The response of seepage meters was evaluated in a nearshore marine env
ironment where water motion effects are more pronounced than in lake s
ettings, where these meters have been used traditionally. Temporal and
spatial variations of seepage, as well as potential artifacts, were e
valuated using empty and 1000-ml pre-filled bag measurements. Time-ser
ies measurements confirmed earlier observations that anomalously high
fluxes occur during the early stages (less than or equal to 10 min) of
collection. As deployment rimes increased (30-60 min), measured flow
rates stabilized at a level thought to represent the actual seepage fl
ux. Pre-filling the plastic measurement bags effectively alleviated th
is anomalous, short-term influx. Reliable seepage measurements require
d deployment times sufficient to allow a net volume of at least 150 mi
into the collection bag. Control experiments, designed by placing see
page meters inside sand-filled plastic swimming pools, served as indic
ators of external effects on these measurements, i.e. they served as s
eepage meter blanks. When winds were under 15 knots, little evidence w
as found that water motion caused artifacts in the seepage measurement
s. Tidal cycle influences on seepage rates were negligible in the pres
ent study area, but long-term temporal variations (weeks to months) pr
oved substantial. Observed long-term changes in groundwater flux into
the Gulf of Mexico correlated with water table elevation at a nearby m
onitoring well. (C) 1997 Academic Press Limited.