SPATIAL VARIABILITY IN IN-SITU AEROBIC RESPIRATION AND DENITRIFICATION RATES IN A PETROLEUM-CONTAMINATED AQUIFER

Citation
Mh. Schroth et al., SPATIAL VARIABILITY IN IN-SITU AEROBIC RESPIRATION AND DENITRIFICATION RATES IN A PETROLEUM-CONTAMINATED AQUIFER, Ground water, 36(6), 1998, pp. 924-937
Citations number
46
Categorie Soggetti
Water Resources","Geosciences, Interdisciplinary
Journal title
ISSN journal
0017467X
Volume
36
Issue
6
Year of publication
1998
Pages
924 - 937
Database
ISI
SICI code
0017-467X(1998)36:6<924:SVIIAR>2.0.ZU;2-U
Abstract
An extensive series of single-well, push-pull tests was performed to q uantify horizontal and vertical spatial variability in aerobic respira tion and denitrification rates in a petroleum-contaminated aquifer, Th e results indicated rapid consumption of injected O-2 or NO3- in shall ow and deep test intervals across a large portion of the site, Compute d first-order rate coefficients for aerobic respiration ranged from 0. 15 to 1.69 h(-1) in the shallow test interval, and from 0.08 to 0.83 h (-1) in the deep test interval. The largest aerobic respiration rates occurred on the upgradient edge of the contaminant plume where concent rations of petroleum hydrocarbons and dissolved O-2 were relatively hi gh. Computed first-order rate coefficients for denitrification ranged from 0.09 to 0.42 h(-1) in the shallow test interval, and from 0.11 to 0.28 h(-1) in the deep test interval. The largest denitrification rat es occurred on the downgradient edge of the plume where hydrocarbon co ncentrations were relatively high but dissolved oxygen concentrations were small. The rates reported here represent maximal rates of aerobic respiration and denitrification, as supported by high concentrations of electron accepters in the injected test solutions. Production of di ssolved CO2 during aerobic respiration and denitrification tests provi ded evidence that O-2 and NO3- consumption was largely due to microbia l activity. Additional evidence for microbial NO3- consumption was pro vided by reduced rates of NO3- consumption when dissolved O-2 was inje cted with NO3-, and by increased N2O production when C2H2 was injected with NO3-.