KEGS/BCGS Roundup Breakfast 2018

KEGS/BCGS Roundup Breakfast – Tuesday, January 23, 2017

Speaker: Dr. Jaymie Matthews, UBC Astronomy Professor

Title: Asteroseismology: Stealing the geophysicists’ rule book and launching it into space

Date/Time: 2018-01-23 @ 7:30am – 9:00am

Location: Princess Louisa Room, The Fairmont Waterfront Hotel
900 Canada Place, Vancouver, BC V6C 3L5

Registration: Online at www.kegsonline.org (Deadline Jan 22, 2017)

Abstract:

Astronomers have been updating the biography of the Sun for decades, at the same time trying to confirm models of its internal structure. Like the Earth – of which we can sample directly less than 0.2% of its total depth – most of the interior of the Sun is hidden from direct view. Except for neutrinos from the solar core, we receive direct information only from a surface layer of gas whose depth is only 0.05% of the radius of the Sun.

Astronomers, faced with the same challenge that geophysicists had tackled before us when they wanted probe the deep interior of the Earth, turned to the rule book of geoseismology. For the Sun, we could apply principles of global seismology and eventually local time-distance seismology, using the intrinsic vibrations of the Sun caused by sound waves propagating in the solar interior. Much of this was possible for the Sun with telescopes grounded on Earth, because of the extremely high signal-to-noise and surface spatial sampling possible for solar observations. But when it came to extending this technique to the distant stars, by asteroseismology, it was necessary not to toss out the rule book, but to toss it up, into space.

Canada’s first space telescope, called MOST, was one of the pioneers, later joined by the French CoRoT space mission and eventually NASA’s Kepler satellite. These are the most sophisticated stellar lightmeters ever built, and launching them into space launched a revolution in ultraprecise photometry of stars and exoplanets. That in turn launched a revolution in our ability to seismically probe distant stars, and to put our own Sun in better context by studying the interiors of other suns. Not just ‘middle-aged’ suns like our own, but senior suns, and teen suns, and baby suns, and even suns still in the womb.

Even for our own Sun, the seismic data are driving the physics, so we need to include what used to be considered third-order effects lost in the noise, if we’re to match models to observed frequencies to within their measured accuracies.

Join me on a voyage through space and time, where the guide book contains the principles of time series analysis and mathematical inversion, to see how far we have come in the last 15 years, and the exciting frontiers that are ahead of us.

January 2018 – Technical Talk

BCGS Technical Talk – January 18, 2018

Speaker: Doug Schouten, PhD, CRM GeoTomography Technologies Inc.

Title: Muon Tomography Applied to a Dense Uranium Deposit at the McArthur River Mine

Date/Time: Thursday, January 18, 2018

Location: 4th Floor Conference Room, Room 451, 409 Granville St. (UK Building at Granville and Hastings), Vancouver

Abstract:

Muon Tomography Applied to a Dense Uranium Deposit at the McArthur River Mine.
Doug Schouten, PhD, CRM GeoTomography Technologies Inc.

Muon radiography is a means of inferring density by measuring the attenuation of muon (a type of elementary particle naturally abundant from cosmic ray radiation) flux through matter. Muon tomography uses tomographic methods to derive 3D density maps from multiple muon flux measurements.

Measurements of the muon flux were first used by E. P. George (1955) to measure the overburden of a railway tunnel, and by Alvarez et al (1970) in searches for hidden chambers within pyramids. More recently, muon radiography has been used in volcanology, and has also been considered for industrial and security applications. CRM Geotomography Technologies, Inc. (CRM), a spin-off from TRIUMF, is bringing muon tomography technology to bear in mineral  exploration.

In this talk, I will report on the first application of muon tomography for imaging dense uranium deposits within the Athabasca Basin in Canada, performed by CRM at Cameco and Areva’s McArthur River mine in Northern Saskatchewan. I will demonstrate the applicability of muon tomographic imaging using data acquired at a depth of about six hundred meters underground. I will show that the statistical significance of the known uranium deposit signature in the muon data is very high (larger than five standard deviations), and I will report on the very good compatibility of the corresponding 3D density inversion with drill assay data from the deposit. I will also briefly recap other recent progress by CRM in various applications of muon tomography.