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X-ray Diffraction (XRD) and Forensic Geology X-ray diffraction pattern for goethite X-ray diffractometer (XRD) laboratory
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Structure of minerals Structure of minerals Minerals consist of an orderly array of atoms chemically bonded to form a particular crystalline structure. Internal atomic arrangement in ionic compounds is determined by ionic size.
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Geometric packing of various ions Figure 3.8
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Crystal Lattice: the three dimensional molecular structure of a mineral. (Shape of the “unit cell.”) the various ions that make up the mineral. Geometry + chemistry! Structure of Minerals
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Halite (rock salt) Structure of Minerals
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Diagram illustrating Bragg’s law. = angle of incidence and diffraction when Bragg’s law conditions are met. d = inter-planar spacing.
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Bragg’s Law λ = 2d(sinθ) where: λ = x-ray wavelength d = spacing between planes of atoms in crystal θ = x-ray incidence angle (Bragg angle) also: d = λ /2sin θ sin θ = λ /2d
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XRD Laboratory
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