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首页> 外文期刊>Journal of Environmental Sciences >Emission characteristics of carbon dioxide in the semiarid Slipa grandis steppe in Inner Mongolia, China
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Emission characteristics of carbon dioxide in the semiarid Slipa grandis steppe in Inner Mongolia, China

机译:内蒙古半干旱Slipa grandis草原的二氧化碳排放特征

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Using the static opaque chamber method, the soil respiration rates (SR) were measured through the continuous experiments in situ, in semiarid Stipa grandis steppe in Xilin River Basin of Inner Mongolia, China from June 2001 to June 2003, in parallel, the difference between the SR and the ecosystem respiration rates (TER) were compared. The results indicated that the seasonal variations of the SR and TER were obvious with higher emissions in growing season and a relatively low efflux level in non-growing season, furthermore, the negative effluxes were found in the observation site in winter; the annual CO2 efflux of total ecosystem ranged from 160.5 gC/(m~2 centre dot a) to 162.8 gC/(m~2 centre dot a) and that of soil ranged from 118.7 gC/(m~2 centre dot a) to 152.3 gC/(m~2 centre dot a). The annual SR accounted for about 74.0 percent to 93.5 percent of the annual TER, but the results of Analysis of Variance (ANOVA) indicated that the difference between the annual average TER and SR did not reach the significance level of 0.05. The TER was under similar environmental controls as SR, in growing seasons of drought years, the variations of soil moisture at 0-10 cm and 10-20 cm depth could account for 79.1 percent-95.6 percent of the changes of the SR and TER, but in non-growing season, more than 75 percent of the variations of the SR and TER could be explained by the changes of the ground temperature of soil surface layers.
机译:采用静态不透明腔室法,通过连续实验原位测量了2001年6月至2003年6月内蒙古锡林河流域半干旱针叶草原针茅草原的土壤呼吸速率(SR)。比较了SR和生态系统呼吸速率(TER)。结果表明,SR和TER的季节变化明显,生长季节的排放量较高,非生长季节的排放量相对较低,冬季观测点的负排放量较大。整个生态系统的年CO2排放量从160.5 gC /(m〜2中心点a)到162.8 gC /(m〜2中心点a)和土壤的年均CO2排放量从118.7 gC /(m〜2中心点a)到152.3 gC /(m〜2中心点a)。年度SR约占年度TER的74.0%至93.5%,但方差分析(ANOVA)结果表明,年度平均TER和SR之间的差异未达到0.05的显着性水平。 TER处于与SR类似的环境控制下,在干旱年份的生长季节中,0-10 cm和10-20 cm深度的土壤水分变化可能占SR和TER变化的79.1%-95.6%,但是在非生长期,SR和TER变化的75%以上可以通过土壤表层地面温度的变化来解释。

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