Home Physical Sciences Magnetic and microscopic characterization of magnetite nanoparticles adhered to clay surfaces
Article
Licensed
Unlicensed Requires Authentication

Magnetic and microscopic characterization of magnetite nanoparticles adhered to clay surfaces

  • Cecilia Galindo-Gonzalez , Joshua M. Feinberg EMAIL logo , Takeshi Kasama , Lionel Cervera Gontard , Mihály Pósfai , Ilona Kósa , Juan D.G. Duran , Jaime E. Gil , Richard J. Harrison and Rafal E. Dunin-Borkowski
Published/Copyright: April 1, 2015
Become an author with De Gruyter Brill

Abstract

When suspended in solution, clay platelets coated with nanometer-scale magnetite particles behave as magnetorheologic fluids that are important to a variety of industrial applications. Such dual-phase assemblages are also similar to natural aggregates that record the direction and intensity of the Earth’s magnetic field in lake and marine depositional environments. This study characterizes the mineralogical structure and magnetic behavior of montmorillonite platelets coated with aggregates of nanometerscale magnetite crystals. The distribution of magnetite crystal sizes in three different clay-magnetite assemblages was directly measured using conventional transmission electron microscopy and agrees within error with estimates derived from magnetic hysteresis measurements. Magnetic hysteresis and low field susceptibility measurements combined with electron holography experiments indicate that all three samples behave superparamagnetically at room temperature, and show increasing levels of single domain behavior as the samples are cooled to liquid nitrogen temperatures. At such low temperatures, magnetostatic interactions are observed to partially stabilize otherwise superparamagnetic grains in flux closure structures.

Received: 2008-12-6
Accepted: 2009-4-19
Published Online: 2015-4-1
Published in Print: 2009-8-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Bonded interactions in silica polymorphs, silicates, and siloxane molecules
  2. Spatially heterogeneous burial and high-P/T metamorphism in the Crescent Formation, Olympic Peninsula, Washington
  3. Quantitative microstructural characterization of natrojarosite scale formed during high-pressure acid leaching of lateritic nickel ore
  4. Magnetic and microscopic characterization of magnetite nanoparticles adhered to clay surfaces
  5. Single crystal growth of wadsleyite
  6. Elastic behavior and phase stability of pollucite, a potential host for nuclear waste
  7. Crystal structure determination of anandite-2M mica
  8. Excess heat capacity and entropy of mixing in high structural state plagioclase
  9. Cannibalization of an amphibole-rich andesitic progenitor induced by caldera-collapse during the Matahina eruption: Evidence from amphibole compositions
  10. Experimental constraints on rutile saturation during partial melting of metabasalt at the amphibolite to eclogite transition, with applications to TTG genesis
  11. Mineralogical stability of phyllosilicates in hyperalkaline fluids: Influence of layer nature, octahedral occupation and presence of tetrahedral Al
  12. Plumbophyllite, a new species from the Blue Bell claims near Baker, San Bernardino County, California
  13. Simultaneous aluminum, silicon, and sodium coordination changes in 6 GPa sodium aluminosilicate glasses
  14. Mineral chemistry and alteration of rare earth element (REE) carbonates from alkaline pegmatites of Mount Malosa, Malawi
  15. The carbonatation of gypsum: Pathways and pseudomorph formation
  16. Calcium L2,3-edge XANES of carbonates, carbonate apatite, and oldhamite (CaS)
  17. Thermochemistry of a synthetic Na-Mg-rich triple-chain silicate: Determination of thermodynamic variables
  18. Change in compressibility of δ-AlOOH and δ-AlOOD at high pressure: A study of isotope effect and hydrogen-bond symmetrization
  19. Crystal structure and iron topochemistry of erionite-K from Rome, Oregon, U.S.A.
  20. First-principles energetics and structural relaxation of antigorite
  21. Letter. Evidence in favor of small amounts of ephemeral and transient water during alteration at Meridiani Planum, Mars
  22. Letter. Native aluminum: Does it exist?
  23. Letter. Hydration state and activity of aqueous silica in H2O-CO2 fluids at high pressure and temperature
Downloaded on 11.2.2026 from https://www.degruyterbrill.com/document/doi/10.2138/am.2009.3167/html
Scroll to top button