2020
DOI: 10.1007/s13202-020-00998-y
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Thermodynamic modeling and correlations of CH4, C2H6, CO2, H2S, and N2 hydrates with cage occupancies

Abstract: The present work focuses on developing a framework for accurate prediction of thermodynamic conditions for single-component hydrates, namely CH4, CO2, N2, H2S, and C2H6 (coded in MATLAB). For this purpose, an exhaustive approach is adopted by incorporating eight different equations of states, namely Peng–Robinson, van der Waals, Soave–Redlich–Kwong, Virial, Redlich–Kwong, Tsai-Teja, Patel, and Esmaeilzadeh–Roshanfekr, with the well-known van der Waals–Platteeuw model. Overall, for I–H–V phase region, the Viria… Show more

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Cited by 6 publications
(4 citation statements)
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“…It also allocates materials efficiently and reasonably in the military and urban management. In large-scale urban construction, the planning of roads, sports venues, parking lots, green spaces, etc., enables the rational distribution of facilities and the efficient use of resources [14,15].…”
Section: Ggis Technology Geographic Information Systemmentioning
confidence: 99%
“…It also allocates materials efficiently and reasonably in the military and urban management. In large-scale urban construction, the planning of roads, sports venues, parking lots, green spaces, etc., enables the rational distribution of facilities and the efficient use of resources [14,15].…”
Section: Ggis Technology Geographic Information Systemmentioning
confidence: 99%
“…[12] presents the formulae for estimating bubble-point pressure and the formation volume factor of crude oil with four basic oil properties: temperature, gas solubility, oil API gravity and gas-specific gravity as predictors. In [13], the SR methodology was used to develop a correlation to predict thermodynamic conditions for hydrates' formation. In [14], explicit approximations of widely used hydraulics, the Colebrook equation for flow friction obtained with SR method are considered.…”
Section: Methods and Modelsmentioning
confidence: 99%
“…The basin is distributed in an area of 5.8 × 10 5 km 2 and the main sources of sediments in the Arabian Sea are the Indus River, which discharges in the northernmost part of the Arabian Sea and the Tapti and Narmada Rivers and ends in the Gulf of Combay. The Kerala-Konkan basin contains 109,000 km 3 Cenozoic sediments [40]. The sediments on the west coast are primarily globigerina clay [39].…”
Section: Kerala-konkan Basinmentioning
confidence: 99%
“…Gas hydrates are formed when the guest molecules of suitable size and shape are captured through van der Waals forces in the well-defined cages of host molecules [1]. The molecules of water and gas chemically interact to construct an ice-like crystalline structure [2], which is stable at an absolute pressure and temperature range [3]. The bottom of the stability area of hydrate structures is designated with the Bottom-Simulating Reflectors (BSR), which are parallel to the seafloor at a sub-bottom depth of a specific hundred meters [4,5].…”
Section: Introductionmentioning
confidence: 99%