Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-09T08:15:18.663Z Has data issue: false hasContentIssue false

Chapter 7 - Wavelet amplification in an inhomogeneous plasma

Published online by Cambridge University Press:  02 May 2010

V. Y. Trakhtengerts
Affiliation:
Institute of Applied Physics, Russian Academy of Sciences
M. J. Rycroft
Affiliation:
Cranfield University, UK
Get access

Summary

In Chapter 6 the case of a whistler-mode wave with a given amplitude was considered. However, many processes which influence cyclotron maser behaviour demand a selfconsistent approach, which takes into account the feedback effects of gyroresonant electrons on the wave field.

The first step in this approach is an analysis of the linear amplification (or damping) of a whistler-mode wave by electrons with different velocity distributions. This problem was tackled in Chapters 3 and 4 for a monochromatic whistler-mode wave. There it was shown that the cyclotron amplification for a broad velocity distribution function (|Δv|/v ∼ 1) is the same for homogeneous and weakly inhomogeneous plasmas (compare Sections 3.2 and 3.4). The situation with amplification by well-organized electron beams (such as a step-like deformation or a delta-function in v-velocity space) is more complicated (see Sections 3.3 and 3.5) and strongly differs from the cases of homogeneous and weakly inhomogeneous plasmas. This difference is as follows. First, the hydrodynamic type of instability of a well-organized beam in a homogeneous plasma is replaced by the kinetic-type instability in an inhomogeneous plasma. Secondly, the amplification in inhomogeneous plasmas strongly depends on the spatial gradients of the plasma parameters, specifically the plasma density and magnetic field strength. The amplification of a monochromatic wave is large very close to the equatorial plane of a magnetic flux tube. It decreases sharply (and even changes sign for a delta-function distribution) beyond this interval.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2008

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
×