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在模拟垃圾填埋场土壤覆盖层的甲烷氧化逆流实验室系统中,氟氯化碳和氢氯氟烃的生物降解能力。

Capacity for biodegradation of CFCs and HCFCs in a methane oxidative counter-gradient laboratory system simulating landfill soil covers.

作者信息

Scheutz Charlotte, Kjeldsen Peter

机构信息

Environment & Resources, Building 115, Technical University of Denmark, DK-2800 Lyngby, Denmark.

出版信息

Environ Sci Technol. 2003 Nov 15;37(22):5143-9. doi: 10.1021/es026464+.

Abstract

The attenuation of methane and four chlorofluorocarbons was investigated in a dynamic methane and oxygen counter-gradient system simulating a landfill soil cover. Soil was sampled at Skellingsted Landfill, Denmark. The soil columns showed a high capacity of methane oxidation with oxidation rates of 210 g m(-2) d(-1) corresponding to a removal efficiency of 81%. CFC-11 and to a lesser extent also CFC-12 were degraded in the active soil columns. The average removal efficiency was 90% and 30% for CFC-11 and CFC-12, respectively. Soil gas concentration profiles indicated that the removal was due to anaerobic degradation, which was verified in anaerobic batch experiments where CFC-11 was rapidly degraded. HCFC-21 and HCFC-22 were also degraded in active soil columns (61% and 41%, respectively), but compared to the CFCs, the degradation was located in the upper oxic part of the column with overlapping gradients of methane and oxygen. High oxidation rates of methane and HCFCs were obtained in soil microcosms incubated with methane. When increasing the column inlet flow, the oxidation zone was moved upward in the column, and the removal efficiency of methane and HCFCs decreased. The removal of CFCs was, however, less affected since the anaerobic zone expanded with increasing inlet flow rates. This study demonstrates the complexity of landfill soil cover systems and shows that both anaerobic and aerobic bacteria may play a very important role in reducing the emission of not only methane but also trace components into the atmosphere.

摘要

在一个模拟垃圾填埋场土壤覆盖层的动态甲烷与氧气反向梯度系统中,研究了甲烷和四种氯氟烃的衰减情况。土壤取自丹麦的斯凯林斯特德垃圾填埋场。土壤柱显示出较高的甲烷氧化能力,氧化速率为210 g m(-2) d(-1),对应的去除效率为81%。CFC-11以及程度稍轻的CFC-12在活性土壤柱中被降解。CFC-11和CFC-12的平均去除效率分别为90%和30%。土壤气体浓度剖面表明,去除是由于厌氧降解,这在厌氧批次实验中得到了验证,在该实验中CFC-11被快速降解。HCFC-21和HCFC-22在活性土壤柱中也被降解(分别为61%和41%),但与氯氟烃相比,降解发生在柱体上部的有氧部分,甲烷和氧气的梯度重叠。在与甲烷一起培养的土壤微观环境中,获得了较高的甲烷和HCFCs氧化速率。当增加柱体入口流量时,氧化区在柱体中向上移动,甲烷和HCFCs的去除效率降低。然而,氯氟烃的去除受影响较小,因为厌氧区随着入口流量的增加而扩大。这项研究证明了垃圾填埋场土壤覆盖系统的复杂性,并表明厌氧和好氧细菌在减少不仅甲烷而且微量成分向大气中的排放方面都可能发挥非常重要的作用。

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