Differences in soil properties of dry evergreen and dry deciduous forests in the Sakaerat Environmental Research Station.
Differences in soil properties of dry evergreen and dry deciduous forests in the Sakaerat Environmental Research Station.
复制标题
萨卡拉环境研究站干燥常绿林和干燥落叶林土壤性质的差异。
DOI:
10.3759/tropics.8.61
复制
发表时间:
1998
期刊:
影响因子:
0.7
通讯作者:
Kanzaki Mamoru
中科院分区:
文献类型:
--
作者:
Sakurai Katsutoshi;Tanaka Shin;Ishizuka Satoshi;Kanzaki Mamoru
To clarify the soil-plant relationship in the Sakaerat Environmental Research Station (SERS), northeast Thailand, soil survey was conducted in the two major types of forest, i.e., dry evergreen forest (DEF) and dry dipterocarp forest (DDD. In addition, DDF with fire protection treatment since 1967 (FPDDD was also selected as a study plot to know the effect of protection of land cover during dry season on both soil and vegetation. As a result of the soil analysis, such as soil hardness, soil morphological, physical, chemical, and mineralogical properties, the current vegetation in the SERS seemed to be affected greatly by the strength of the impacts (fue) given to the forest. If no fire protection is attempted in the DDR soil erosion due to loss oforganic matter on the surface soil is easily brought about. Soil properties such as clay content and associated properties (water holding capacity, cation exchange capacity, water penneability, and moisture content) become worse easily and shortly, after soil erosion. The various soil properties of the FPDDF can be considered in the intermediate condition between those of DDF and DEF. The stronger the impact of fire is, the more the soil erosion occurs. On the basis of soil properties, the following mechanism can be suggested to explain the current vegetation; once the original vegetation was desroyed, DEF type forest could not regenerate easily in such a dry and infertile soil condition, and therefore, the other type of vegetation, i.e., DDF, is found elsewhere in northeast Thailand at present. The extremely dry soil condition currently found in the DDF is not intrinsic property of a forest soil. It is created by the removal of the vegetation which used to be there. The fire protected DDF suggests it.