STUDY ON THE DEW POINT TEMPERATURE IN AREAS COVERED BY COLLUVIAL MESAVOID SHALLOW SUBSTRATUM (CRYSTALINE SCHISTS SCREE) IN THE LEAOTA MOUNTAINS, 2014

摘要

This paper present and discussed the results of the monitoring of the dew point values, recorded in October and November 2014, in an ecological station in the Leaota Mountains. In this station, two polls were located in areas covered by colluvial mesovoid shallow substratum (MSS) formed by epi- and mesometamorphic crystalline schists. In the ecological station s we located in the Leaota Mountains, almost always we found condensation on the walls of the polls tubes placed at different depths. Most often in spring or autumn or in other cold days, the dew point is more revealing regarding the recording actual amount of moisture in the air, than the relative humidity indicator. This work is part of a larger project that seeks correlations between ecological factors (humidity, temperature and dew point) registered in various types of screes (limestone and crystalline schists) and some zoocenotic components (invertebrates). This research aim to know the impo rtance of mesovoid shallow substratum for invertebrates or small vertebrates fauna and represents a premiere for Leaota Mountains, not only regarding the continuous monitoring of some ecologic factors of these types of ecosystems (MSS), rarely researched even at global level, and also regarding the inventory of the invertebrate fauna in scree for these mountains.