New International Skeleton Tables for the Thermodynamic Properties of Ordinary Water Substance

Sato, Haruo; Uematsu, M.; Watanabe, Koichi; Saúl, Andrés; Wagner, Wolfgang

doi:10.1063/1.555812

Cited by 71 publications

(39 citation statements)

References 0 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…which is accurate to 4% for 200-290 • C; and to 10% in the range 100-300 • C. More accurate estimates are given in Steam Tables (Sato et al 1988). The density of water, from 100 to 300 • C, is approximately (Elder 1981) ρ = 10 3 1 − 3.3 × 10 −6 T 2 kg m −3…”

Section: Large Vl/dmentioning

confidence: 84%

A Mathematical Model of Rainfall-Controlled Geothermal Fields

Weir¹

2008

Transp Porous Med

View full text Add to dashboard Cite

A mathematical model is developed, using a hydrothermal spring concept, for those geothermal fields which are controlled by infiltrated rainfall. Two limiting regimes are identified: when rainfall infiltration is so great that isothermal conditions exist in most of the downflow regions; and when rainfall infiltration is so small that a constant geophysical temperature gradient results. In either case, the ratio of downflow to upflow areas, and the energy output per unit area, are fixed, but the typical size of a geothermal field remains indeterminate. The additional assumption that the horizontal length scale of the downflow region is determined by the depth of the main heat sources, fixes the characteristic mass flows, energy outputs, and the number of geothermal fields in a geothermal region. These model predictions are compared with field data, and are shown to be in approximate agreement with geothermal field characteristics in the Taupo Volcanic Zone of New Zealand. The temperature dependence of water viscosity uses a correlation of Wooding (J. Fluid Mech. 2:273-285, 1957), while the temperature dependence of water density, enthalpy and boiling point use correlations from Elder (Geothermal Systems 508, 1981).

show abstract

Section: Large Vl/dmentioning

confidence: 84%

A Mathematical Model of Rainfall-Controlled Geothermal Fields

Weir¹

2008

Transp Porous Med

View full text Add to dashboard Cite

show abstract

“…The values of V c were taken from Sato et al [28], Goodwin [29], Steele et al [30] and Poling et al [31] for water, methanol, n-butyl acetate and n-pentyl acetate, respectively. The molar volume at 303.15 K were calculated from the density given in a previous work [19].…”

Section: Surface Tensionmentioning

confidence: 99%

Surface and interfacial tensions of the systems water + n-butyl acetate + methanol and water + n-pentyl acetate + methanol at 303.15 K

Santos

Ferreira

Fonseca

2003

Fluid Phase Equilibria

View full text Add to dashboard Cite

Surface and interfacial tensions of the systems water + n-butyl acetate + methanol and water + n-pentyl acetate + methanol at 303. AbstractThe surface tension in the homogeneous domain of the ternary liquid mixtures water + n-butyl acetate + methanol and water + n-pentyl acetate + methanol as well as of the constituent binaries has been measured at 303.15 K and atmospheric pressure. The respective excess surface tension was correlated as a function of the composition using empirical and thermodynamic-based relations. The liquid interfacial tension was measured in the liquid-liquid equilibrium range at the same conditions of temperature and pressure.A new equation is proposed to correlate the excess surface tension of binary mixtures. This equation can be obtained from the Butler equation and correlates well the excess surface tension data.The prediction of the surface tension of the binary and ternary systems has been made using the Sprow and Prausnitz model. The Fu et al. and Li et al. models were also applied to predict that property in the ternary systems.The liquid interfacial tension of the ternary systems was correlated and predicted using the relations proposed by Li and Fu and Fu et al., respectively, with satisfactory results.

show abstract

“…A typical geothermal gradient in Japan is approximately 3°C/100 m [6], suggesting the temperature of the groundwater at the depth of 500 m to be 35°C to 45°C. The speciation of metal ions and their behaviour in solutions could be affected by their thermal conditions, since the properties of water such as density, dielectric constant, ion product, viscosity, etc., vary remarkably with temperature [7][8][9][10]. Hence, stability constants at elevated temperature are needed to accomplish more reliable prediction of actinides migration behaviour.…”

Section: Introductionmentioning

confidence: 99%