Physico-Chemical Properties of Soil in the High Forest Zone of Ghana Associated with Logged Forest and with Areas Converted to Teak (Tectona grandis Linn. F)
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University of Ghana
Abstract
Salifu, K. F. 1997. Physico-chemical properties of soils associated with logged forest and areas
converted to teak (Tectona grandis Linn. F). M.Sc.F thesis, Faculty of Forestry, Lakehead
University, Thunder Bay. 104 pp. Major advisor Dr. W. L. Meyer.
Keywords: Tectona grandis Linn. F, logged forest, physico-chemical properties, total nutrients,
nutrient concentration, regression analysis.
The rapid and extensive introduction of teak to satisfy a predicted wood shortage in
Ghana has given rise to the question of the short/long-term effects that management of
teak plantations might have on soil properties. No research data is currently available to
answer this question.
Physico-chemical properties of soils were compared under two distinct forest covers (logged
native forest, and teak plantations) at three different forest reserves (Bosomoa, Tain II and Yaya)
located in the Kintampo, Dormaa - Ahenkro, and Sunyani Forest Districts, respectively in The
High Forest zone of Ghana. One-Way analyses of variance (ANOVA) was used for the
comparisons. Ages of the plantations used for the study ranged from 15 to 29 years. A total of
28 [20m x 20m] random sample plots representing 14 teak/logged forest pairs were included in
the study. Three hundred fifty (350) soil samples were collected in June, 1997 and analyzed for
their physico-chemical properties.
Within the Bosomoa and Yaya locations, nitrogen (N), and magnesiumn (Mg) concentrations
and organic matter (OM) contents in the surface soil horizons were significantly higher under
logged forest than under teak plantations. Also phosphorus (P) and potassium (K)
concentrations were significantly higher under logged forest at Bosomoa. Similarly, total
nutrients were generally higher in soils under adjacent logged forest compared to teak
plantations in the Bosomoa and the Yaya locations. Higher nutrient concentrations and contents
in soils under logged forest was due to more undergrowth, litter and organic matter under
logged forest. Higher nutrients under logged forest may also be due to a lesser demand for
these nutrients by tree species in logged forest. Lower soil macro-nutrient concentration and
contents in soils under teak was due to lower organic matter content under teak cover. Lower
nutrients in soils under teak plantations may also be associated with higher nutrient demand, and
nutrient immobilization by teak. At the Tain II sites, there were no significant differences
among soil nutrient concentrations and contents under teak and native logged forest. Soil
exposure due to bush fires at Bosomoa sites resulted in higher surface soil horizon bulk
densities (Db’s) under teak plantation (1.33 g cm'5). In contrast, surface soil horizon Db’s under
teak plantation were lower at Tain II (1.23 g cm ’) and at Yaya sites (1.10 g cm'3). There were no
significant differences in Db’s between vegetation types within locations.
Regression models were developed for Db of soils under teak cover, using easily measurable
soil variables such as OM, Clay, silt, volume of coarse fragments and soil pH. Equations
relating Db of soils under teak cover to these soil variables are presented for Bosomoa and Tain
II. The models can be used to explain Db at the study locations and on comparable sites.
Description
Thesis (MSc) - University of Ghana, 1997