Robert C Burruss (Former Employee)
Science and Products
Filter Total Items: 69
Measurement of clathrate hydrates via Raman spectroscopy Measurement of clathrate hydrates via Raman spectroscopy
Raman spectra of clathrate hydrate guest molecules are presented for three known structures ( I ( sI), II ( sII), and H ( sH)) in the following systems: CH4 ( sI), CO2 ( sI), C3H8 ( sII), CH4 + CO2 ( sI), CD4 + C3H8 ( sII), CH4 + N2 ( sI), CH4 + THF-d8 ( sII), and CH4 + C7D14 ( sH). Relative occupancy of CH4 in the large and small cavities of sI were determined by deconvoluting the ν1...
Authors
A. K. Sum, R.C. Burruss, E.D. Sloan
A perspective on the Louisiana wetland loss and coastal erosion problem A perspective on the Louisiana wetland loss and coastal erosion problem
[No abstract available]
Authors
S.J. Williams, G.W. Stone, A.E. Burruss
A composite phase diagram of structure H hydrates using Schreinemakers' geometric approach A composite phase diagram of structure H hydrates using Schreinemakers' geometric approach
A composite phase diagram is presented for Structure H (sH) clathrate hydrates, In this work, we derived the reactions occurring among the various phases along each four-phase (Ice/Liquid water, liquid hydrocarbon, vapor, and hydrate) equilibrium line. A powerful method (though seldom used in chemical engineering) for multicomponent equilibria developed by Schreinemakers is applied to...
Authors
A. P. Mehta, T. Y. Makogon, R.C. Burruss, R. F. Wendlandt, E. D. Sloan
Constraints on the thermal history of Taylorsville Basin, Virginia, U.S.A., from fluid-inclusion and fission-track analyses: Implications for subsurface geomicrobiology experiments Constraints on the thermal history of Taylorsville Basin, Virginia, U.S.A., from fluid-inclusion and fission-track analyses: Implications for subsurface geomicrobiology experiments
Microbial populations have been found at the depth of 2621-2804 m in a borehole near the center of Triassic Taylorsville Basin, Virginia. To constrain possible scenarios for long-term survival in or introduction of these microbial populations to the deep subsurface, we attempted to refine models of thermal and burial history of the basin by analyzing aqueous and gaseous fluid inclusions...
Authors
H.-Y. Tseng, T.C. Onstott, R.C. Burruss, D. S. Miller
Nucleation, growth, and disassociation of methane gas hydrate microscope observations in a natural fluid inclusion in fluorite Nucleation, growth, and disassociation of methane gas hydrate microscope observations in a natural fluid inclusion in fluorite
No abstract available.
Authors
R.C. Burruss, J. Reynolds
Gas hydrate reservoir characteristics and economics Gas hydrate reservoir characteristics and economics
No abstract available.
Authors
R.C. Burruss, T. S. Collett
Science and Products
Filter Total Items: 69
Measurement of clathrate hydrates via Raman spectroscopy Measurement of clathrate hydrates via Raman spectroscopy
Raman spectra of clathrate hydrate guest molecules are presented for three known structures ( I ( sI), II ( sII), and H ( sH)) in the following systems: CH4 ( sI), CO2 ( sI), C3H8 ( sII), CH4 + CO2 ( sI), CD4 + C3H8 ( sII), CH4 + N2 ( sI), CH4 + THF-d8 ( sII), and CH4 + C7D14 ( sH). Relative occupancy of CH4 in the large and small cavities of sI were determined by deconvoluting the ν1...
Authors
A. K. Sum, R.C. Burruss, E.D. Sloan
A perspective on the Louisiana wetland loss and coastal erosion problem A perspective on the Louisiana wetland loss and coastal erosion problem
[No abstract available]
Authors
S.J. Williams, G.W. Stone, A.E. Burruss
A composite phase diagram of structure H hydrates using Schreinemakers' geometric approach A composite phase diagram of structure H hydrates using Schreinemakers' geometric approach
A composite phase diagram is presented for Structure H (sH) clathrate hydrates, In this work, we derived the reactions occurring among the various phases along each four-phase (Ice/Liquid water, liquid hydrocarbon, vapor, and hydrate) equilibrium line. A powerful method (though seldom used in chemical engineering) for multicomponent equilibria developed by Schreinemakers is applied to...
Authors
A. P. Mehta, T. Y. Makogon, R.C. Burruss, R. F. Wendlandt, E. D. Sloan
Constraints on the thermal history of Taylorsville Basin, Virginia, U.S.A., from fluid-inclusion and fission-track analyses: Implications for subsurface geomicrobiology experiments Constraints on the thermal history of Taylorsville Basin, Virginia, U.S.A., from fluid-inclusion and fission-track analyses: Implications for subsurface geomicrobiology experiments
Microbial populations have been found at the depth of 2621-2804 m in a borehole near the center of Triassic Taylorsville Basin, Virginia. To constrain possible scenarios for long-term survival in or introduction of these microbial populations to the deep subsurface, we attempted to refine models of thermal and burial history of the basin by analyzing aqueous and gaseous fluid inclusions...
Authors
H.-Y. Tseng, T.C. Onstott, R.C. Burruss, D. S. Miller
Nucleation, growth, and disassociation of methane gas hydrate microscope observations in a natural fluid inclusion in fluorite Nucleation, growth, and disassociation of methane gas hydrate microscope observations in a natural fluid inclusion in fluorite
No abstract available.
Authors
R.C. Burruss, J. Reynolds
Gas hydrate reservoir characteristics and economics Gas hydrate reservoir characteristics and economics
No abstract available.
Authors
R.C. Burruss, T. S. Collett