The relative ecological importance of a number of habitat factors was established by using sampling equitability of habitat variables and mutual information between variables and species distribution, as calculated by the ecological profiles technique. Important factors that were distinguished include magnesium, calcium and sodium content of the soil, as well as textural properties such as the coarse sand and clay content. Properties of the B soil horizon were often more important than those of the A horizon. Die relatiewe ekologiese belangrikheid van ‘n aantal habitatfaktore is vasgestel deur van onpartydige monster-neming asook van die gemeenskaplike inligting tussen die verspreiding van habitatveranderlikes en spesies, soos bereken deur die ekologiese profiele-tegniek, gebruik te maak. Belangrike faktore wat onderskei is, sluit die magnesium-, kalsium-en natriuminhoud van die grond, asook teksturele kenmerke soos growwe sand en klei-inhoud in. Kenmerke van die B-horison is dikwels meer belangrik as dié van die A-horison.
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G.J. Bredenkamp (1985) studied this question.
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