[GRASS-user] r3.in.xyz

Francois Chartier fra.chartier at gmail.com
Mon Jul 9 06:17:01 PDT 2018


Thanks moritz.  I will try this. I have about 300 m of elevation to
interpolate so i might group by thickness bands of 2 metres etc.
Is there a way i can make a batch mode where i prep all the xy p by
elevation and then interpolate automatically onw after another all slices?

On Mon, Jul 9, 2018, 03:01 Moritz Lennert, <mlennert at club.worldonline.be>
wrote:

> Le Sun, 1 Jul 2018 13:27:03 -0400,
> Francois Chartier <fra.chartier at gmail.com> a écrit :
>
> > Hi,
> >
> > I am reposting the initial question:
> >
> > “I am working with a data set that consists of borehole logs with a
> > Top of a layer (layer 1) and the top of the underlying layer (layer
> > 2) (which is also the bottom of the overlying layer 1).  Everything
> > in between the elevation of top of layer 1 and top of layer 2
> > correspond to a Layer 1 property.
> >
> > The thickness of Layer 1 varies and this layer may not exist
> > everywhere (pinches out).  Above the Layer the property is different;
> > in other words the property only starts below the Top of layer 1
> > until the underlying Top of the next layer. Not sure of the
> > capabilities of the interpolation in Grass and working with a very
> > large data set (i cannot link every top of layers together), my first
> > approach was to create a each Layer property for every elevation
> > slice along each Borehole axis, interpolating soil properties at
> > every elevation between Boreholes.
> >
> > The key question is can v.vol.rst (changed this from r3.in.xyz)
> > interpolate in 3D without a Property at every elevation slice,
> > • while respecting the condition that above the Top of the layer 2,
> > the property corresponds to the Overlying top layer 1, and
> > • that the property is continuous until the next underlying layer 3 -
> > can someone confirm this? To provide a bit of background, borehole
> > data bases, identify the top of layer as encountered when drilling
> > downwards, and provide the elevation of the next layer (pick); in
> > between the soil property is the same, however there is no data
> > points.  When interpolating, while there is no data point in between
> > the two geological picks, the property should still have weight in
> > the interpolation process.”
> >
>
> v.vol.rst is a tool to interpolate a continuous value into a 3D space.
> So, I do not think that it is the tool you are looking for.
>
> As already mentioned before:
>
> > You probably want to use something like r.to.rast3. This would mean
> > interpolating each layer separately into 2D elevation maps and then
> > assemble them into 3D using r.to.rast3.
>
> Have you tried this approach ?
>
> Moritz
>
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