SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 13 May 2009
Published in Soil Sci Soc Am J 73:1113-1118 (2009)
DOI: 10.2136/sssaj2008.0297
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Robinson, D. A.
Right arrow Articles by Doyle, T. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Robinson, D. A.
Right arrow Articles by Doyle, T. E.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Robinson, D. A.
Right arrow Articles by Doyle, T. E.
Related Collections
Right arrow Tropical Soils
Right arrow Structure and Properties
Right arrow Time Domain Reflectometry, TDR

SOIL PHYSICS

The Dielectric Response of the Tropical Hawaiian Mars Soil Simulant JSC Mars-1

David A. Robinsona,*, Scott B. Jonesb, J. Mark Blonquist, Jr.b, Robert Heinseb, Inma Lebrona and Timothy E. Doylec

a Dep. of Food Production, Univ. of the West Indies, St. Augustine, Trinidad & Tobago
b Dep. of Plants, Soils and Climate, Utah State Univ., Old Main Hill, Logan, UT 84322
c Dep. of Physics, Utah State Univ., Old Main Hill, Logan, UT 84322

* Corresponding author (darearthscience{at}yahoo.com).

The observation of low dielectric values <2, consistent with the bright areas of the surface of Mars, is completely counter to expectation for soils dominated by mafic minerals, especially Fe minerals and pyroxenes that tend to have dielectric values two to three times higher than quartz, which has a value of 4.7. To this day, this observation has not been explained. The recent success of the Phoenix lander in locating water on Mars, however, is renewing interest in the use of sensors to determine Martian soil properties. We took measurements on the Hawaiian JSC Mars-1 soil simulant, considered to reflect the properties of the soils of the bright regions of Mars. Our objective was to determine if soil structure and dielectric phase configuration could account for low dielectric responses. We discovered that low dielectric values can be reconciled with mafic, Fe-bearing silicate mineralogy due to the presence of a palagonite structure with internal porosity. Furthermore, dielectric response as a function of water content is startlingly lower than standard soil calibration equations from Earth, meaning that the application of these equations may significantly underestimate water content determined from dielectric measurements—not because of "bound water," but because of the altered dielectric phase configuration due to the palagonite internal pore structure. The implications of this finding for future planetary missions are that all sensors relying on interpreting soil properties from measurements of bulk soil electrical, thermal, or dielectric properties will be similarly affected in the presence of materials with internal porosity.

Abbreviations: WRC, water release curve







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2009 by the Soil Science Society of America.