application of modelling in the assessment of control measures to reduce diffuse pollution dr kevin...
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Application of modelling in the assessment of control measures to reduce diffuse pollution
Dr Kevin Hiscock
School of Environmental SciencesUniversity of East Anglia
Norwich, UK
(E-mail [email protected])
Acknowledgement: Han ZhangFunding: Chinese Scholarship Council & University of East Anglia
OUTLINE of PRESENTATION
• To demonstrate the objective use of groundwater flow and nitrate transport models in the assessment of diffuse pollution control measures
• To estimate the amount of land-use change needed to meet groundwater standards
• To assess the impact of land-use change on groundwater quantity (groundwater recharge and groundwater level)
• To compare arable land conversion to woodland with other agricultural management practices such as cover crops and fertiliser reduction
Background to nitrate pollutionBackground to nitrate pollution
Groundwater qualityGroundwater quality (nitrate)(nitrate)
Nitrate concentration in drinking water < 50mg/l
(Water Framework Directive 2000/60/EC)
Increasing woodland as a land-use change strategy Increasing woodland as a land-use change strategy for controlling diffuse pollutionfor controlling diffuse pollution
Current UK government policy (Current UK government policy (The England Forestry The England Forestry Strategy, Regional Forestry Frameworks, Community Forests Strategy, Regional Forestry Frameworks, Community Forests Partnerships, Farm Woodland Premium SchemePartnerships, Farm Woodland Premium Scheme) aims to ) aims to increase woodland cover (currently only 8.5% in increase woodland cover (currently only 8.5% in England)England)
NVZ - Nitrate Vulnerable Zones NVZ - Nitrate Vulnerable Zones
Pilot case studiesPilot case studies
Water4allWater4all Project Project Lincolnshire LimestoneLincolnshire Limestone Afforestation Afforestation Denmark, GermanyDenmark, Germany Give N reduction potential Give N reduction potential
Increase woodland, less recharge, water shortage? Increase woodland, less recharge, water shortage? Conversion from arable land to woodlandConversion from arable land to woodland
may reduce groundwater recharge and lead to fall of the may reduce groundwater recharge and lead to fall of the groundwater table as trees tend to consume more water than groundwater table as trees tend to consume more water than other vegetationother vegetation ( (Bosch & Hewlett 1982; Blackie 1993, Sahin & Bosch & Hewlett 1982; Blackie 1993, Sahin & Hall 1996; Calder 2003Hall 1996; Calder 2003))
Recharge volume: pine forest < oak woodland < Recharge volume: pine forest < oak woodland <
grasslandgrassland Trees and Drought Project of Lowland England Trees and Drought Project of Lowland England (TaDPoLE)(TaDPoLE)
may aggravate the problem of water shortages due to reduced may aggravate the problem of water shortages due to reduced recharge under forest cover recharge under forest cover ((Farley 2005; Farley 2005; Bending 1997; Calder Bending 1997; Calder 2000; Finch 20012000; Finch 2001))
the recharge of groundwater beneath broadleaved the recharge of groundwater beneath broadleaved woodland and grass sites in a Chalk aquifer study was woodland and grass sites in a Chalk aquifer study was almost the samealmost the same ((Roberts, 2006Roberts, 2006))
Tools and Methods
ArcGIS – ArcMap (Land-use type and area)
Recharge model – vegetation water requirement Visual MODFLOW v4.1 – groundwater flow model
Export coefficient model – nitrogen load and leaching
MT3DMS – nitrate transport model
MODPATH – define abstraction borehole capture zones
N Losses
Leachate concentration
Mass transport modelling
MT3DM
Scenario
predictions
GW Recharge Recharge Model
LCM
N Input
Export coefficient
MODFLOW
GW Flow modelling
Tree species conversion
Land-use change
Agricultural management
PATHLINE
Approach and modelling strategy
Location map of the study area
• West NottinghamshireWest Nottinghamshire, East Midlands
• Area: 50 km N-S Area: 50 km N-S ×× 30 km W-E30 km W-E • Sherwood Sandstone aquiferSherwood Sandstone aquifer
• Sandstone dips eastwards at Sandstone dips eastwards at about 1 in 50 about 1 in 50
• In the east, low-permeabilityIn the east, low-permeability mudstone overlies the sandstone mudstone overlies the sandstone
Dover
Greet
Ryton
IdlePoulter
Meden
Maun
Severn Trent Sandstone
Mudstone
Land-use map (LCM2000)
Arable agriculture covers approximately 75% of outcrop area and receives largequantities of nitrogen (e.g. manure and fertiliser applications to crops)
Nitrate concentration in abstraction boreholes (Unconfined aquifer, data source Severn-Trent Water, year 2007)
0
50
100
0 5 10 15 20 25 30 35 40
Borehole number
Nit
rate
co
nce
ntr
atio
n m
m/l
(mg
/l)
GW nitrate mg/l
3 - 10
11 - 35
36 - 50
51 - 70
71 - 230
SW nitrate mg/l
12 - 10
11 - 35
36 - 50
51 - 70
N loss kg N/yr1634 - 6000
6001 - 12000
12001 - 15000
15001 - 28000
Diffuse N losses and observed NO3- concentrations
Groundwater Flow Modelling
Criteria for model calibration groundwater levels in 27 observation boreholes
(Environmental Agency)
River flows at 10 river gauging stations (National River Flow Archive)
Particle-tracking MODPATH: using calibrated GW model to
generate capture zone of abstraction borehole
85
89
93
97
101
105
109
113
Jan-8
6
Jan-8
8
Dec-8
9
Dec-9
1
Dec-9
3
Dec-9
5
Dec-9
7
Dec-9
9
Dec-0
1
Dec-0
3
Dec-0
5
Gro
un
dw
ate
r H
ea
d (
m)
Observation Head
Calculated Head
20
24
28
32
36
40
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Gro
un
dw
ate
r H
ea
d (
m) Observation Head
Calculated Head
30
34
38
42
46
50
54
Jan-8
6
Jan-8
8
Dec-8
9
Dec-9
1
Dec-9
3
Dec-9
5
Dec-9
7
Dec-9
9
Dec-0
1
Dec-0
3
Dec-0
5
Gro
un
dw
ate
r H
ea
d (
m)
Observation Head
Calculated Head
34
38
42
46
50
54
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Gro
undw
ater
Hea
d (m
)
Observation Head
Calculated Head
Modelled GW level vs. Observed GW level in 1986-Modelled GW level vs. Observed GW level in 1986-20062006
Well 1729DUCHESS PLANTATION
Well 1740 KIGHILL
Well 1793CLIPSTONE FOREST
Well 1722CROSSLEY HILL
Observed vs. simulated river flow
Station 280116 (Ryton)
0
100000
200000
300000
400000
500000
600000
Jan
-86
Jan
-87
Jan
-88
Jan
-89
Jan
-90
Jan
-91
Jan
-92
Jan
-93
Jan
-94
Jan
-95
Jan
-96
Jan
-97
Jan
-98
Jan
-99
Jan
-00
Jan
-01
Jan
-02
Jan
-03
Jan
-04
Jan
-05
Jan
-06
Dis
cha
rge
(m
3 /d)
measured
modelled
Station 28118 (Meden)
0
40000
80000
120000
160000
200000
240000
Jan-9
4
Jan-9
5
Jan-9
6
Jan-9
7
Jan-9
8
Jan-9
9
Jan-0
0
Jan-0
1
Jan-0
2
Jan-0
3
Jan-0
4
Jan-0
5
Jan-0
6
Dis
cha
rge
(m
3/d
)
modelled
measured
GW pathline calculation to determine capture zones Budby
Budby Forest
Nitrate Transport Model
Nitrate concentration recharge Nitrogen losses- Export coefficient modelling GW recharge Nitrate concentration
Criteria for nitrate transport model nitrate concentrations at 24 groundwater
monitoring points (EA) / groundwater abstraction boreholes (STW)
Nitrate concentration = Nitrogen losses / GW recharge
Example: Estimation of N loss for a cell (2 km x 2 km)
Source (462000, 384000)
Area (ha)
Input N (kg/ha)
Export Coef. loading(N/ha)
N loss (kg/yr)
Source Area (ha)/ head
Input N (kg/ha or head)
Export Coef. loading(N/ha)
N loss (kg/yr)
Wheat 55.60 177.1 0.23 2264.8 Perm- grass 39.5 115.5 0.25 1141.7
Winter Barley 22.51 143.3 0.2 645.1 Grazing grass 0.2 123.7 0.05 0.9
Spring Barley 25.53 110.5 0.4 1128.4 Woodland 10.3 10 102.9
Oats 1.29 112.6 0.3 43.6 Set-aside 40.0 30.00 1199.8
Other cereals 11.11 118.7 0.3 395.6 All other land 13.0 5.00 65.0
Potatoes 13.65 168.9 0.39 899.1 Labour 7.5 2.14 15.9
Sugar beet 29.72 105.4 0.17 532.5 Cattle 56.2 70.2 0.16 635.4
Field beans 0.00 32.8 0.48 0.0 Sheep 248.5 10.1 0.17 426.6
Peas 5.57 49.1 0.48 131.3 Pigs 0.0 18.8 0.10 0.0
Oilseed Rape 14.72 175.0 0.42 1081.9 Poultry 14.0 0.6 0.07 0.5
Other arable 14.81 101.5 0.3 451.0 Rough grass 25.2 5.00 126.0
Horticulture 21.22 76.8 0.35 570.4 Broadleaves 35.5 6.00 213.0
Bare fallow 0.15 5 0.8 Conifer 15.5 12.00 186.0
Tem-grass 10.33 176.2 0.25 455.0 Non-agri 5.1 5.00 25.7
Total cell N loss kg N/yr
12738.9
Modelled nitrate distribution and N losses in 2006
0
20
30
40
50
60 mg/l
nitrogen loading 1634 - 5474
5475 - 10183
10184 - 14128
14129 - 20000
20001 - 27482
N kg/yr/cell
0
1
2
3
4
5
6
7
8
9
10
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Nitr
ate
conc
ernt
ratio
n [m
g/l]
Observed value
Modelled value
Modelled and observed groundwater nitrate concentrations
0
10
20
30
40
50
60
70
80
90
100
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Nitr
ate
conc
ernt
ratio
n [m
g/l]
Observed value
Modelled value
0
10
20
30
40
50
60
70
80
90
100
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Nitr
ate
conc
ernt
ratio
n [m
g/l]
Observed value
Modelled value
0
10
20
30
40
50
60
70
80
90
100
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Nitr
ate
conc
ernt
ratio
n [m
g/l]
Observed value
Modelled value
BOUGHTON 2
BURTON JOYCE (confined) PAPPLEWICK
AMEN CORNER 2
Modelled and observed nitrate concentrations (Forest areas)
BUDBY FOREST 1
0
5
10
15
20
25
30
35
40
45
50
Jan-
86
Jan-
88
Dec
-89
Dec
-91
Dec
-93
Dec
-95
Dec
-97
Dec
-99
Dec
-01
Dec
-03
Dec
-05
Nitr
ate
conc
ernt
ratio
n [m
g/l]
Observed value
Modelled value
CLIPSTONE FOREST 3
Model application to scenario prediction
Tree species conversion Conifer Broadleaf Broadleaf Conifer
Land-use Change Arable lands Woodland Arable lands Unfertilised grassland
Land management practices Cover crops in winter Fertiliser reduction
Prediction 1: Effect of tree species conversion on GW
Site 1 Site 2 Site 3
Broadleaf replaces conifer
14.4%5.8 cm
26.3%35.4 cm
8.5%5.3 cm
Conifer replaces broadleaf
-11.7%- 6.5cm
-3.7 %- 2.9cm
-8.3 %- 4.9cm
Changes of GW recharge (%) and water level (cm)
1
2
3
Prediction 2: Effect of land-use change on GW
Arable
27.7%
Grass
15.2%
Conifer
20.2%
Other
17.1%
Broadleaf
19.8%
Arable
?
Grass
15.2%
Conifer
?
Other
17.1%
Broadleaf
?
11935 kg N/yr N Losses 9250 kg N/yr
Soil Leachate NO3-
GW NO3-
99.75 mg/l 89.14 mg/l
62.21 mg/l 50 mg/l
y = 0.521x + 3.4051
R2 = 0.8665
0.0
10.0
20.0
30.0
40.0
50.0
60.0
70.0
80.0
90.0
0.0 20.0 40.0 60.0 80.0 100.0 120.0 140.0 160.0 180.0
Soil NO3 (mg/l)
Gro
undw
ater
NO
3 (m
g/l)
Estimation of proportion of woodland (Far Baulker)
Estimation of area of land-use change required to meet 50 mg/l groundwater nitrate (Far Baulker)
Baseline Increase Woodland Increase Grassland
Arable 50.66% 29.90% 32.25%
Grass 15.20% 15.20% 33.60%
Broadleaf 8.75% 19.13% 8.75%
Conifer 8.30% 18.67% 8.30%
Other 17.10% 17.10% 17.10%
Total wood 17.05% 37.80%
Change +20.75% +18.40%
Effect of land-use change on GW nitrate concentration(Far Baulker)
0
50
100
Jan/86
Jan/88
Dec/89
Dec/91
Dec/93
Dec/95
Dec/97
Dec/99
Dec/01
Dec/03
Dec/05
Dec/07
Dec/09
Dec/11
Dec/13
Dec/15
Dec/17
Dec/19
Dec/21
Dec/23
Dec/25
Time
Nit
rate
co
nc
en
tra
tio
n m
g/l
Observation
baseline
40% w oodland
30% grassland
0
50
100
Jan-86
Jan-88
Dec-89
Dec-91
Dec-93
Dec-95
Dec-97
Dec-99
Dec-01
Dec-03
Dec-05
Dec-07
Dec-09
Dec-11
Dec-13
Dec-15
Dec-17
Dec-19
Dec-21
Dec-23
Dec-25
Time
Nitr
ate
co
nce
ntr
atio
n m
g/l
Observation
average monthly baseline
100% cover crop
Cover CropsTo be applied on spring cultivated cereals, set-aside, horticultural cropsNot to be applied on winter cereals, sugar beet and potato crops
Prediction 3: Effect of Agricultural Practices on GW
Effect of fertiliser reduction on GW nitrate concentration
0
50
100
Jan-86
Jan-88
Dec-89
Dec-91
Dec-93
Dec-95
Dec-97
Dec-99
Dec-01
Dec-03
Dec-05
Dec-07
Dec-09
Dec-11
Dec-13
Dec-15
Dec-17
Dec-19
Dec-21
Dec-23
Dec-25
Time
Nit
rate
co
nc
en
tra
tio
n m
g/l
Observation
baseline
32% fertiliser reduction
40% fertiliser reduction
64% fertiliser reduction
• Groundwater flow and nitrate transport models can represent
historical data appropriately
• Borehole capture zones generated by a calibrated groundwater
model can be used to propose land-used change scenarios
• Calibrated models can be used to assess the effect of land-use
change on both groundwater quantity and quality
• Tree species conversion in specified model cells did not greatly
affect groundwater level, although recharge reduction occurs as a
result of conifer replacing broadleaf forest
• Land-use change has more effectiveness in controlling nitrate
pollution than agricultural management practices used in isolation
Conclusions