WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION最新文献

{"title":"CONTAMINATION OF NEAR-WELL WATER-SATURATED MEDIA: TERMINOLOGY AND APPLICABILITY","authors":"A. A. Tsymbalov","doi":"10.31554/978-5-7925-0584-1-2020-274-277","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-274-277","url":null,"abstract":": The article uses the term \"contamination\"to the formation - well system. The definition of the process of contamination of the near-well environment for the formation-well system is formulated. Recommended conditions for the use of contamination. The work was carried out within the framework of the research Program of LLC \"Archime-des\" Arh. № ТЕR -R 642012-0001.000 \"Research of the processes of colmatation of the near-well environment and development of methods for decolmatation of culverts\".","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"53 2","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114002700","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"CHEMICAL COMPOSITION OF UNDERGROUND WATER SOURCES OF NON-CENTRALIZED WATER SUPPLY IN THE TOMSK REGION OF THE TOMSK OBLAST AND ITS POSSIBLE IMPACT ON HUMAN HEALTH","authors":"Yu. V. Kolubaeva","doi":"10.31554/978-5-7925-0584-1-2020-159-162","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-159-162","url":null,"abstract":": The results of studying the chemical composition of groundwater in non-centralized water supply sources in the Tomsk region of the Tomsk oblast are presented. High concentrations of the following components were found: hardness of water, Na + , K + , SO 4 2- , Cl - , NO 3 - , Fe, Mn, etc. For NO 3 - , Fe and Mn there is a multiple excess of not only background values for this territory but also MPC for drinking water. A review of possible cases of the influence of excess contents of the components of the chemical composition of water on the human body and related diseases is pre-sented.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"249 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134278268","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"FORMATION OF ACIDIC EFFLUENTS FROM DUMPS OF THE KIZEL COAL BASIN (PERM TERRITORY)","authors":"N. Maksimovich, O. Meshcheryakova, O. Berezina, A. Demenev, A. M. Sedinin, V. Khmurchik","doi":"10.31554/978-5-7925-0584-1-2020-239-241","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-239-241","url":null,"abstract":". The coal mining is usually associated with a number of environmental problems, one of them is the ac-cumulation of a significant amount of waste rock in the territories adjacent to the mines. The dumps located on the terri-tory of the Kizel coal basin are investigated in the article. Also the process of their negative impact on the environment are described, as well as earth remote sensing results from images from Santinel-2 satellites and analyzes of dump sam-ples using optical, x-ray, thermal, and electron microscopy methods.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"45 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127071675","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"GEOCHEMICAL FEATURES OF NATURAL WATERS IN THE CENTRAL ECOLOGICAL ZONE OF THE BAIKAL NATURAL TERRITORY (BNT)","authors":"V. Petrov, D. Yakovlev","doi":"10.31554/978-5-7925-0584-1-2020-99-102","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-99-102","url":null,"abstract":"ABSTRAСT: The paper describes the composition of stable components association of the CEZ BNT thermal waters components. It includes Li, B, Na, Si, K, Rb, Sr, Mo, and W. Significant depth formation of the thermal and the pres-ence of this association or its fragments in another type natural waters (e.g. surface, ground) allows to predict that the waters have deep nutrition. A comparison of the distribution of natural waters components concentration allows to as-sume that atmospheric water supply and host rocks are the only source of the waters formation. The distribution of the composition of thermal waters components concentration is related to the temperature and duration of contact with the host rocks.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127504514","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"THE INFLUENCE OF TECTONICS ON THE PROCESS OF WATER-ROCK INTERACTION IN THE FORMATION OF THE CARBON DIOXIDE MINERAL WATER COMPOSITION OF THE ARSHAN-TUNKINSKY DEPOSIT IN THE BAIKAL RIFT ZONE","authors":"Yu. I. Kustov","doi":"10.31554/978-5-7925-0584-1-2020-65-68","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-65-68","url":null,"abstract":"The manifestation of mineral healing waters at the piedmont of the Tunkinsky Alps of the southern spurs of the East Sayan at the exit of the valley of the river Kyngarga in the Tunkinsky depression became known from the end of the 19th century. It was established that this manifestation is confined to the intersection of an angle of 90 of two faults: Tunkinsky, which serves as the boundary between the crystalline rocks of the East Sayan mountain structures and sedimentary rocks of the Tunkinsky rift basin, and Kungarsky, along which the Kyngarga river valley is laid. The Kingarga valley is narrow in width and short in length. The Kyngarga River has a constant water flow, which flows into the river Tunka and further into the river Irkut, which is the main object of the drainage system of the Tunkinsky rift depression. ВВЕДЕНИЕ Источник Аршанский на левом берегу р. Кынгарги очаг разгрузки минеральной воды, насыщенной углекислым газом, был представлен отчётливыми выходами и большим количеством мелких грифонов в месте пересечения двух тектонических разломов: Тункинского и Кынгарского. Наиболее крупные два выхода были каптированы. Расстояние между ними составляло 3 м. Источник открыт в конце XIX столетия и со временем приобрёл широкую популярность у местного населения и жителей городов Иркутска и Улан-Удэ. Воды источника используются для лечебных целей (ванные процедуры и питьевой бювет) [1]. В начале 30-х гг. XX столетия возникла необходимость проведения на участке данного проявления минеральных вод геологоразведочных работ с целью изучения гидрогеологических условий региона, оценки запасов месторождения и возможности расширения построенной здесь водолечебницы. По величине минерализации воды источника слабосолёные, по составу сульфатно-гидрокарбонатные магниевокальциевые, насыщенны двуокисью углерода (CO2) и кремнекислотой (H4SiO4); температура воды в источниках 8.0–8.5 С [4]. ОБЪЕКТЫ И МЕТОДЫ Аршан-Тункинское месторождение углекислых минеральных лечебных вод разведано в северной части Тункинской впадины Байкальского рифта вблизи Аршанского источника углекислых минеральных вод, приуроченного к месту пересечения под углом 90 двух тектонических разломов: Тункинского (широтное направление), ограничивающего северную часть Тункинской рифтовой впадины, и Кынгарского (меридиональное направление), по которому заложена каньёнообразной формы долина р.Кынгарги. Образовавшаяся по Кынгарскому разлому долина по размеру в поперечном сечении является узкой, а по протяжённости короткой. По днищу долины течёт р. Кынгарга, имеющая постоянный водный сток, объём которого поступает в р. Тунку и далее в р. Иркут – основную дренажную систему Тункинской рифтовой впадины (рис.1).","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"49 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129966589","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"GEOCHEMICAL CHARACTERISTICS OF WATER BODIES WITH VARIOUS TROPHICITY USING FILTRATION METHODS","authors":"E. Ivleva, Y. Alekhin","doi":"10.31554/978-5-7925-0584-1-2020-156-158","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-156-158","url":null,"abstract":":The chemical composition of the surface water of two objects with different geochemical composition was investigated. The patterns of distribution of elements in the eutrophic and dystrophic reservoirs of the Vladimir region were considered. A series of filtration experiments were carried out for these objects without replacing the mem-brane (continuous filtration) in order to determine the proportion of trace elements in colloidal and dissolved fractions and the association of trace elements in natural water.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"3 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114163974","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"RIFTOGENIC UNITY OF ULTRA-FRESH WATERS AND HYDROCARBONS OF THE BAIKAL REGION","authors":"Yu. N. Didenkov, Z. Proskuryakova, V. V. Haustov, M. Martynova, V. A. Chereneva","doi":"10.31554/978-5-7925-0584-1-2020-327-330","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-327-330","url":null,"abstract":": The performed studies substantiate the existence of a source of renewable ultrapress water and hydrocarbons in rift geodynamic conditions. The studies are carried out on the basis of the developed principles of structural and hydrogeological analysis and the results of thermodynamic simulation using the Selector software The revealed regularity allows us to conclude that the most studied natural resources necessary for mankind owe their origin to the same geological processes that accompany modern degassing of the planet.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"5 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134439282","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"TRACE ELEMENTS IN GROUND WATERS AND SURFACE WATERS OF THE SENTSA RIVER BASIN (EASTERN SAYAN RIDGE)","authors":"S. Alexeev, L. Alexeeva","doi":"10.31554/978-5-7925-0584-1-2020-11-14","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-11-14","url":null,"abstract":": The paper presents the first data on the distribution of trace elements in ground waters and surface waters of the Sentsa River basin (Eastern Sayan Ridge). It is shown that the Khoyto-Gol thermal waters are significantly en-riched in Li, Be, B, Si, Mn, Ge, As, Br, Rb, Sr, Cs, Ba, W and depleted in Al, P, Cu, Zn, Ag relative to river waters and rainwater. The REE distribution spectra in ground waters and surface waters are characterized by a strongly positive Eu anomaly and the prevalence of light REE over heavy REE.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"17 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125813550","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"VAPOR-GAS TRANSFER OF CHEMICAL ELEMENTS UNDER LOW-TEMPERATURE CONDITIONS (FIELD AND LABORATORY EXPERIMENTS)","authors":"S. Bortnikova, N. Yurkevich, A. Devyatova, S. S. Volynkin","doi":"10.31554/978-5-7925-0584-1-2020-22-25","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-22-25","url":null,"abstract":": The article presents the results of a study of the elemental composition of condensates collected at the Ursk sulfide waste heaps (Kemerovo region). The composition of the vapor-gas phase under ambient conditions was compared with the composition obtained in laboratory experiments by heating the waste material to 60°C. Element con-centrations in condensates collected at the waste heaps significantly exceed background values. In the adjacent territory at a distance of 100 and 200 m the metal content does not reach the background. In the condensates of laboratory experiments, many chemical elements were determined, including Au, Zr, Cs, U, Tl. A high positive correlation between the compositions of condensates and the compositions of aqueous extracts extracted from parallel samples was established. This suggests that the sources of elements in condensed gas-vapor streams are secondary sulfates formed during the oxidation of sulfides. The most mobile elements during transport in the vapor – gas phase are alkaline (Li, Cs, Na, K), alkaline earth (Ca, Sr), chalcofilic metals Hg, Zn, Cu, and metalloids As, Sb, Se.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"76 2 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130813328","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"ESTIMATION OF FACTORS OF THE MECHANISM OF FORMATION OF DRAINAGE WATERS OF VARIOUS TECHNOLOGICAL TYPES OF ORES OF COPPER SANDSTONE DEPOSITS BY THERMODYNAMIC MODELING OF THE «WATER-ROCK-GAS» SYSTEM","authors":"O. A. Limantseva, B. Ryzhenko","doi":"10.31554/978-5-7925-0584-1-2020-394-397","DOIUrl":"https://doi.org/10.31554/978-5-7925-0584-1-2020-394-397","url":null,"abstract":"SUMMARY: In the paper the physical and chemical conditions are considered for the formation of the chemical com-position of waters draining rocks and ores of the copper sandstone deposit, with more attention to the main factors of their acidification. Thermodynamic simulation of water-rock-gas system shows that pyrite percentage is key factor for aggressive medium formation at pyrite content more than 1% and lgf O 2 >-20. Relative water filtration speed expressed by mass of rock (R) to mass of Water (W) decreases aqueous pH at R/W>0.1.","PeriodicalId":208191,"journal":{"name":"WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION","volume":"73 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131038776","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}