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Crystal Field Theory - Tetrahedral and Square Planar Complexes02:46

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Crystal field theory (CFT) is applicable to molecules in geometries other than octahedral. In octahedral complexes, the lobes of the dx2−y2 and dz2 orbitals point directly at the ligands. For tetrahedral complexes, the d orbitals remain in place, but with only four ligands located between the axes. None of the orbitals points directly at the tetrahedral ligands. However, the dx2−y2 and dz2 orbitals (along the Cartesian axes) overlap with the ligands less than...
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In the late 1800s, the revelation that light extended beyond visible wavelengths led to the discovery of X-rays by Wilhelm Roentgen. Recognized as high-energy electromagnetic radiation with short wavelengths, X-rays prompted exploration into their interaction with crystals. Max von Laue proposed in 1912 that the periodic arrangement of atoms, ions, or molecules in crystals would cause them to diffract X-rays, a hypothesis confirmed through experiments with copper sulfate and zinc sulfide...
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Related Experiment Video

Updated: Apr 22, 2026

Measurements of Long-range Electronic Correlations During Femtosecond Diffraction Experiments Performed on Nanocrystals of Buckminsterfullerene
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Light scattering by hexagonal columns in the discrete dipole approximation.

P J Flatau, B T Draine

    Optics Express
    |October 17, 2014
    PubMed
    Summary

    This study models light scattering by hexagonal ice crystals using wave and geometric optics. Results show geometric optics accurately predicts large ice crystal halos, while smaller crystals exhibit halo broadening and spillover.

    Area of Science:

    • Atmospheric optics
    • Light scattering by ice crystals

    Background:

    • Ice crystals in the atmosphere cause optical phenomena like halos.
    • Understanding light scattering is crucial for interpreting atmospheric optics.

    Purpose of the Study:

    • To calculate light scattering by hexagonal ice prisms using wave and geometric optics.
    • To investigate the applicability of geometric optics for modeling halo formation.
    • To suggest methods for retrieving ice crystal sizes from halo properties.

    Main Methods:

    • Maxwell's equations in the discrete dipole approximation were used for calculations.
    • Birefringence effects were included.
    • Scattering was analyzed for size parameters up to x = 400.

    Main Results:

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    • Wave optics and geometric optics showed excellent agreement for large size parameters in the outer halo region.
    • Smaller ice crystals predicted halo broadening and "spillover" into angles less than 22 degrees.
    • Halo polarization was also analyzed.

    Conclusions:

    • Geometric optics is applicable for modeling large ice crystal halos.
    • Halo broadening and spillover in smaller crystals offer potential for size retrieval.
    • Methods based on halo width, power at < 22 degrees, and polarization can estimate ice crystal sizes.