Vasily Andreevich Kuznetsov

A comparative analysis of the composition of lysimetric waters for 2021–2022 was carried out. for two groups
of stationary soil lysimeters in the city. Th e fi rst group of lysimeters is formed by the system: fallow — grass
phytocenosis — overgrown fallow — spruce forest — mixed and broad-leaved plantation, developing on the
same type of mantle loam. Th e second group of lysimeters represents soils with diff erent types of tillage: conventional
plowing, extra-deep planting according to Bushinsky, plowing according to Mosolov, deep plowing
according to Kachinsky.
For both groups, the same type of migration of components is shown, in which the most migrating elements are
carbon, mono- and divalent cations, and chloride ion, with minimal migration of iron, manganese, and aluminum.
In the group of lysimeters under various types of vegetation, as the tree canopy develops and, accordingly, the
intensity of the biological cycle increases in migrating waters, the concentration of such important biophilic elements
as magnesium, calcium, potassium, and carbon increases signifi cantly, and among anions, chloride and sulfate ions.
Th is determines, within the framework of the cluster analysis, two diff erent subgroups in terms of the composition of
natural waters: the fi rst one is formed by the fallow-grass phytocenosis — overgrown fallow system, and the second
one combines tree plantations.
In the group of lysimeters with diff erent tillage, a cluster characterizes the composition of water in lysimeters with
reclamation plowing according to Mosolov and deep plowing according to Kachinsky. At the same time, individual
aggregates form lysimeters with conventional plowing and ultra-deep planting according to Bushinsky. This is explained
by the fact that in this group of lysimeters, the initially created soil profi le design is transformed, which is
characterized by the placement of eluvial and illuvial soil horizons in various combinations and at diff erent depths
depending on the type of plowing.

For landscape conditions in the upper reaches of the river Klyazma, Solnechnogorsk district, Moscow region, the height and reserves of snow cover were investigated, and the chemical composition of the snow was determined. The basis for considering the component composition of snow cover was the geochemical taxonomy of chemical elements based on the characteristics of water migration and abundance.

Data from 23 snow sampling points were interpolated in SAGA GIS using the inverse distance weighting (IDW) method. On this basis, zones differing in the chemical composition of snow are identified. One of the zones is confined to the M-10 Moscow-St. Petersburg highway, while the second borders on populated areas. The area close to the highway is characterized by increased levels of calcium, sodium, aluminum, and chloride ions in the snow cover. The second zone, bordering populated areas, is characterized by a high content of calcium, copper, and manganese in the snow. For the third zone, low concentrations of components in the snow were observed, which are characteristic of a superaquatic landscape due to the distance from sources of pollution.

The studied composition of snow waters belongs to the bicarbonate-sodium-calcium-chloride class. It has been shown that the height and reserves of snow cover are partially controlled by two factors: the type of elementary landscape and the type of ecosystem. Against this background, the spatial distribution of concentrations of elements and anions in snow is predominantly controlled by the anthropogenic factor.

The features of vegetation and terrestrial detritus within the boundaries of the Chashnikovo UOPEC in the upper reaches of the Klyazma River have been studied, theses ecosystems corresponding with coniferous-deciduous forests conditions. Based on the ecological scales of L.G. Ramensky and E. Landolt, as well as the ecological-cenotic classification of A.A. Nitsenko, a grouping of terrestrial ecosystems differing in trophic and humidification levels was obtained by the method of main components. Within the studied territory, based on the ecological and cenotic structure of living ground cover, three groups of phytocenoses were identified — moderately wet forest phytocenoses with a predominance of spruce, wet forests with a predominance of small–leaved species, as well as phytocenoses of dryland and floodplain meadows. For all sampling points, the classification and stocks of litter, as well as their spatial distribution within the phytocenosis, were assessed. The studied ecosystems vary significantly in litter stocks from high values in the tree trunk spaces of spruce forests – about 5 kgm-2 – to extremely low values – less than 0.5 kgm-2 — in upland and floodplain meadows, which determines the high heterogeneity of potential carbon accumulation within the territory. The typological affiliation of litter is interconnected with stocks only at the biogeocenotic level in relation to spruce forests, but this pattern does not work at a higher level when considering ecosystems at the landscape level.