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Spatial Variations On Methane Emissions From Zoige Alpine Wetlands Of Southwest China

机译:中国西南部佐伊格高山湿地甲烷排放量的空间变化

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This study was aimed to understand the spatial variation of CH_4 emissions from alpine wetlands in Southwest China on a field-scale in two phenological seasons, namely the peak growing season and the spring thaw. Methane emission rates were measured at 30 plots, which included three kinds of environmental types: dry hummock, Carex muliensis and Eleocharis ualleculosa sites. There were highly spatial variations of methane emissions among and within different environmental types in both phenological seasons. Mean methane emission rates ranged from 1.1 to 37.0 mg CH_4 m~(-2) h(-1) in the peak growing season and from 0.004 to 0.691 mg CH_4 m~(-2) h~(-1) in the spring thaw. In the peak growing season, coefficients of variation (CV) averaged 38% among environmental types and 64% within environmental types; while in the spring thaw, CV were on the average 61% among environmental types and 96% within environmental types. The key influencing factors were the standing water table and the plant community height in the peak growing season, while in the spring thaw, no significant correlations between factors and methane emissions were found.
机译:本研究旨在了解中国西南高山湿地CH_4排放量在两个物候季节的田间尺度上的空间变化,即高峰生长期和春季解冻。在30个样地中测量了甲烷排放率,其中包括三种环境类型:干山岗,穆里斯苔草(Carex muliensis)和拟南芥(Eleocharis ualleculosa)。在两个物候季节中,不同环境类型之间和之内的甲烷排放量存在很大的空间差异。春季融化期平均甲烷排放速率在1.1至37.0 mg CH_4 m〜(-2)h〜(-1)范围内,在0.004至0.691 mg CH_4 m〜(-2)h〜(-1)范围内。 。在高峰生长期,环境类型之间的变异系数(CV)平均为38%,环境类型内部的变异系数(CV)平均为64%;而在春季解冻时,环境类型中的CV平均为61%,环境类型中的CV平均为96%。主要影响因素是生长期高峰期的地下水位和植物群落高度,而在春季融化时,甲烷和甲烷排放之间没有显着相关性。

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