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首页> 外文期刊>Clays and clay minerals >DISSOLUTION OF BRUCITE ON THE (001) SURFACE AT NEUTRAL pH: IN SITU ATOMIC FORCE MICROSCOPY OBSERVATIONS
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DISSOLUTION OF BRUCITE ON THE (001) SURFACE AT NEUTRAL pH: IN SITU ATOMIC FORCE MICROSCOPY OBSERVATIONS

机译:中性pH下(001)表面水镁石的溶解:原位原子显微镜观察

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The dissolution of brucite, Mg(OH)_2, on the (001) surface was investigated using in situ atomic force microscopy in solutions at near-neutral pH. Dissolution proceeded by the formation of crystallographically oriented triangular etch pits with monolayer step and expansion of the pits. The sides of the triangle are parallel to the [100], [110] and [010] directions of the brucite structure, and the orientation of lines from the center of the triangle to the three apices are along the [210], [110] and [120] directions. This orientation may produce pit edges where OH groups coordinate to two Mg~(2+). Although triangular etch pits with monolayer depth formed mostly at random on the (001) surface, concentric pits penetrating several layers were also observed. Etch pits with spiral steps were rarely observed. Coalescence of the pits resulted in stranded terraces that diminished in size rapidly and formed a rounded irregular form. The step-retreat velocity around the triangular pit is 0.015—0.04 nm/s at pH 5—8. The retreat velocity around the stranded terraces was about three times more rapid than that around the triangular etch pits.
机译:使用原位原子力显微镜在接近中性pH的溶液中研究水镁石Mg(OH)_2在(001)表面上的溶解。溶解通过形成具有单层台阶的晶体学定向的三角形蚀刻凹坑并扩展凹坑而进行。三角形的边平行于水镁石结构的[100],[110]和[010]方向,从三角形的中心到三个顶点的直线方向沿[210],[110] ]和[120]方向。这种取向可以产生凹坑边缘,其中OH基团与两个Mg〜(2+)配位。尽管在(001)表面上随机形成了单层深度的三角形刻蚀坑,但也观察到了穿透几层的同心坑。很少观察到带有螺旋台阶的蚀刻坑。坑的聚结导致搁浅的梯田,梯田的大小迅速减小,并形成圆形不规则形状。在pH 5-8时,三角形凹坑周围的步进退带速度为0.015-0.04 nm / s。搁浅平台周围的后退速度比三角形蚀刻坑周围的后退速度快三倍。

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