NPS Inputs and EOS Targets
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Transcript of NPS Inputs and EOS Targets
NPS Inputs and EOS TargetsDeveloping EOS targets
based on Nutrient Balance in the
Chesapeake Bay Watershed Model
Nutrient Balance EOS Targets
Where do the targets come from? How Are
Targets Distributed? (Why) Do they differ from Phase 4.3?
Fate and transport of N and P Model Scale Refined Land Uses Newer Research Information
How Does This Affect Delivered Loads?
Where Do Targets Come From
Calculated Mass Balance of known inputs and outputs on land uses
Estimates of attenuation/delivery factors: Literature Review Of In-Stream
Concentrations assigned “back-stream” to likely upland sources
Addresses uncertainty in input/output estimates
Calculating Balance: Inputs/Outputs
Pervious Surfaces: Inputs: Fertilizer, Manure, N-fixation,
Atmospheric Deposition Outputs: Crop Removal, de-nitrification,
volatilization Residual: Nitrogen (mobile) and
Phosphorus (mobile and immobile) The residual is that which may reach the
stream
The Mass-Balance Approach
Determine all input types (I): Atmospheric Deposition Fertilizer Application (where applicable) Manure Application (where applicable) Legume Fixation (where applicable)
Determine all outputs (O): Removal via harvest (potentially largest) Volatilization/De-nitrification (low to high) Sequestration in refractory organic matter (small) Sequestration/Attenuation in lower order streams
Eligible for Losses to the watershed outlet (E)
)()( ASVHLMFA OOOOIIIIE
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0.1
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Distributing EOS Targets Based on distribution around Median
Balance/Median In-stream Value From lit. review
Addresses uncertainty in the exact application rates, and attenuation of in-stream studies
EOS Target can NOT exceed Eligible Balance
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-20 0 20 40 60 80 100
Median Balance (LWM) Median In-Stream (LWM)
Ex: 45.1 Balance => 39.6 EOS
Impervious EOS – Mass Balance
Urban Impervious surfaces a little more difficult to characterize
Inputs: Atmospheric Deposition (from Atmospheric model) Miscellaneous
Direct Automobile Deposition (difficult to estimate) Other Sources (animals, trash spillage, etc.)
Outputs: Little to no attenuation of N and P is expected to occur
on impervious surfaces Outputs are known from urban studies, generally based
on Event Mean Concentration (EMC) Mass Balance:
E = m + A ; A = atmospheric, m = miscellaneous
Estimating M from NURP/NSDQ
Quantify the misc. on impervious surfaces from EMC
Assumptions: Rainfall = runoff on impervious surface = 40” / ac-
year NURP/NSDQ Average EMC on highly impervious
(>80%) 2.2 mg/L This EMC represents mean value in watershed EMCs already include any attenuation Assume that “m” is constant, and the only variable
is atmospheric Acreage of impervious will be the greatest factor in
loading 12.74 lb-N/ac mean atmospheric deposition m = EMC*Runoff - A
Calculations: yrac
lbN
yrac
lbNconv
L
mg
yracM
05.574.12.
2.2"40
Change in TN Land Targets Between Phase 4.3 and Phase 5
Started with similar targets to Phase 4.3
Not enough Nitrogen to calibrate rivers Analysis of targets vs export
We expect Nitrogen targets to be scale dependent. Targets vs river loads Independent studies
TN Comparison Modeled vs. Estimator (using P4.3 targets in P5)
Compared ESTIMATOR loads to upstream EOF targets
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Coastal Plain Piedmont VR and Pied Valley and Ridge AP and VR Appalachian Plateau
Delivery F
acto
r
Resolution
Double Nitrogen targets from all land uses in non-coastal plain segments (eyeball estimate).
Phosphorus does not have a similar reduction mechanism and the targets are not scale-dependent
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Coastal Plain Piedmont VR and Pied Valley and Ridge AP and VR Appalachian Plateau
De
liv
ery
F
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r
Change in scale
Nitrogen is Always Reduced in Rivers
Simulated river miles Phase 4 – 2,479 Phase 5 – 10,237
National SPARROW model (1997): First order rate coefficients are scale dependent Rivers < 1000 cfs = 0.38/day Rivers between 1000 and 10000 cfs = .12/day Rivers > 10000 cfs = 0.04/day
Considerable literature on denitrification Many Seitzinger articles Nitrogen budgets (e.g. Howarth)
Delivered: Phase 5 Versus Phase 4.3
Phase 5 Nitrogen targets are roughly 2X that of Phase 4.3.
Phosphorus remains nearly the same. Attenuation in lower (as compared to 4.3)
order streams is now simulated, thus the EOS must approach the EOF
Consequently, Phase 5 N attenuation is much greater then 4.3
Overall loads are similar, however, they will not be exactly the same since 1) the modeling period is different, 2) the model is more accurately calibrated
Phase 5 Versus 4.3 (delivered)
Old School New School
Similar Lesson: ~4.5 Million Lbs N
~17%
Attenuatio
n
~41% A
ttenuatio
n