Soil-landform relationships at two localities in Papua New Guinea

Two test areas, each of several hectares, in denudational terrain in the lowlands and highlands of Papua New Guinea were intensively studied to establish the association between soil conditions and landforms. Whether soils were allocated either to the great soil groups of a classification based on the 7th Approximation or to FAO soil units, an extremely wide range of soils occurred in each of the land units that could be distinguished on the basis of landform. Defensible statements concerning soil distribution were achieved only by limiting the categories of soil to the level of soil orders and by restricting the number of land units to three or four. Even so, the statistical significance of the relationships was very low.These results indicate that current techniques and sampling densities used in photointerpretative land resource surveys in terrains typical of Papua New Guinea can produce only very generalized information on soil distribution. To obtain reliable predictions of soil information at the level commonly implied in such surveys, further intensive studies on the relationships between attributes of soil, landform and vegetation are required.