R. Jakobsen et al., H-2 CONCENTRATIONS IN A LANDFILL LEACHATE PLUME (GRINDSTED, DENMARK) - IN-SITU ENERGETICS OF TERMINAL ELECTRON-ACCEPTOR PROCESSES, Environmental science & technology, 32(14), 1998, pp. 2142-2148
Empirical H-2 concentration ranges are currently related to specific r
edox processes, assuming steady-state conditions at which only one mic
robiologically mediated redox process occurs due to competetive exclus
ion of others. Here the first H-2 data from a landfill leachate plume
are presented, and an alternative partial equilibrium approach is used
. The approach implies that TEAPs (terminal electron-accepting process
es) occur at negative Delta G(r) values, close to thermodynamic equili
brium, and that the fermentative H-2 production is overall rate limiti
ng. It eliminates the steady-state prerequisite and may explain the oc
currence of concomitant TEAPs. Concentrations of H-2 and redox process
reactants and products were measured in 52 sampling points, downgradi
ent of the Grindsted Landfill (Denmark), and used to calculate in situ
Delta G(r) values of TEAPs, assuming partial equilibrium. H-2 general
ly ranged from 0.004 to 0.88 nM, with most values around 0.2 nM. Fe re
duction was, according to the empirically defined ranges, the most pro
minent TEAP, but concomitant methanogenesis and sulfate reduction occu
rred as well. This indicated a need for an alternative approach to exp
laining the H-2 distribution, and the measured H-2 concentrations are
viewed as being controlled by a partial equilibrium. A derived theoret
ical relation between H-2 concentrations and temperature indicates tem
perature effects to be more important than currently appreciated. Calc
ulated in situ Delta G(r) values can, combined with a threshold value,
predict which TEAPs can occur via H-2 oxidation. For our samples, Del
ta G(r) for methanogenesis was always >-7 kJ/mol, and CO2 reduction sh
ould only occur in stagnant porewater at higher H-2 concentrations or
by directinterspecies transfer. In contrast, sulfate and Fe reduction
occur close to or slightly below a threshold of -7 kJ/mol H2 and may o
ccur concomitantly at partial equilibrium.