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Soil chemical properties as related to forest succession in a highland area in north‐east Tasmania
Author(s) -
ELLIS R. C.,
GRALEY A. M.
Publication year - 1987
Publication title -
australian journal of ecology
Language(s) - English
Resource type - Journals
eISSN - 1442-9993
pISSN - 0307-692X
DOI - 10.1111/j.1442-9993.1987.tb00951.x
Subject(s) - ecological succession , climax , climax community , soil water , mineralization (soil science) , rainforest , loss on ignition , grassland , vegetation (pathology) , secondary succession , cation exchange capacity , soil type , ecology , agronomy , chemistry , biology , environmental chemistry , medicine , pathology
The relationship between vegetational type and a number of soil chemical factors was examined in secondary successions from fire‐maintained eucalypt/grass to climax rainforest communities growing on uniform granitic soil parent material. Canonical variates analysis, which utilized the following variables: pH; loss on ignition; total N, P, K, Ca, and Mg; cation exchange capacity and exchangeable Ca, K, and Mg; and potentially mineralizable N, revealed close overall similarity between surface soils of adjacent types, and significant differences among those of types distant from each other in the successional sequences. Exchangeable Ca, mineralizable N, total N. P, and Mg, and pH all differed significantly among soils of the vegetational types. However, the only identifiable gradients in soil properties that were detected within a successional sequence were in total and mineralizable N, which tended to increase, and pH, which generally tended to decrease with progression towards the climax vegetation. Nitrification was promoted by the presence of Acacia dealbata and apparently inhibited by the presence of Leptospermum lanigerum; it was more rapid in soils beneath late successional vegetation than in those from climax vegetation or early stages of succession, and was inhibited in soil from old (> 200 years) grassland. It was concluded that differences among soils in chemical composition and rates of mineralization of N were due to differences in species composition of the vegetational types that they carried for the time being.