The article discusses the practice of using the "SWOT analysis" method for planning the use of municipal land resources. The object of the study was municipalities on the territory of the Republic of Sakha (Yakutia). The research technology includes two stages. The first stage is the study of municipal land management programs. The second stage is field research: a survey of experts in a small group using electronic means of communication and a personal conversation with experts. Electronic means of communication were used to interview experts who could not be contacted in person due to the following reasons - the remoteness of the experts' location, restrictions on personal contacts in connection with the Covid-19 pandemic. As a result of the conducted research, the positive aspects of the activities of the municipal property management committees, as well as conditions that reduce the effectiveness of the work of the committees, have beenidentified.
The elemental composition of the soil was studied in the mesorelief of the former water area of the Yudinsky stretch of Lake Chany. The study was carried out in two soil sections that are in geochemical conjugation: meadow-chernozem weakly-solodic loamy sand soil in the eluvial landscape position and meadow-marsh saline heavy-loamy soil in the accumulative landscape. Soils differ significantly in both redox and acid-base conditions: the distribution of humus in the soil profile, pH values, the content of physical clay, cation exchange capacity. Distribution of the predominant number of macroand microelements (with the exception of silicon) in the saline agrolandscape of the Prichanovskaya depression is characterized by their accumulation in the meadowmarsh saline heavy loam soil as a result of water migration and subsequent fixation in the form of slow-moving compounds. The content of elements in the accumulative position is on average 2-3 times higher than in the eluvial one. Macroelements iron and aluminum migrate down the relief in the form of sesquioxides in the composition of the clay fraction. The accumulation of calcium and magnesium is associated with the carbonatization of the soil profile. Trace elements zinc, copper, cadmium, lead are deposited on the alkaline barrier in the profile of meadow chernozem soil at a depth of 95 cm and below, in a meadow-marsh saline soil from the surface, molybdenum is concentrated in the upper horizons of the soil profile on the evaporation barrier, manganese on humus and gley meadow-bog soil, nickel and cobalt on humus and clay, chrome in salt accumulations. An imbalance of copper and molybdenum, iron and manganese, calcium and strontium is observed in the soils of both the eluvial and accumulative positions, which indicates a deficiency of molybdenum and manganese and an excess of strontium in the landscape soils in general. There is an excess of permissible sanitary and hygienic standards for the content of strontium and barium in the accumulative positions in the entire thickness of the soil profile of meadow-marsh saline heavy-loamy soil. The content of arsenic and, especially, boron exceeds the MPC values in the landscape as a whole.
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