access icon free Study of the influence between magnesium ions and calcium ions on the morphology and size of coprecipitation in microemulsion

A series of inverse-microemulsion quasi-ternary system phase diagrams of CTAB + n-butanol + n-hexane + brine (MgCl2/CaCl2) is systematically drawn by adjusting the ratio of MgCl2 and CaCl2. On this basis, a microemulsion has been prepared with five different molar ratios of magnesium ions to calcium ions, and a calcium carbonate and magnesium carbonate coprecipitation product is obtained by reaction with an equimolar amount of sodium carbonate. The samples were characterised by scanning electron microscopy (SEM), a Fourier transform infrared (FTIR) spectrometer and X-ray diffraction (XRD). The SEM photographs indicated that when the content of Ca2+ was higher, some large fusiform aggregates of coprecipitation particles were formed in solution, but with the content of Mg2+ increased gradually, they eventually formed small and uniform sphere particles. The measurement results of XRD and FTIR indicated that the crystal structures of calcium carbonate in coprecipitation changed gradually from vaterite into aragonite and finally turned into being amorphous with the increasing of the proportion of magnesium ions.

Inspec keywords: solid-state phase transformations; precipitation (physical chemistry); infrared spectra; Fourier transform spectra; phase diagrams; crystal structure; organic compounds; magnesium compounds; scanning electron microscopy; X-ray diffraction; aggregates (materials); amorphisation; microemulsions; calcium compounds

Other keywords: inverse-microemulsion quasiternary system phase diagrams; MgCO3; CaCO3; coprecipitation; aragonite; calcium carbonate; SEM; molar ratios; FTIR; CTAB-n-butanol-n-hexane-brine system; crystal structures; X-ray diffraction; vaterite; magnesium carbonate; scanning electron microscopy; magnesium ions; Fourier transform infrared spectrometer; sodium carbonate; XRD; fusiform aggregates; calcium ions

Subjects: Emulsions and suspensions; Crystal structure of specific inorganic compounds; Infrared and Raman spectra in inorganic crystals; Constant-composition solid-solid phase transformations: polymorphic, massive, and order-disorder; Solid-solid transitions; Phase diagrams of other materials

References

    1. 1)
    2. 2)
    3. 3)
      • 21. Folk, R.L.: ‘The natural of history of crystalline calcium carbonate; effect of magnesium content and salinity’, J. Sedimentol. Pet., 1974, 44, pp. 4053.
    4. 4)
    5. 5)
    6. 6)
    7. 7)
    8. 8)
    9. 9)
    10. 10)
    11. 11)
      • 1. Lowenstam, H.A.: ‘Spicular morphology and mineralogy in some Pyuridae (Ascidiacea)’, Bull. Mar. Sci., 1989, 45, pp. 243252.
    12. 12)
      • 31. Yang, S.H., Wu, G.H.: ‘Model of ionic hydrate and calculation of hydration energy’, J. Inorg. Chem., 1988, 4, pp. 124129.
    13. 13)
    14. 14)
    15. 15)
    16. 16)
    17. 17)
    18. 18)
    19. 19)
    20. 20)
    21. 21)
    22. 22)
      • 2. Zenger, D.H.: ‘Sedimentary carbonate minerals’ (Springer, Berlin,Germany, 1973).
    23. 23)
    24. 24)
    25. 25)
    26. 26)
    27. 27)
    28. 28)
    29. 29)
    30. 30)
      • 22. Lahann, R.W.: ‘A chemical model for calcite crystal growth and morphology control’, J. Sedimentol. Pet., 1978, 48, pp. 337347.
    31. 31)
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