Lack of large datasets in soil protection studies and environmental en
gineering applications may deprive these fields of achieving accurate
spatial estimates as derived with geostatistical techniques. A new est
imation procedure, with the acronym Co_Est, is presented for situation
s involving primary and secondary datasets of sizes generally consider
ed too small for geostatistical applications. For these situations, we
suggest the transformation of the secondary dataset into the primary
one using pedotransfer functions. The transformation will generate a l
arger set of the primary data which subsequently can be used in geosta
tistical analyses. The Co_Est procedure has provisions for handling me
asurement errors in the primary data, estimation errors in the convert
ed secondary data, and uncertainty in the geostatistical parameters. T
wo different examples were used to demonstrate the applicability of Co
_Est. The first example involves estimation of hydraulic conductivity
random fields using 42 measured data and 258 values estimated from bor
ehole profile descriptions. The second example consists of estimating
chromium concentrations Scorn 50 measured chromium data and 150 values
estimated from a relationship between chromium and copper concentrati
ons. The examples indicate that in situations where the size of the pr
imary data is small, Co Est can produce estimates which are comparable
to cokriging estimates.