5 research outputs found
ZEOLITE-CONTAINING TRIPOLI OF KHOTYNETS DEPOSIT (OREL REGION): MINERAL COMPOSITION, SORPTION PROPERTIES AND FORMATION CONDITIONS
Link for citation: Belousov P.E., Karelina N.D., Morozov I.A., Rudmin M.A., Milyutin V.V., Nekrasova N.A., Β Rumyantseva Β A.O., Zakusina O.V., Krupskaya Β V.V. Zeolite-containing tripoli of Khotynets deposit (Orel region): mineral composition, sorption properties and formation conditions. Bulletin of the Tomsk Polytechnic University. Geo Πssets Engineering, 2023, vol. 334, no. 5, ΡΡ.70-84.In Rus.
The relevance of the work is caused by the need to develop the mineral resource base of high-quality sorption materials in Russia, as well as to study the properties of natural sorbents with a view to their further application in practice. The aim of the work is to study the features of the geological structure, conditions of formation, mineral composition and sorption properties of zeolite-containing tripoli from the Khotynets deposit. The object of the study is the Khotynets deposit of zeolite-containing tripoli, studied by the field team of the Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of Sciences RAS in 2019β2020. Methods: XRD, XRF, FTIR, optical and scanning electron microscopy, determination of SSA and pore size distribution, CEC, experiments on the sorption of cesium, strontium and copper. The paleotectonic reconstruction was carried out as well. Results. The productive strata of the Khotynets deposit consists of three benches, the main useful components of which are minerals of the zeolite, opal-cristobalite and smectite group. Their total content reaches 80 %. The formation of the deposit occurred in three stages and is associated with the primary accumulation of biochemogenic silica in coastal sea waters, the removal of terrigenous clay material from the nearby land, their further compaction, and processing of the accumulated material at the diagenesis stage. The formation of clinoptillolite is associated with an increase in pH and the dissolution of the opal-cristobalite and clay material as a result of the secondary impact of low-temperature deep solutions. The performed experiments showed that this mineral material has high sorption characteristics with respect to cesium and copper and can be used as a component of sorption mixtures for the purification of polluted waters
Zeolite-containing Tripoli of Khotynets deposit (Orel region): mineral composition, sorption properties and formation conditions
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΡΠ°Π±ΠΎΡΡ ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½Π° Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎ-ΡΡΡΡΠ΅Π²ΠΎΠΉ Π±Π°Π·Ρ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ Π²ΡΡΠΎΠΊΠΎΠΊΠ°ΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ ΡΠΎΡΠ±ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΡΡΡΡ Π ΠΎΡΡΠΈΠΈ, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΡΠ²ΠΎΠΉΡΡΠ² ΠΏΡΠΈΡΠΎΠ΄Π½ΡΡ
ΡΠΎΡΠ±Π΅Π½ΡΠΎΠ² Ρ ΡΠ΅Π»ΡΡ ΠΈΡ
Π΄Π°Π»ΡΠ½Π΅ΠΉΡΠ΅Π³ΠΎ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΡ Π½Π° ΠΏΡΠ°ΠΊΡΠΈΠΊΠ΅. Π¦Π΅Π»ΡΡ ΡΠ°Π±ΠΎΡΡ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΈΠ·ΡΡΠ΅Π½ΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠ΅ΠΉ Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΡΡΠΎΠ΅Π½ΠΈΡ, ΡΡΠ»ΠΎΠ²ΠΈΠΉ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ, ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π° ΠΈ ΡΠΎΡΠ±ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠ²ΠΎΠΉΡΡΠ² ΡΠ΅ΠΎΠ»ΠΈΡΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠ΅Π³ΠΎ ΡΡΠ΅ΠΏΠ΅Π»Π° Π₯ΠΎΡΡΠ½Π΅ΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ. ΠΠ±ΡΠ΅ΠΊΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΡΠ²Π»ΡΠ΅ΡΡΡ Π₯ΠΎΡΡΠ½Π΅ΡΠΊΠΎΠ΅ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠ΅ ΡΠ΅ΠΎΠ»ΠΈΡΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠ΅Π³ΠΎ ΡΡΠ΅ΠΏΠ΅Π»Π°, ΠΈΠ·ΡΡΠ΅Π½Π½ΠΎΠ΅ ΠΏΠΎΠ»Π΅Π²ΡΠΌ ΠΎΡΡΡΠ΄ΠΎΠΌ ΠΠ½ΡΡΠΈΡΡΡΠ° Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΡΡΠ΄Π½ΡΡ
ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ, ΠΏΠ΅ΡΡΠΎΠ³ΡΠ°ΡΠΈΠΈ, ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ³ΠΈΠΈ ΠΈ Π³Π΅ΠΎΡ
ΠΈΠΌΠΈΠΈ Π ΠΠ Π² 2019-2020 Π³Π³. ΠΠ΅ΡΠΎΠ΄Ρ: ΡΠ΅Π½ΡΠ³Π΅Π½ΠΎΡΠ°Π·ΠΎΠ²ΡΠΉ ΠΈ ΡΠ΅Π½ΡΠ³Π΅Π½ΠΎΡΠ»ΡΠΎΡΠ΅ΡΡΠ΅Π½ΡΠ½ΡΠΉ Π°Π½Π°Π»ΠΈΠ·, ΠΠ-ΡΠΏΠ΅ΠΊΡΡΠΎΡΠΊΠΎΠΏΠΈΡ, ΠΎΠΏΡΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΈ ΡΠΊΠ°Π½ΠΈΡΡΡΡΠ°Ρ ΡΠ»Π΅ΠΊΡΡΠΎΠ½Π½Π°Ρ ΠΌΠΈΠΊΡΠΎΡΠΊΠΎΠΏΠΈΡ, ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΡΠ΄Π΅Π»ΡΠ½ΠΎΠΉ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΈ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΠΏΠΎΡ ΠΏΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ°ΠΌ, Π΅ΠΌΠΊΠΎΡΡΡ ΠΊΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΎΠ±ΠΌΠ΅Π½Π°, ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΡ ΠΏΠΎ ΡΠΎΡΠ±ΡΠΈΠΈ ΡΠ΅Π·ΠΈΡ, ΡΡΡΠΎΠ½ΡΠΈΡ ΠΈ ΠΌΠ΅Π΄ΠΈ. Π’Π°ΠΊΠΆΠ΅ Π±ΡΠ»Π° ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Π° ΠΏΠ°Π»Π΅ΠΎΡΠ΅ΠΊΡΠΎΠ½ΠΈΡΠ΅ΡΠΊΠ°Ρ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΡ. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½Π°Ρ ΡΠΎΠ»ΡΠ° Π₯ΠΎΡΡΠ½Π΅ΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ ΡΠΎΡΡΠΎΠΈΡ ΠΈΠ· ΡΡΠ΅Ρ
ΠΏΠ°ΡΠ΅ΠΊ, ΠΎΡΠ½ΠΎΠ²Π½ΡΠΌΠΈ ΠΏΠΎΠ»Π΅Π·Π½ΡΠΌΠΈ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠ°ΠΌΠΈ ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²Π»ΡΡΡΡΡ ΠΌΠΈΠ½Π΅ΡΠ°Π»Ρ Π³ΡΡΠΏΠΏΡ ΡΠ΅ΠΎΠ»ΠΈΡΠ°, ΠΎΠΏΠ°Π»-ΠΊΡΠΈΡΡΠΎΠ±Π°Π»ΠΈΡΠ° ΠΈ ΡΠΌΠ΅ΠΊΡΠΈΡΠ°. ΠΡ
ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ Π΄ΠΎΡΡΠΈΠ³Π°Π΅Ρ 80 %. ΠΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ ΠΏΡΠΎΠΈΡΡ
ΠΎΠ΄ΠΈΠ»ΠΎ Π² ΡΡΠΈ ΡΡΠ°ΠΏΠ° ΠΈ ΡΠ²ΡΠ·Π°Π½ΠΎ Ρ ΠΏΠ΅ΡΠ²ΠΈΡΠ½ΡΠΌ Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΠ΅ΠΌ ΠΊΡΠ΅ΠΌΠ½Π΅Π·Π΅ΠΌΠ° Π² ΠΏΡΠΈΠ±ΡΠ΅ΠΆΠ½ΡΡ
ΠΌΠΎΡΡΠΊΠΈΡ
Π²ΠΎΠ΄Π°Ρ
, ΡΠ½ΠΎΡΠΎΠΌ ΡΠ΅ΡΡΠΈΠ³Π΅Π½Π½ΠΎΠ³ΠΎ Π³Π»ΠΈΠ½ΠΈΡΡΠΎΠ³ΠΎ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π° Ρ Π±Π»ΠΈΠ·Π»Π΅ΠΆΠ°ΡΠ΅ΠΉ ΡΡΡΠΈ, Π΄Π°Π»ΡΠ½Π΅ΠΉΡΠΈΠΌ ΡΠΏΠ»ΠΎΡΠ½Π΅Π½ΠΈΠ΅ΠΌ ΠΈ ΠΏΠ΅ΡΠ΅ΡΠ°Π±ΠΎΡΠΊΠΎΠΉ Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½Π½ΠΎΠ³ΠΎ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π° Π½Π° ΡΡΠ°Π΄ΠΈΠΈ Π΄ΠΈΠ°Π³Π΅Π½Π΅Π·Π°. ΠΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΊΠ»ΠΈΠ½ΠΎΠΏΡΠΈΠ»ΠΎΠ»ΠΈΡΠ° ΡΠ²ΡΠ·Π°Π½ΠΎ Ρ ΠΏΠΎΠ²ΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΡΠ ΠΈ ΡΠ°ΡΡΠ²ΠΎΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΎΠΏΠ°Π»ΠΊΡΠΈΡΡΠΎΠ±Π°Π»ΠΈΡΠΎΠ²ΠΎΠ³ΠΎ ΠΈ Π³Π»ΠΈΠ½ΠΈΡΡΠΎΠ³ΠΎ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π° Π² ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠ΅ Π²ΡΠΎΡΠΈΡΠ½ΠΎΠ³ΠΎ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ Π½ΠΈΠ·ΠΊΠΎΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ½ΡΡ
Π³Π»ΡΠ±ΠΈΠ½Π½ΡΡ
ΡΠ°ΡΡΠ²ΠΎΡΠΎΠ². ΠΡΠΎΠ²Π΅Π΄Π΅Π½Π½ΡΠ΅ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΡ ΠΏΠΎΠΊΠ°Π·Π°Π»ΠΈ, ΡΡΠΎ Π΄Π°Π½Π½ΠΎΠ΅ ΡΡΡΡΠ΅ ΠΎΠ±Π»Π°Π΄Π°Π΅Ρ Π²ΡΡΠΎΠΊΠΈΠΌΠΈ ΡΠΎΡΠ±ΡΠΈΠΎΠ½Π½ΡΠΌΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ°ΠΌΠΈ ΠΏΠΎ ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡ ΠΊ ΡΠ΅Π·ΠΈΡ ΠΈ ΠΌΠ΅Π΄ΠΈ ΠΈ ΠΌΠΎΠΆΠ΅Ρ ΠΏΡΠΈΠΌΠ΅Π½ΡΡΡΡΡ Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠ° ΡΠΎΡΠ±ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠΌΠ΅ΡΠ΅ΠΉ ΠΈ Π±Π°ΡΡΠ΅ΡΠΎΠ² Π΄Π»Ρ ΠΎΡΠΈΡΡΠΊΠΈ Π·Π°Π³ΡΡΠ·Π½Π΅Π½Π½ΡΡ
Π²ΠΎΠ΄.The relevance of the work is caused by the need to develop the mineral resource base of high-quality sorption materials in Russia, as well as to study the properties of natural sorbents with a view to their further application in practice. The aim of the work is to study the features of the geological structure, conditions of formation, mineral composition and sorption properties of zeolite-containing tripoli from the Khotynets deposit. The object of the study is the Khotynets deposit of zeolite-containing tripoli, studied by the field team of the Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of Sciences RAS in 2019-2020. Methods: XRD, XRF, FTIR, optical and scanning electron microscopy, determination of SSA and pore size distribution, CEC, experiments on the sorption of cesium, strontium and copper. The paleotectonic reconstruction was carried out as well. Results. The productive strata of the Khotynets deposit consists of three benches, the main useful components of which are minerals of the zeolite, opal-cristobalite and smectite group. Their total content reaches 80 %. The formation of the deposit occurred in three stages and is associated with the primary accumulation of biochemogenic silica in coastal sea waters, the removal of terrigenous clay material from the nearby land, their further compaction, and processing of the accumulated material at the diagenesis stage. The formation of clinoptilolite is associated with an increase in pH and the dissolution of the opal-cristobalite and clay material as a result of the secondary impact of low-temperature deep solutions. The performed experiments showed that this mineral material has high sorption characteristics with respect to cesium and copper and can be used as a component of sorption mixtures for the purification of polluted waters
The Errors of Trotskyism : a symposium.
Includes bibliographical references.Introduction: our party's view, [by] J.T. Murphy.--The need to study October, by L. Trotsky.--How one should not write the history of October, [by] L. Trotsky.--Bolshevism or Trotskyism? by G. Zinoviev.--Leninism or Trotskyism? by Comrade Stalin.--Leninism or Trotskyism? by L. Kamenev.--How should the history of October be written? by G. Sokolnikov.--A misleading description of the "German October", by O.W. Kuusinen.--The lessons of October, by N. Krupskaya.--Comrade Trotsky's letter to the Central Committee of the R.C.P.--Resolution of the Central Committee of The R.C.P.Mode of access: Internet.labd: In original paper covers