Home Physical Sciences Nanomorphology of montmorillonite particles: Estimation of the clay edge sorption site density by low-pressure gas adsorption and AFM observations
Article
Licensed
Unlicensed Requires Authentication

Nanomorphology of montmorillonite particles: Estimation of the clay edge sorption site density by low-pressure gas adsorption and AFM observations

  • Christophe Tournassat EMAIL logo , Alexander Neaman , Frédéric Villiéras , Dirk Bosbach and Laurent Charlet
Published/Copyright: March 31, 2015
Become an author with De Gruyter Brill

Abstract

Dry and in situ (fluid-cell) Atomic Force Microscopy (AFM) and Low-Pressure Gas Adsorption experiments were used to investigate the surfaces of pure Na-smectite particles. These two techniques permit the identification of different surfaces of the platelets (lateral, basal, and interlayer surfaces) and to quantify their surface area. Calculation of the surface area was done for AFM, by measuring directly the dimensions of the clay particles on AFM images, and for gas adsorption experiments, by applying the Derivative Isotherm Summation (DIS) procedure designed by Villiéras et al. (Villiéras et al. 1992, 1997a, 1997b).

In the present study, we find a discrepancy between measurements of the basal and interlayer surface area. This difference is due to the stacking of platelets in dry conditions compared to their dispersion in aqueous suspension. A particle is estimated to be formed of nearly 20 stacked layers in the dehydrated state used in the gas adsorption experiment, whereas it is estimated to be composed of only 1 or 2 layers in aqueous suspension, on the basis of AFM measurements. However, the two techniques give similar results for the lateral surface area of the platelets (i.e., about 8 m2/g) and the perimeter to area ratio value of the particles because the stacking of platelets does not alter these values. This correlation confirms the effectiveness of the interpretation of the gas adsorption experiments lowest pressure domains as the adsorption on lateral surfaces.

The lateral surface area has important implications in the calculation of specific sorption site density on clay material. The relevance of the lateral surface area value (8 m2/g) was tested subsequently with sorption data found in the literature. Based on those results, we show that one essential parameter for the calculation of particle edge-site density is the mean perimeter to area ratio value. This parameter can be obtained by microscopic techniques but the measurement is tedious. The good correlation between the AFM results and the DIS-method results confirms that the latter procedure offers a quick and reliable alternative method for the measurement of the lateral surface area. AFM experiments can be further conducted to constrain the dispersion around the DIS value and the anisotropy of suspended particles.

Received: 2002-11-29
Accepted: 2003-4-14
Published Online: 2015-3-31
Published in Print: 2003-11-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Partial equilibrium of radiogenic and stable isotope systems in garnet peridotite during ultrahigh-pressure metamorphism
  2. Experimental determination of Au solubility in rhyolite melt and magnetite: Constraints on magmatic Au budgets
  3. Surface oxidation of chalcocite (Cu2S) under aqueous (pH = 2–11) and ambient atmospheric conditions: Mineralogy from Cu L- and O K-edge X-ray absorption spectroscopy
  4. Determination of molar absorptivity of IR fundamental OH-stretching vibration in rhyolitic glasses
  5. The effect of radiation damage on local structure in the crystalline fraction of ZrSiO4: Investigating the 29Si NMR response to pressure in zircon and reidite
  6. The structural behavior of Al3+ in peralkaline melts and glasses in the system Na2O-Al2O3-SiO2
  7. Hydromaghemite, an intermediate in the hydrothermal transformation of 2-line ferrihydrite into hematite
  8. Carbon isotope “stratigraphy” in a single graphite crystal: Implications for the crystal growth mechanism of fluid-deposited graphite
  9. Woodruffite: A new Mn oxide structure with 3 × 4 tunnels
  10. Calderonite, a new lead-iron-vanadate of the brackebuschite group
  11. Low-temperature microdiamond aggregates in the Maksyutov Metamorphic Complex, South Ural Mountains, Russia
  12. Crystal structure of protoanthophyllite: A new mineral from the Takase ultramafic complex, Japan
  13. Crystallization of AlPO4-SiO2 solid solutions from granitic melt and implications for P-rich melt inclusions in pegmatitic quartz
  14. On the formation of peridotite-derived Os-rich PGE alloys
  15. Viscosity of hydrous rhyolitic melts inferred from kinetic experiments, and a new viscosity model
  16. Geothermobarometry and U-Pb Geochronology of metapelitic granulites and pelitic migmatites from the Lokoho region, Northern Madagascar
  17. The aperiodic states of zircon: an ab initio molecular dynamics study
  18. Cathodoluminescence investigations on the Popigai, Ries, and Lappajärvi impact diamonds
  19. Isomorphous cation substitution in dioctahedral phyllosilicates by means of ab initio quantum mechanical calculations on clusters
  20. Alacranite, As8S9: structural study of the holotype and re-assignment of the original chemical formula
  21. Influence of layer charge on the hydroxyl stretching of trioctahedral clay minerals: A vibrational study of synthetic Na- and K-saponites
  22. Stacking faults and twin boundaries in sphalerite crystals from the Trepcˇa mines in Kosovo
  23. Letters. Rock-forming moissanite (natural α-silicon carbide)
  24. Water solubility in carbonatite melts
  25. Trace element partitioning between mantle wedge peridotite and hydrous MgO-rich melt
  26. Rubidium- and cesium-dominant micas in granitic pegmatites
  27. Nanoscale mineralogy of arsenic in a region of New Hampshire with elevated As-concentrations in the groundwater
  28. Micro- and nanochemistry of fly ash from a coal-fired power plant
  29. Thermal behavior of dental enamel and geologic apatite: An infrared spectroscopic study
  30. Black carbon pollution of speleothems by fine urban aerosols in tourist caves
  31. Decay-induced biomineralization of the saguaro cactus (Carnegiea gigantea)
  32. The distribution of zeolites and their effects on the performance of a nuclear waste repository at Yucca Mountain, Nevada, U.S.A.
  33. Transformation of 2-line ferrihydrite to 6-line ferrihydrite under oxic and anoxic conditions
  34. Iron-rich precipitates in a mine drainage environment: Influence of pH on mineralogy
  35. Efflorescent iron sulfate minerals: Paragenesis, relative stability, and environmental impact
  36. Secondary mineralogy and microtextures of weathered sulfides and manganoan carbonates in mine waste-rock dumps, with implications for heavy-metal fixation
  37. Acquisition and evaluation of thermodynamic data for morenosite-retgersite equilibria at 0.1 MPa
  38. On the thermochemistry of the solid solution between jarosite and its chromate analog
  39. The Composition and Morphology of Amphiboles from the Rainy Creek Complex, Near Libby, Montana
  40. Composition, Fe3+/ΣFe, and crystal structure of non-asbestiform and asbestiform amphiboles from Libby, Montana, U.S.A.
  41. A rapid and accurate procedure for the determination of refractive indices of regulated asbestos minerals
  42. Ferrous saponite from the Deccan Trap, India, and its application in adsorption and reduction of hexavalent chromium
  43. Nanomorphology of montmorillonite particles: Estimation of the clay edge sorption site density by low-pressure gas adsorption and AFM observations
  44. Medieval stained glass in a Mediterranean climate: Typology, weathering and glass decay, and associated biomineralization processes and products
  45. The structure of disordered mackinawite
  46. The reactivity of seven Mn-oxides with Cr3+aq: A comparative analysis of a complex, environmentally important redox reaction
  47. Sorption mechanisms of Sr and Pb on zeolitized tuffs from the Nevada test site as a function of pH and ionic strength
  48. Letters. Tailoring calcite: Nanoscale AFM of coccolith biocrystals
Downloaded on 9.3.2026 from https://www.degruyterbrill.com/document/doi/10.2138/am-2003-11-1243/html
Scroll to top button