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Maximum gas hydrate saturation was observed at the local gas hydrate reflector within gas hydrate stability zone where electrical resistivity logs also shows ~20%% gas hydrate saturation in few intervals from anisotropic modeling approach (Fig. 7b).
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In some cases, the maximum temperature exceeded that of gas hydrate stability, which could have led to hydrate dissociation.
Samples of gas hydrates obtained at a maximum gas flow rate during the deposition contained up to 15 mass % of methane, 12 mass % of ethane, 13 mass % of propane, and 23 mass % of carbon dioxide.
The maximum limit for dissolved oxygen in monoethylene glycol (MEG) used as gas hydrate inhibitor is usually set to 10 20 ppb.
Seabed photos show the presence of gas hydrate outcrops and benthic communities in the vicinity of maximum seafloor backscatter intensities and many of the morphological features.
The gas hydrate saturation estimated from electrical resistivity log and core data shows maximum 20%% pore spaces saturated with gas hydrate from anisotropic modeling, which is comparable to gas hydrate saturation along seismic profile estimated from inverted velocity constrained by logs.
A novel three-dimensional natural gas hydrate physical simulation device, with a capacity of 0.196 m3 and maximum operating pressure of 32 MPa, was designed and developed to study the accumulation and exploitation of hydrate-bearing sediment in the natural environment.
Alternatively, gas hydrate saturations computed for these sites using effective medium models are found maximum up to 16% and 22%.
Gas hydrate can be modeled either as part of the pore fluid (gas hydrate in-pore) or as part of the load-bearing sediment matrix (gas hydrate in-frame) (Helgerud et al. 1999).
Spatial distribution of gas hydrate saturation along 2D seismic profile from inverted velocity observed during acoustic impedance inversion varies maximum up to 10 15 % of the pore volume (Fig. 11).
The difference of maximum temperatures is about 8 K, that is, the equilibrium curve of H2+ tetra-n-butyl ammonium bromide mixed gas hydrate shifts to the high-temperature side from that of H2+ tetrahydrofuran mixed gas hydrate.
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