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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >GYPSUM GROWTH IN THE PRESENCE OF BACKGROUND ELECTROLYTES STUDIED BY SCANNING FORCE MICROSCOPY
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GYPSUM GROWTH IN THE PRESENCE OF BACKGROUND ELECTROLYTES STUDIED BY SCANNING FORCE MICROSCOPY

机译:扫描力显微镜研究背景电解质存在下石膏的生长

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Background electrolytes in aqueous solutions can strongly influence the growth rate of gypsum, which can be easily shown from bulk growth experiments. However, such experiments cannot be used to decipher the actual mechanism unambiguously. We have used Scanning Force Microscopy in order to characterize the microtopography of the gypsum (010) surface, to determine the dominate step-generating process, and to investigate the influence of NaNO3 and NaCl as background electrolytes on the growth kinetics of monolayer steps. Due to surface defects, the step density can be inhomogeneous, resulting in variability in bulk growth rate data. Two-dimensional nucleation (birth and spread) has been found to be the dominant process that forms new steps on the (010) surface. Surface nuclei may be bounded by [100] and [001] steps, judging from the shape and orientation of the smallest observed surface islands during growth. In addition, ab initio molecular orbital calculations show that [100] and [001] steps on the (010) surface of gypsum have nearly identical energies. Nevertheless, well beyond the nucleation stage, growth occurs on the (010) surface via the advance of monolayer steps (representing one growth slice, 7 Angstrom in height) parallel to [101] and [001]. Steps parallel to [101] migrate faster than [001] steps, in agreement with ab initio calculations which show that [101] steps have a considerably higher energy than [001] steps. The step displacement velocity of the fast growth direction parallel to [101] is increased in the presence of NaCl, relative to NaNO3, as background electrolytes, whereas the slow growth direction parallel to [001] shows no background electrolyte effect. The different growth kinetics for the two major growth directions in the presence of different electrolytes can be explained by the difference in step energies. On the basis of our data, it appears very likely that a specific interaction between [101] steps and Cl- in solution results in an increased dehydration frequency for hydrated Ca2+ near [101] step-edge regions relative to NO3- containing supersaturated solutions. [References: 60]
机译:水溶液中的背景电解质会极大地影响石膏的生长速度,这可以从本体生长实验中轻松看出。但是,这样的实验不能用来明确地解释实际机制。我们使用扫描力显微镜来表征石膏(010)表面的微观形貌,确定主要的台阶生成过程,并研究作为背景电解质的NaNO3和NaCl对单层台阶生长动力学的影响。由于表面缺陷,台阶密度可能不均匀,从而导致整体增长率数据变化。已经发现二维成核(出生和扩展)是在(010)表面形成新台阶的主要过程。从生长过程中观察到的最小表面岛的形状和方向来看,表面核可能受[100]和[001]步骤限制。另外,从头算的分子轨道计算表明,在石膏的(010)表面上的[100]和[001]台阶具有几乎相同的能量。然而,远远超过成核阶段,通过平行于[101]和[001]的单层台阶(代表一个生长片,高度为7埃)的前进,在(010)表面上发生了生长。平行于[101]的步骤比[001]步骤的迁移速度更快,这与从头算起的结果一致,该计算表明[101]步骤的能量要比[001]步骤高得多。相对于NaNO3,存在NaCl作为背景电解质时,平行于[101]的快速生长方向的阶跃位移速度增加,而平行于[001]的缓慢生长方向无背景电解质的影响。在存在不同电解质的情况下,两个主要生长方向的不同生长动力学可以通过阶跃能量的差异来解释。根据我们的数据,很可能[101]步骤与Cl-溶液之间的特定相互作用导致[101]台阶边缘区域附近的水合Ca2 +的脱水频率相对于含NO3的过饱和溶液而言增加了。 [参考:60]

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