Abstract
Diurnal cycles of soil temperature and heat flux measured on the Pampa de La Joya, Peru are analyzed harmonically. A theory of thermal diffusion put forth by H. H. Lettau (1962) is used to determine the relative calibration of the soil heat flux plates and the relative depth intervals between the flux plates in comparison with the soil temperature profile. The absolute value of the soil heat flux is based on an allowed range of values for the density of the soil.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
