Abstract
Calcium concentration and calcite supersaturation (Ω) needed for calcium carbonate nucleation and crystal growth in Pyramid Lake (PL) surface water were determined during August of 1997, 2000, and 2001. PL surface water has Ω values of 10–16. Notwithstanding high Ω, calcium carbonate growth did not occur on aragonite single crystals suspended PL surface water for several months. However, calcium solution addition to PL surface-water samples caused reproducible calcium carbonate mineral nucleation and crystal growth. Mean PL surface-water calcium concentration at nucleation was 2.33 mM (n = 10), a value about nine times higher than the ambient PL surface-water calcium concentration (0.26 mM); mean Ω at nucleation (109 with a standard deviation of 8) is about eight times the PL surface-water Ω. Calcium concentration and Ω regulated the calcium carbonate formation in PL nucleation experiments and surface water. Unfiltered samples nucleated at lower Ω than filtered samples. Calcium concentration and Ω at nucleation for experiments in the presence of added particles were within one standard deviation of the mean for all samples. Calcium carbonate formation rates followed a simple rate expression of the form, rate (mM/min) = A (Ω) + B. The best fit rate equation “Rate (Δ mM/Δ min) = −0.0026 Ω + 0.0175 (r = 0.904, n = 10)” was statistically significant at greater than the 0.01 confidence level and gives, after rearrangement, Ω at zero rate of 6.7. Nucleation in PL surface water and morphology of calcium carbonate particles formed in PL nucleation experiments and in PL surface-water samples suggest crystal growth inhibition by multiple substances present in PL surface water mediates PL calcium carbonate formation, but there is insufficient information to determine the chemical nature of all inhibitors.
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Acknowledgments
The authors acknowledge help and encouragement of the PL Paiute Tribal Council and the PL Natural Resource Building staff during this work. Fieldwork was done with the assistance of David Fellenz (a USGS Volunteer, Lawrence University, Appleton, WI), Micaela Reddy (USGS Volunteer, Denver, CO), Julie Reddy (USGS Volunteer, Denver, CO), and Paul Schuster (USGS, NRP, CB, Boulder, CO). George Molino of Cutthroat Charters, Reno, NV, and Dan Mosley of the Pyramid Lake Piaute Tribe Environmental Department, Nixon, NV facilitated lake-water sampling logistics. Scott Charlton (USGS, NRP, BRR, CB, Denver, CO) assisted in data analysis and chemical speciation calculation. Charmaine Gunther (USGS, NRP, CB, Denver, CO) assisted in the preparation of the report. Review comments by David Parkhurst (USGS, NRP, CB, Denver, CO) and David Naftz (USGS, WRD, Salt Lake City, UT) and an anonymous reviewer significantly improved the manuscript. Anthony Hoch held a National Research Council-USGS Research Fellowship during this research. Funding for the work is by the USGS, NRP. The use of trade names and product names in this paper is for identification purposes only, and does not constitute endorsement by the USGS.
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Reddy, M.M., Hoch, A. Calcium Carbonate Nucleation in an Alkaline Lake Surface Water, Pyramid Lake, Nevada, USA. Aquat Geochem 18, 95–113 (2012). https://doi.org/10.1007/s10498-011-9150-3
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DOI: https://doi.org/10.1007/s10498-011-9150-3