Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-05T04:14:01.974Z Has data issue: false hasContentIssue false

13 - Primordial Power: Geothermal and Nuclear

Published online by Cambridge University Press:  05 March 2015

Alan R. Carroll
Affiliation:
University of Wisconsin, Madison
Get access

Summary

At daybreak on July 4, 1054, a Chinese astronomer named Yang Weide noted the appearance of a new “guest star” in the eastern sky, near the more familiar reference star Tianguan (now known as Zeta Tauri). The appearance of a guest star was an exceedingly rare event considered to carry great geopolitical significance; the emperor Renzong therefore was duly notified. The new star remained visible during the daytime for 23 days, and finally disappeared from the night sky after 642 days. At the time, the Song dynasty was a world technological leader, having introduced paper money, gunpowder, and use of the magnetic compass for marine navigation. They did not yet have the telescope, however, and so could not know that the new guest star had been replaced by a much dimmer but still luminescent interstellar cloud, the Crab Nebula (Figure 13.1).

Yang's guest star was in fact a supernova, which has since been named SN 1054. It formed by the collapse of an aging star, which originally had a mass many times that of our own Sun. As it exhausted its core fuel supply, the star eventually reached a point where the energy released by nuclear fusion could no longer counteract the unimaginably large gravitational forces pulling inward. A violent implosion ensued, immediately followed by an explosion that temporarily made SN 1054 one of the brightest objects in the galaxy. Within seconds, the energy of this explosion also spawned a suite of new chemical elements, which were immediately hurled outward into interstellar space. Among them was one of the rarest naturally occurring elements of all, uranium.

Born of extreme violence, uranium remains inherently unstable or “radioactive” for the rest of its life, fated to spontaneous and inexorable decay to lighter elements. Some of these second-generation or “daughter” elements are themselves unstable, experiencing further decay until the process eventually reaches its end with drearily dull but reliably stable lead.

Type
Chapter
Information
Geofuels
Energy and the Earth
, pp. 261 - 286
Publisher: Cambridge University Press
Print publication year: 2015

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Brown, G., and Garnish, J., 2004, Geothermal energy: An overview, in Boyle, G., ed., Renewable Energy, 2nd ed.: Oxford, Oxford University Press, p. 342–382.Google Scholar
Burchfield, J. D., 1975, Lord Kelvin and the Age of the Earth: New York, Sci Hist Pub, 260 p.CrossRefGoogle Scholar
Carbon, M. W., 2006, Nuclear Power: Villain or Victim? 2nd ed.: Madison, WI, Pebble Beach, 108 p.Google Scholar
Dahlkamp, F. J., 1993, Uranium Ore Deposits: Berlin, Springer-Verlag, 460 p.CrossRefGoogle Scholar
Dickson, M. H., and Fanelli, M., eds., 2003, Geothermal Energy: Utilization and Technology: Paris, United Nations Educational, Scientific, and Cultural Organization, 205 p.
Duffield, W. A., and Sass, J. H., 2003, Geothermal-clean power from the Earth's heat: U.S. Geological Survey Circular 1249, 36 p.Google Scholar
Jaupart, C., and Mareschal, J.-C., 2011, Heat Generation and Transport in the Earth: Cambridge, Cambridge University Press, 464 p.Google Scholar
Jefferson, C. W., Thomas, D. J., Gandhi, S. S., Ramaekers, P., Delaney, G., Brisbin, D., Cutts, C., Quirt, D., Portella, P., and Olson, R. A., 2007, Unconformity associated uranium deposits of the Athabasca Basin, Saskatchewan and Alberta, in Goodfellow, W. D., ed., Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods: Geological Association of Canada, Mineral Deposits Division, Special Publication No. 5, p. 273–305.Google Scholar
KamLAND Collaboration, 2011, Partial radiogenic heat model for Earth revealed by geoneutrino measurements: Nature Geoscience, v. 4, p. 647–651.
McBride, J.P., Moore, R. E., Witherspoon, J. P., and Blanco, R. E., 1978, Radiological impact of airborne effluents of coal and nuclear plants: Science, v. 202, p. 1045–1050.Google ScholarPubMed
McKay, A. D., and Miezitis, Y., 2001, Australia's uranium resources, geology and development of deposits: AGSO – Geoscience Australia, Mineral Resource Report 1, 196 p.
Murray, R. L., Nuclear Energy – an Introduction to the Concepts, Systems, and Applications of Nuclear Processes, 4th ed.: Oxford, Pergamon Press,437 p.
Pollack, H. N., Hurter, S. J., and Johnson, J. R., 1993, Heat flow from the Earth's interior: Analysis of the global data set: Reviews of Geophysics, v. 31., p. 267–280.CrossRefGoogle Scholar
Pyle, D. M., 1995, Mass and energy budgets of explosive volcanic eruptions: Geophysical Research Letters, v. 22, p. 563–566.CrossRefGoogle Scholar
Taylor, S. R., and McLennan, S. M., 2009, Planetary Crusts: Cambridge, Cambridge University Press, 378 p.Google Scholar
Tester, J. W. (and 17 coauthors), 2006, The Future of Geothermal Energy: Impact of Enhanced Geothermal Systems (EGS) on the United States in the 21st Century: Cambridge, MA, Massachusetts Institute of Technology, 372 p.Google Scholar

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×