Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.
Science. 2013 Aug 23;341(6148):885-9. doi: 10.1126/science.1230915.
Recent experimental observations of the onset of calcium carbonate (CaCO3) mineralization suggest the emergence of a population of clusters that are stable rather than unstable as predicted by classical nucleation theory. This study uses molecular dynamics simulations to probe the structure, dynamics, and energetics of hydrated CaCO3 clusters and lattice gas simulations to explore the behavior of cluster populations before nucleation. Our results predict formation of a dense liquid phase through liquid-liquid separation within the concentration range in which clusters are observed. Coalescence and solidification of nanoscale droplets results in formation of a solid phase, the structure of which is consistent with amorphous CaCO3. The presence of a liquid-liquid binodal enables a diverse set of experimental observations to be reconciled within the context of established phase-separation mechanisms.
最近对碳酸钙 (CaCO3) 矿化起始的实验观察表明,出现了一群簇,这些簇比经典成核理论所预测的更稳定而不是不稳定。本研究使用分子动力学模拟来探测水合碳酸钙簇的结构、动力学和热力学,并使用格子气模拟来探索成核前簇群体的行为。我们的结果预测在观察到簇的浓度范围内,通过液-液分离形成致密液相。纳米尺度液滴的聚结和凝固导致固相的形成,其结构与非晶 CaCO3 一致。液-液双相的存在使一组多样化的实验观察结果能够在已建立的相分离机制的框架内得到协调。