
Town of Eliot: 2025 Comprehensive Plan Marine Resources || 200
DISSOLVED OXYGEN
The PREP Report sets a dissolved oxygen threshold
of 5 mg/L. When it drops below this level, there
are negative impacts for aquatic life. The report
documents no signicant trends in dissolved oxygen
levels in the Great Bay Estuary.
While dissolved oxygen levels mostly “remain well
above 5 mg/L in the bays and open waters located at
the center of the Great Bay and in Portsmouth Harbor”,
there are mixed results for the Upper Piscataqua River
station. The report notes that “low dissolved oxygen
events do occur in the Upper Piscataqua River” among
other locations, but also that “both the Great Bay and
the Upper Piscataqua River Stations remain consistently
above the 5 mg/L threshold”.
TOTAL SUSPENDED SOLIDS
“Total suspended solids are particles suspended
in the water column measured as the dry weight
of particles ltered from a known volume of water.
They can consist of phytoplankton or pieces of plant
matter, but most total suspended solids are generally
made up of inorganic particles, such as sediment.
Sources of suspended solids include erosion from
streambanks, salt marshes, and the upland portion
of the watershed. Surface water inows, stormwater
runoff, and wastewater treatment euent all can
deliver total suspended solids to estuaries. In addition
to external sources of suspended solids, they can
also originate from resuspension within an estuary.
Increasing suspended sediments reduces water
clarity and light availability for primary producers
such as eelgrass, seaweeds, and phytoplankton. High
total suspended solid values can also negatively
impact oyster feeding and the aesthetic value of our
estuaries.” - PREP State of our Estuaries 202311
The PREP report finds that total suspended solid
(TSS) concentrations are generally higher now than
they were in 1989, but “appear to be decreasing in
recent years”. The Upper Piscataqua River station has
seen no significant change in TSS from 2007 to 2021,
with the range of median values at this station being
generally lower than all other stations except the
Lamprey River.12
Riverbank erosion has been identied as an issue along
various parts of the Piscataqua River in Eliot, such as
around the Boat Basin. Future erosion could put upward
pressure on TSS concentrations.
In summary, there are positive trends in the
Piscataqua Region for reduced nitrogen loads. That
is tentative good news for fish, shellfish, benthic
invertebrates, eelgrass, and water clarity. However,
wetter years could lead to increased loading through
added nonpoint source pollution from stormwater
runoff.
As a PREP municipality, Eliot can play a role in
reducing nitrogen loading. Through our shared
sewer system and Intermunicipal Agreement (IMA)
with the Town of Kittery, we have an avenue for
discussing point source nitrogen loading issues (if
any) with the Kittery wastewater treatment plant. For
nonpoint source nitrogen loading, septic systems
and stormwater management are key topic areas.
PREP’s Municipal Guide, discussed below, has
recommendations for each of these.
For more on stormwater management, see
Water Resources.
Photo from New Hampshire Sea Grant
“Fish and many other organisms need dissolved oxygen in the
water to survive. Dissolved oxygen levels can decrease due to
various factors, including rapid changes in wind, temperature,
and salinity, as well as prolonged periods of dense cloud cover.
Dissolved oxygen levels can also decrease because of nutrient
inputs. When nutrient loading is too high, phytoplankton and
seaweed can bloom and then die, after which bacteria and
other decomposers use oxygen to break down the dead organic
matter.” – PREP State of Our Estuaries 20239