Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Evgenya S Shelobolina"'
Autor:
Evgenya S Shelobolina, Hiromi eKonishi, Huifang eXu, Jason eBenzine, Mai Yia eXiong, Tao eWu, Marco eBlöthe, Eric eRoden
Publikováno v:
Frontiers in Microbiology, Vol 3 (2012)
The biogeochemistry of phyllosilicate-Fe redox cycling was studied in a Phalaris arundinacea (Reed Canary Grass) dominated redoximorphic soil from Shovelers Sink, a small glacial depression near Madison, WI. The clay size fraction of Shovelers Sink s
Externí odkaz:
https://doaj.org/article/d6160e90f67b4638b24eef34ea73f635
Publikováno v:
American Mineralogist. 106:69-81
A correlation between methanogenesis and dolomite formation has been reported; however, the mechanism underlying this association is not fully understood. In this study, we conducted forced carbonate precipitation experiments at room temperature in c
Autor:
Dorian V. Lust, Grace E. Dickerman, Albert E. Parker, Johanna M. Schultz, Diane K. Walker, Evgenya S. Shelobolina
Publikováno v:
Biofouling. 34:826-834
The inactivation of Pseudomonas aeruginosa biofilms grown on glass under high shear stress and exposed to a range of dissolved ozone concentrations (2, 5 and 7 ppm) at 10 and 20 min was investigated. The regression equation, log reduction (biofilm) =
Autor:
Evgenya S. Shelobolina, Christopher A. Gorski, Ravi K. Kukkadapu, Aron M. Griffin, Huifang Xu, Tao Wu, Eric E. Roden
Publikováno v:
Geomicrobiology Journal. 34:231-241
Dissimilatory microbial reduction of solid-phase Fe(III)-oxides and Fe(III)-bearing phyllosilicates (Fe(III)-phyllosilicates) is an important process in anoxic soils, sediments and subsurface materials. Although various studies have documented the re
Autor:
Evgenya S, Shelobolina, Diane K, Walker, Albert E, Parker, Dorian V, Lust, Johanna M, Schultz, Grace E, Dickerman
Publikováno v:
Biofouling. 34(7)
The inactivation of
Publikováno v:
Astrobiology. 15:331-340
Basaltic glass (BG) is an amorphous ferrous iron [Fe(II)]-containing material present in basaltic rocks, which are abundant on rocky planets such as Earth and Mars. Previous research has suggested that Fe(II) in BG can serve as an energy source for c
Autor:
Zhizhang Shen, Fangfu Zhang, Evgenya S. Shelobolina, Hiromi Konishi, Huifang Xu, Brandon J. Converse, Eric E. Roden
Publikováno v:
American Mineralogist. 100:483-494
Because of its rare occurrence in modern sediments, as well as the difficulty in synthesizing it under low-temperature conditions in the laboratory, the origin of sedimentary dolomite has remained a long-standing enigma, often referred to as the “d
Publikováno v:
American Mineralogist. 97:556-567
The origin of dolomite is a long-standing enigma in sedimentary geology. It has been proposed that microorganisms, especially anaerobic microorganisms, can overcome kinetic barriers to facilitate dolomite precipitation, although their specific role i
Autor:
Hailiang Dong, Evgenya S. Shelobolina, Jing Zhang, Junjie Yang, Jinwook Kim, Ravi K. Kukkadapu
Publikováno v:
Chemical Geology. 291:206-216
In situ technetium-99 (99Tc) immobilization by Fe(II) associated with clay minerals is a potential cost-effective method for Tc remediation at contaminated sites. The oxidation state of Fe is constantly cycled in sedimentary environments, however the
Publikováno v:
Applied and Environmental Microbiology. 77:6036-6042
Some nitrate- and Fe(III)-reducing microorganisms are capable of oxidizing Fe(II) with nitrate as the electron acceptor. This enzymatic pathway may facilitate the development of anaerobic microbial communities that take advantage of the energy availa