H. Bourennane et al., Comparison of kriging with external drift and simple linear regression forpredicting soil horizon thickness with different sample densities, GEODERMA, 97(3-4), 2000, pp. 255-271
This study examines two mapping method's sensitivity to the sampling densit
y of the variable of interest, which is the thickness of a silty-clay-loam
(TSCL) horizon. The two methods are simple linear regression (SLR) and univ
ersal kriging with external drift (UKEXD). As slope gradient (beta) derived
from a DEM, is available for the whole study area and linearly related to
TSCL horizon, was used for TSCL prediction by SLR and by UKEXD. The accurac
y performance of TSCL prediction using these methods was assessed by compar
ison with another group of 69 sample points (validation sample) where the T
SCL is actually measured. In the validation procedure for the two methods,
two indices were calculated from the validation sample (measured values) an
d predicted values. These two indices are the mean error (ME) and the root
mean square error (RMSE). The results showed that UKEXD was more accurate t
han the SLR. The improvement of the accuracy of the prediction from SLR to
UKEXD was about 38%. To examine the effect of sampling density of TSCL (var
iable of interest) on the performance of both mapping methods, five subsets
of 40, 50, 75, 100 and 125 observation sites of TSCL were randomly selecte
d from the 150 sites of the prediction sample. For each subset, a predictio
n of TSCL was performed over the study area by: (i) SLR; (ii) UKEXD. The va
lidation sample was used to compare the performance of the two methods acco
rding to the sample size of the variable of interest. The results show that
whatever the sample size may be, UKEXD performs on average more accurate p
redictions than SLR. Moreover, the results indicate that UKEXD performed be
tter when the sample size of the variable of interest increases. On the con
trary, the performances with the linear regression remain stable whatever t
he sample size map be. (C) 2000 Elsevier Science.V. All rights reserved.