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Evaluation
The initially flat and then getting steeper drop down in the water water
•
content with increasing pF is characteristic of very fine grained and clay
substrates.
The hydraulic conductivity at pF 2 is very high, but the curve then is even
•
more steep than in the case of clay.
The description of the data with models is not a problem, however in dry
•
areas completely unsure. Suitable models are e.g. the van Genuchten
model, or Kosugi model.
86 | Addendum
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