Mineralogy, Analytical chemistry, Basalt, Melt inclusions and Olivine are his primary areas of study. His Mineralogy research is multidisciplinary, relying on both Fourier transform infrared spectroscopy, Carbonate, Silicate and Dissolution. His studies deal with areas such as Sulfide and Pyrrhotite as well as Silicate.
His work in Analytical chemistry tackles topics such as Mineral redox buffer which are related to areas like Redox. His work in Basalt addresses issues such as Electron microprobe, which are connected to fields such as Drop and Phenocryst. The study incorporates disciplines such as Partition coefficient, Mole fraction and Inclusion in addition to Melt inclusions.
His primary areas of study are Analytical chemistry, Geochemistry, Mineralogy, Basalt and Silicate. In general Analytical chemistry, his work in Infrared spectroscopy is often linked to XANES linking many areas of study. The concepts of his Geochemistry study are interwoven with issues in Sulfide, Plagioclase and Oceanic crust.
Roman E. Botcharnikov studies Mineralogy, focusing on Melt inclusions in particular. His research integrates issues of Electron microprobe, Trace element, Mineral redox buffer and Olivine in his study of Basalt. His studies link Dissolution with Silicate.
Roman E. Botcharnikov mostly deals with Geochemistry, Analytical chemistry, Mantle, Sulfide and Melt inclusions. His study in Geochemistry is interdisciplinary in nature, drawing from both Ophiolite, Plagioclase and Oceanic crust. His research in Analytical chemistry intersects with topics in Scheelite, Basalt, Quartz and Oxidation state.
Roman E. Botcharnikov has included themes like Mössbauer spectroscopy, Trace element and Mineral redox buffer in his Basalt study. Melt inclusions is a subfield of Olivine that Roman E. Botcharnikov studies. His biological study spans a wide range of topics, including Silicate, Crystallization and Phenocryst.
His main research concerns Mineral redox buffer, Olivine, Basalt, Melt inclusions and Phenocryst. His Mineral redox buffer research incorporates elements of Subduction, Mantle wedge, Mid-ocean ridge, Slab and Spinel. His studies in Olivine integrate themes in fields like Plagioclase and Gabbro.
In his research, Oxidation state is intimately related to Analytical chemistry, which falls under the overarching field of Basalt. His Melt inclusions study is concerned with the field of Crystallization as a whole. His Phenocryst research integrates issues from Ophiolite, Vanadium and Silicate.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Sulfur K-edge XANES analysis of natural and synthetic basaltic glasses: Implications for S speciation and S content as function of oxygen fugacity
Pedro J. Jugo;Max Wilke;Roman E. Botcharnikov.
Geochimica et Cosmochimica Acta (2010)
Solubility of H2O- and CO2-bearing fluids in tholeiitic basalts at pressures up to 500 MPa
T. A. Shishkina;R. E. Botcharnikov;F. Holtz;R. R. Almeev.
Chemical Geology (2010)
The effect of water activity on the oxidation and structural state of Fe in a ferro-basaltic melt
R. E. Botcharnikov;J. Koepke;Francois Holtz;C. McCammon.
Geochimica et Cosmochimica Acta (2005)
High gold concentrations in sulphide-bearing magma under oxidizing conditions
Roman E. Botcharnikov;Robert L. Linnen;Robert L. Linnen;Max Wilke;Francois Holtz.
Nature Geoscience (2011)
Phase Relations and Liquid Lines of Descent in Hydrous Ferrobasalt—Implications for the Skaergaard Intrusion and Columbia River Flood Basalts
R. E. Botcharnikov;R. R. Almeev;J. Koepke;F. Holtz.
Journal of Petrology (2008)
Amorphous Materials: Properties, structure, and Durability: Oxidation state of iron in hydrous phono-tephritic melts
Jan A. Schuessler;Roman E. Botcharnikov;Harald Behrens;Valeria Misiti.
American Mineralogist (2008)
Experimental Simulation of Closed-System Degassing in the System Basalt–H2O–CO2–S–Cl
Priscille Lesne;Simon C. Kohn;Jon Blundy;Fred Witham.
Journal of Petrology (2011)
Solubility of H2O and CO2 in ultrapotassic melts at 1200 and 1250 °C and pressure from 50 to 500 MPa
Harald Behrens;Valeria Misiti;Carmela Freda;Francesco Vetere;Francesco Vetere.
American Mineralogist (2009)
The effect of H2O on olivine crystallization in MORB: Experimental calibration at 200 MPa
Renat R. Almeev;François Holtz;Jürgen Koepke;Fleurice Parat.
American Mineralogist (2007)
Solubility and speciation of C-O-H fluids in andesitic melt at T=1100-1300°c and P=200 and 500 MPa
R.E. Botcharnikov;H. Behrens;F. Holtz.
Chemical Geology (2006)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below:
University of Hannover
Russian Academy of Sciences
University of Hannover
University of Bristol
University of Münster
GEOMAR Helmholtz Centre for Ocean Research Kiel
University of Tasmania
University of Tasmania
University of Tokyo
University of Southern California
University of Oxford
ETH Zurich
Chinese Academy of Sciences
University of Porto
Hebrew University of Jerusalem
Oak Ridge National Laboratory
National Health Research Institutes
Tohoku University
Gifu University
Oak Ridge National Laboratory
54gene
University of Salford
University of Pecs
University of Bergen
University of California, San Diego
Tilburg University