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Paysages virtuels et analyse de scénarios pour évaluer les impacts ...

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The life-cycle analysis survey conducted in 2003 with the farmers (Payrau<strong>de</strong>au <strong>et</strong> al., 2006) located the<br />

farmsteads of the catchment, and <strong>de</strong>picted a typology of the farming activities composed of four farm-types:<br />

- dairy (13 farmsteads), which concerned 33% of the total agricultural area;<br />

- pig (6 farmsteads), 34%;<br />

- dairy-pig (10 farmsteads), 19%;<br />

- other (8 farmsteads), 14%, which artificially grouped (i) farmsteads of unknown activity, and (ii)<br />

farmsteads with marginal farm activities.<br />

Given the locations of the farmsteads (Payrau<strong>de</strong>au <strong>et</strong> al., 2006) and of their fields (Bor<strong>de</strong>nave <strong>et</strong> al., 2005),<br />

we associated a distance-to-farmstead to each field. The eucli<strong>de</strong>an distance b<strong>et</strong>ween the farmstead and the<br />

centroid of the field polygons seemed a reasonable estimator of the accessibility of the fields because the<br />

road n<strong>et</strong>work is rather <strong>de</strong>nse and isotropic in this catchment. Fig. III.19.c shows the distance-to-farmstead of<br />

the field in year 2000 and the road n<strong>et</strong>work of Naizin.<br />

The nine original classes of soil waterlogging <strong>de</strong>scribed in the soil map of the catchment (Walter and Curmi,<br />

1998) were aggregated into the following classes (Fig. III.19.b):<br />

- 1 (well-drained): no soil redoximorphic feature within the first 80 cm. This class represents 43% of<br />

the total agricultural area;<br />

- 2 (intermediate): weak soil redoximorphic features at <strong>les</strong>s than 80 cm, 44%;<br />

- 3 (waterlogged): intense redoximorphic features from the surface, 13%.<br />

Each field was characterized by the dominant soil hydromorphy class represented within its limits. This<br />

waterlogging attribute can be consi<strong>de</strong>red constant through time since most of the artificial drainage systems<br />

were s<strong>et</strong>up before 1993 in this catchment.<br />

The topography of the catchment is relatively smooth (mean slope is below 5%, with maximal values of<br />

14%), its highest point is at 136 m above the sea level while its outl<strong>et</strong> is at 60 m (Walter and Curmi, 1998).<br />

The overall gentle slopes are not limiting for the preparation and cultivation of crops.<br />

Agronomic constraints on the agricultural landuse of Naizin<br />

Besi<strong>de</strong> the crop succession itself, which is known to play a key role in the farm management of soil fertility<br />

and nutrients dynamics (Thornton and Jones, 1998), we tested the relevance of four presumed spatial driving<br />

factors of crop transition in Naizin:<br />

- farm-type: farmstead sharing the same activity and main production (milk, pigs, <strong>et</strong>c.) are submitted<br />

to the similar constraints (Thenail and Baudry, 2004). Moreover, the life-cycle analysis also<br />

revealed that fields of some farmsteads of Naizin were outsi<strong>de</strong> the surveyed area, and similarly, that<br />

some surveyed fields of Naizin belonged to farmsteads located just outsi<strong>de</strong> the catchment divi<strong>de</strong>s.<br />

The existence of these sparse field patterns ma<strong>de</strong> it more relevant to study the agricultural driving<br />

factors of crop transition at the farm-type scale instead of the farm scale;<br />

III. Stochastree, un modèle <strong>de</strong> successions <strong>de</strong> cultures basé sur <strong>de</strong>s arbres <strong>de</strong> décision stochastique – p. 76

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