Journal
JOURNAL OF MINERALOGICAL AND PETROLOGICAL SCIENCES
Volume 102, Issue 3, Pages 174-181Publisher
JAPAN ASSOC MINERALOGICAL SCIENCES
DOI: 10.2465/jmps.060327a
Keywords
calcite-aragonite; carbonate precipitation in aqueous solution; metastable nucleation; strontium; Ostwald rule
Categories
Ask authors/readers for more resources
Alternating layers of calcite and aragonite, precipitated from mineral spring in fracture zones of serpentine mass, occur at Kashio, Oosika mura, Nagano Prefecture, Japan. Element mapping by means of Micro-area Xray Fluorescence (MXRF) conclusively demonstrated that strontium concentrates more in aragonite layer, and not in calcite layer. Other elements including magnesium show no positive correlation with aragonite precipitation. MXRF analyses of aragonite samples from other localities and origins also indicated concentration of Sr as major impurity component, demonstrating that Sr plays essential role in metastable nucleation of aragonite in the precipitation of CaCO3 polymorphs from aqueous solution. This can be understood on the basis of modifications of surface energy term in CaCO3 nucleation in the presence of Sr. Temperature changes trigger to increase the Sr concentration in mineral spring, leading to metastable nucleation of aragonite.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available