,甚至对于Cladium jamaicense的根,都没有检测到氧化,对于泥炭中的样品活性最高。沉积物。根系相关氧化速率的大小表明地下植物表面可能不会显着增加甲烷消耗的总容量。但是,这些数据共同支持了这样一种观念,即甲烷氧化的分布和活性对来自大沼泽地的大气通量的大小有重大影响。

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