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Spatial and temporal distribution of methane in an extensive shallow estuary, south India

机译:印度南部广阔浅河口甲烷的时空分布

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Sedimentary methane (CH4) ???uxes and oxidation rates were determined over the wet and dry seasons (four measurement campaigns)in Pulicat lake,an extensive shallow estuary in south India. Dissolved CH4 concentrations were measured at 52 locations in December 2000.The annual mean net CH4 ???ux from Pulicat lake sediments was 3.7 ?— 109 g yra?’1 based on static chamber measurements. A further 1.7 ?— 109 g yra?’1 was estimated to be oxidized at the sediment-water interface. The mean dissolved concentration of CH4 was 242 nmol la?’1 (ranging between 94 and 501 nmol la?’1) and the spatial distribution could be explained by tidal dynamics and freshwater input.Sea a€“air exchange estimates using models, account only for a??13%(0.5 ?— 109 g yra?’1) of the total CH4 produced in sediments, whereas ebullition appeared to be the major route for loss to the atmosphere (a??63% of the net sediment ???ux).We estimated the total atmospheric source of CH4 from Pulicat lake to be 0.5 to 4.0 ?— 109 g yra?’1.
机译:在印度南部一个宽阔的浅河口Pulicat湖,测定了干季和湿季的甲烷(CH4)通量和氧化速率(四个测量活动)。 2000年12月在52个地点测量了溶解的CH4浓度。根据静室测量结果,Pulicat湖沉积物的年均CH4净净ux为3.7?-109 g yra?-1。估计在沉积物-水界面上还会有1.7?-109 g yra?1被氧化。 CH4的平均溶解浓度为242 nmol la?'1(介于94至501 nmol la?'1之间),其空间分布可以用潮汐动力学和淡水输入来解释。沉积物中产生的CH4的CH4仅占总排放量的13%(0.5?-109 g yra?'1),而沸腾似乎是向大气损失的主要途径(占总沉积物的63%?我们估计来自Pulicat湖的CH4的总大气来源为0.5至4.0?-109 g yra?1。

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