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首页> 外文期刊>Journal of Environmental Engineering >Spatial and temporal temperature distributions in municipal solid waste landfills
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Spatial and temporal temperature distributions in municipal solid waste landfills

机译:城市生活垃圾填埋场的时空温度分布

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Long-term spatial and temporal variations in temperatures have been investigated in covers, wastes, and liners at four municipal solid waste landfills located in different climatic regions: Alaska, British Columbia, Michigan, and New Mexico. Temperatures were measured in wastes with a broad range of ages from newly placed to old (up to 40 years). The characteristic shape of waste temperature versus depth relationships consisted of a convex temperature profile with maximum temperatures observed at central locations within the middle third fraction of the depth of the waste mass. Lower temperatures were observed above and below this central zone, with seasonal fluctuations occurring near the surface and steady and elevated values (above mean annual earth temperature) near the base of the landfills. Heat gain and long-term temperatures were directly affected by placement temperatures. Sustained concave temperature profiles were observed for winter waste placement. The highest heat gain and resulting high temperatures were observed in Michigan followed by British Columbia, New Mexico, and Alaska. The high heat gain in Michigan was attributed to coupled precipitation/moisture content and waste density. The time-averaged waste temperature ranges were 0.9-33.0, 14.4-49.2, 14.8-55.6, and 20.5-33.6°C in Alaska, British Columbia, Michigan, and New Mexico, respectively. Temperature increases occurred rapidly (over multiple years) in British Columbia and then dissipated for tens of years. Longer periods of temperature increase were observed at the other sites. Temperatures, temperature increases, and heat gain were higher during anaerobic decomposition of wastes than aerobic decomposition. A parametric study indicated that use of insulating materials over covers decreased temperature variations compared to uninsulated conditions for prevention of frost penetration or desiccation and for optimum methane oxidation. Overall, thermal regime of landfills is controlled by climatic and operational conditions.
机译:已经对位于不同气候区域的四个城市固体垃圾掩埋场(阿拉斯加,不列颠哥伦比亚省,密歇根州和新墨西哥州)的覆盖物,废物和衬里的温度进行了长期的时空变化研究。测量了从新放置到旧的各种年龄的垃圾中的温度(最长40年)。废物温度与深度关系的特征形状由凸形温度曲线组成,最高温度在废物质量深度的中间三分之一部分的中心位置观察到。在该中心区域的上方和下方观察到较低的温度,地表附近出现季节性波动,而垃圾填埋场底部附近出现稳定和升高的值(高于平均每年地球温度)。热量和长期温度直接受到放置温度的影响。观察到冬季废物放置时凹面温度曲线保持不变。在密歇根州观察到最高的热量获取和由此产生的高温,其次是不列颠哥伦比亚省,新墨西哥州和阿拉斯加。密歇根州的高热量获取归因于降水/水分含量和废物密度的结合。在阿拉斯加,不列颠哥伦比亚省,密歇根州和新墨西哥州,时间平均废物温度范围分别为0.9-33.0、14.4-49.2、14.8-55.6和20.5-33.6°C。在不列颠哥伦比亚省,温度升高迅速(持续数年),然后耗散了数十年。在其他地点观察到更长的温度升高期。废物的厌氧分解过程中的温度,温度升高和热量获取要高于好氧分解过程。一项参数研究表明,与非绝缘条件相比,在覆盖物上使用隔热材料可降低温度变化,从而防止霜冻渗透或干燥以及最佳的甲烷氧化。总体而言,垃圾填埋场的热状况受气候和操作条件的控制。

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