2018
DOI: 10.32014/2018.2518-170x.5
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The Forming of Fresh Underground Waters of the Akmola Region

Abstract: NAS RK is pleased to announce that News of NAS RK. Series of geology and technical sciences scientific journal has been accepted for indexing in the Emerging Sources Citation Index, a new edition of Web of Science. Content in this index is under consideration by Clarivate Analytics to be accepted in the Science Citation Index Expanded, the Social Sciences Citation Index, and the Arts & Humanities Citation Index. The quality and depth of content Web of Science offers to researchers, authors, publishers, and ins… Show more

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Cited by 3 publications
(3 citation statements)
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“…The sampling included taking water samples for hydrochemical (complete and typical) analyzes during experimental hydrogeological studies. Considering the data from experiments and the experience of several scientists in the study area, a more qualitative analysis of groundwater was carried out (Mitrofanova et al, 2017;Osipov et al, 2017;Romanova et al, 2017).…”
Section: Methodsmentioning
confidence: 99%
“…The sampling included taking water samples for hydrochemical (complete and typical) analyzes during experimental hydrogeological studies. Considering the data from experiments and the experience of several scientists in the study area, a more qualitative analysis of groundwater was carried out (Mitrofanova et al, 2017;Osipov et al, 2017;Romanova et al, 2017).…”
Section: Methodsmentioning
confidence: 99%
“…The intensification of combustion fuel mixture at the air-petrol thermal tools with ejector nozzle, made with perforations in the region of the initial section of the jet considered in the assumption of the creation on this site of powerful shock waves. Shock waves are formed when meeting with obstacle in a cylindrical nozzle (surface roughness ejected cold air) at the end of the supersonic gas jet from the nozzle of the main burner [1,2].…”
Section: Intensification Of Combustion Fuel Mixture In Petrolair Thermentioning
confidence: 99%
“…In the Kyrgyz Alatau, such movement of the permafrost boundary can take place only in the basins of the Aspara and Merke rivers. Unlike Zailiysky Alatau, the lower boundary of permafrost here is located at around 3400 m [11,12]. When raising its border by 583 m, permafrost rocks almost completely disappear in the basins of these rivers, or the groundwater recharge area will increase by 176.4 km 2 , including 115 km 2 in the Aspara river basin and 61.4 km 2 in Merke.…”
mentioning
confidence: 99%