Organic coprecipitates with calcite: NMR spectroscopic evidence.
Dissolved organic ligands are well known to interact strongly with the calcite surface, altering precipitation and dissolution rates, crystal morphology, and possibly the ability of calcite to sequester metal contaminants. We show, using NMR spectroscopic techniques, that some of the citrate molecules present in a solution of precipitating calcite are incorporated structurally into the calcite crystal. Calcite grown by a seeded constant-addition method contains approximately 1 wt % coprecipitated citrate and yields 13C{1H} cross-polarization magic-angle spinning NMR spectra that contain broad peaks for citrate plus a signal from carbonate. Results from 13C{1H} heteronuclear correlation NMR experiments show that citrate is located in close spatial proximity to carbonate groups. In addition, calcite/citrate coprecipitates contain about 0.4 wt % excess water, which is not present as fluid inclusions, and some of which occurs as rigid structural water. These results suggestthat water and hydrogen-bonding interactions play a role in the interface between included organic molecules and the calcite host. Additional NMR data obtained for calcite coprecipitates of aspartic and glutamic acids suggest they are also incorporated structurally but at concentrations much lower than for citrate, whereas no evidence was found for phthalate incorporation.
Phillips
Brian L
BL
Center for Environmental Molecular Science, Department of Geosciences, State University of New York, Stony Brook, New York 11794-2100, USA. brian.phillips@sunysb.edu
Lee
Young J
YJ
Reeder
Richard J
RJ
D002119:Calcium Carbonate / Q000737:chemistry*; D002247:Carbon Isotopes; D011232:Chemical Precipitation; D019343:Citric Acid / Q000737:chemistry*; D006860:Hydrogen Bonding; D009682:Magnetic Resonance Spectroscopy; D014867:Water / Q000737:chemistry
D002247:Carbon Isotopes; D014867:Water; D019343:Citric Acid; D002119:Calcium Carbonate