Skip to main content Accessibility help
×
Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-20T17:44:06.011Z Has data issue: false hasContentIssue false

5 - Ultra high energy gamma-rays

Published online by Cambridge University Press:  06 July 2010

P. V. Ramana Murthy
Affiliation:
Tata Institute of Fundamental Research, Mumbai, India
A. W. Wolfendale
Affiliation:
University of Durham
Get access

Summary

Introduction

Studies of ultra high energy gamma-rays (UHEGR) i.e. γ-rays at energies greater than 100 GeV, provide us with information on the conditions existing in remote celestial regions, such as magnetic and electric fields, matter and radiation densities, and on the acceleration mechanisms of charged particles. Additionally such studies have an important bearing on the problem of the origin of the cosmic radiation. There is, as yet, no universally accepted identification of either the sources or the mechanisms of production of cosmic rays, though, as was pointed out in Chapter 4, there are strong arguments made in favour of some. The problem is confounded by the fact that cosmic rays, almost all of which are charged particles, undergo frequent deflections in the interstellar magnetic fields, making it impossible to know the source directions. Thus, even a primary cosmic ray proton of energy as high as 1015 eV has a Larmour radius in the ISM of only ∼ 0.3pc and has its initial direction almost isotropised. Electrically neutral radiation is free from this problem. The more commonly occurring neutral particles are neutrons, neutrinos and γ-rays. Neutrons are unstable; they would not survive in most cases from source to Earth even after allowing for relativistic time dilatation, with a decay mean free path of only 9.2 (E/1015 eV) pc. Neutrinos, being weakly interacting, are not easy to detect, γ-rays, on the other hand, are ideal as their production and interaction cross sections are rather high and they are stable.

Type
Chapter
Information
Gamma-ray Astronomy , pp. 173 - 232
Publisher: Cambridge University Press
Print publication year: 1993

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.)

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
×