Showing posts with label geology. Show all posts
Showing posts with label geology. Show all posts

Wednesday, February 24, 2010

X-Ray Fluorescence Spectrometry

LinkGrand.com

(or XRF spectrometry) an analytical method in geology for determination of a wide range of elements in bulk rock specimens. Rock samples are prepared as ground powder compressed into flat cylinders or fused into coin-like flat discs and then excited with X-ray radiation. The radiation causes the removal of an ELECTRON from an ORBITAL, and when it is replaced, the surplus energy is emitted as a characteristic, secondary, X-ray. The X-ray is measured by the spectrometer and the intensity of the radiation compared to a standard to enable concentrations to be calculated. The technique is widely used in analysing rock samples both for major elements and certain TRACE ELEMENTS. Concentrations of trace elements as low as 1 to 10 parts per million can be detected although, in many instances, the quantities are higher.

Taken from Dictionary of Science

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X-ray fluorescence (XRF) is the emission of characteristic "secondary" (or fluorescent) X-rays from a material that has been excited by bombarding with high-energy X-rays or gamma rays. The phenomenon is widely used for elemental analysis and chemical analysis, particularly in the investigation of metals, glass, ceramics and building materials, and for research in geochemistry, forensic science and archaeology.

Taken from Wikipedia





Wednesday, January 20, 2010

X-Ray Crystallography

LinkGrand.com

(or X-ray diffraction---XRD - crystallography) a technique used in geology to identify minerals, and biology or chemistry to work out the structure of complex molecules. It involves directing a beam of X-rays at a CRYSTAL and the rays are diffracted off the planes of atoms in the crystal. By repeating the procedure and then calculating the spacing between atomic planes, a representation of the crystal's structure can be determined.

Taken from Dictionary of Science

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X-ray crystallography is a method of determining the arrangement of atoms within a crystal, in which a beam of X-rays strikes a crystal and diffracts into many specific directions. From the angles and intensities of these diffracted beams, a crystallographer can produce a three-dimensional picture of the density of electrons within the crystal. From this electron density, the mean positions of the atoms in the crystal can be determined, as well as their chemical bonds, their disorder and various other information.


Since many materials can form crystals — such as salts, metals, minerals, semiconductors, as well as various inorganic, organic and biological molecules — X-ray crystallography has been fundamental in the development of many scientific fields. In its first decades of use, this method determined the size of atoms, the lengths and types of chemical bonds, and the atomic-scale differences among various materials, especially minerals and alloys. The method also revealed the structure and functioning of many biological molecules, including vitamins, drugs, proteins and nucleic acids such as DNA. X-ray crystallography is still the chief method for characterizing the atomic structure of new materials and in discerning materials that appear similar by other experiments. X-ray crystal structures can also account for unusual electronic or elastic properties of a material, shed light on chemical interactions and processes, or serve as the basis for designing pharmaceuticals against diseases.


In an X-ray diffraction measurement, a crystal is mounted on a goniometer and gradually rotated while being bombarded with X-rays, producing a diffraction pattern of regularly spaced spots known as reflections. The two-dimensional images taken at different rotations are converted into a three-dimensional model of the density of electrons within the crystal using the mathematical method of Fourier transforms, combined with chemical data known for the sample. Poor resolution (fuzziness) or even errors may result if the crystals are too small, or not uniform enough in their internal makeup.


X-ray crystallography is related to several other methods for determining atomic structures. Similar diffraction patterns can be produced by scattering electrons or neutrons, which are likewise interpreted as a Fourier transform. If single crystals of sufficient size cannot be obtained, various other X-ray methods can be applied to obtain less detailed information; such methods include fiber diffraction, powder diffraction and small-angle X-ray scattering (SAXS). In all these methods, the scattering is elastic; the scattered X-rays have the same wavelength as the incoming X-ray. By contrast, inelastic X-ray scattering methods are useful in studying excitations of the sample, rather than the distribution of its atoms.


Taken from Wikipedia


Wednesday, January 13, 2010

Joint


1
in geology, fractures in rock that may occur as parallel sets or, more commonly, in an irregular and less systematic manner. Where a set of joints can be identified, it can usually be related to tectonic (that is to do with deformation of the Earth) stresses and the geometry of the rock body. There are several types of joint: unloading joints, which are caused by the release of stress on rocks at depth as overlying rocks are removed by erosion; cooling joints, which occur in igneous bodies; and joints that are related to regional deformation (on a wide scale).

2 In biology, the point at which bones and the surrounding tissues meet. They may be fixed joints (as in the cranium), slightly movable (e.g., joints in the spine) or freely movable (e.g., knee, arm). The movable joint types also differ -- ball and socket (hip) or hinge (elbow).

Taken from Dictionary of Science