H. Behrens, DETERMINATION OF WATER SOLUBILITIES IN HIGH-VISCOSITY MELTS - AN EXPERIMENTAL-STUDY ON NAALSI3O8 AND KALSI3O8 MELTS, European journal of mineralogy, 7(4), 1995, pp. 905-920
The solubility of water in melts of albitic (Ab: NaAlSi3O8) and orthoc
lasic (Or: KAlSi3O8) compositions was re-investigated at T = 1100 degr
ees C and at pressures between 0.5 and 5.0 kbar. The influence of star
ting materials, sample preparation, run procedure and analytical metho
ds on the solubility data was investigated systematically. Different a
nalytical techniques (Karl-Fischer titration (KFT), near-infrared spec
troscopy (NIR), 105 degrees C weight loss and weight loss on ignition)
give consistent results under certain conditions, whereas water-speci
fic methods (KFT and NIR) have a higher precision. The lowest solubili
ties of water were found for samples of exact feldspathic composition.
An excess of several wt% of SiO2 relative to a feldspar composition h
as a negligible effect on water solubility, but an excess of Na2O or A
l2O3 relative to NaAlSi3O8 increases the solubility by ca. 3 percent r
elative per wt% of excess oxide. At P = 5 kbar, significantly higher s
olubilities than reported in previous studies were obtained (11.60 wt%
H2O for Ab and 10.32 wt% H2O for Or). This is attributed to drying of
run products at 105 degrees C in previous studies. At P = 2 kbar, exp
eriments using single glass pieces, crystal plates or glass pieces emb
edded in glass powder as starting materials yielded a water solubility
of 5.95 wt% for Ab melts, which is less than solubilities determined
in previous studies. The reliability of the new solubility data could
be confirmed by reversals. The water solubility in Ab melts at P = 5 k
bar increases apparently with the ratio of fluid to melt. This effect
is probably caused by formation of strongly hydrated quench products o
n the melt body and diffusional exchange between both during cooling.