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16篇 您的检索式:作者名="Gorlenko"
    题名 作者 年代 出处 被引量
1Microbial communities of the stratified soda Lake Doroninskoe (Transbaikal region)显示文摘V. M. Gorlenko S. P. Buryukhaev E. B. Matyugina S. V. Borzenko Z. B. Namsaraev I. A. Bryantseva E. N. Boldareva D. Yu. Sorokin B. B. Namsaraev 2010Microbiology2010,,3:3
2The deep cold biosphere:facts and hypothesis显示文摘Vorobyova E Soina V Gorlenko M 1997FEMS Microbiology Reviews1997,20,:1
3The deep cold biosphere:facts and hypothesis显示文摘Vorobyova E Soina V Gorlenko M 1997FEMS Microbiology Reviews1997,20,:1
4Water regime and variations in hydrochemical characteristics of the soda Salt Lake Khilganta (Southeastern Transbaikalia)显示文摘Z. B. Namsaraev V. M. Gorlenko S. P. Buryukhaev D. D. Barkhutova V. D. Dambaev L. E. Dulov V. V. Sorokin B. B. Namsaraev 2010Water Resources2010,,4:1
5Microorganisms and enzyme activity in permafrost after removal of long-term cold stress显示文摘Vorobyova E Soina V Gorlenko M 1996Advances in Space Research1996,18,:1
6The deep cold biosphere:facts and hypothesis显示文摘Vorobyova E Soina V Gorlenko M 1997FEMS Microbiology Reviews1997,20,:1
7No wires attached: Usability challenges in the connected mobile world显示文摘Gorlenko L Merrick R 2003IBM Systems Journal2003,42,4:1
8Prokaryotic Communities of the north-eastern Mongolian soda lakes显示文摘Sorokin D Y Gorlenko V M Namsaraev B B 2004Hydrobiologia2004,522,:1
9Growth of Chloroflexus aurantiacus on media with different organic compounds and pathways of their metabolism显示文摘Krasilnikova EN Keppen OI Gorlenko VM 0,,:1
10The deep cold bi- osphere: facts and hypothesis显示文摘Vorobyova E Soina V Gorlenko M etal 1997FEMS Microbiol Reviews1997,20,34:1
11History of the study of biodiversity of photosyn- thetic bacterhz 显示文摘Gorlenko V M 2004Microbiology2004,73,5:1
12Differentiation of soil microbial communities by multisubstrate testing显示文摘Gorlenko M V Kozhevin P A 1994Microbiology1994,63,:1
13Specific features of nitrogen fixation in the termiteReticulitermes lucifugus 显示文摘Vecherskii MV Kostina NV Gorlenko MV Dobrovol'skaya TG Umarov MM 2008Biol Bull2008,35,5:1
14No wires attached: Usability challenges in the connected mobile world显示文摘GORLENKO L MERRICK R 2003IBM Systems Journal2003,42,4:1
15Mechanisms of cast structure and stressed state formation in Hadfield steel显示文摘The paper describes the investigation of mechanisms of cast structure formation in Hadfield steel depending on the changes in the cooling rate of a casting in the following two temperature ranges: crystallization temperature(1,200-1,390 °С) and the temperature of excessive phase separation(560-790 °С). Changes in the cooling rate of the crystallization temperature range from 1.1 to 25.0 °С·s^(-1) result in the reduction of the average size of austenite grains from 266 to 131 μm. At the same time, the magnitude of developing shrinkage stresses changes from +195 to 0 MPa. When the cooling rate is higher than 16 °С·s^(-1), no shrinkage stresses are formed in the casting. Changes in the cooling rate of the casting in the temperature range of the excessive phase separation influence the number of phases, their morphology and chemical composition, the values of phase stresses, and the possibility of martensitic transformation. Changing in the cooling rate from 0.24 to 5.46 °С·s^(-1) results in the decrease of the amount of the excessive phase from 14.8% to 2.1%, which is composed of eutectic and carbides depending on the cooling rate, their quantitative ratio and morphology change. Such changes in the microstructure are reflected on the changes of value of developing phase stresses. When the cooling rate is 0.24 °С·s^(-1), it is +100 MPa, while the increase of the cooling rate to 1.4 °С·s^(-1) results in the decrease of tensile stresses to 0 MPa and their qualitative stresses change to compressive ones. Further increase of the cooling rate results in the increase of the value of compressive stresses. When the cooling rate is 5.5 °С·s^(-1), their value reaches-92 MPa. Martensite forming in the structure of Hadfield steel is possible if the cooling rate of the casting in the range of excessive phase separation is less than 0.25 °С·s^(-1).Dmitri Gorlenko Konstantin Vdovin Nikolay Feoktistov 2016China Foundry2016,13,6:1
16Climate Change and Geochemistry May Explain the Finding of Marine Cyanobacteria in a Continental Saline Lake显示文摘1 Introduction Alkaline Lake Khilganta located in a steppe zone of South Siberia(N 50°42’535,E 115°06’086)is unique among adjacent lakes because of a development of a thick(up to 3 cm)cyanobacterial mat dominatedZorigto NAMSARAEV Vladimir GORLENKO Boris KUZNETSOV Bair NAMSARAEV 2014Acta Geologica Sinica(English Edition)2014,88,S1:0
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