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231224s2013 xx |||||o 00| ||eng c |
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|a 10.1016/j.wasman.2013.02.017
|2 doi
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|a pubmed24n0754.xml
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|a (NLM)23540355
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|a (PII)S0956-053X(13)00105-0
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|a DE-627
|b ger
|c DE-627
|e rakwb
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|a eng
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| 100 |
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|a Wimmer, Bernhard
|e verfasserin
|4 aut
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| 245 |
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|a Stable isotope signatures for characterising the biological stability of landfilled municipal solid waste
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|c 2013
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
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|2 rdamedia
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|a ƒa Online-Ressource
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|2 rdacarrier
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|a Date Completed 05.05.2014
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|a Date Revised 09.09.2013
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|a published: Print-Electronic
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|a Citation Status MEDLINE
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|a Copyright © 2013 Elsevier Ltd. All rights reserved.
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|a Stable isotopic signatures of landfill leachates are influenced by processes within municipal solid waste (MSW) landfills mainly depending on the aerobic/anaerobic phase of the landfill. We investigated the isotopic signatures of δ(13)C, δ(2)H and δ(18)O of different leachates from lab-scale experiments, lysimeter experiments and a landfill under in situ aeration. In the laboratory, columns filled with MSW of different age and reactivity were percolated under aerobic and anaerobic conditions. In landfill simulation reactors, waste of a 25year old landfill was kept under aerobic and anaerobic conditions. The lysimeter facility was filled with mechanically shredded fresh waste. After starting of the methane production the waste in the lysimeter containments was aerated in situ. Leachate and gas composition were monitored continuously. In addition the seepage water of an old landfill was collected and analysed periodically before and during an in situ aeration. We found significant differences in the δ(13)C-value of the dissolved inorganic carbon (δ(13)C-DIC) of the leachate between aerobic and anaerobic waste material. During aerobic degradation, the signature of δ(13)C-DIC was mainly dependent on the isotopic composition of the organic matter in the waste, resulting in a δ(13)C-DIC of -20‰ to -25‰. The production of methane under anaerobic conditions caused an increase in δ(13)C-DIC up to values of +10‰ and higher depending on the actual reactivity of the MSW. During aeration of a landfill the aerobic degradation of the remaining organic matter caused a decrease to a δ(13)C-DIC of about -20‰. Therefore carbon isotope analysis in leachates and groundwater can be used for tracing the oxidation-reduction status of MSW landfills. Our results indicate that monitoring of stable isotopic signatures of landfill leachates over a longer time period (e.g. during in situ aeration) is a powerful and cost-effective tool for characterising the biodegradability and stability of the organic matter in landfilled municipal solid waste and can be used for monitoring the progress of in situ aeration
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|a Journal Article
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|a Research Support, Non-U.S. Gov't
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|a Carbon isotope
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|a In situ aeration
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|a Landfill leachate
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|a Lysimeter
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| 650 |
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|a δ(13)C
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| 650 |
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|a Carbon Isotopes
|2 NLM
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| 650 |
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|a Solid Waste
|2 NLM
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| 650 |
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|a Water Pollutants, Chemical
|2 NLM
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| 650 |
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|a Methane
|2 NLM
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| 650 |
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|a OP0UW79H66
|2 NLM
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| 700 |
1 |
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|a Hrad, Marlies
|e verfasserin
|4 aut
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1 |
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|a Huber-Humer, Marion
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Watzinger, Andrea
|e verfasserin
|4 aut
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| 700 |
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|a Wyhlidal, Stefan
|e verfasserin
|4 aut
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|a Reichenauer, Thomas G
|e verfasserin
|4 aut
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| 773 |
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|i Enthalten in
|t Waste management (New York, N.Y.)
|d 1999
|g 33(2013), 10 vom: 15. Okt., Seite 2083-90
|w (DE-627)NLM098197061
|x 1879-2456
|7 nnns
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| 773 |
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|g volume:33
|g year:2013
|g number:10
|g day:15
|g month:10
|g pages:2083-90
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|u http://dx.doi.org/10.1016/j.wasman.2013.02.017
|3 Volltext
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