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Landscape scale assessment of

nitrogen interactions

Pierre CELLIER, Albert BLEEKER, Eva BØGH, Lutz BREUER, Nicolas

BRUEGGEMANN, Tommy DALGAARD, Ulrike DRAGOSITS, Jean-Louis

DROUET, Patrick DURAND, Enzo MAGLIULO, Jørgen OLESEN

Lech RYSZKOWSKI, Mark THEOBALD, Mark SUTTON



INRA (F), ECN (NL), Univ. Roskilde (DK), Univ. Giessen (D),

IMK-IFU (D), DIAS (DK), CEH (UK), RCAFE (PL)









Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

How can be seen a landscape with a

nitrogen perspective?

A patchwork of sources and sinks of N in the natural (fields,

forests, natural ecosystems) and « man-made » environments

(building, villages, roads)

(both largely determined by human activities in the past and present)

with a significant fraction of sources and sinks managed by man

and possible mitigation on both.





Special focus on rural landscapes

where large amounts of N are

manipulated

 agricultural areas with livestock,

pigs, poultry, …





What are the interactions between these sources and sinks,

and the consequences on N2O fluxes?

Courtesy J.E. Olesen ?? on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Open Science Conference

What happens to reactive nitrogen

emitted to the atmosphere and the soil

in such areas?









Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Local recapture of ammonia

by tree-belts close to a source

B. Loubet et al. (collab INRA / CEH)

10

10 Canopy Length

L15= 15 m

m

8



Using a lagrangian-stochastic model









z (m)

6









z (m)

(MODDAS-2D, Loubet et al., 2006) to estimate

4

NH3 deposition and concentration field close

to a source (animal housing) surrounded 2

2.1%

NH3 Concentration

(2.1%) (g m-3)

by a tree belt of different widths 00

10

10 Canopy Length 0

8

30 = 30 m

L m Scenario)

(Base

10

20









z (m)

30

6 40









z (m)

50

10

16

L 4 60

70

Animal housing









14 2 80





00 4.6%

(4.6%)

90

100

12

10

10

10 Canopy Length

8 60 m

Tree

z (m)

Z (m)









L = 70 m

z (m)





8

Belt 6

z (m)









6

4



4

2

7.1%

(7.1%)

2

00



00 0

90

10

100

20

110

30 130 40

120 140

50 150

60160 70

0

0 10 20

x (m) 40

30 50 60 70

70 x (m)

x (m)

X (m)

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Ammonia deposition can induce

large input to neighbour ecosystems

NORTH

100

Deposition 80

Kg N ha-1 y-1

60









Distance to the farm (m)

240-280

200-240 40









EAST

WEST



160-200 20









FARM

120-160

0

80-120

-20

40-80

0-40 -40



-60

0









60

20



40

-60



-40









80



100

-20









Distance to the farm (m)

from Fowler et al. (1998) SOUTH from Fowler et al. (1998)



 are there N2O emissions induced by these hot-spots of NH3 deposition?



Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Atmospheric deposition from « source »

to « sink » fields

8



7



6

wind

5



4



3



2



1



0

1 2 3 4 5

S1

S3 Deposition = 6.4% of the emissions

6 7 8







8



7



6 wind

5



4



3



2



1



0

1 2 3 4 5 6 7 8

S1

S4

Deposition = 3.4% of the emissions

8



7



6 wind

5



4



3



2



1



0

1 2 3 4 S1

S3 Deposition = 8.2% of the emissions

5 6 7 8









Bare soil where slurry has been applied  large ammonia emission

Grassland with LAI = 2

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Nitrate transfer and N2O emissions at

catchment scale in shallow groundwater systems

N2O emission







Nitrate

leaching

Denitrification



Nitrate

transfer



Nitrate

recapture

by crops

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Consequence of hydrological transfer

on N2O emission at catchment scale

Soil-groundwater interaction zone









Distributed denitrification









TNT2

Model





Distributed N concentration in groundwater

from Patrick Durand, INRA Rennes

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Transfer of nitrogen by the atmosphere and the

hydrology can create delocalized hot-spots of

N2O emission (indirect emission) at local scale,

and modify the GHG balance at landscape scale.



This is sensitive to the arrangement of landscape

elements (farm, vegetation, humid zones, …)









Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Atmospheric N2 Nitrous Oxide

fixed to reactive

(N2O)

nitrogen (NR)





Nitrogen oxides Ammonium nitrate

(NOx) in rain (NH4NO3)

NR

Further emission

Fertilizer

Ammonia of NOx & N2O

manufacture NR (NH3) carrying on

the cascade





Crops for food &

animal feed



The

Livestock farming

Nitrogen Natural ecosystems





Cascade Leached Nitrate

(NO3-) Nitrate in

streamwaters



Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Accounting for the farm dimension

allows to ensure …



• Accounting of all emissions (housing, field work, transport, indirect, …)

• N and C flows consistency

• N/C allocation to fields (amount+timing)

• Estimate at farm scale (see e.g. GreenGrass results)

• …

• Link with management

• Link with mitigation options



Moreover, the farm is a part of the landscape









Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Nitrogen flows on a mixed cattle farm

(FASSET model, DIAS, DK)

Manure

104 76 Import of

store Animals feed+straw

10 39

94

N2 129 Sale of

milk+meat

59 Crop

NH3 Above-ground 51 Sale of

11(+11) Below-ground plant prod.

85 105 238

13 Import of

116 64

Soil 74 fertiliser

<1 6 76

<1

2 Nitrous oxide emissions:

N2O NO3 7933 kg CO2-eq/ha/yr

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Two examples of output from a farm model

Emissions per kg milk produced

2.2









Greenhouse gas emissions (kg CO2-eq kg-1milk)

Emissions Conventional

Organic

2.0

component

per Animals

1.8





Animal Pre- Pre-chain1.6



chain

1.4

use House

Manure 1.2

anure Field

1.0

12 14 16 18 20 22 24 26 28

Field Farm N efficiency, output/input (%)



 Integrate all components  Allows to compare farming system

at farm scale on farm scale basis

(FASSET model, DIAS, DK)

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Organization of farm activity in space:

example of an INRA experimental farm

Heifers

Dairy cows

Hay night pasture from

Jean-Louis FIORELLI

FARM

INRA Mirecourt

Calves

grassland

Steers Dairy cows

Heifers cropland

day pasture



Calves

Heifers

N used at farm scale is not

Hay disposed randomly nor

uniformly to land

 need to consider spatial

+ slurry/manure management interactions

+ hay / silage management

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

A ± common scale to all « processes »

NORTH

100

n 80

y-1

60









Distance to the farm (m)

40









EAST

WEST









20

FARM









0



-20



-40



-60

0









60

20



40

-60



-40









80



100

-20









Distance to the farm (m)

er et al. (1998) SOUTH

1 km

100 m



100 m – 1 km



 typical scale of 100-101 km²

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Need for a coupled model

The biophysical model The farm model needs

(ecosystem/atmosphere a biophysical model to

/hydrology) needs a • improve emission

farm model to estimates at field

• allocate N and C to • account for the

field characteristics of the

• ensure consistency at environment

farm/regional scale

• link with decision  Need decision rules

making to allocate N in space



Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

The landscape scale in NitroEurope:

development of the NitroScape model



Controller

programme

Local and regional atmospheric dispersion





Nested atmospheric model

Meteorol.

input data

Landscape database & GIS

Landscape database & GIS





Emission / deposition

Landscape

Landscape inventory Farm management model



database input data

Non-agric Forest & Grass Arable Farm buildings

sources shrubland fields fields & manure stores

Soils &

hydrology Multi-ecosystem model

input data Choosing the

Output maps Leaching / uptake relevant models :

datasets & • atmospheric

• hydrological

scenarios Distributed hydrological model



Model data exchange

• ecosystem

• farm

Lateral transfer in catchments

N & C flux

(in a consistent way)

GIS

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Concepts of model linking





Model C

Database

(input data)

Model A

Database

Wrapper (input data)

Calls models

Model A & database,

Model C Provides

input Database

= A+B from & Model A Model C (input data)

collects

Model B output to DB

at iterations



Model B Model B







Re-coding Linked models (1) Linked models (2)

(OpenMI, Palm, MCT,

…)



Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

NEU-C4 : establishing a network of landscape sites



NitroEurope – NEU Landscape network









Leadburn

Bjerringbro





Turew



Vel Vanla



Naizin

- Different climatic conditions

Piana del Sele

- Different farming systems

- High N inputs but ≠ levels

- Mixing of fields/farms and natural

ecosystems  deposition

- Landscape size : ≈ 5 km x 5 km

- Local involvement of farmers

Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006

Summary:

landscape scale analysis must be made in

the context of nitrogen research because:

• Complexity of the environment and possible interactions between,

physical, biological and human « environments »

• Scale of management/decision making,of application for abatement

options

• Need for understanding basic processes and interactions at this

scale and interactions between natural environment and processes

and decision-making

• Help to account for the environment in N management and

mitigation options

• Helpfull to upscale from farm/field emission to regional scale, and

make balances at landscape and farm scale









Open Science Conference on the GHG Cycle in the Northern Hemisphere, Sissi-Lassithi, Crete, 14th-17th November 2006



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