Quantification of classical and non-classical crystallization pathways in calcite precipitation
Crystal precipitation from aqueous solution occurs through multiple pathways. Besides the classical ion-by-ion addition, non-classical crystallization mechanisms, such as multi-ion polymer and nano-particle attachment, could be of great significance under certain circumstances. These non-classical crystallization processes have been observed with advanced microscopy, yet detailed quantification of their contribution in mineral precipitation remains challenging. Building from paired Ca and Sr isotope observations, we develop a new theoretical framework to quantify the relative contribution of classical and non-classical crystallization pathways on the precipitation of the calcium carbonate mineral calcite, one of the most common precipitates in nature. We demonstrate that the classical (ion-by-ion) crystallization pathway alone is insufficient to account for the observed isotope behaviors and, thus, the entire calcite precipitation process. We present a new kinetic surface reaction model to incorporate the non-classical crystallization pathway. This new model, for the first time, enables the detailed characterization of the roles of classical and non-classical crystallization mechanisms in calcite precipitation. The results suggest that the relative contribution of non-classical crystallization pathways increases with saturation state and can, under high supersaturation levels, be comparable to or greater than precipitation driven by the classical crystallization pathway. The presented theoretical framework readily explains observed trace element partitioning and isotope fractionation behaviors during calcite precipitation and can be further expanded onto other mineral systems to gain insights into crystal growth mechanisms.