31 research outputs found
Mathematical simulation and forecast of watercourse deformations of Tom river within the limits of Tomsk city (Western Siberia)
The mathematical model of watercourse deformations of Tom river within the limits of Tomsk city on river stretch 74,8...58,3 km from a mouth is developed and evaluated. Distribution of the intensity of vertical bottom deformations along the river, tractional and suspended discharge of the load is determined for periods of high, average and low water content. It is shown, that conserving natural and anthropogenic conditions of formation of sediment runoff of the river Tom within the limits of Tomsk city, formed in 2003-2006, definite river-bed level lowering is probable in the next decade and further forming of the island in the south part of a city. Effectiveness evaluation of channel dredging on the river Tom is carried out, and the forecast of watercourse deformations is given under different variants of anthropogenic impact on the strea
Comparative characterisation of forest litter on sod-podzolic soils of Forest Experimental Dacha in RSAUβMAA named after K.A. Timiryazev
Forest litter under linden and pine forests was studied at the Forest Experimental Dacha of the RSAUβMAA named after K.A. Timiryazev. Despite significant differences in physical and chemical parameters between the litter formed under the conditions of different forest communities, the properties of sod-podzolic soils formed under both vegetation types are quite similar. The litter under linden forest has higher ash content, it is less acidic and contains almost 2 times more exchangeable bases, the content of hydrogen and nitrogen is higher by 0.82 wt% and 0.66 wt%, respectively. The litter of linden and pine forests, according to the atomic ratios HΒ :Β C, CΒ :Β N and the degree of oxidation, are equal to 1.82, 30.3, -0.92 and 1.64, 45.7, -0.71, respectively; the litter of linden forests differs from litter of pine forests in the higher content of aliphatic, nitrogen-rich, reduced organic compounds. In the litter of linden forests concentration coefficients of phosphorus and magnesium 1.2 times higher; of carbon, potassium and aluminium β 1.3 times higher; of calcium β 1.4 times higher; of nitrogen β 1.8 times higher, and of silicon β 3 times higher, than in the litter of pine trees. However, the concentration factor of manganese in the pine forest litter is 1.9 times higher compared to the litter of linden. According to the results of UV spectroscopy, water-soluble organic matter of pine forest litter, unlike water-soluble organic matter of linden forest litter, is more enriched by components of aromatic origin. This is evidenced by higher values of SUVA254 and lower values of coefficients E2/E3 and E4/E6
Changes in chemical composition of drilling waste water in taiga zone of Western Siberia (the Russian Federation) on the basis of thermodynamic approach
Conditions of contaminant distribution in the wetland water of Western Siberia (the Russian Federation)
(Table 5b) Chemical composition of natural waters from small rivers of the Lower Tom' Basin
(Table 5c) Chemical composition of natural perched groundwaters outside apparent swamps of the Lower Tom' Basin
Geochemistry of surface and groundwaters from lower Tom Basin wetland, western Siberia
New data are reported on the major- and trace-component compositions of acidic and weakly acidic low-concentration wetland waters and other water types. Special attention was given to dissolved organic compounds: fulvic and humic acids, bitumens, and hydrocarbons. The first comprehensive data are presented for organic trace components in the wetland waters of western Siberia: alkanes, pentacyclic terpenoids, steranes, alkylbenzenes, naphthalenes, phenanthrenes, tetraarenes, etc
Composition of swamp waters from the lower Tom' River Basin
New data on chemical and trace component compositions of acidic and low acidic swamp waters and other types of low mineralized waters are reported in the paper. Special attention is paid to dissolved organic compounds: fulvic and humic acids, bitumen, and hydrocarbons. For the first time detailed data on organic trace components (alkanes, pentacyclic terpenoids, steranes, alkylbenzenes, naphthalenes, phenanthrenes, tetraarenes, etc.) in the swamp waters of the Western Siberia: are reported