A field-scale ace
ta
te amendmen
t experimen
t wasperformed in a con
tamina
ted aquifer a
t Old Rifle, CO
tos
timula
te in si
tu microbial reduc
tion of U(VI) in groundwa
ter.To evalua
te
the microorganisms responsible for microbialuranium reduc
tion during
the experimen
t,
13C-labeledace
ta
te was in
troduced in
to well bores via bio-
traps con
tainingporous ac
tiva
ted carbon beads (Bio-Sep). Incorpora
tionof
the
13C from labeled ace
ta
te in
to cellular DNA andphospholipid fa
tty acid (PLFA) biomarkers was analyzed inparallel wi
th geochemical parame
ters. An enrichmen
t ofac
tive
ta.gif" BORDER=0 >
-proteobacteria was demons
tra
ted in downgradien
tmoni
toring wells:
Geobacter domina
ted in wells closer
to
the ace
ta
te injec
tion gallery, while various sulfa
te reducerswere prominen
t in differen
t downgradien
t wells. Theseresul
ts were consis
ten
t wi
th
the geochemical evidence ofFe(III), U(VI), and SO
42- reduc
tion. PLFA profiling of bio-
traps suspended in
the moni
toring wells also showed
theincorpora
tion of
13C in
to bac
terial cellular lipids. Communi
tycomposi
tion of downgradien
t moni
toring wells basedon quinone and PLFA profiling was in general agreemen
twi
th
the
13C-DNA resul
t. The direc
t applica
tion of
13C label
to biosys
tems, coupled wi
th DNA and PLFA analysis,which combined de
tailed
taxonomic descrip
tion wi
th aquan
ti
ta
tive measure of me
tabolic diversi
ty, allowediden
tifica
tion of
the me
tabolically ac
tive por
tion of
themicrobial communi
ty during reduc
tion of U(VI).