The concentration and temperature dependences of the imaginary part of the permittivity of water with conducting impurities are determined on the basis of mathematical modeling and experimental studies. It is shown that the values of permittivity imaginary part of water samples of thermokarst lakes calculated using the Stogrin formulas and measured are different. Experimental data on the permittivity of water bodies of the test area at the operating frequency of an aerospace vehicle in the temperature range is needed for interpretation of remote sensing results of the Earth.
Access to the requested content is limited to institutions that have purchased or subscribe to SPIE eBooks.
You are receiving this notice because your organization may not have SPIE eBooks access.*
*Shibboleth/Open Athens users─please
sign in
to access your institution's subscriptions.
To obtain this item, you may purchase the complete book in print or electronic format on
SPIE.org.
INSTITUTIONAL Select your institution to access the SPIE Digital Library.
PERSONAL Sign in with your SPIE account to access your personal subscriptions or to use specific features such as save to my library, sign up for alerts, save searches, etc.