Stable Phase Diagram of Quaternary Water–Salt System Li+, Na+, Cs+//SO42––H2O at T = 298.2 K

2019 ◽  
Vol 64 (3) ◽  
pp. 1222-1227 ◽  
Author(s):  
Jingfeng Liu ◽  
Jingjun Pan ◽  
Ying Zeng ◽  
Xia Liu ◽  
Xudong Yu ◽  
...  
Keyword(s):  
Phase Diagram ◽  
Salt System ◽  
Stable Phase ◽  
Water Salt ◽  
Stable Phase Diagram

Stable-Phase Diagram of the Quaternary Water–Salt System K+, Rb+, Cs+//SO42––H2O at T = 323.2 K

2022 ◽  
Author(s):  
Ying Zeng ◽  
Ke Wang ◽  
Hanlin Tong ◽  
Xinxin Lv ◽  
Yuhua He ◽  
...  
Keyword(s):  
Phase Diagram ◽  
Salt System ◽  
Stable Phase ◽  
Water Salt ◽  
Stable Phase Diagram

Stable Phase Diagram of the Quaternary Water–Salt System K+, Rb+, Cs+//SO42––H2O at T = 298.2 K

2020 ◽  
Vol 65 (10) ◽  
pp. 4751-4761
Author(s):  
Hanlin Tong ◽  
Ying Zeng ◽  
Xudong Yu ◽  
Wenzhang Zuo ◽  
Wannian Ying ◽  
...  
Keyword(s):  
Phase Diagram ◽  
Salt System ◽  
Stable Phase ◽  
Water Salt ◽  
Stable Phase Diagram

Stable Phase Diagram of the Quaternary Water–Salt System Li+, Na+, Rb+//SO42–·H2O at 298.2 and 323.2 K (P = 94.5 kPa)

2021 ◽  
Author(s):  
Wannian Ying ◽  
Ying Zeng ◽  
Xinxin Lv ◽  
Hanlin Tong ◽  
Wenzhang Zuo ◽  
...  
Keyword(s):  
Phase Diagram ◽  
Salt System ◽  
Stable Phase ◽  
Water Salt ◽  
Stable Phase Diagram

Stable Phase Diagram of the Quaternary Water–Salt System Li+, Na+, Mg2+//SO42––H2O at T = 323 K

2019 ◽  
Vol 65 (1) ◽  
pp. 133-139
Author(s):  
Wenzhang Zuo ◽  
Ying Zeng ◽  
Xudong Yu ◽  
Wannian Ying ◽  
Hanlin Tong ◽  
...  
Keyword(s):  
Phase Diagram ◽  
Salt System ◽  
Stable Phase ◽  
Water Salt ◽  
Stable Phase Diagram

scholarly journals Solubility in the Na,Ca||SO4,HCO3-H2O system at 25 °C

2019 ◽  
Vol 6 (4) ◽  
pp. 130-137
Author(s):  
L. Soliev ◽  
M. T. Jumaev ◽  
A. M. Varkaeva ◽  
Kh. R. Makhmadov ◽  
G. Sinoi
Keyword(s):  
Phase Diagram ◽  
Phase Equilibria ◽  
Water Solubility ◽  
Liquid Waste ◽  
Salt System ◽  
Aluminum Production ◽  
Reliability Of Results ◽  
Reference Information ◽  
Water Salt ◽  
Scientific Base

Water solubility at 25 °C was studied in the four-component water-salt system comprised of sodium and calcium sulfates and hydrocarbonates in order to determine the concentration parameters of solution and crystallization of the constituent salts and to experimentally verify the phase equilibria in the geometric images of the system predicted previously by the translation method. The prediction of possible phase equilibria in geometric images of the system, followed by plotting its phase diagram, appreciably decreases the time and material costs of experimentation and improves the reliability of results. Our results can serve both as reference information and as a scientific base for optimizing the parameters of natural and artificial processes, in particular, the recycling of salt from liquid waste of aluminum production facilities.

scholarly journals Mutual Solubility of Pyridine Base-Water-Salt System

1958 ◽  
Vol 78 (8) ◽  
pp. 837-841 ◽  
Author(s):  
Sozaburo Arakawa ◽  
Taro Kawaguchi ◽  
Hiromasa Kato
Keyword(s):  
Mutual Solubility ◽  
Salt System ◽  
Pyridine Base ◽  
Water Salt

The water-salt system of Rare-Earth Element

2015 ◽  
pp. 765-767
Author(s):  
Larisa Grigorieva ◽  
Angela Orlova
Keyword(s):  
Rare Earth ◽  
Rare Earth Element ◽  
Earth Element ◽  
Salt System ◽  
Water Salt

Phase diagram of the LiNO3-NaNO3-NaCl-Sr(NO3)2 salt system

2015 ◽  
Vol 89 (4) ◽  
pp. 634-638
Author(s):  
A. I. Rasulov ◽  
A. M. Gasanaliev ◽  
A. K. Mamedova ◽  
B. Yu. Gamataeva
Keyword(s):  
Phase Diagram ◽  
Salt System

Hydrochemistry Research of Intercrystalline with Pore Brine and Pre-3D Modelling of Heibeiwadi Brine Deposit

2018 ◽  
Vol 783 ◽  
pp. 170-175
Author(s):  
Huang Song
Keyword(s):  
Phase Diagram ◽  
Qaidam Basin ◽  
Central Area ◽  
Research Area ◽  
3D Modelling ◽  
Salting Out ◽  
Characteristics Analysis ◽  
Water Salt ◽  
The Stability ◽  
Brine Layer

Intercrystalline and pore brine develop extensively in the Heibewadi research area which is located at south foot of Altun mountain of Qaidam basin. In central area, intercrystalline brine’s depths range from 5m to 90m. In northwest, south area and central deeper area, pore brine develops under intercrystalline brine layer. The 2 types of aquifers have strong yield property, TDS is 200-350g/l with average of 276g/l. Main salt compound can be mined out economically. According to analysis result of intercrystalline brine, TDS, Cl-, Na+, K+, Mg2+, Li+ irons’ grades are very steady. That mean intercrystalline brine exist in the water-salt system under balance. Only the stability of Ca2+ and SO42- are slightly poor. According the Kurtosis characteristics analysis, Ca2+, SO42- are no-normal positively platykurtic distribution, K+, Cl- and PH are normal positively platykurtic distribution. These 2 groups fall into a sub-class. And the combined with normal negatively platykurtic distribution-TDS and fall into platykurtic distribution group. Mg2+, Li+ are normal positively peaked distribution; Na+ is normal negatively peaked distribution. They all belong to peaked distribution group. According to Na+, K+, Mg2+//Cl-H2O quarternary phase diagram and Na+, K+, Mg2+//Cl-SO42-H2O pentabasic phase diagram, the chlorite and magnesium sulfate subtype have different hydro chemical characteristics and salting-in and salting-out rules.

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