Evaluation of Pesticide Scenarios for the Registration Procedure

Appendix B Description of Hamburg Scenario

1.1 Conceptual Model

The conceptual model given in the FOCUS groundwater scenario for Hamburg describes a 2 m deep sandy soil column containing six different horizons. This sandy media is rather homogeneous and macropore flow is not considered.

1.2 Data

The climate and soil data for the Hamburg scenario are described in "FOCUS groundwater scenarios in the EU review of active substances" - The report of the work of the Groundwater Scenarios Workgroup of FOCUS (FOCUS, 2000). (http://viso.ei.jrc.it/focus/gw/).

1.2.1     Climate

The precipitation and the mean annual temperature are within the range of 601 to 800 mm and 5 to 12.5°C, respectively. More information can be found in Kördel et al. (1989).

Figure 1 and 2 illustrate PELMO´s FOCUS-standard output for the annual water balance in mm separated into evapotranspiration (volatilisation), runoff (surface runoff) and percolation for use of respectively winter and spring cereals. The figures show that for the application of the winter cereals instead of spring cereals will give a larger percolation through the soil, less surface runoff, and less evaporation. The origin of these climate data is not clear and is not to be found in Kördel et al. (1989).

Figure 1. Annual water balance including evapotranspiration, runoff and percolation for the Hamburg scenario when applying winter cereals annually.

Figure 1. Annual water balance including evapotranspiration, runoff and percolation for the Hamburg scenario when applying winter cereals annually.

Figure 2. Annual water balance including evapotranspiration, runoff and percolation for the Hamburg scenario when applying spring cereals annually.

Figure 2. Annual water balance including evapotranspiration, runoff and percolation for the Hamburg scenario when applying spring cereals annually.

1.2.2     Soil

The soil texture and hydraulic properties incorporated in PELMO for the six horizons are described in Table B1 and B2. The Hamburg soil profile has a very low organic matter content below a depth of 60 cm, which could increase the leaching to the groundwater (Boesten, 1991).

Table B1. Soil texture (FOCUS groundwater scenarios in the EU review of active substances)

Horizon Depth Classification pH-
H2O
pH-
KCl
Texture om oc Bulk density Depth
Factor
  Cm       <2 mm
[%]
2-50
mm
[%]
>50
mm
[%]
[%] [%] [gcm-3] [-]
Ap 0-30 Sandy loam 6.4 5.7 7.2 24.5 68.3 2.6 1.5 1.5 1.0
BvI 30-60 Sandy loam 5.6 4.9 6.7 26.3 67 1.7 1 1.6 0.5
BvII 60-75 Sand 5.6 4.9 0.9 2.9 96.2 0.34 0.2 1.56 0.3
Bv/Cv 75-90 Sand 5.7 5.0 0.0 0.2 99.8 0.0 0.0 1.62 0.3
Cv 90-100 Sand 5.5 4.8 0.0 0.0 100 0.0 0.0 1.6 0.3
Cv 100-200 Sand 5.5 4.8 0.0 0.0 100 0.0 0.0 1.6 0.0

Table B2. Soil hydraulic properties, Van Genuchten/Mualem parameters. *AW: Plant available water in the layer.

Depth qs qs a N M Water content Ksat l AW*
            10kPa 1600kPa      
  [m³m-3] [m³m-3] [m-1] - - [m³m-3] [m³m-3] [ms-1] - [mm]
0-30 0.3910 0.0360 1.491 1.4680 0.3188 0.292 0.064 23.330 0.500 68.4
30-60 0.3700 0.0300 1.255 1.5650 0.3610 0.277 0.047 31.670 0.500 69.0
60-75 0.3510 0.0290 1.808 1.5980 0.3742 0.229 0.040 28.330 0.500 28.4
75-90 0.3100 0.0150 2.812 1.6060 0.3773 0.163 0.022 28.330 0.500 21.2
90-100 0.3100 0.0150 2.812 1.6060 0.3773 0.163 0.022 28.330 0.500 14.1
100-200 0.3100 0.0150 2.812 1.6060 0.3773 0.163 0.022 28.330 0.500  

 



Version 1.0 August 2007, © Danish Environmental Protection Agency