Abstract
This paper explores the origins, formation processes, properties, and characteristics of meadow-alluvial soils found in the Jizzakh desert, as well as their morphological structure. The article delves into the role of soil-forming factors, the conditions of their formation, and the significance of parent rocks and deposits in shaping the mechanical structure of the soil. The granulometric composition of meadow-alluvial soils, including the quantity of dust and clay particles and the total amount of microaggregates, is examined. The mechanical composition of arable and sub-arable soils is described, along with the lithological structure and structural composition of the salt profile.
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