PROCESSES CONTROLLING MG-CALCITE COLLOID PRECIPITATION WITHIN MARAMEC SPRING, MISSOURI
Both XRD and SEM-EDS techniques were utilized to examine colloidal particles collected both by on-site vacuum filtration centrifuging spring water samples. Organic debris, diatoms, quartz, smectite, and illite were detected as well as unidentified sulfur-bearing phases. XRD analysis also revealed the presence of both dolomite and high-Mg calcite (~29.7° two-theta, CuKα). The dolomite likely is derived from the erosion of the Gasconade Formation, which hosts many springs and caves in the region. SEM examination of micron-sized particles of Mg-calcite did not reveal any corrosion pits or impact features. The particles displayed such delicate features that they undoubtedly were precipitated in and remained suspended by the turbulent spring water. Approximately 100 carbonate particles were hand separated under a microscope, digested in acid, and analyzed chemically to reveal a composition of ~8 mole% MgCO3. Modeling of the Maramec Springs system data using MINTEC and PHREEQ software yielded negative saturation indices (SI) of -0.9 to -0.7. Unrealistically large increases in alkalinity, temperature, and aCa are required to reach calcite saturation (SI=0). Shifting the pH from 7.0 to 7.8, however, would induce saturation by converting HCO3- into CO32-. How the Maramec system circumvents this transformation is unresolved but suggests a reaction involving Ca2+ directly with HCO3- ions.