Vegetation of Southeast Asia Studies of Forest Types 1963-1965
Vegetation of Southeast Asia Studies of Forest Types 1963-1965
Vegetation of Southeast Asia Studies of Forest Types 1963-1965
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Under natural conditions the boundaries between tropical forests<br />
and savannas depend, generally speaking, upon the humidity factor.<br />
An exact determination, however, <strong>of</strong> the amount <strong>of</strong> rain necessary for<br />
the existence <strong>of</strong> forests is very difficult. General considerations<br />
which lead to the establishment <strong>of</strong> rain factors, aridity coefficients,<br />
and climatic types <strong>of</strong> formulae do not include the important physio-<br />
Ipgical factors <strong>of</strong> plant transpiration or the existence <strong>of</strong> subterranean<br />
water reserves which may be stored at great depths in tropical<br />
soils.<br />
The data on water requirements <strong>of</strong> forests from classical plant<br />
ecology are based upon the assumption that the present distribution<br />
<strong>of</strong> tropical forests and savannas corresponds to the ecological conditions<br />
<strong>of</strong> their environment. 'It is known, especially from researches<br />
in central equatorial Africa, that great areas <strong>of</strong> savannas,<br />
now occupying deteriorated soils, were forested in former times.<br />
More reliable data are obtained from the direct determination<br />
<strong>of</strong> transpiration values, which are scarce because <strong>of</strong> difficulty to<br />
obtain, or from a computation based on the knowledge <strong>of</strong> the total<br />
precipitation and <strong>of</strong> drainage water <strong>of</strong> an entire river basin covered<br />
by equatorial forest.<br />
The practical importance <strong>of</strong> such data is emphasized. For example,<br />
it is possible to distinguish savannas which can be reclaimed.<br />
A consideration <strong>of</strong> all the facts involved indicates how this reclamation<br />
can best be done. It is clear that agricultural methods<br />
used in temperate regions are inappropriate when applied to tropical<br />
lowland soils. Such practices disturb the water balance <strong>of</strong> tropical<br />
soils, favor serious surface erosion, cause internal, leaching <strong>of</strong><br />
soils, and there is evidence that they produce an irreversible degradation<br />
<strong>of</strong> soil fertility.<br />
Raymond, M. Carices Indochinenses Necnon Siamenses. Memoires du Jordan<br />
Botanique de Montreal, No. 53. 125 pp. Montreal. Feb. 1959.<br />
ReinJeing, O.A., and G.W. Gross. The kao pan seedless Siamese pummelo<br />
and its culture. Philippine Journal Science. 19: 389-^37. 1921.<br />
Rich, R. W. Aerial photography as a means <strong>of</strong> measuring plant Tver<br />
and composition. In Techniques and Methods <strong>of</strong> Measuring Understory<br />
<strong>Vegetation</strong>. Proceedings <strong>of</strong> a Sympos.ium at Tifton, Georgia, pp.<br />
79-81. Oct. 1958.<br />
Richards, P.W. The Tropical Rain <strong>Forest</strong> - An ecological study. 5^0 pp.<br />
%3 text figs, and 15 places. Univ. Press, Cambridge. 1952.<br />
This is probably the most authoritative and comprehensive reference<br />
on this vast and complicated subject. It contains 17 chapters,<br />
divided into 6 parts. Part 1 - Treats with structure and<br />
•physiognomy <strong>of</strong> the Tropical Rain forest; Part 2 - The Environment;<br />
Part 3 - Floristic composition <strong>of</strong> Climax communities; Part 4 -<br />
Primary successions; Part 5 - Tropical Kain forest under limiting<br />
conditions; and Part 6 - -Man and the Tropical Rain forest.<br />
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