Paper No. 0
Presentation Time: 2:00 PM
SEASONAL AND STORM RESPONSE OF SEDIMENT TRANSPORT IN A KARST SYSTEM
We sampled sediment in a seep and in a well drilled into a
karst conduit near Easton, PA. The sediment concentrations
in the well were low (around 10 mg/L) in the late spring
and summer, and increased in the fall and early winter to
600-900 mg/L. The high sediment concentrations were
associated with seasons that received less rainfall,
suggesting that lower sediment occurs when repeated rain
flushes the karst system. In contrast, the ion
concentrations varied throughout the year with no seasonal
pattern, showing a high coefficient of variation (29%)
indicative of conduit flow. The seep had lower sediment
concentrations than the well, less than 15 mg/L through the
year. The seep was monitored hourly during a storm event,
and sediment concentrations followed a pattern similar to
the storm intensity. The highest sediment yield (13 mg/L)
matched the time the ion concentration
was most diluted. The travel time from storm peak to
sediment peak was approximately 5 hours. Travel time was
also monitored through the year using temperature spikes
after storm events. For 11 storms, the average travel time
was 4.5 hours, but the range was 1 to 15 hours. These data
show the potential variation in sediment transport due to
both storms and seasonality. This variation implies
sampling for microbes or contaminants that can bind to
sediment in karst must consider the temporal heterogeneity
of the system.