Abstract:

Seyfe Lake (Kırşehir, Turkey) is located in Central Anadolu and has an important status in terms of the characteristics of the water area as a geographical location. It has been shown that the soil with the SCL body has a mild and strong alkaline characteristic, has a lot of salt (15.7 dS m-1), a lot of cranberry (516.6 g kg-1) and a low organic substance (20.5 g kg-1). The moist aggregate stability and weakness limits of the soil (plastic limit, liquid limit, plastic index) values have been determined to be significantly affected by the amount of organic substance, the total amount of grain and grain of the soil. It has been shown that the amount of received P is excessive (26.18 mg kg-1), Cu is sufficient (1.19 mg kg-1), Mn is very low (3.06 mg kg-1), Zn and Fe are less (0.30 mg kg-1, 0.36 mg kg-1). The main variable cation element in the soil was Na, followed by Ca, K and Mg, respectively. In the area within the closed pool, the lack of rainfall, the high evaporation and drainage system are problematic, as well as the importance of sodium that causes problems in terms of soil alkalicity in the ranking and the increased total salty is pH>8 and has a high purple content, the research area should be followed in terms of alkalicity and salty.

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