Evolving short-term (less than 5 yr) compositional changes in hydrocarbon c
harge from some Eugene Island Block 330 (EI-330) wells are demonstrated. St
orage, analytical, and production artifacts are shown to be minimal. In som
e wells, compositions remain constant from 1985 to 1993, whereas in others
in the same reservoir, significant changes are observed. In some cases, tem
poral variability is greater than spatial variability. Maximum temporal cha
nge is strongest for specific compounds: toluene and C-6 to C-9 normal alka
nes, but is also observed to a lesser extent for higher-molecular-weight co
mponents (up to n-C-32). Principal coordinate analysis shows the highest de
gree of overall temporal compositional change over an 8-yr period in the sh
allowest wells where there is also evidence of biodegradation. Small tempor
al compositional changes are also observed in two deeper wells that are bel
ow the thermal window favorable for biodegradation. An exception is an unus
ual oil, where a very large increase in toluene, as well as smaller changes
in a number of n-alkanes, was observed in 1993. The delta C-13 compound-sp
ecific isotopic signature of toluene, in addition to several other C-7-C-8
compounds in this oil, yields convincing evidence that it is related to the
same family as other EI-330 oils and unlikely to be due to a drilling or l
aboratory contaminant. Minor isotopic differences in other C-7 compounds (1
.5 parts per thousand) are consistent with extensive gas washing of this oi
l. The short-term compositional changes in EI-330 oils are attributed to ga
s washing, which causes overprinting of biodegraded oils with light n-alkan
es in shallower GA and HB reservoirs where oils are currently being biodegr
aded in situ. Patterns of smaller changes in heavier compounds in both shal
lower and deeper wells are also consistent with this interpretation. Copyri
ght (C) 2001 Elsevier Science Ltd.