Spelling suggestions: "subject:"main forest"" "subject:"gain forest""
1 |
The ecology of seedlings in Central Amazonian forest fragmentsMalvido-Benitez, Julieta January 1995 (has links)
No description available.
|
2 |
Forest structure and dynamics in the Beni Biosphere Reserve, BoliviaComiskey, James Andrew January 1999 (has links)
No description available.
|
3 |
An investigation into the relationship between anthropology and conservation of the environmentStoneman, Catherine January 1999 (has links)
No description available.
|
4 |
The practical application of arbuscular mycorrhizal fungi for reforestation in IndonesiaSetiadi, Yadi January 1995 (has links)
No description available.
|
5 |
Ecological studies on rain forests at three altitudes on Bukit Belalong, BruneiPendry, Colin A. January 1994 (has links)
Altitudinal zonation of rain forests was investigated on Bukit Belalong (913m), Brunei. Mean annual rainfall was 4100mm at 45m and 5500mm at 913m. Mean annual temperatureswere 25.7°C (45m) and 21.8°C (913m). Three 0.25ha plots were set up at each of three altitudes. At 200m and 500m there was evergreen lowland rain forest and at 850m there was lower montane rain forest (LMRF). The Dipterocarpaceae had the highest proportion of basal area throughout, but their importance declined in the LMRF where the Fagaceae, Myrtaceae and Lauraceae were increasingly important. Soils in the LMRF were more organic and had higher concentrations of total nitrogen and phosphorus and the soils from 500m were the most acid and least base saturated. Rates of nitrogen mineralisation and soil concentrations of inorganic nitrogen did not differ significantly among altitudes. The rates (t ha-1 yr-1) of total small litterfall and leaf litterfall were significantly lower in the LMRF (10.6 and 7.9 at 200m; 10.5 and 7.9 at 500m; 8.3 and 6.0 at 850m). Litterfall nutrient concentrations were similar among altitudes, but smaller quantities of litterfall nutrients were cycled at 850m. The mass (t ha-1) of the small litter layer was similar throughout (5.2 at 200m; 6.1 at 500m; 5.2 at 850m) but leaf litter kL values were lower at 850m (2.4 at 200m; 2.4 at 500m; 2.0 at 850m). Fine root (<5mm) mass (t ha-1) in the top 100cm of soil was 8.3 (200m); 12.0 (500m); 10.6 (850m). Rates (t ha-1 yr-1) of fine root growth (estimated by ingrowth bags) were 0.9 (200m); 2.2 (500m); 0.5 (850m). A bioassay experiment using rice was made at 30m and 913m. Nutrients were more limiting in the montane soil, but climate was of overriding importance for rice growth. It seems that the LMRF is not nutrient limited and the lower temperatures at 850m are the primary cause of the change in species composition and reduction of stature there.
|
6 |
Plant diversity after rain-forest fires in Borneo /Eichhorn, Karl August Otto, January 1900 (has links)
Thesis (doctoral)--Universiteit Leiden, 2006. / Includes bibliographical references (p. [91]-99).
|
7 |
Modelling forest dynamics and management of natural tropical rain forestsRamdass, Indarjit January 1987 (has links)
No description available.
|
8 |
Dipterocarp regeneration in tropical rain forest gaps of different sizesBrown, N. D. January 1990 (has links)
No description available.
|
9 |
Tradition versus modernity in the rain forest environment with particular reference to peninsular MalaysiaHassan, Ahmad Sanusi January 1998 (has links)
No description available.
|
10 |
Interactions between leaf-cutting ants and forest regeneration in AmazoniaVasconcelos, Heraldo Luis de January 1994 (has links)
No description available.
|
Page generated in 0.0652 seconds