Thank you David, that is a much longer answer that I would have written
;) but you explained the problem very well.
I would just like to add to that: you can at any time check the Taxonomy
points we are using for supervised training:
https://github.com/ISRICWorldSoil/SoilGrids250m/blob/master/grids/models/TAXNWRB/TAXNWRB_observed.kmz
https://github.com/ISRICWorldSoil/SoilGrids250m/blob/master/grids/models/TAXOUSDA/TAXOUSDA_observed.kmz
Indeed, even though USDA Soil Taxonomy is one of the most comprehensive
and most detailed classification systems, we have only dozen of points
for Argentina, Chile etc, so yes if you have some ground truth data from
existing surveys - please forward and we will add them to the training data.
Gracias,
T. (Tom) Hengl
Researcher @ ISRIC - World Soil Information
Url:
http://www.isric.org/tomhengl
Network:
http://profiles.google.com/tom.hengl
Publications:
http://scholar.google.com/citations?user=2oYU7S8AAAAJ
ORCID ID:
http://orcid.org/0000-0002-9921-5129
Important note: I do not work on Wednesdays (parental leave).
On 14-09-17 22:18, Rossiter, David wrote:
> Hello Miguel,
>
> I am copying my answer to Tom Hengl, who is the brains behind SoilGrids, he may be able to add some information.
>
> 1. SoilGrids is based on a global-scale machine-learning model, and there is no way to adjust it for local knowledge. What you see is how a machine learns, based on a large number of (global) calibration points. One solution is to add known points to WoSIS
http://www.isric.org/explore/wosis, our profile database; this will improve predictions. That page explains how to contribute.
>
> 2. The most probable class, in this case Ustox, is “competing” with other classes. In SoilGrids, choose “Class Probabilities” instead of “Predicted most probable class”, and you will see a legend showing how probable is the Ustox. For example, in the area around La Rioja, probabilities range from near 0 to about 30%; most of the areas where Ustox is most probable are at about 20%. Other classes have their own probalility. In that area Ustolls are not at all probable, arouind 5%, Ustalfs a bit more, about 10-15%. So you can see just how much one class is favoured over the others.
>
> 3. A particular problem with ST classes is the poor or obsolete classification of profiles worldwide. We can only go by the classification given to us, we can not reclassify everything from the profile description, even if we had time. So SoilGrids is probably more useful for the soil properties themselves. Look at the SOC at various depths, I think you will find that a much more realistic picture. You could use those maps to do your own classification, at least in part.
>
> 4. We encourage you to use SoilGrids as a prior layer, as a covariate in your own mapping using the same methods, which are documented (and R code provided) on the SoilGrids web pages. If you have more or more accurate points and youl work in a smaller area, the prior (global) predictions will be corrected.
>
> I hope this is useful information.
>
> Recibe un saludo cordial de mi parte, atentamente,
>
> Rossiter, D G (David)
> Guest Researcher
> ISRIC - World Soil Information
>
david.r...@wur.nl<mailto:
david.r...@wur.nl>
>
>
>
>
>
> On 13 Sep 2017, at 20:39, Miguel Alejandro Becerra <
mabe...@agro.unc.edu.ar<mailto:
mabe...@agro.unc.edu.ar>> wrote:
>
> Hello David,
> I was checking
soilgrids.org/<
http://soilgrids.org/> and I noticed that a large area of Argentina (and Chile) it is supposed to have Oxisols when it is not true. At least in Argentina the most part of the supposed Oxisols are occupied by Mollisols (in particular Ustolls) or Alfisols.
> I do not know how the prediction is made but I hope that it can be improved in the future.
> I'll be glad to collaborate if you need any help.
>
> Best regards.
>
>
> --
> Ing. Agr. M. Alejandro Becerra
> Cátedra de Topografía
> FCA-UNC
>