Özet:

The army is identified as a search site for the Greşilköy neighborhood and nearby forest land. In the soil areas that are developed on the Gabro skiers, the amount of silk and sand increases with the increasing soil depth. As a result of the separation of the Gabro-type stones, the silk-rich soil has been determined to develop. It is observed that the quantities of quarters in the upper areas of the developing soil on Gabro have increased, and the quantities of feldispates, pyroxens, amphibols and olivin have decreased, and the formation of new fiber minerals. In developing soil areas on Gabro, such as CaO, MgO, Na 2O, K 2O and P 2O 5, the quantities of oxyts, according to the main ski, have been observed to decrease. The main element oxide that does not decline here is Al 2O 3, Fe 2O 3 and TiO 2. In all locations, trace elements such as Co, Sr, Cd are moved vertically within the soil ecosystem, and semi-mobil trace elements such as Cu, Ni, Ba, Zn are removed from the same system, and immobile trace elements such as Pb, Cr, Zr, Nb, Ce are gathered in the soil ecosystem. The data obtained from the combined profile is included in the North American Steam Content (NASC) main and trace element distribution range. Only a large amount of Pb is measured in the area of land A.