We measured turbidity along a transect from channel to marsh interior,
from in June 2016 to January 2017. We measured turbidity (NTU) with optical
back scatter sensors along a shore normal transect. The transect consisted
of three turbidity sensors, with one in the channel (YSI 6600), and two on
the marsh surface (referred to as the channel sensor and marsh sensors,
respectively). The “marsh edge sensor” was 2.4m from the channel edge
(Seapoint, RBR Solo) and the “marsh interior sensor” was 18m from the edge
(Seapoint, RBR Duo). The sensors measured every 15 minutes and were equipped
with automatic wipers to reduce biofouling. Sensors were cleaned and
maintained and the data downloaded on approximately bimonthly site visits.
Following retrieval, the turbidity time series data was filtered to remove
any erroneous points and times when the sensors were fouled or exposed
(Ganju et al. 2005).
Turbidity data was converted to suspended sediment concentration (SSC) via
a combination of in situ field sampling and laboratory calibrations using
sediment collected from the site. In the field, we measured turbidity with
an additional sensor at various locations around the site and at different
tidal stages, and collected a water sample in conjunction with each reading.
In the lab, we created sediment-water slurries with a range of SSC and used
a turbidity sensor to measure the slurries while they were kept in constant
motion to avoid sediment settling. We compared sensor turbidity measurements
to total suspended solid measurements obtained via vacuum filtration of
water samples from the site and lab-created water-sediment slurries. The
y-intercept value was set to zero, resulting in the equation SSC (mg/L)
=1.33*Sensor Turbidity (NTU) (R2=0.9345, n=26, p<<0.001).