ACETATE AND PROPIONATE IN LANDFILL LEACHATES - IMPLICATIONS FOR THE RECOGNITION OF MICROBIOLOGICAL INFLUENCES ON THE COMPOSITION OF WATERS IN SEDIMENTARY SYSTEMS
Dac. Manning, ACETATE AND PROPIONATE IN LANDFILL LEACHATES - IMPLICATIONS FOR THE RECOGNITION OF MICROBIOLOGICAL INFLUENCES ON THE COMPOSITION OF WATERS IN SEDIMENTARY SYSTEMS, Geology, 25(3), 1997, pp. 279-281
Routine monitoring of landfill leachates provides information concerni
ng aqueous systems in which anaerobic microbiological processes influe
nce mater chemistry. Propionate and acetate are substrate and product,
respectively, of metabolism by bacteria that have an obligate syntrop
hic relationship with sulfate-reducing bacteria. The stoichiometry of
the bacteriological metabolic reactions indicates a 1:1 molar proporti
onality for acetate and propionate, This is observed for landfill leac
hates, consistent with the known biological control on their organic a
cid anion contents. Similar data for oil-field waters show the same 1:
1 molar proportionality for reservoirs where bacterial sulfate reducti
on is known to take place, at temperatures up to about 95 degrees C, i
n contrast to the 3:2 proportionality (acetic acid:propionic acid) obs
erved in higher temperature systems. These observations suggest that 1
:1 molar proportionality for acetate and propionate may be characteris
tic of natural systems where anaerobic bacterial activity occurs, incl
uding bacterial sulfate reduction.