Engineered and subsequent intrinsic in situ bioremediation of a diesel fuel contaminated aquifer

被引:19
|
作者
Hunkeler, D
Höhener, P
Zeyer, J
机构
[1] ETH, Swiss Fed Inst Technol, Inst Terr Ecol, CH-8952 Schlieren, Switzerland
[2] Swiss Fed Inst Technol, EPFL, ENAC, ISTE,LPE, CH-1015 Lausanne, Switzerland
[3] Univ Neuchatel, Ctr Hydrogeol, CH-2007 Neuchatel, Switzerland
关键词
bioremediation; petroleum hydrocarbons; groundwater; redox processes;
D O I
10.1016/S0169-7722(02)00059-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A diesel fuel contaminated aquifer in Menziken, Switzerland was treated for 4.5 years by injecting aerated groundwater, supplemented with KNO3 and NH4H2PO4 to stimulate indigenous populations of petroleum hydrocarbon (PHC) degrading microorganisms. After dissolved PHC concentrations had stabilized at a low level, engineered in situ bioremediation was terminated. The main objective of this study was to evaluate the efficacy of intrinsic in situ bioremediation as a follow-up measure to remove PHC remaining in the aquifer after terminating engineered in situ bioremediation. In the first 7 months of intrinsic in situ bioremediation, redox conditions in the source area became more reducing as indicated by lower concentrations of SO42- and higher concentrations of Fe(II) and CH4. In the core of the source area, strongly reducing conditions prevailed during the remaining study period (3 years) and dissolved PHC concentrations were higher than during engineered in situ bioremediation. This suggests that biodegradation in the core zone was limited by the availability of oxidants. In lateral zones of the source area, however, gradually more oxidized conditions were reestablished again, suggesting that PHC availability increasingly limited biodegradation. The total DIC production rate in the aquifer decreased within 2 years to about 25% of that during engineered in situ bioremediation and remained at that level. Stable carbon isotope analysis confirmed that the produced DIC mainly originated from PHC mineralization. The total rate of DIC and CH4 production in the source area was more than 300 times larger than the rate of PHC elution. This indicates that biodegradation coupled to consumption of naturally occurring oxidants was an important process for removal of PHC which remained in the aquifer after terminating engineered measures. (C) 2002 Elsevier Science B.V All rights reserved.
引用
收藏
页码:231 / 245
页数:15
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