AIT Austrian Institute of Technology GmbH, Health and Environment Department, Environmental Resources and Technologies, Konrad-Lorenz-Strasse 24, 3430 Tulln, Austria.
Waste Manag. 2013 Oct;33(10):2083-90. doi: 10.1016/j.wasman.2013.02.017. Epub 2013 Mar 27.
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.
垃圾渗滤液的稳定同位素特征受城市固体废物(MSW)填埋场内部过程的影响,主要取决于填埋场的好氧/厌氧阶段。我们研究了实验室实验、淋溶实验和原位曝气条件下填埋场中不同渗滤液的 δ(13)C、δ(2)H 和 δ(18)O 的同位素特征。在实验室中,用不同年龄和反应性的 MSW 填充柱子,在好氧和厌氧条件下进行渗滤。在填埋场模拟反应器中,将 25 年历史的垃圾保持在好氧和厌氧条件下。淋溶设施中填充了机械切碎的新鲜垃圾。在甲烷产生开始后,原位对淋溶容器中的废物进行曝气。连续监测渗滤液和气体组成。此外,还定期收集和分析旧垃圾填埋场的渗漏水,以监测原位曝气前后的渗漏水。我们发现,好氧和厌氧废物之间渗滤液中溶解无机碳(δ(13)C-DIC)的 δ(13)C 值存在显著差异。在好氧降解过程中,δ(13)C-DIC 的特征主要取决于废物中有机物的同位素组成,导致 δ(13)C-DIC 值为-20‰至-25‰。在厌氧条件下产生甲烷会导致 δ(13)C-DIC 值增加到+10‰及更高,具体取决于 MSW 的实际反应性。在填埋场曝气过程中,剩余有机物的好氧降解导致 δ(13)C-DIC 值降低到约-20‰。因此,渗滤液和地下水中的碳同位素分析可用于追踪 MSW 填埋场的氧化还原状态。我们的结果表明,对填埋场渗滤液的稳定同位素特征进行较长时间的监测(例如在原位曝气期间)是一种强大且具有成本效益的工具,可用于表征填埋场中城市固体废物的生物降解性和稳定性,并可用于监测原位曝气的进展。