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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Isotope and dissolved gas evidence for nitrogen attenuation in landfill leachate dispersing into a chalk aquifer
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Isotope and dissolved gas evidence for nitrogen attenuation in landfill leachate dispersing into a chalk aquifer

机译:同位素和溶解气体证明垃圾渗滤液分散到白垩质含水层中氮的衰减

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摘要

The authors present data for the chemical, stable isotope (C-13/C-12, N-15/N-14 and S-34/S-32), and dissolved gas (N-2, Ar, O-2 and CH4) composition of groundwaters sampled in and around a landfill site in Cambridgeshire, England. Decomposition of 3 x 10(6) m(3) of largely domestic waste, placed in unlined quarries, has given rise to the formation of an NH4-rich leachate dispersing as a plume into the surrounding Middle Chalk aquifer. In addition to identifying zones of methanogenesis and SO4 reduction, the data indicate processes of NH4 transformation by either assimilation or oxidation, and losses by formation of N-2. Depending on the mixing ratio between leachate and background water, it may be possible to account for all NH4 loss by combined nitrification + denitrification in a system where there are abrupt temporal and spatial changes in redox conditions. Crown Copyright (c) 2005 Published by Elsevier Ltd. All rights reserved.
机译:作者提供了化学,稳定同位素(C-13 / C-12,N-15 / N-14和S-34 / S-32)以及溶解气体(N-2,Ar,O-2和CH4)在英格兰剑桥郡的垃圾填埋场内及其附近采样的地下水成分。分解为3 x 10(6)m(3)的大部分生活垃圾,这些垃圾被置于无衬砌的采石场中,形成了富含NH4的浸出液,并以烟流的形式散布到周围的中粉笔含水层中。除了确定产甲烷和SO4还原的区域外,数据还表明了通过同化或氧化作用进行NH4转化的过程,以及通过形成N-2造成的损失。根据渗滤液和背景水之间的混合比例,在氧化还原条件下时空发生突然变化的系统中,通过硝化+反硝化联合处理所有的NH4损失是可能的。 Crown版权所有(c)2005,由Elsevier Ltd.发行。保留所有权利。

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