Research of the Arctic Soils Using an Artificial Neural Network
Bazarbayeva T.A. Urymbaeva A.A. Kubesova G.T. Mamyrbekova A.K. Mylkaidarov A.T. Umbetbekov A.T.
2021Polish Society of Ecological Engineering (PTIE)
Journal of Ecological Engineering
2021#22Issue 91 - 12 pp.
Desert-Arctic soils - balasamy (W-C1), are found in the most northerly position in the Arctic. These soils are characterized by a light granulometric composition and are formed in the areas recently released from glaciers, and develop under a crust of blue-green algae. Arctic soils (AO-AY-BC-C) are common on loamy and gravelly-loamy soils (Severnaya Zemlya, Novaya Zemlya, Franz Josef Land, North of the Taimyr Peninsula). They are characterized by wedge-shaped horizons, and are formed in the form of polygons with a diameter of 0.5–1.0 m under moss-shrub vegetation. Carbonate pelozems (WSA-SSA) are found on deluvial deposits of carbonate rocks on loamy-gravelly soils. The vegetation cover is represented by lichens and rare specimens of flowering plants. In the Arctic tundra, on the most drained areas on loamy and gravelly-loamy soils, humified weak-clay (gley) soils (AO-A-CRMg-C(D)) are common. In terms of morphology and chemistry, these soils are similar to Arctic soils, but differ from them in the large development of wedge-shaped horizons. In this work, the composition of Arctic soils was studied using a neural network.
Arctic soils , composition , pelozems
Text of the article Перейти на текст статьи
Department of UNESCO on Sustainable Development, Al-Farabi Kazakh National University, Almaty, Kazakhstan
K. Zhubanov Aktobe Regional University, Aktobe, Kazakhstan
Akhmet Yassawi International Kazakh-Turkish University, Turkestan, Kazakhstan
Department of UNESCO on Sustainable Development
K. Zhubanov Aktobe Regional University
Akhmet Yassawi International Kazakh-Turkish University
10 лет помогаем публиковать статьи Международный издатель
Книга Публикация научной статьи Волощук 2026 Book Publication of a scientific article 2026