Influence Pedogenetical Cover on the Production Capacity of Forest Resorts Trasc??u Mountains

摘要

Trascau Mountains are an extension to the northeast of the Metalliferous Mountains. Petrographic structure is very complex, represented by basalt, crystalline, sandstone, limestone, crystalline limestone, gneiss, dacites, etc.. However determined the formation of a varied terrain (ridges, knolls volcanic steep keys, caves) and hence a very varied soils cover. Were inventoried and analyzed a total of four soil types found in wooded area in the Mountains Trascau. Soils were represented by: rendzinia, districambosoils, eutricambosoils and albic luvisols. Due to the extremely varied microrelief of territory, most soils are skeletal, edaphic small and medium-volume, some shallow. Forrest sites in this area belongs to mixed mountain level FM 2 and premountain-mountain beech level FM 1 +FD 4 , with at most middle production capacity, fact given in the first way by relief conditions, but also the meted soils, soils that are skelletic.