Isothermal measurement of heats of hydration in zeolites by simultaneous thermogravimetry and differential scanning calorimetry

被引:11
作者
Neuhoff, Philip S. [1 ]
Wang, Jie [1 ]
机构
[1] Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA
关键词
analcime; calorimetry; chabazite; enthalpy; hydration; natrolite; thermal analysis; thermodynamics; zeolite;
D O I
10.1346/CCMN.2007.0550302
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
A calorimetric method for determining isothermal partial and integral heats of hydration reactions (Delta(H) over bar (R,T,P) and Delta(H) over tilde (R,T,P), respectively) in zeolites and other mineral hydrates is presented. The method involves immersing a dehydrated sample in a humid gas stream under isothermal conditions within a thermal analysis device that records simultaneous differential scanning calorimetric (DSC) and thermogravimetric analysis (TGA) signals. Monitoring changes in sample mass (corresponding to extent of reaction progress) coincident with a quantitative measurement of heat flow allows for direct detection of Delta(H) over bar (R,T,P) as a function of the extent of hydration, which can be integrated to determine Delta(H) over tilde (R,T,P). In addition, it eliminates uncertainties associated with imprecise knowledge of the starting and final states of a sample during hydration. Measurement under isothermal conditions removes uncertainties associated with heat capacity effects that complicate interpretations of DSC measurements of dehydration heats conducted under traditional scanning temperature conditions. Example experiments on the zeolites natrolite, analcime and chabazite are used to illustrate strategies for quantifying Delta(H) over tilde (R,T,P) and Delta(H) over tilde (R,T,P) and minimizing errors associated with baseline uncertainties. Results from this method agree well with previously published values determined by other calorimetric techniques and regression of phase equilibrium data. In the case of chabazite, the results allowed detailed measurements of the variation in Delta(H) over bar (R,T,P) for energetically different water types encountered progressively as the sample absorbed water. This technique complements and in many cases improves the quality of thermodynamic data obtained through phase equilibrium observations and other calorimetric techniques.
引用
收藏
页码:239 / 252
页数:14
相关论文
共 65 条
[1]   POSITION OF CATIONS AND WATER-MOLECULES IN HYDRATED CHABAZITE - NATURAL AND NA-EXCHANGED, CA-EXCHANGED, SR-EXCHANGED AND K-EXCHANGED CHABAZITES [J].
ALBERTI, A ;
GALLI, E ;
VEZZALINI, G ;
PASSAGLIA, E ;
ZANAZZI, PF .
ZEOLITES, 1982, 2 (04) :303-309
[2]  
ALBERTI A, 1983, NEUES JB MINER MONAT, P135
[3]   A PARTIALLY DISORDERED NATROLITE - RELATIONSHIPS BETWEEN CELL PARAMETERS AND SI-AL DISTRIBUTION [J].
ALBERTI, A ;
VEZZALINI, G .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1981, 37 (APR) :781-788
[4]  
[Anonymous], 1995, US GEOLOGICAL SURVEY
[5]  
BALGORD WD, 1973, ADV CHEM SER, P189
[6]  
BARANY R, 1962, US BUREAU MINES REPO
[7]  
BARRER RM, 1971, ADV CHEM SER, V102, P105
[8]  
Baur WH, 1996, NEUES JB MINER MONAT, P171
[9]  
Bish DL, 2003, AM MINERAL, V88, P1889
[10]   Stability of hydrous minerals on the martian surface [J].
Bish, DL ;
Carey, JW ;
Vaniman, DT ;
Chipera, SJ .
ICARUS, 2003, 164 (01) :96-103