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Quantitative analysis of moisture content and temperature of landfill soil cover and their effect on methane emission.

机译:垃圾填埋场土壤水分和温度的定量分析及其对甲烷排放的影响。

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The amount of methane that vent from landfills is dependent on the physical, chemical and biological components of the soil cover. Especially moisture content and temperature of the soil are known as the major controlling factors. Previous studies have attempted to correlate moisture content and temperature with methane emission by collecting soil samples from landfill soil covers and analyzing them in the laboratory for moisture content determination. However, the moisture content of the soil continuously changes within minutes to hours as a result of change in temperature. In-situ moisture content measurement is therefore, very critical to capture the continuous change of moisture content. The presented study used Time Domain Reflectometry (TDR) to measure in-situ moisture content.; Moisture content, temperature and methane data of the landfill soil cover were collected and analyzed. Attributes of soil grain size such as D 10, D30, D60 and uniformity coefficient, C u, of the soil were analyzed and their influence on moisture content and methane emission was examined. Methane emission showed good temporal correlation with soil temperature, however, no significant relationship between moisture content and methane emission was observed.; The author used kriging and polynomial regression methods to characterize the spatial distribution of moisture content and methane emission. Spatial distribution of soil attributes was also analyzed to examine its effect on those variables. The spatial pattern of moisture content was quite similar to that of uniformity coefficient, Cu and that of clay content of the soil but strongly contrasted to that of methane emission.
机译:从垃圾填埋场排放的甲烷量取决于土壤覆盖物的物理,化学和生物成分。特别是土壤的水分含量和温度是主要的控制因素。以前的研究试图通过从垃圾填埋场的土壤覆盖层中收集土壤样品并在实验室中进行分析以测定水分含量,从而将水分含量和温度与甲烷排放量相关联。然而,由于温度的变化,土壤的水分含量在数分钟至数小时内连续变化。因此,现场水分含量测量对于捕获水分含量的连续变化非常关键。提出的研究使用时域反射仪(TDR)来测量原位水分含量。收集并分析了垃圾填埋场土壤覆盖物的水分含量,温度和甲烷数据。分析了土壤粒径的属性,例如D 10,D30,D60以及土壤的均匀度系数C u,并研究了它们对水分和甲烷排放的影响。甲烷排放与土壤温度具有良好的时间相关性,但是,水分含量与甲烷排放之间没有显着关系。作者使用克里金法和多项式回归方法来表征水分含量和甲烷排放的空间分布。还分析了土壤属性的空间分布,以检查其对这些变量的影响。水分含量的空间格局与均匀度系数,铜和土壤粘土含量的格局十分相似,但与甲烷排放呈强烈对比。

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