Bäumler Rupert, Kögel-Knabner Ingrid
Technische Universität München, Department für Okologie, Am Hochanger 2, D-85350 Freising-Weihenstephan, Germany.
J Environ Qual. 2008 Jan 4;37(1):146-53. doi: 10.2134/jeq2006.0191. Print 2008 Jan-Feb.
Landfill sites are potential sources of hazardous emissions by degradation and transformation processes of waste organic matter. Its chemical composition and microbial degradability are key factors for risk management, after-care, and estimation of potential emissions. The aim of the study is to provide information about composition and extent of transformation of waste organic matter in four landfill sites in Bavaria, Southern Germany by means of (13)C NMR spectroscopy, acid-hydrolyzable carbohydrates, chloroform-methanol extractable lipids, acid-hydrolyzable proteins, and lignin compounds after CuO oxidation. Ten samples of about 20 to 25 yr, 15 to 20 yr, and 5 to 10 yr of deposition each were taken at 2 m depth intervals by grab drilling till 10-m depth. Increasing temperatures from about 15 degrees C at 2-m depth to >40 degrees C at 10-m depth are found at some of the sites, representing optimum conditions for mesophile methane bacteria. Moisture contents of 160 to 310 g kg(-1) (oven dry), however, provide limiting conditions for anaerobic biodecay. Spectroscopic and chemical variables generally indicate a low extent of biodegradation and transformation at all sites despite a considerable heterogeneity of the samples. Independent of the time and depth of deposition more than 50% of the carbohydrate fraction of the waste organic matter provide a high potential for methane emissions and on-site energy production. There was no significant accumulation of long-chain organic and aromatic compounds, and of lignin degradation products even after more than 25 yr of rotting indicating higher extent of decomposition or stabilization of the waste organic matter. Installation of seepage water cleaning and recirculation systems are recommended to increase suboptimal moisture contents with respect to microbial methanogenesis, energy production, and long-term stabilization of municipal solid waste.
垃圾填埋场是废弃有机物通过降解和转化过程产生有害排放物的潜在来源。其化学成分和微生物可降解性是风险管理、后期维护以及潜在排放估算的关键因素。本研究的目的是通过¹³C核磁共振光谱、酸水解碳水化合物、氯仿 - 甲醇可提取脂质、酸水解蛋白质以及氧化铜氧化后的木质素化合物,提供关于德国南部巴伐利亚州四个垃圾填埋场中废弃有机物的组成和转化程度的信息。通过抓取钻探,每隔2米深度采集十个样本,每个填埋场分别采集沉积约20至25年、15至20年和5至10年的样本,直至10米深度。在一些场地发现温度从2米深度处约15摄氏度升高到10米深度处>40摄氏度,这代表了嗜温甲烷菌的最佳条件。然而,160至310克/千克(烘干)的水分含量为厌氧生物降解提供了限制条件。尽管样本存在相当大的异质性,但光谱和化学变量总体上表明所有场地的生物降解和转化程度较低。与沉积时间和深度无关,超过50%的废弃有机物碳水化合物部分具有产生甲烷排放和现场能源生产的高潜力。即使经过超过25年的腐烂,长链有机化合物、芳香族化合物以及木质素降解产物也没有显著积累,这表明废弃有机物的分解或稳定程度较高。建议安装渗流水净化和再循环系统,以提高不利于微生物产甲烷、能源生产和城市固体废物长期稳定的亚最佳水分含量。