Sediment and Nutrient Trends at Long-term Sites
The Susquehanna River Basin Commission estimates flow adjusted
concentration trends in nutrients, sediment, and trends in discharge as
part of the Chesapeake Bay Program's annual trend update. Trends in discharge
indicate the natural changes in hydrology. Changes in flow and the cumulative
sources of flow (base flow and overland runoff) affect the observed concentrations
and the estimated loads of nutrients and suspended sediment. The Flow
Adjusted Concentration (FAC) is the concentration after the effects of
flow are removed. Trends in FAC indicate that changes have occurred in
the processes that deliver constituents to the stream system. This is
the concentration that relates to the effects of nutrient-reduction activities
and other actions taking place in the watershed.
Tends in FAC are calculated based on the USGS water year,
October 1 to September 30, using the USGS 7-parameter, log-linear regression
model (ESTIMATOR) for nutrient trends and the Seasonal Kendall test is
used to find trends in discharge. Slope, p-value and sigma (error) values
are taken from the DECTIME variable of the ESTIMATOR output. These values
are then used to calculate flow adjusted trends using the following equations;
Trend = 100*(exp(Slope *(end yr – begin
yr)) – 1)
Trend minimum= 100*(exp((Slope – (1.96*sigma)) *(end yr –
begin yr)) – 1)
Trend maximum= 100*(exp((Slope + (1.96*sigma)) *(end yr – begin
yr)) – 1)
The slope value determines whether trends are increasing
or decreasing (positive slope means trends are increasing while negative
slope means trends are decreasing). Trends are only reported when the
p-value is < 0.05. If a parameter has more than 20% of its reported
values below the method detection limit, no trend is reported and BMDL
is listed.
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