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An Introduction to Astronomy Part III: Light and Telescopes Lambert E. Murray, Ph.D. Professor of Physics The Electromagnetic Spectrum Visible light is only a small region of the electromagnetic spectrum. Types of Spectra Continuous Spectra – This “blackbody” spectrum arises from the heating of an object. – The temperature of the object determines its color. Emission Line Spectra – This arises when electrons loose energy and emit radiation at wavelengths that are specific to the chemical makeup of the substance. Absorption Line Spectra – This is the opposite of emission spectra - it arises when electrons gain energy and absorb radiation at wavelengths that are specific to the chemical makeup of the substance. Color Temperature and Stars Color Spectra Types of Spectra Hydrogen Absorption Spectra Atomic Structure Atoms consist of a very small, heavy nucleus made up of protons and neutrons surrounded by a “cloud” or electrons. Atoms are not charged – they have the same number of protons as electrons. The chemical nature of atoms is determined by the number of protons. A neutron is approximately the same size as a proton, but has no charge. Atoms with the same number of protons, but different numbers of neutrons are called isotopes. Some isotopes are radioactive. Basic Atomic Structure Absorption and Emission Excitation and Ionization Spectroscopic Notation of Ions OI is the designation of neutral oxygen OII means one electron has been removed due to ionization OIII means two electrons have been removed by ionization In a hot gas we may find highly ionized elements, such as Fe XIV. Each ionic species has its own unique spectrum. Radioactive Isotopes Many elements have different isotopes Each isotope has the same chemical properties, but different numbers of neutrons in the nucleus. Some isotopes are unstable (radioactive). Radioactive isotopes change from one elementary species to another according to a radioactive decay rate characteristic of the parent isotope. Radioactive Decay Color Spectra Color and Temperature Color Temperature and Wein’s Law Wein’s Law states that the wavelength at which most of the light energy is emitted is given by the equation: lmax=1/T The Stephan-Boltzmann Law The Inverse-Square Law Scattering of Blue Light by Dust The Doppler Shift This is the shift of wavelength and frequency as the source and receiver move toward or away from each other. A red-shift occurs when the source and receiver are moving away from each other. A blue-shift occurs when the source and receiver are moving toward each other. Using the Doppler Shift Possible Emission Spectrum of a Star Proper Motion and Radial Motion Radiation from the Sun The total amount of energy incident upon the earth’s outer atmosphere is called the solar constant: 0.139 watt/sq-cm (about 10 inches square would give 100 watts). This is the total intensity for all wavelengths combined. As we have already pointed out, solar radiation in certain wavelengths is greater than in others and depends upon the surface temperature of the Sun. Solar Spectrum Optical Telescopes There are two principle types of optical telescopes: – Refractors – Reflectors Refracting telescopes use lenses to bend and focus the light. Reflecting telescopes use mirrors to reflect and focus the light. An Astronomical Refracting Telescope A Refracting Telescope This is a picture of the world’s largest refracting telescope, found in the University of Chicago’s Yerkes Observatory in Williams Bay, Wisconsin. A Reflecting Telescope Principle Objectives of the Telescope A telescope has two principle objectives: – To gather as much light from a star, planet, or planetary satellite as possible so that the image appears as bright as possible. – To produce a magnified image Magnification may make the object appear bigger Magnification increases the ability to resolve different features which are close together. Both the light gathering capacity of a telescope and its ability to resolve small features depend upon the diameter of the objective lens or mirror of the telescope. Magnification Increasing the size of the telescope increases the brightness and the resolution of the image. Improved Resolution with and Increase in Primary Mirror Size Principle Disadvantages of Refracting Telescopes The light must pass through the lenses, thus the size of the lenses are limited because of the way they must be supported (around the edge). – If the lenses are too big, gravity will make them sag and distort the image. – Long focal length lenses are thinner, so the largest diameter refracting telescopes have very long focal lengths. A single lens will bend different wavelengths (colors) by slightly different amounts, creating chromatic aberration. This can be corrected using special lenses – but these are much more difficult to manufacture and must be thicker and heavier, so that quality achromatic lenses must be smaller in size to prevent them from sagging. Correcting Chromatic Aberration Two different kinds of glass, with different refractive indexes must be used, and the lens curvatures must be properly matched. Principle Advantages of A Reflecting Telescope A concave mirror can be supported over its entire back surface dimension. Such a mirror can therefore be made much larger than the largest refracting telescopes. However, if the size of the mirror is too large, gravitational distortions will occur when the mirror’s orientation is changed. Since light does not pass through a mirror, mirrors are not subject to the problem of chromatic aberrations. Principle Disadvantages of Reflecting Telescopes The focal point of a concave mirror is in front of the mirror – in the light path. Thus, the entire area of the mirror cannot be utilized to capture light from the object observed. It sometimes creates difficulties to locate the observer at the focal point of the mirror. Types of Reflectors Schematic of the Hale Reflecting Telescope An example of a prime-focus reflecting telescope. Newtonian Reflecting Telescope A Hybrid Telescope Spherical Mirrors Exhibit Spherical Aberration Inexpensive reflectors have spherical mirrors, and thus suffer from spherical aberration. Spherical lenses also exhibit spherical aberrations. Research-Grade Telescopes Use Parabolic Mirrors Atmospheric Influence on Astronomy The atmosphere greatly influences what can be studied from the Earth’s surface. – The atmosphere is not transparent in certain regions of the spectrum. There are several “windows” to the heavens – An optical window – An infrared window – A radio window – Turbulence in the atmosphere causes stars to “twinkle” and reduces the resolution of the telescopes. – “Seeing” refers to atmospheric turbulence. – Light pollution limits our ability to see faint objects. To overcome this limitation, we send satellites beyond the earth’s atmosphere. Absorption by Gases in the Atmosphere Oxygen and Ozone absorb strongly in the ultraviolet, while Carbon Dioxide and Water Vapor absorb strongly in the infrared. Saturn in: Visible Radio The Hubble Space Telescope Hubble Images vs. Ground-Based Images Hubble Images Color Images Toward the Next Generation Telescopes One way to make larger reflecting telescopes is to make many smaller mirrors act as a single, much larger mirror. These hybrid reflectors have electronic adjustments for each individual mirror. New techniques are allowing us to change the position of each individual element of these multielement telescopes by small amounts to counteract the effects of the atmosphere. Multiple Mirrors can be Utilized to Act as a Single, Large Mirror visible radio X-ray infrared Gamma ray End of Part III