Influence of polyacrylamide on the precipitation of gypsum in sodium chloride solutions

Some natural processes can seal porous rocks, cracks, and joints in soil formations. The precipitation of sparingly soluble calcium salts can either stop the flow of brines into mines or isolate particularly contaminated areas. Gypsum (CaSO 4 ‧2H 2 O), which has a low solubility in water (2.6 g/L at...

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Published inEnvironmental earth sciences Vol. 82; no. 23; p. 565
Main Authors Kistanova, Natalya S., Chashchukhina, Anna D., Kudryashova, Olga S., Khayrulina, Elena A.
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer Berlin Heidelberg 01.12.2023
Springer Nature B.V
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Summary:Some natural processes can seal porous rocks, cracks, and joints in soil formations. The precipitation of sparingly soluble calcium salts can either stop the flow of brines into mines or isolate particularly contaminated areas. Gypsum (CaSO 4 ‧2H 2 O), which has a low solubility in water (2.6 g/L at 25 °C), creates a long-lasting insulating layer. Natural mineral formation happens very slowly, and only a small amount of the matter gets through the porous medium of soil and rocks. Supersaturated solutions of sparingly soluble calcium salts with crystallisation inhibitors are used to create artificial geochemical barriers that mimic natural processes. This research looks into the effects of PAM and NaCl on the precipitation of calcium sulphate dihydrate from supersaturated solutions. The efficiency of PAM inhibition was confirmed by studying the processes of spontaneous salt crystallisation from 0.15 mol/L CaSO 4 solutions at 25 °C. The presence of both PAM and NaCl in the solution had a synergistic effect. The induction period of gypsum crystallisation in the presence of NaCl required 33 h at a 500 ppm PAM. XRD results proved that the salt precipitated as CaSO 4 ‧2H 2 O. The morphology of gypsum crystals changed in the presence of a polymer in supersaturated solutions.
ISSN:1866-6280
1866-6299
DOI:10.1007/s12665-023-11260-z