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Asmectite (from Ancient Greek σμηκτός (smēktós) 'lubricated'; from σμηκτρίς (smēktrís) 'walker's earth,fuller's earth';lit. 'rubbing earth; earth that has the property of cleaning')[1] is a mineral mixture of various swelling sheet silicates (phyllosilicates), which have a three-layer 2:1 (TOT) structure and belong to the clay minerals. Smectites mainly consist ofmontmorillonite, but can often contain secondary minerals such asquartz andcalcite.[2]
In clay mineralogy, smectite is synonym of montmorillonite (also the name of a pure clay mineral phase) to indicate a class of swelling clays. The term smectite is commonly used in Europe and in the UK while the term montmorillonite is preferred in North America, but both terms are equivalent and can be used interchangeably. For industrial and commercial applications, the term bentonite is mostly used in place of smectite or montmorillonite.
The 2:1 layer (TOT) structure consists of twosilica (SiO2)tetrahedral (T) layers which are electrostatically cross-linked via an Al2O3 (gibbsite), or Fe2O3,octahedral (O) central layer. The TOT elementary layers are not rigidly connected to each other but are separated by a free space: the interlayer hosting hydratedcations andwater molecules. Smectite can swell because of the reversible incorporation of water and cations in the interlayer space.
The TOT layers are negatively charged because of the isomorphic substitution of Si(IV) atoms by Al(III) atoms in the two external silica tetrahedral layers and because of the replacement of Al(III) or Fe(III) atoms by Mg2+ or Fe2+ cations in the inner gibbsite octahedral layer. As the +4 charges born by Si(IV), and normally compensated by −4 charges from the surrounding oxygen atoms, become +3 due to the substitution of Si(IV) by Al(III), an electrical imbalance occurs: +3 −4 = −1. The excess of negative charges in the TOT layer has to be compensated by the presence of positive cations in the interlayer. The same reasoning also applies to the gibbsite central layer of the TOT elementary unit when an Al3+ ion is replaced by a Mg2+ ion in a gibbsite octahedra. The electrical imbalance is: +2 −3 = −1.
The maincations in the smectite interlayers are Na+ and Ca2+. Thesodium cations are responsible for the highest swelling of smectite whilecalcium ions have lower swelling properties. Calcium smectite has significantly less swelling capacity than sodium smectite but is also less prone to shrinking when desiccated.[3]
The degree of hydration of the cations and their corresponding hydrated radii explain the swelling or the shrinking behaviour of phyllosilicates. Other cations such as Mg2+ and K+ ions exhibit even a more contrasted effect: highly hydratedmagnesium ions are "swellers" as invermiculite (totally expanded interlayer) while poorly hydratedpotassium ions are "collapsers" like inillite (totally collapsed interlayer).
As the interlayer space of smectites is more open and so more easily accessible to water and cations, smectites exhibit the highestcation-exchange capacity (CEC) of clay minerals commonly found in the soils. Only more expandablevermiculite and some rarer alumino-silicate minerals (zeolites) with inner channel structure can exhibit a higher CEC than smectite.
Smectites are formed from theweathering ofbasalt,gabbro, and silica-richvolcanic glass (e.g.,pumice,obsidian,rhyolite,dacite). Many smectites are formed involcanichydrothermal system (such asgeyser system) where hot water percolating through theporous matrix or thecracks of thevolcanic ash deposit (pumice,pozzolan) dissolves most ofamorphoussilica (up to 50 wt.% of SiO2 can be dissolved), leaving smectite in place. This mechanism is responsible for the formation of the bentonite deposit (Serrata deNijar) ofCabo de Gata in the south-east region ofAlmeria inAndalusia (Spain). Wyoming MX-80bentonite was formed in a similar way during theCretaceous Period when volcanic ashes were falling in an inner sea on the American continent. The highlyporous (with a large and easily accessiblespecific surface) and very reactive volcanic ashes rapidly reacted withseawater. Because of silicahydrolysis, most ofsilica was dissolved in seawater and removed from the ashes giving rise to the formation of smectites. Smectites found in many marine clay deposits are often formed in this way as it is the case for the Ypresian Clays found in Belgium and very rich in smectites.
Smectites are commonly used in very diverse industrial applications. In civil engineering works, it is routinely used as a thickbentonite slurry when excavating deep and narrow trenches in the ground to support the lateral walls and to avoid their collapse. It is also used asmud fordrilling fluids. Smectites, more commonly called bentonite, are candidate as buffer and backfill materials to fill the space around high-levelradioactive waste in deep geological repositories. Smectites also serve as additive inpaints or asthickening agent for various preparations.
Terre qui a la propriété de nettoyer. Earth that has the property of cleaning
