Journal cover Journal topic
Solid Earth An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.380 IF 2.380
  • IF 5-year value: 3.147 IF 5-year
    3.147
  • CiteScore value: 3.06 CiteScore
    3.06
  • SNIP value: 1.335 SNIP 1.335
  • IPP value: 2.81 IPP 2.81
  • SJR value: 0.779 SJR 0.779
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 32 Scimago H
    index 32
  • h5-index value: 31 h5-index 31
Discussion papers
https://doi.org/10.5194/sed-6-487-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/sed-6-487-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Submitted as: research article 11 Feb 2014

Submitted as: research article | 11 Feb 2014

Review status
This discussion paper is a preprint. It has been under review for the journal Solid Earth (SE). The revised manuscript was not accepted.

Is there a layer deep in the Earth that uncouples heat from mechanical work?

S. J. Burns1 and S. P. Burns2,3 S. J. Burns and S. P. Burns
  • 1Materials Science Program, Department of Mechanical Engineering, University of Rochester, Rochester, New York 14627, USA
  • 2National Center for Atmospheric Research, Boulder, Colorado 80301, USA
  • 3Department of Geography, University of Colorado, Boulder, Colorado 80309, USA

Abstract. The thermal expansion coefficient is presented as the coupling between heat energy and mechanical work. It is shown that when heat and work are uncoupled then very unusual material properties occurs: for example, acoustic p waves are not damped and heat is not generated from mechanical motion. It is found that at pressures defined by the bulk modulus divided by the Anderson–Grüneisen parameter, then the thermal expansion coefficient approaches zero in linear-elastic models. Very large pressures always reduce thermal expansion coefficients; the importance of a very small or even negative thermal expansion coefficient is discussed in relation to physical processes deep in the core and mantle of Earth. Models of the thermal expansion coefficients based on interatomic potentials which are always relegated to isometric conditions preclude any changes in volume due to temperature changes. However, it is known that the pressures in the Earth are large enough to effectively reduce thermal expansion coefficients to near zero which decouples heat from mechanical work.

S. J. Burns and S. P. Burns
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
S. J. Burns and S. P. Burns
S. J. Burns and S. P. Burns
Viewed  
Total article views: 1,163 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
637 487 39 1,163 29 34
  • HTML: 637
  • PDF: 487
  • XML: 39
  • Total: 1,163
  • BibTeX: 29
  • EndNote: 34
Views and downloads (calculated since 11 Feb 2014)
Cumulative views and downloads (calculated since 11 Feb 2014)
Cited  
Saved  
Discussed  
No discussed metrics found.
Latest update: 19 Oct 2019
Publications Copernicus
Download
Citation