What do you use in a runoff model if you do not have Edaphological (soil) data for an area? How would you simulate infiltration?
I am using MIKESHE by DHI to create a water balance model, more specifically a runoff model. In this software you add various data like daily precipitation, Temperature, snow melt, land uses from corine database (including root depth LAI etc) and you also add the catchment shape files and the DEM, and more. The problem comes when you need to know the field capacity of the soil, or the Permanent wilting point and the hydraulic conductivities - for every soil type defined from a shape file. But in my area there are no edaphological maps, so some people use geological maps and try to derive some soil classes. For example: limestone > hondrococcus soil > big permeability K = from ... to... .
Or use some hydrolithological maps that have the K ( hydraulic conductivity) ready to use.. but you wont know the Fc or PwP.
One idea is to make an overlay of the hydraulithological maps with the geological and use both so I can extract some info about the soil type. But there is another problem, what happens to the mountainous areas that there is no soil, like the bold mountain slopes? I cannot see these on my map except if I use Google Earth and then digitize the image with polygons. Too much. Or if use the slope and say for example that in slopes of 20% or above there can\t be any soil. Do you have any ideas?