Heat capacity and thermodynamic functions of partially dehydrated sodium and zinc zeolite A (LTA)
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Matthew S. Dickson
, Jason J. Calvin
Abstract
Zeolite A (LTA) is an industrially important zeolite that exhibits sorption-induced framework flexibility, the thermodynamics of which are poorly understood. In this work, we report heat capacity measurements on zinc and sodium zeolite A from 1.8 to 300 K and compare the heat capacity of water in sodium zeolite A with that of water in other zeolites. The heat capacity of zeolitic water varies significantly depending on the hydration level and identity of the host zeolite, and more tightly bound water exhibits strong inflections in its heat capacity curve. This suggests a combination of efects, including diferences in water-framework binding strength and hydration-dependent flexibility transitions. We also report fits of the heat capacity data using theoretical functions, and we report values for
Funding statement: This work was financially supported by a grant from the U.S. Department of Energy under grant DE-SC0016446. Sample synthesis was supported by the U.S. Department of Energy, Office of Basic Energy Sciences, under grant DE-FG02-97ER14749.
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Articles in the same Issue
- Highlights and Breakthroughs
- Crustal melting: Deep, hot, and salty
- MSA Presidential Address
- Petrogenetic and tectonic interpretation of strongly peraluminous granitic rocks and their significance in the archean rock record
- Partial melting and P-T evolution of eclogite-facies metapelitic migmatites from the Egere terrane (Central Hoggar, South Algeria)
- High-pressure, halogen-bearing melt preserved in ultrahigh-temperature felsic granulites of the Central Maine Terrane, Connecticut (U.S.A.)
- Targeting mixtures of jarosite and clay minerals for Mars exploration
- Zirconolite from Larvik Plutonic Complex, Norway, its relationship to stefanweissite and nöggerathite, and contribution to the improvement of zirconolite end-member systematics
- Nanomineralogy of hydrothermal magnetite from Acropolis, South Australia: Genetic implications for iron-oxide copper gold mineralization
- Effect of magnesium on monohydrocalcite formation and unit-cell parameters
- Formation pathway of norsethite dominated by solution chemistry under ambient conditions
- A model for the kinetics of high-temperature reactions between polydisperse volcanic ash and SO2 gas
- Redox control and measurement in low-temperature (<450 °C) hydrothermal experiments
- Heat capacity and thermodynamic functions of partially dehydrated sodium and zinc zeolite A (LTA)
- P-V-T measurements of Fe3C to 117 GPa and 2100 K: Implications for stability of Fe3C phase at core conditions
- New Mineral Names
- Erratum
- Book Review