M. Mcleod et al., A SOIL-LANDSCAPE MODEL FOR CLOSE-JOINTED MUDSTONE, GISBORNE-EAST CAPE, NORTH-ISLAND, NEW-ZEALAND, Australian Journal of Soil Research, 33(3), 1995, pp. 381-396
A soil-landscape model, comprising 12 land components at a scale of 1
: 5000, has been developed in Neogene close-jointed mudstone in the Gi
sborne-East Cape region of the North Island, New Zealand. In a validat
ion, soil order was predicted correctly in 81% of observations, soil g
roup in 80%, soil subgroup in 63% and soilform in 60% of observations.
A simplified model based on 11 land components for use at a scale of
1 : 50 000 has also been validated. Here soil order was predicted corr
ectly in 71% of observations, soil group in 73% and soil subgroup in 4
9% of observations. For application with a digital elevation model (1
: 50 000), the number of land components was amalgamated to five. Here
the soil order and soil group were predicted correctly in 63% of obse
rvations and soil subgroup in 40% of observations during validation. I
n all trials, the percentage of correct observations increased if a se
cond choice or subdominant soil class was allowed. It took 2 person-we
eks to produce a soil map from the 1 :50 000 form of the model over 40
0 km2 of steep and hilly country by photo interpretation of stereo aer
ial photographs, compared with 1 day of applying computer algorithms o
n the digital elevation model (DEM). The soil-landscape model succinct
ly relates soil class to land component and it enables improved target
ing of farm and planning inputs by empowering existing research into s
oil fertilizer requirements and soil physical properties.