Me. Bottcher et Pl. Gehlken, DEHYDRATION OF NATURAL GAYLUSSITE (NA2CA(CO3)(2)CENTER-DOT-5H(2)O) AND PIRSSONITE (NA2CA(CO3)(2)CENTER-DOT-2H(2)O) AS ILLUSTRATED BY FTIR SPECTROSCOPY, Neues Jahrbuch fur Mineralogie Monatshefte, (2), 1996, pp. 73-91
The FTIR spectra of natural gaylussite (Na2Ca(CO3)(2) . 5H(2)O) and pi
rssonite (Na2Ca(CO3)(2) . 2H(2)O) are reported between 400 and 4000 cm
(-1), and the effect of heating up to 500 degrees C on the mid-infrare
d spectra of quenched reaction products is investigated. Upon heating,
the hydrated carbonates lose their crystallisation water and transfor
m directly to Na2Ca(CO3)(2). The mid-infrared spectrum of Na2Ca(CO3)(2
) is reported for the first time and the absorption bands are assigned
to specific vibrational modes. Under the chosen conditions, dehydrati
on temperatures are between 60 degrees and 90 degrees C for gaylussite
, and between 110 degrees and 200 degrees C for pirssonite. Gaylussite
and pirssonite are heated up to 360 degrees C directly or as prepared
KBr pellets. Depending on the experimental conditions chosen, differe
nces in the FTIR spectra of quenched carbonates are observed. A short
Na-K exchange between (dissolved) KBr and Na2Ca(CO3)(2) in a self-gene
rated water-steam atmosphere within the prepared KBr pellets is suppos
ed to be the reason for different FTIR spectra and formation of (Na,K)
(2)Ca(CO3)(2) solid-solutions is suggested. No cation exchange is obse
rved upon heating gaylussite and pirssonite dispersed in KBr pellets t
o temperatures below the dehydration temperature.