4 research outputs found
Geochemical groundwater peculiarities of Paleogene sediments in S-E Western Siberia artesian basin
The geochemical peculiarities of groundwater in Paleogene deposits in southeastern part of Western Siberia artesian basin are considered in the paper. Landscape, climate, geostructural and hydrogeological conditions define the water composition and quality peculiarities in this region. It has been established that ion-saline composition, mineralization and water quality changes arre governed by the horizontal zonal distribution. Groundwater of taiga landscapes generally is in equilibrium with kaolinite and quartz, mainly involving Ca- and Mg-montmorillonite, illite, carbonate minerals, sometimes barite. Groundwater in woodland grass and grassland, together with previously mentioned minerals, is usually in equilibrium with barite, colestine, and particularly, fluorite and gypsum. As a result, all relevant elements are removed from the groundwater and their accumulation level is restricted
ΠΠ·Π°ΠΈΠΌΠΎΡΠ²ΡΠ·Ρ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ ΠΈ Π½Π΅ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ Π²Π΅ΡΠ΅ΡΡΠ² ΠΏΡΠΈ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ ΠΌΠΎΡΠ΅Π²ΡΡ ΠΊΠ°ΠΌΠ½Π΅ΠΉ
Macro- and microscopic structural features of human urolyths have been studied to reveal the relation between organic and inorganic components and the role of the latter in the process of urolyth formation and growth. The combined study of the shape, color, surface, mineral and organic composition, and internal structure and zoning of 788 urolyths has been performed. Crystallomorphological, polarization-optical, X-ray-diffraction, electron-microscopic, chemical, neutron-activation, and computer technologies of study of the urolyth structure have been used. It has been found that macroscopic characteristics of uroluths (color, shape, surface, and size) did not reflect the chemical composition of urolyths. In the structure of abundance of urolyths in Tomskand the Tomsk Region, oxalates (58%) and urolyths of complex mineral composition (29%)Β prevail. It has been found that an urolyth is an organomineral aggregate having the internal structure formed by a rhythm of alternation of organic and inorganic layers and the character of arrangement of individual mineral crystals, and the internal structure is independent of the chemical composition of the urolyth andΒ uniform in urolyths of different chemical composition. The most part of urolyths has a mixed (44%) or druzy (35%) type of crystal arrangement and theΒ combined (45%) or grainy (31%) rhythm of alternation of organic and inorganic components.ΠΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ ΠΌΠ°ΠΊΡΠΎ- ΠΈ ΠΌΠΈΠΊΡΠΎΡΠΊΠΎΠΏΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΡΡΡΠΊΡΡΡΠ½ΡΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΠΌΠΎΡΠ΅Π²ΡΡ
ΠΊΠ°ΠΌΠ½Π΅ΠΉ ΡΠ΅Π»ΠΎΠ²Π΅ΠΊΠ° Ρ Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ΠΌ Π²Π·Π°ΠΈΠΌΠΎΡΠ²ΡΠ·ΠΈ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΈ Π½Π΅ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΎΡΡΠ°Π²Π»ΡΡΡΠΈΡ
ΠΈ ΡΠΎΠ»ΠΈ ΠΏΠΎΡΠ»Π΅Π΄Π½Π΅ΠΉ Π² ΠΏΡΠΎΡΠ΅ΡΡΠ΅ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΈ ΡΠΎΡΡΠ° ΠΊΠ°ΠΌΠ½Ρ. ΠΡΠΏΠΎΠ»Π½Π΅Π½ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ½ΠΎΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ ΡΠΎΡΠΌΡ, ΡΠ²Π΅ΡΠ°, Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠ° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ, ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²ΠΎΠ², Π° ΡΠ°ΠΊΠΆΠ΅ Π²Π½ΡΡΡΠ΅Π½Π½Π΅ΠΉ ΡΡΡΡΠΊΡΡΡΡ ΠΈ Π·ΠΎΠ½Π°Π»ΡΠ½ΠΎΡΡΠΈ 788 ΠΌΠΎΡΠ΅Π²ΡΡ
ΠΊΠ°ΠΌΠ½Π΅ΠΉ. ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½Ρ ΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅, ΠΏΠΎΠ»ΡΡΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎ-ΠΎΠΏΡΠΈΡΠ΅ΡΠΊΠΈΠ΅, ΡΠ΅Π½ΡΠ³Π΅Π½ΠΎΡΡΡΡΠΊΡΡΡΠ½ΡΠ΅, ΡΠ»Π΅ΠΊΡΡΠΎΠ½Π½ΠΎ-ΠΌΠΈΠΊΡΠΎΡΠΊΠΎΠΏΠΈΡΠ΅ΡΠΊΠΈΠ΅, Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΠ΅, Π½Π΅ΠΉΡΡΠΎΠ½Π½ΠΎ-Π°ΠΊΡΠΈΠ²Π°ΡΠΈΠΎΠ½Π½ΡΠ΅, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΊΠΎΠΌΠΏΡΡΡΠ΅ΡΠ½ΡΠ΅ ΡΠ΅Ρ
Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΡΡΡΠΎΠ΅Π½ΠΈΡ ΡΡΠΎΠ»ΠΈΡΠΎΠ². Π£ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ ΠΌΠ°ΠΊΡΠΎΡΠΊΠΎΠΏΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΡΠΈΠ·Π½Π°ΠΊΠΈ ΠΊΠ°ΠΌΠ½Ρ (ΡΠ²Π΅Ρ, ΡΠΎΡΠΌΠ°, Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΈ ΡΠ°Π·ΠΌΠ΅ΡΡ) Π½Π΅ ΠΎΡΡΠ°ΠΆΠ°ΡΡ Π΅Π³ΠΎ Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π°. Π ΡΡΡΡΠΊΡΡΡΠ΅ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΠΌΠΎΡΠ΅Π²ΡΡ
ΠΊΠ°ΠΌΠ½Π΅ΠΉ Π² Π³. Π’ΠΎΠΌΡΠΊΠ΅ ΠΈ Π’ΠΎΠΌΡΠΊΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ ΠΏΡΠ΅ΠΎΠ±Π»Π°Π΄Π°ΡΡ ΠΎΠΊΡΠ°Π»Π°ΡΡ (58%) ΠΈ ΠΊΠ°ΠΌΠ½ΠΈ ΡΠ»ΠΎΠΆΠ½ΠΎΠ³ΠΎ ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π° (29%). ΠΡΡΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ ΠΌΠΎΡΠ΅Π²ΠΎΠΉ ΠΊΠ°ΠΌΠ΅Π½Ρ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΡΠ³Π°Π½ΠΎΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΡΠΌ Π°Π³ΡΠ΅Π³Π°ΡΠΎΠΌ, ΠΈΠΌΠ΅ΡΡΠΈΠΌ Π²Π½ΡΡΡΠ΅Π½Π½ΡΡ ΡΡΡΡΠΊΡΡΡΡ, ΡΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½Π½ΡΡ ΡΠΈΡΠΌΠΎΠΌ ΡΠ΅ΡΠ΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΡΠ»ΠΎΠ΅Π² Π²Π΅ΡΠ΅ΡΡΠ² ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΈ Π½Π΅ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΡΡΠΎΠ΅Π½ΠΈΡ ΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΎΠΌ ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΡ ΠΎΡΠ΄Π΅Π»ΡΠ½ΡΡ
ΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠ² ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ², ΠΏΡΠΈ ΡΡΠΎΠΌ Π²Π½ΡΡΡΠ΅Π½Π½ΡΡ ΡΡΡΡΠΊΡΡΡΠ° Π½Π΅ Π·Π°Π²ΠΈΡΠΈΡ ΠΎΡ Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π° ΠΊΠ°ΠΌΠ½Ρ ΠΈ ΠΎΠ΄Π½ΠΎΡΠΈΠΏΠ½Π° Ρ ΠΊΠ°ΠΌΠ½Π΅ΠΉ ΡΠ°Π·Π½ΠΎΠ³ΠΎ Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π°. ΠΠΎΠ»ΡΡΠ°Ρ ΡΠ°ΡΡΡ ΠΌΠΎΡΠ΅Π²ΡΡ
ΠΊΠ°ΠΌΠ½Π΅ΠΉ ΠΈΠΌΠ΅Π΅Ρ ΡΠΌΠ΅ΡΠ°Π½Π½ΡΠΉ (44%) ΠΈΠ»ΠΈ Π΄ΡΡΠ·ΠΎΠ²ΠΈΠ΄Π½ΡΠΉ (35%) ΡΠΈΠΏ ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΡ ΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠ² ΠΈ ΠΊΠΎΠΌΠ±ΠΈΠ½ΠΈΡΠΎΠ²Π°Π½Π½ΡΠΉ (45%) ΠΈΠ»ΠΈ Π·Π΅ΡΠ½ΠΈΡΡΡΠΉ (31%) ΡΠΈΡΠΌ ΡΠ΅ΡΠ΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π½Π΅ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠΎΡΡΠ°Π²Π»ΡΡΡΠΈΡ
Relation of organic and inorganic substances in formation of urolyths
Macro- and microscopic structural features of human urolyths have been studied to reveal the relation between organic and inorganic components and the role of the latter in the process of urolyth formation and growth. The combined study of the shape, color, surface, mineral and organic composition, and internal structure and zoning of 788 urolyths has been performed. Crystallomorphological, polarization-optical, X-ray-diffraction, electron-microscopic, chemical, neutron-activation, and computer technologies of study of the urolyth structure have been used. It has been found that macroscopic characteristics of uroluths (color, shape, surface, and size) did not reflect the chemical composition of urolyths. In the structure of abundance of urolyths in Tomskand the Tomsk Region, oxalates (58%) and urolyths of complex mineral composition (29%)Β prevail. It has been found that an urolyth is an organomineral aggregate having the internal structure formed by a rhythm of alternation of organic and inorganic layers and the character of arrangement of individual mineral crystals, and the internal structure is independent of the chemical composition of the urolyth andΒ uniform in urolyths of different chemical composition. The most part of urolyths has a mixed (44%) or druzy (35%) type of crystal arrangement and theΒ combined (45%) or grainy (31%) rhythm of alternation of organic and inorganic components