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SOIL PROTECTION Catalunya - the Balearic Islands / Principality of Andorra

 
 

soil protection (general information)

 

Vienna Soil Declaration

 

soil functions

sustainability criteria

degradation and control processes

soil protection criteria

soil quality indicators

soil maps

what is soil information used fort?

the purpose of soil maps

soil series and correlation

characteristics of a soils map

management and interpretation of soil information on a digital interface

Soil Series and Soil Types catalogue of Catalonia

presentation

criteria

soil Types (> 2010)

soil Series (1993 - 2009)

CHARACTERISTICS OF A MAP

ZOOM EFFECT: the degree of accuracy of a soil map

When using digital maps it is important to take into account the fact that:

– despite appearing to be completely homogenous, as they are presented with
   delineations of the same colour or symbol, polygons may have
   inclusions which cannot be represented. The minimum surface area
   that can be represented on the map with the map remaining legible
    is a 5 mm square.

– although the limits between delineations (polygons) are represented
   on the map by a line, they should not be interpreted as
   discontinuities in a landscape, as the lateral variation
   of the soils is gradual. Furthermore, the positions of the
   different limits relate to a specific degree of precision
   and an acceptable degree of error, although the latter has
   been considerably reduced since GPS systems became available.

– in order to increase the predictive capacity of a map it is necessary
   to return to the field and increase the density of observations.
   Zooming in and increasing the surface area of each delineation
   on a soil map (and apparently its scale) using computer technology
   does not automatically imply a parallel increase in the quality or
   predictive capacity of the map in question.




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