Özet:

This article is aimed at illustrating the characteristics of the chromium kambisol soil that develops in the mountainous and hollow surfaces of the Servak area. Precambrian - These soils located on the rocks in the Holosen age range usually occur in a thick soil layer. Especially in areas where the curvature increases and the effects of erosion are strongly felt, the soil is well absorbed. However, these soils located on the Inwestern Anatolian border are usually located in a semi-dry - semi-humid climate area, the soil formation period occurs only in a short time period of the year. For this reason, the study began with the investigation of the factors that influenced the formation of the soil. The maps used in the study are provided by the Map General Command, the General Directorate for Mining and Inspection, the Ministry of Food, Agriculture and Animal Industry, and are converted into targeted maps. Because the climate has a significant impact on the formation of the soil, the meteorological data related to the field are provided by the State Meteorological General Directorate. The data obtained were processed according to the purpose, the climate characteristics of the field were revealed and the temperature map with the rain related to the field was drawn. After these studies, the work area was divided into squares with a range of 5 km in order to determine where the land samples will be taken. 19 land samples were taken to represent the surface of the soil (0-30 cm) and the gold (31-60 cm). The land samples obtained with land burgus or with the opening of their profiles up to 1 meter have been analyzed in the laboratory of the Ministry of Agriculture, Agriculture and Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture of the Ministry of Agriculture. Thus, within the physical and chemical characteristics of chromic pigs, the characteristics such as pH, total salt, variable cations, organic substance, shell content and one-right distribution (texture) have been revealed. These features are transferred to the Arc GIS 10.2 software, which has obtained the distribution maps on the physical, chemical macro and micro-elements distribution of the soil. Then the land profiles were opened and identified in the appropriate places in order to reveal the horizontal structure of the land. The chromic cams located on mountainous lands cover the wide areas of Nazaran to the other types of land of Uşak. According to the research results, the main characteristic of chromic shells, which are often thin textured, neutrally reactive, is that the soil is thin or less thin. There is no problem in these fields where no drenage problems are seen. Because the chromic spots are located in curved areas, a significant portion of organic substance is removed from the soil by erosion. Therefore, the organic content of these substances is low. The magnesium content is measured above the value it should be. Erosion, the misuse of the soil and the overuse of fertilizer are classified as the main problems of these soils. In the results section of the study, a number of problems have been identified and solutions proposals have been listed.