Özet:

In this study, the physical-chemical characteristics of surface soil samples formed on different main materials in the Afyon-Kandıklı district have been determined, the reverse distance weight enterpolation (IDW) method has created local distribution maps. In the study with the aim of evaluating the state of the soil formed on different main material; the pH of the soil found on the main material of the shell was determined at the levels of light alkaline, the shell content was high, and the micro-element content was determined at the levels of nonsense. The variation in the characteristics of the soil that is usually within the middle-degree texture group is determined at high levels. The content of the soil, curl and Ca of the soil formed on the main material of tuberculosis and and andecites has been detected at low levels. The percentage of organic substance in the thin and weak myrs are determined at the lowest levels, while the lowest organic substance is determined in the alivons that occur with the break-down of the main materials of the thin, the thin and the thin. The potassium content of the soil formed on the main material of alivium was mostly sufficient in agricultural areas, while in curved areas at lower levels. In the basalt and vokanite formed on the main material in the soil, the microelement has been detected at sufficient levels. The study found that the distribution of macro and micro elements was significantly affected by the variety of the main material and the land use / land coverage.

Anahtar Kelimeler:

Özet:

In this study; the physico-chemical and nutrient elements of the surface soil samples formed on different parent materials in the Afyon - Sandıklı district were determined, and spatial distribution maps were created through the interverse distance weighted interpolation (IDW) method. In the study conducted to evaluate the condition of the soils formed on different materials; The soil reaction of the soils on the limestone parent material is slightly alkaline, the lime content was high, and the micro element contents were determined at the deficiency levels. The variation in the properties of soils, which are generally in the moderate-fine texture group, was determined at high levels. Clay, lime and Ca content of soils formed on tuff and andesite parent material were found at low levels. While the rate of organic matter in the sloping and weak pasture areas was moderate and low, the lowest organic matter was determined in the mudstone, sandstone and conglomerate parent materials that alluviums occur with their disintegration-decomposition. The potassium content of the soils formed on the alluvium parent material was found to be at a sufficient level in agricultural areas and at a lower level in inclined areas. In addition, in the soils formed on basalt and volcanite parent material, micro elements were determined at sufficient levels. As a result of the study, they determined that the distribution of macro and micro elements was significantly affected by the type of parent material and land use/land cover.