Effects of compost biocovers on gas flow and methane oxidation in a landfill cover

被引:56
作者
Abichou, Tarek [1 ]
Mahieu, Koenraad [2 ]
Yuan, Lei [3 ]
Chanton, Jeffery [4 ]
Hater, Gary [5 ]
机构
[1] Florida State Univ, Dept Civil & Environm Engn, Tallahassee, FL 32310 USA
[2] Florida State Univ, Dept Civil & Environm Engn, Tallahassee, FL 32306 USA
[3] Geosyntec Consultants, Columbia, MD 21046 USA
[4] Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA
[5] Waste Management Inc, Bioreactors BioSites & New Technol, Cincinnati, OH 45211 USA
基金
美国国家科学基金会;
关键词
ATMOSPHERIC METHANE; SOIL; EMISSIONS; MODEL; FLUX; CH4;
D O I
10.1016/j.wasman.2008.11.007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Previous publications described the performance of biocovers constructed with a compost layer placed on select areas of a landfill surface characterized by high emissions from March 2004 to April 2005. The biocovers reduced CH4 emissions 10-fold by hydration of underlying clay soils, thus reducing the overall amount of CH4 entering them from below, and by oxidation of a greater portion of that CH4. This paper examines in detail the field observations made on a control cell and a biocover cell from January 1, 2005 to December 31, 2005. Field observations were coupled to a numerical model to contrast the transport and attenuation of CH4 emissions from these two cells. The model partitioned the biocover's attenuation of CH4 emission into blockage of landfill gas flow from the underlying waste and from biological oxidation of CH4. Model inputs were daily water content and temperature collected at different depths using thermocouples and calibrated TDR probes. Simulations of CH4 transport through the two soil columns depicted lower CH4 emissions from the biocover relative to the control. Simulated CH4 emissions averaged 0.0 g m(-2) d(-1) in the biocover and 10.25 g m(-2) d(-1) in the control, while measured values averaged 0.04 g m(-2) d(-1) in the biocover and 14 g m(-2) d(-1) in the control. The simulated influx of CH4 into the biocover (2.7 g m(-2) d(-1)) was lower than the simulated value passing into the control cell (29.4 g m(-2) d(-1)), confirming that lower emissions from the biocover were caused by blockage of the gas stream. The simulated average rate of biological oxidation predicted by the model was 19.2 g m(-2) d(-1) for the control cell as compared to 2.7 g m(-2) d(-1) biocover. Even though its V-max was significantly greater, the biocover oxidized less CH4 than the control cell because less CH4 was supplied to it. (c) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1595 / 1601
页数:7
相关论文
共 30 条
  • [1] Characterization of methane flux and oxidation at a solid waste landfill
    Abichou, T
    Powelson, D
    Chanton, J
    Escoriaza, S
    Stern, J
    [J]. JOURNAL OF ENVIRONMENTAL ENGINEERING, 2006, 132 (02) : 220 - 228
  • [2] Methane flux and oxidation at two types of intermediate landfill covers
    Abichou, Tarek
    Chanton, Jeffery
    Powelson, David
    Fleiger, Jill
    Escoriaza, Sharon
    Lei, Yuan
    Stern, Jennifer
    [J]. WASTE MANAGEMENT, 2006, 26 (11) : 1305 - 1312
  • [3] [Anonymous], 2005, HYDRUS SOFTWARE SERI
  • [4] [Anonymous], COLORADO STATE U HYD
  • [5] ASTM, 2000, D155600 ASTM
  • [6] Effect of CH4 concentrations and soil conditions on the induction of CH4 oxidation activity
    Bender, M
    Conrad, R
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 1995, 27 (12) : 1517 - 1527
  • [7] Methane oxidation in a neutral landfill cover soil: Influence of moisture content, temperature, and nitrogen-turnover
    Boeckx, P
    VanCleemput, O
    [J]. JOURNAL OF ENVIRONMENTAL QUALITY, 1996, 25 (01) : 178 - 183
  • [8] Fluxes of methane between landfills and the atmosphere: natural and engineered controls
    Bogner, J
    Meadows, M
    Czepiel, P
    [J]. SOIL USE AND MANAGEMENT, 1997, 13 (04) : 268 - 277
  • [9] LANDFILL CH4 - RATES, FATES, AND ROLE IN GLOBAL CARBON-CYCLE
    BOGNER, J
    SPOKAS, K
    [J]. CHEMOSPHERE, 1993, 26 (1-4) : 369 - 386
  • [10] LANDFILLS AS ATMOSPHERIC METHANE SOURCES AND SINKS
    BOGNER, J
    SPOKAS, K
    BURTON, E
    SWEENEY, R
    CORONA, V
    [J]. CHEMOSPHERE, 1995, 31 (09) : 4119 - 4130