- Soil can be divided into different soil layers (improvement unsaturated zone, soil moisture) - For vertical transfer from unsat zone to sa…
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- Soil can be divided into different soil layers (improvement unsaturated zone, soil moisture) - For vertical transfer from unsat zone to saturated zone user can choose between sbm concept or brooks-corey approach, flux between unsat layers always with brooks-corey approach and unit gradient assumption - Changed lateral transfer method 2 (integration of Ksat over waterdepth) - Some more testing required (Rhine case?, water balance components, difference with wflow_sbm.py (1 layer))
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