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Overview – Nutrient Fate and Transport
Mark B. David
University of Illinois at Urbana-Champaign
Presented at Building Science Assessments for State-Level Nutrient
Reduction Strategies
Nov. 13, 2012
What I will cover
• what the problem is
• N and P sources, balances, and river exports in the Mississippi River Basin (MRB)– Illinois as example
– what is going to the Gulf
• importance of modified hydrology (tile drainage)
• timing of flow and nutrients; fate
• myths; the challenge ahead
What is the problem?• both local and
downstream water quality problems from nitrate and total P
– local: algal production due to P; drinking water for N
– downstream: hypoxia in the Gulf of Mexico
• USEPA requiring nutrient criteria in flowing waters
Hypoxic zone, 2012
What was new (in 2007, now old)
• reaffirmed previous assessment
• importance of spring (April, May, June) nitrate
• now phosphorus recognized as having role in Gulf
• no one answer to fix problem– both agriculture and people (sewage effluent)
• recommended 45% reduction in N and P going down Mississippi River
Mississippi River Basin
Nitrogen
Water F
lux (m
illion m
3)
0
200000
400000
600000
800000
1000000
1200000
Riverin
e N F
lux
(million
metric ton
s N yr
-1)
0.0
0.5
1.0
1.5
2.0
2.5
19551960
19651970
19751980
19851990
19952000
20052010
2015
0.0
0.5
1.0
1.5
2.0
2.5
Nitrate-N
Ammonium
Total N
Particulate/organic N
Mississippi River Basin Phosphorus
Water F
lux (m
illion m
3)
0
200000
400000
600000
800000
1000000
1200000
19551960
19651970
19751980
19851990
19952000
20052010
2015
Riverin
e P F
lux
(million
metric ton
s yr-1
)
0.00
0.05
0.10
0.15
0.20
0.25
Total P
Soluble reactive P
Major Mississippi Subbasins
Major Mississippi Subbasins
Nutrient loads for 2001 to
2010
0
10
20
30
40
50
Subbasin
Miss-Clinton
Miss-Grafton
Missouri-Om
aha
Missouri-Herm
ann
Miss-Thebes
Ohio-Cannelton
Ohio-Grand Chain
Arkansas-Little Rock
Red River-Alexandra
Lower Miss
Nutrient load (1,000 m
etric tons N or P
yr-1
)0
50
100
150
200
250
300
350
2001-20052006-2010
Total P
Nitrate-N
Nutrient yields for 2001 to
2010
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Subbasin
Miss-Clinton
Miss-Grafton
Missouri-Om
aha
Missouri-Herm
ann
Miss-Thebes
Ohio-Cannelton
Ohio-Grand Chain
Arkansas-Little Rock
Red River-Alexandra
Lower Miss
Nutrient yield (kg N
or P ha
-1 yr
-1)
0
2
4
6
8
10
12
14
16
2001-20052006-2010
Total P
Nitrate-N
Spring nitrate, upper Miss and Ohio
Water F
lux (cm
)
0
5
10
15
20
25
30
1975 1980 1985 1990 1995 2000 2005 2010 20150
5
10
15
20
25
30
Mississippi River at Grafton
Ohio River at Grand Chain, IL
Riverin
e Nitrate-N
Flu
x (m
illion m
etric tons N
)
0.00
0.05
0.10
0.15
0.20
0.25
0.30
1975 1980 1985 1990 1995 2000 2005 2010 20150.00
0.05
0.10
0.15
0.20
0.25
0.30
Mississippi River at Grafton
Ohio River at Grand Chain, IL
1975 1980 1985 1990 1995 2000 2005 2010 2015
Sp
ring
Nitra
te (to
ns N
yr-1
)
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7MRB Grafton and Ohio
Source of spring nitrate
County Level Analysis of Mississippi River Basin
• counties in MRB (all 1768)
• 1997 to 2006 annual data on fertilizer, crops, animals, people, deposition
• predictive model from watersheds applied to all MRB counties
• both N and P
From David et al. (2010)
Nutrient Balances
inputs
-
+
-
+
- outputs
Annual N Fertilizer Applications
Fertilizer (kg N ha-1)0.0 - 11.2
11.3 - 27.2
27.3 - 45.4
45.5 - 65.9
66.0 - 107.1 From David et al. (2010)
Drain
0.0 - 5.1
5.2 - 16.3
16.4 - 31.7
31.8 - 51.4
51.5 - 81.8
Tile drainage is concentrated in the corn belt
Fraction of county
From David et al. (2010)
nni
-5 - 20
20 - 40
40 - 60
60 - 200
Net N Inputs (NNI)
kg N ha-1
Some counties negative, N from soil mineralization
Illinois N budgetthrough
2012
0
20
40
60
80
100
Nitrogen (kg N
ha-1
)
0
20
40
60
80
100
120
Fertilizer
1950 1960 1970 1980 1990 2000 20100
10
20
30
40
50 Net Nitrogen Inputs
ManureHuman consumption
Grain harvest
NOy deposition
Legume N
Linking N balances to N Export
• hydrology overwhelming factor
– channelization, tile drainage
• can look at watershed N export as a fraction of net N inputs
– most studies, about 25%
– however in MRB we know it is larger in critical areas
– can be > 100% in heavily tile drained watersheds
Drainage by tiles and ditches
Patterned tile systems
Embarras River - Camargo
Embarras River
19931994
19951996
19971998
19992000
20012002
20032004
20052006
20072008
20092010
20112012
NIT
RA
TE
(mg N
L-1
)
0
5
10
15
20
Embarras River
Water Year
19951996
19971998
19992000
20012002
20032004
20052006
20072008
20092010
20112012
Nitrate E
xport (kg
N h
a-1
yr-1
)
0
10
20
30
40
50
60
Predicted N Yield (kg N/ha)
0.00 - 3.00
3.01 - 7.50
7.51 - 10.00
10.01 - 15.00
15.01 - 25.00
Modeled January to June Nitrate Export
Best model includes fertilizer, sewage effluent,and tile drainage
Components of P Mass Balances
• net P inputs
= inputs – outputs
inputs (fertilizer)
outputs (grain harvest - human and animal consumption)
• net indicates additions or removals from soil
• little P (relative to N) is lost to streams, but it is biologically important
• surface runoff and tile leaching
• manure
From Jacobson et al. (2011)
Fertilizer P Row Crop %
Manure P Net P Inputs
Modeled January to June Total P
From Jacobson et al. (2011)
Illinois P budgetthrough
2012
0
5
10
15
20
Phosphorus (kg P
ha-1
)
0
5
10
15
20
Fertilizer
1950 1960 1970 1980 1990 2000 2010-10
-5
0
5
10
15
20
Balance
ManureHuman consumption
Grain harvest
P from fields to rivers –
Embarras River
From Gentry et al. (2007)
Particulate P from
fields to rivers
From Gentry et al. (2007)
Importance of a Few Storm Events
From Royer et al. (2006)
Fate of N
• limited in-stream losses of nitrate during high flow periods
– Lake Shelbyville
– Saylorville Reservoir
• retention times too short
• spring nitrate, headed to Gulf
Depth/Time of Travel (m yr-1)
0.1 1 10 100 1000 10000
N R
em
ove
d (%
)
0
20
40
60
80
100Lake Shelbyville, IllinoisGarnier et al. (1999)Royer et al. (2004)Saylorville Reservoir, Iowa
Crumpton equation
Fate of P
• some sediment removal
• problem of sediment already in streams/rivers
– stream bank, bed erosion
• algal biomass can move downstream
• no way to easily get out of system (like nitrate)
Source: Clay Soil and Water Conservation District, Minnesota
What we know about nutrient sources
• Upper Mississippi and Ohio subbasins are the major source of nitrate and total P– even more so in critical
spring period
• the tile drained cornbelt is clearly identified
• mass balance of P has greatly decreased, but not N
What can we do in agriculture?
• given, – it is not typically over fertilization
based on current rates and yields
– may be zero or negative N & P balances in some areas of the tile drained Midwest
• three types of conservation practices could help– nutrient-use efficiency
– in-field management
– off-site measures
Potential Efficiencies -SAB report
Jan08
Jul08
Jan09
Jul09
Jan10
Jul10
Jan11
Jul11
Jan12
Nitra
te-N
Co
nce
ntra
tion
(mg
N L
-1)
0
5
10
15
20
25
30Corn-Corn-Soy MiscanthusSwitchgrass Prairie
Perennial biofuels quickly reduce nitrate loss
From Smith et al. (2013)
Point sources in MRB?
• sewage effluent and industrial (22% of annual N and 34% of P)
• however, only 14% (N) and 20% (P) of spring load
• not going to solve problem, but could help for P
A few myths
• no-till solves all problems
• a few (bad) actors are the problem
• over application of N (or P) is most of the problem
• just targeting a few fields will solve most of the problem
• edge of field denitrification can solve the problem
• the response will take a long time (decades?)
What’s making it difficult
• more corn (and fertilizer)
• more intensive tile drainage
• warmer winters
• more intense winter/spring precipitation
• fall N in Illinois, Indiana, Ohio
• the intensity of agriculture across the cornbelt
• many (most?) practices to reduce nutrient loss don’t increase yield
Conclusions
• N and P balances don’t relate well to nitrate and P loss across the MRB (but could increase losses in a drought year)
• counties with high fertilizer inputs have high crop fractions (& corn acres) and tile drainage– all lead to nitrate loss
– corn & soybeans on tile drained land much more important than manure, deposition, or sewage effluent
• P from both surface runoff and tiles– sewage effluent also important
• high winter/spring flow and nutrient losses are a challenge, and seem to be getting worse
Job ahead for us
• 45% reductions in N and P will be quite difficult in upper MRB
• we haven’t really started
– not in any meaningful way
• variety of methods and costs
– many or most unrelated to yields
• scale of problem is impressive
• but, we do know how to do it!