Growth of Calcite in Confinement
Slow growth of calcite in confinement is abundant in Nature and man-made materials. There is ample evidence that such confined growth may create forces that fracture solids. The thermodynamic limits are well known, but since confined crystal growth is transport limited and difficult to control in ex...
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doaj-ce9e840398234ab1858b78b9993753f72020-11-24T21:45:06ZengMDPI AGCrystals2073-43522017-12-0171236110.3390/cryst7120361cryst7120361Growth of Calcite in ConfinementLei Li0Felix Kohler1Anja Røyne2Dag Kristian Dysthe3Condensed Matter Section and Physics of Geological Processes, Department of Physics, University of Oslo, P. O. Box 1048 Blindern, 0316 Oslo, NorwayCondensed Matter Section and Physics of Geological Processes, Department of Physics, University of Oslo, P. O. Box 1048 Blindern, 0316 Oslo, NorwayCondensed Matter Section and Physics of Geological Processes, Department of Physics, University of Oslo, P. O. Box 1048 Blindern, 0316 Oslo, NorwayCondensed Matter Section and Physics of Geological Processes, Department of Physics, University of Oslo, P. O. Box 1048 Blindern, 0316 Oslo, NorwaySlow growth of calcite in confinement is abundant in Nature and man-made materials. There is ample evidence that such confined growth may create forces that fracture solids. The thermodynamic limits are well known, but since confined crystal growth is transport limited and difficult to control in experiments, we have almost no information on the mechanisms or limits of these processes. We present a novel approach to the in situ study of confined crystal growth using microfluidics for accurate control of the saturation state of the fluid and interferometric measurement of the topography of the growing confined crystal surface. We observe and quantify diffusion-limited confined growth rims and explain them with a mass balance model. We have quantified and modeled crystals “floating” on a fluid film of 25–50 nm in thickness due to the disjoining pressure. We find that there are two end-member nanoconfined growth behaviors: (1) smooth and (2) rough intermittent growth, the latter being faster than the former. The intermittent growth rims have regions of load- bearing contacts that move around the rim causing the crystal to “wobble” its way upwards. We present strong evidence that the transition from smooth to rough is a generic confinement-induced instability not limited to calcite.https://www.mdpi.com/2073-4352/7/12/361crystal growthcalcitemicrofluidicnanoconfinementreflection interference contrast microscopy |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Lei Li Felix Kohler Anja Røyne Dag Kristian Dysthe |
spellingShingle |
Lei Li Felix Kohler Anja Røyne Dag Kristian Dysthe Growth of Calcite in Confinement Crystals crystal growth calcite microfluidic nanoconfinement reflection interference contrast microscopy |
author_facet |
Lei Li Felix Kohler Anja Røyne Dag Kristian Dysthe |
author_sort |
Lei Li |
title |
Growth of Calcite in Confinement |
title_short |
Growth of Calcite in Confinement |
title_full |
Growth of Calcite in Confinement |
title_fullStr |
Growth of Calcite in Confinement |
title_full_unstemmed |
Growth of Calcite in Confinement |
title_sort |
growth of calcite in confinement |
publisher |
MDPI AG |
series |
Crystals |
issn |
2073-4352 |
publishDate |
2017-12-01 |
description |
Slow growth of calcite in confinement is abundant in Nature and man-made materials. There is ample evidence that such confined growth may create forces that fracture solids. The thermodynamic limits are well known, but since confined crystal growth is transport limited and difficult to control in experiments, we have almost no information on the mechanisms or limits of these processes. We present a novel approach to the in situ study of confined crystal growth using microfluidics for accurate control of the saturation state of the fluid and interferometric measurement of the topography of the growing confined crystal surface. We observe and quantify diffusion-limited confined growth rims and explain them with a mass balance model. We have quantified and modeled crystals “floating” on a fluid film of 25–50 nm in thickness due to the disjoining pressure. We find that there are two end-member nanoconfined growth behaviors: (1) smooth and (2) rough intermittent growth, the latter being faster than the former. The intermittent growth rims have regions of load- bearing contacts that move around the rim causing the crystal to “wobble” its way upwards. We present strong evidence that the transition from smooth to rough is a generic confinement-induced instability not limited to calcite. |
topic |
crystal growth calcite microfluidic nanoconfinement reflection interference contrast microscopy |
url |
https://www.mdpi.com/2073-4352/7/12/361 |
work_keys_str_mv |
AT leili growthofcalciteinconfinement AT felixkohler growthofcalciteinconfinement AT anjarøyne growthofcalciteinconfinement AT dagkristiandysthe growthofcalciteinconfinement |
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