Dusting the galaxy.Cosmic dust is one of the two major inhabitants of interstellar space in our and other galaxies (gas clouds are the other). In visible light the dust manifests its presence in a negative, subtractional way by absorbing light and so dimming and reddening the appearance of stars. However, the dust scatters X-rays and so provides halos for the images of point X-ray sources belonging to our galaxy. By studying those halos, Christopher W. Mauche and Paul Gorenstein of the Harvard-Smithsonian Center for Astrophysics The Harvard-Smithsonian Center for Astrophysics (CfA) is located in Cambridge, Massachusetts. It consists of the Harvard College Observatory and the Smithsonian Astrophysical Observatory. The Center is located at 60 Garden Street. in Cambridge, Mass., have deduced something about the size of the dust grains and their density and composition. Using observations of the Imaging Proportional Counter on the Einstein Observatory satellite, they found first that the intensity of X-ray halos represents an amount of dust consistent with what astrophysicists had calculated from the observed absorption of visible light. In a paper submitted to the ASTROPHYSICAL JOURNAL, they report that the halos cannot be caused by dust grains of a uniform size; there must be a certain distribution of sizes. Theorists have proposed two mathematical schemes for such a distribution, the Mathis-Rumpl-Nordsieck (MRN MRN Motor Racing Network MRN Medical Record Number MRN Magnetic Resonance Neurography MRN Medicare Remittance Notice MRN Matières Radioactives Naturelles MRN Meteorological Rocket Network MRN Manufacturers Resource Network ) formula and the Oort-van de Hulst formula. Although both formulas could account for the halos, the totality of evidence makes Mauche and Gorenstein favor the MRN, which is basically a power law distribution, that is, the number of grains of a given size is proportional to some power of that size. The average size of the grains is about 0.1 micrometer micrometer (mīkrŏm`ətər, mī`krōmē'tər). 1 Instrument used for measuring extremely small distances. (1/10,000 of a millimeter) and their density about 1 grain per hundred cubic kilometers (10.sup.-12 per cubic centimeter). Chemically there are two components: graphite grains ranging from 0.005 to 1 micrometer and "silicate silicate, chemical compound containing silicon, oxygen, and one or more metals, e.g., aluminum, barium, beryllium, calcium, iron, magnesium, manganese, potassium, sodium, or zirconium. Silicates may be considered chemically as salts of the various silicic acids. " (which could be enstatite enstatite Common silicate mineral in the pyroxene family. It is the stable form of magnesium silicate (MgSiO3, often with up to 10% iron) in magnesium- and iron-rich igneous rock types. , olivine olivine (ŏlĭv`ēn), an iron-magnesium silicate mineral, (Mg,Fe)2SiO4, crystallizing in the orthorhombic system. , silicon carbide, iron or magnetite magnetite (măg`nətīt), lustrous black, magnetic mineral, Fe3O4. It occurs in crystals of the cubic system, in masses, and as a loose sand. ) grains ranging from 0.025 to 0.25 micrometer. From all this Mauche and Gorenstein could calculate that approximately all of the silicon, magnesium and iron and 60 percent of the carbon in the interstellar medium is locked up in dust grains. These figures correspond, they say, to what astrophysicists can calculate independently from the observed composition of the interstellar gas. |
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