![]() ![]() Pitzer parameter, unlike-charged interactions (kg 2/mol 2) Cl:įaraday’s constant (96,485.3329 A.s/mol) F 1, F 2, F 3 Parameters related to the Wang model for BPE calculations C ![]() Pitzer binary interaction parameter (kg 2/mol) b, s, n Pitzer parameter, second virial coefficient (kg/mol) B ij′: Modified Debye–Hückel parameter (kg 1/2/mol 1/2) A, BĬonstants used in McCleskey multi-component model for electrical conductivity B ij, B ϕ ij Since the thermal conductivity has no multi-component model, a novel and straightforward model is proposed with excellent accuracy. Besides, guidelines for choosing some correlations are also discussed. The correlations are summarized in tabular forms and assessed based on their accuracy against available experimental data. The properties are comprehensive to include all saline water types, i.e., brackish water, seawater, high saline water from basins, lakes, produced water from oil and gas hydraulic fracturing, and so on. Since the thermodynamic properties are reviewed in part I of the paper, this part (# II) focuses on the thermophysical properties involving viscosity, surface tension, electrical conductivity, thermal conductivity, osmotic coefficient, activity coefficient, and thermal expansivity. The key parameters that influence the properties are considered, such as multi-component composition, high salinity, temperature, and pressure. Particularly striking is the reproducibility and self-consistency of the results obtained.This paper reviews the thermophysical properties of saline water correlations and data. Although the present instrument is severely limited in range, the feasibility of measurements at elevated temperatures and pressures by means of the oscillation-type viscometer is clearly demonstrated. The results show good agreement with previously published data and the deviations of experimental points from smoothed curves do not exceed 0.05 per cent. The maximum change in viscosity, at any given temperature over the pressure range covered is 5 per cent. The viscosity of water is shown to have a negative pressure coefficient below 35 C and a positive coefficient above that temperature. The results for compressed water, obtained with the aid of an oscillating sphere, represent absolute measurements, and cover a range from 3 to 340 atm and from 20 to 186 C. The measurements were carried out by means of an oscillating-body-type viscometer in order to develop an alternative method of measurement to the usually employed capillary viscometer, and also to provide an independent check on published data. The paper reports the results of an investigation of the viscosity of steam and compressed water. Journal of Verification, Validation and Uncertainty Quantification.Journal of Thermal Science and Engineering Applications.Journal of Offshore Mechanics and Arctic Engineering.Journal of Nuclear Engineering and Radiation Science.Journal of Nondestructive Evaluation, Diagnostics and Prognostics of Engineering Systems.Journal of Nanotechnology in Engineering and Medicine.Journal of Micro and Nano-Manufacturing.Journal of Manufacturing Science and Engineering.Journal of Engineering Materials and Technology.Journal of Engineering for Sustainable Buildings and Cities.Journal of Engineering for Gas Turbines and Power.Journal of Engineering and Science in Medical Diagnostics and Therapy.Journal of Electrochemical Energy Conversion and Storage.Journal of Dynamic Systems, Measurement, and Control.Journal of Computing and Information Science in Engineering.Journal of Computational and Nonlinear Dynamics.Journal of Autonomous Vehicles and Systems.ASME Letters in Dynamic Systems and Control.ASCE-ASME Journal of Risk and Uncertainty in Engineering Systems, Part B: Mechanical Engineering.Mechanical Engineering Magazine Select Articles. ![]()
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