TECHNICAL PAPERS
Nov 1, 2005

Heat Generation in Municipal Solid Waste Landfills

Publication: Journal of Geotechnical and Geoenvironmental Engineering
Volume 131, Issue 11

Abstract

This study was conducted to investigate thermal aspects of municipal solid waste landfills as a function of operational conditions and climatic region. Spatial and temporal distributions of waste temperatures were determined at four landfills located in North America (Michigan, New Mexico, Alaska, and British Columbia). Temperatures of wastes at shallow depths (extending to 6 to 8 m depth) and near the edges of a cell (within approximately 20 m) conformed to seasonal temperature variations, whereas steady elevated temperatures (23 to 57°C) with respect to air and ground temperatures were reached at depth and at central locations. Waste temperatures decreased from the elevated levels near the base of landfills, yet remained higher than ground temperatures. Thermal gradients in the range of approximately 30 to +22°Cm with average absolute values typically less than 5°Cm were measured within the wastes. Heat content (HC) of wastes was determined as the difference between measured waste mass temperatures and unheated baseline waste temperatures at equivalent depths. Peak HC values ranged from 12.5 to 47.8°Cdayday . The peak HCs were directly correlated with waste placement rates and initial waste temperatures, and they occurred at a specific average precipitation (2.3mmday) beyond which further precipitation did not contribute to heat generation. HC was determined to conform to exponential growth and decay curve relationships as a function of climatic and operational conditions. Heat generation was determined based on HC using 1D heat transfer analysis. The heat generation values ranged from 23 to 77MJm3 without losses and were significantly higher than biochemical prediction models, yet lower than values from incineration analyses. Overall, the highest values for temperatures, gradients, HC, and heat generation were observed in Michigan, followed by British Columbia, Alaska, and New Mexico. Integrated analysis of temperature and gas composition data indicated that temperature increases and HC values were greater during anaerobic decomposition than aerobic decomposition. Sustained high temperatures and heat generation occurred in wastes under anaerobic conditions.

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Acknowledgments

This study has been supported by the National Science Foundation (GOALI grant number CMS-9813248, SGER grant number CMS-0301032, and a 2004 AAAS/NSF WISC grant). The assistance of the partner landfills (Sauk Trail Hills Development, Corralitos Regional Landfill, Anchorage Regional Landfill, and Vancouver Landfill) is greatly appreciated.

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Go to Journal of Geotechnical and Geoenvironmental Engineering
Journal of Geotechnical and Geoenvironmental Engineering
Volume 131Issue 11November 2005
Pages: 1330 - 1344

History

Received: Jan 3, 2005
Accepted: Apr 29, 2005
Published online: Nov 1, 2005
Published in print: Nov 2005

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Authors

Affiliations

Nazli Yeşiller, A.M.ASCE
Associate Professor, Dept. of Civil and Environmental Engineering, Wayne State Univ., Detroit, MI 48202.
James L. Hanson, M.ASCE
Assistant Professor, Civil and Environmental Engineering Dept. California Polytechnic State Univ., San Luis Obispo, CA 93407.
Wei-Lien Liu, S.M.ASCE
Graduate Research Assistant, Dept. of Civil and Environmental Engineering, Wayne State Univ., Detroit, MI 48202.

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