Michael,

Kriging with External Drift, as implemented in the GSLIB set of programs
(Deutsch & Journel) is distinct from Universal Kriging, in that the
"External Drift" is intended to be defined by a secondary variable that you,
the user, "believe" incorporates some information of relevance to the
primary variable that you are working with.  

The "External Drift" could also be a kriged array of values based on kriging
some sparse secondary variable (onto a regular grid) that you also feel
contains information of relevance.  You can also specify a "trend"
mathematically, but the original intent was to incorporate a secondary
variable "relevant" to estimation of the first.

An example would be: you have sparse porosity measurements in an oil field,
but you have a regular array of 3-D seismic amplitudes covering that same
area.  Your external drift variable would be seismic amplitude and your
primary variable would be porosity.  Obviously the two are not precisely the
same, but "hopefully" they are related.  

It is up to you, the user, to specify external drift terms that "make sense"
physically.  Obviously, this is a matter of interpretation, and you are the
one responsible for justifying your choices.

I suggest you read the sections on Kriging with External Drift beginning on
page 70 and 96 of the Deutsch and Journel (1998) book, "GSLIB Geostatistical
Software Library and User's Guide," by Oxford University Press.  I'm sure
there are other papers out there on this methodology, but if you are talking
about the GSLIB program, then it's best to go to the documentation
associated with that program.

Best regards,  

Chris

Christopher A. Rautman, Ph. D., P.G.
Underground Storage Technology Department
Sandia National Laboratories
P. O. Box 5800; MS-0706
Albuquerque, New Mexico  87185-0706
505-844-2109; fax: 505-844-4426



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