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Geometric Anisotropy

A semi-variogram $/gamma(h_u, h_v, h_w)$ or a covariance $C(h_u, h_v, h_w)$ has a geometric anisotropy when the anisotropy can be reduced to isotropy by a mere linear transformation of the coordinates:

/begin{displaymath}/gamma(h_u, h_v, h_w) = /gamma'(/sqrt{h_u'^2 + h_v'^2 + h_w'^2})/end{displaymath}


/begin{displaymath}/mbox{anisotropic} / / / / / / / / / / / / / / / / /mbox{isotropic}/end{displaymath}

with

/begin{displaymath}h_u' = a_{11}h_u + a_{12}h_v + a_{13}h_w,/end{displaymath}


/begin{displaymath}h_v' = a_{21}h_u + a_{22}h_v + a_{23}h_w,/end{displaymath}


/begin{displaymath}h_w' = a_{31}h_u + a_{32}h_v + a_{33}h_w,/end{displaymath}

or, in matrix form,

/begin{displaymath}{/boma h}' = A.{/boma h},/end{displaymath}

where $A = a_{ij}$ represents the matrix of transformation of the coordinates, and ${/boma h}$ and ${/boma h}'$ are column-vectors of the coordinates.

An example is given in Figure 4.6, which shows four semi-variograms for four horizontal directions $/alpha_1, /alpha_2, /alpha_3, /alpha_4$. Spherical models with identical sills and ranges of $a_{/alpha_1}, a_{/alpha_2}, a_{/alpha_3}, a_{/alpha_4}$ have been fitted to these semi-variograms. The directional graph of the ranges, i.e., the variation of the ranges $a_{/alpha_i}$ as a function of the direction $/alpha_i$, is also shown in Figure 4.5. There are three possible cases.

Figure 4.5: Ranges in Case of Anisotropy.
/begin{figure}/begin{center}
/mbox
{/beginpicture
/setcoordinatesystem units <1c...
...5
/put {$a_{/alpha_{4}}$} [b] at -1.3 0.75
/endpicture}
/end{center}/end{figure}

Figure 4.6: Geometric Anisotropy.
/begin{figure}/begin{center}
/mbox
{/beginpicture
/setcoordinatesystem units <1c...
...0.0 3.25 2.6 /
/plot 4.55 0.0 4.55 2.6 /
/endpicture}
/end{center}/end{figure}

(i)
The graph can be approximated to a circle of radius $a$, i.e., $a_{/alpha_i}
/cong a$, for all horizontal directions $/alpha_i$ and the phenomenon can thus be considered as isotropic and characterized by a spherical model of range $a$.
(ii)
The graph can be approximated by an ellipse, i.e., by a shape which is a linear transform of a circle. By applying this linear transformation to the coordinates of vector $/boma h$, the isotropic case is produced (circular graph). The phenomenon is a geometric anisotropy.
(iii)
The graph cannot be fitted to a second-degree curve and the second type of anisotropy must be considered, i.e., zonal anisotropy in certain directions, $/alpha_4$, for example, on Figure 4.5.

If, instead of transition structures of range $a_{/alpha_i}$ as in Figure 4.5, the directional semi-variograms are of the linear type, $/gamma_{/alpha_i}(h_i) =
/omega_{/alpha_i} h_i$, then the directional graphs of the inverses of the slopes at the origin $/omega_{/alpha_i}$ will be considered. A hypothesis of isotropy, geometric anisotropy or zonal anisotropy will then be adopted according to whether or not this directional graph can be fitted to a circle or an ellipse.


next up previous contents
Next: Correction of Geometric Anisotropy Up: Anisotropies Previous: Anisotropies   Contents
Rudolf Dutter 2003-03-13