A calibrated Four-Electrode Probe (FEP) was used for inexpensive and i
ndirect determinations of salinity-sensor Electrical Conductivity (EC)
in a plot at Cauto Valley, Cuba. Two transects were made in the North
-South (N-S) and East-West (E-W) directions. Laboratory measurements o
f soil EC were also made from samples taken on a 50-m spaced square gr
id. A linear semivariogram was obtained for the salinity-sensor EC mea
surements at the E-W transect, which agrees with the topographical slo
pe of the plot and with the expected soil salinity variation. It also
coincides with the spatial structure of laboratory-measured soil EC. A
cross-validation analysis has shown that EC semivariograms obtained f
rom FEP measurements can characterize the soil EC spatial variation in
a similar way as semivariograms of laboratory-measured soil EC. Thus,
the distance between samples for soil salinity maps can be based on t
he semivariogram's range of salinity-sensor EC measurements. (C) 1998
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