The Provision of the Modern and Special Features of Arealing of the Mountains and Black Lands in the Gedebey District

The Provision of the Modern and Special Features of Arealing of the Mountains and Black Lands in the Gedebey District by Aliyev Zakir Huseyn Oglu

Open Access Journal of Biogeneric Science and Research

It is well known that the classification of brown soils was first made in 1949 by IP Gerasimov. Although 69 years have passed since the first classification to date, brown soil has not yet been able to occupy its place in the classification. Thus, to substantiate the aforementioned idea, we have many years of theoretically and practically analyzed data. It is known that brown soils are widely formed in the Balkan Peninsula and around the Mediterranean (European and African coasts).  This information was published in the works of the 6^th International Congress of Soil Science, held in Paris in 1956. The last classification of Azerbaijani lands was given by ME Salayev [1], where the author was especially interested in the search for correlation between the nomenclature system of the land and the system of nomenclature of the world with a more detailed study of the diagnostic parameters of soils.  

Thus, when analyzing the results of SE Salayev's observations, attention is drawn to the specificity of mountain and brown soils from other types of soil and the relief and climatic complexity of the mountainous terrain. As noted by Salayev ME, brown soils were formed on both flat and mountainous background. However, it should be borne in mind that the brown soils in Azerbaijan have largely formed their genetic characteristics in the complex exposition of the mountainous relief and retained their classic morphological features. You don't have to go very far to justify this idea. Thus, it is possible to encounter mountainous brown and mountainous lands in the northeastern part of the Lesser Caucasus, with a large range of Gadabay. Brown soils are associated with the gray-brown soils formed in the foothills and forests of the Gadabay region from the south. In the upper border, brown mountain-forest lands create a transition to dark brown soils. The brown area of ​​the forest zone has developed from 400-500m up to 1100-1200m, mainly under oak and partly forest.

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