Höhener Patrick, Dakhel Nathalie, Christophersen Mette, Broholm Mette, Kjeldsen Peter
Laboratoire de Chimie et Environnement, Université de Provence, Case 29, 3, Place Victor Hugo, F-13331 Marseille Cedex 3, France.
J Contam Hydrol. 2006 Dec 15;88(3-4):337-58. doi: 10.1016/j.jconhyd.2006.07.007. Epub 2006 Sep 8.
The natural attenuation of volatile organic compounds (VOCs) in the unsaturated zone can only be predicted when information about microbial biodegradation rates and kinetics are known. This study aimed at determining first-order rate coefficients for the aerobic biodegradation of 13 volatile petroleum hydrocarbons which were artificially emplaced as a liquid mixture during a field experiment in an unsaturated sandy soil. Apparent first-order biodegradation rate coefficients were estimated by comparing the spatial evolution of the resulting vapor plumes to an analytical reactive transport model. Two independent reactive numerical model approaches have been used to simulate the diffusive migration of VOC vapors and to estimate degradation rate coefficients. Supplementary laboratory column and microcosm experiments were performed with the sandy soil at room temperature under aerobic conditions. First-order kinetics adequately matched the lab column profiles for most of the compounds. Consistent compound-specific apparent first-order rate coefficients were obtained by the three models and the lab column experiment, except for benzene. Laboratory microcosm experiments lacked of sensitivity for slowly degrading compounds and underestimated degradation rates by up to a factor of 5. Addition of NH3 vapor was shown to increase the degradation rates for some VOCs in the laboratory microcosms. All field models suggested a significantly higher degradation rate for benzene than the rates measured in the lab, suggesting that the field microbial community was superior in developing benzene degrading activity.
只有在了解微生物降解速率和动力学信息的情况下,才能预测非饱和带中挥发性有机化合物(VOCs)的自然衰减。本研究旨在确定13种挥发性石油烃有氧生物降解的一级速率系数,这些烃类在一个非饱和砂土现场实验中以液体混合物的形式人工注入。通过将生成的蒸汽羽流的空间演化与一个分析性反应传输模型进行比较,估算了表观一级生物降解速率系数。已使用两种独立的反应性数值模型方法来模拟VOC蒸汽的扩散迁移并估算降解速率系数。在有氧条件下,于室温下对砂土进行了补充性实验室柱实验和微观实验。对于大多数化合物,一级动力学与实验室柱实验结果充分匹配。除苯以外,三种模型和实验室柱实验获得了一致的化合物特异性表观一级速率系数。实验室微观实验对缓慢降解的化合物缺乏敏感性,且将降解速率低估了高达5倍。在实验室微观实验中,添加NH3蒸汽可提高某些VOCs的降解速率。所有现场模型均表明,苯的降解速率显著高于实验室测量值,这表明现场微生物群落更善于发挥苯降解活性。