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Thermal Decomposition AND ACID/BASE ABSORPTION of MAGNESIUM CARBONATES. Rafael Snell- Feikema , Neil Mehta, and Dr. Thomas DeVore. Introduction.
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Thermal Decomposition AND ACID/BASE ABSORPTION of MAGNESIUM CARBONATES Rafael Snell-Feikema, Neil Mehta, and Dr. Thomas DeVore
Introduction • The ternary system MgCO3-Mg(OH)2-H2O encompasses a great many magnesium carbonate and magnesium hydrate minerals, most of which are naturally produced in caves ( W.B. White; Environmental Geology (1997) 30: 46-58 )
Introduction • Specifically, we are interested in: • Hydromagnesite: Mg5(CO3)4(OH)2-4H2O. • Nesquehonite: MgCO3-3H2O • Brucite: Mg(OH)2 ( W.B. White; Environmental Geology (1997) 30: 46-58 )
Applications • Thermal and chemical stability leads to widespread use in industrial and commercial applications including perfume retainers, fire retardants, rubber reenforcers, and antacids. • Of more immediate focus is a possible method of carbon sequestration through use of brucite. Here, nesquehonite and hydromagnesite are possible intermediates or end products† †V. Vágvölgyi; M. Hales; R.L. Frost; A. Locke; J. Kristóf; E. Horváth; J Therm Anal Calorim (2008) 94:523-528
Samples studied - hydromagnesite • Acros “MgCO3” • Fisher “MgCO3” • Synthesized Mg5(CO3)4(OH)2 † • Dissolved 0.01 moles magnesium sulfate in 50 mL of water. • Dissolved 0.01 moles sodium hydrogen carbonate in 50 mL of water. • Heated to boiling and mixed. • Vacuum filtered the precipitate. • Air dried for twenty-four hours. †Z. Zhang; Y. Zheng; Y. Ni; Z. Liu; J. Chen; X. Liang; J. Phys. Chem. B 2006, 110, 12969-12973
Samples studied - nesquehonite • While attempting to create MgCO3, we accidentally made a very good sample of nesquehonite • Used the same process as the one which produced hydromagnesite†, but changed the temperature via use of ice water – replicating the change in conditions that occurs in caves • Dissolved 0.01 moles magnesium sulfate in 50 mL of water. • Dissolved 0.01 moles sodium hydrogen carbonate in 50 mL of water. • Heated to boiling and mixed. • Vacuum filtered the precipitate. • Air dried for twenty-four hours. †Z. Zhang; Y. Zheng; Y. Ni; Z. Liu; J. Chen; X. Liang; J. Phys. Chem. B 2006, 110, 12969-12973
Samples studied - brucite • Fisher Mg(OH)2 • Actually competent commercial sample
Background information • Fourier Transform Infrared Spectroscopy (FTIR) • Shoot some light at some stuff • Said stuff does certain unique things in the way it absorbs light • Gives us a fingerprint of each piece of a sample
IRs †N. Koga; Y. Yamane; J Therm Anal Calorim (2008) 93:963-971 ‡J. Lanas; J.I. Alvarez; ThermochimicaActa(2004) 421:123-132
Experimental TGA • Analysis was done using a MettlerToledo TGA /SDTG 851e • N2 flow rates: purge = 150 ml/ min; protect = 50 ml/ min • Capped and uncapped 70 ml alumina cells
Experimental EGA • EGA-FTIR was done on a Thermo Nicolet 6700
IRs – Fisher decomposition Temperature (K) 425 575 625 675 725 925
Open cell mass loss • Step 1 matches in both cases and is fairly slight, low temperature – it’s surface drying • Accounting for this addition to the mass, we can approximate the other steps Mg5(CO3)4(OH)2-4H2O <=> Mg5(CO3)4(OH)2 +4H2O Mg5(CO3)4(OH)2 <=> 2Mg(CO3)+ 3MgO + 2CO2 + H2O (overlapping step #2) Mg(CO3) <=> MgO + CO2
Kinetics Theory • DTG data can be used to find activation energy via the Kissinger equation† : • Where β is the heating rate and T is the temperature at the maximum reaction rate • Graphing ln(β/T2) vs 1000/T gives -E/R as the slope in kJ/mol †X.W. Liu; L. Feng; H.R. Li; P. Zhang; P. Wang ; J Therm Anal Calorim (2012) 107:407-412
Kinetics - decarbonation †X.W. Liu; L. Feng; H.R. Li; P. Zhang; P. Wang ; J Therm Anal Calorim (2012) 107:407-412
Observations • MgCO3 (s) <=> MgO(s) + CO2 (g) • As the pressure of CO2 rises, it drives the equilibrium to the left, causing the apparent decomposition to occur at a higher temperature. • Amorphous MgCO3 turns to crystalline MgCO3 at 808 K, which then decomposes rapidly, giving the observed “new” transition. • Fisher and Acros vary due to differing apparent densities • Fisher and our synthesized sample vary due to differing morphologies† †D. Bhattacharjya; T. Selvamani; I. Mukhopadhyay; J Therm Anal Calorim (2012) 107:439-445; “Thermal decomposition of hydromagnesite: Effect of morphology on the kinetic parameters”
Introduction, part II • Aside from carbon sequestration, magnesium minerals (again due to their high thermal and chemical stability) can be used to neutralize harmful VOCs such as industrial gasses, paint fumes, and agricultural waste • As such, it is useful to study absorption of an acid onto essential forms of the ternary system as well as desorption afterwards • Chemicals studied: • Hydromagnesite(Mg5(CO3)4(OH)2-4H2O) • Nesquehonite (MgCO3-3H2O) • Brucite (Mg(OH)2) • Magnesia (MgO)
Desorption, Hydromagnesite-HOAC • Ran out of time • Desorption products can be assumed through the other compounds and through what we already know • INSERT PRODUCTS
Conclusions • MgCO3 is a conspiracy made up by the chemistry illuminati • Ternary systems found in caves are kinda complex • Carbon sequestration on to Mg(OH)2 with the possible product of nesquehonite and the possible intermediate of hydromagnesite is actually very practical • Acetic acid absorbs to varying degrees on to each compound (although fairly easily on all of them) • RANK HERE
Acknowledgements • Dr. Reisner (X-ray diffraction lab) Research Corporation Departmental Development Grant #7957 NSF: MRI 0340245 (TGA-MS) NSF: DMR 0315345 (XRD) NSF: REU - 1062629