SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 58:1301-1307 (1994)
© 1994 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
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 Elder, A. N.
Right arrow Articles by Rasmussen, T. C.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Elder, A. N.
Right arrow Articles by Rasmussen, T. C.
Agricola
Right arrow Articles by Elder, A. N.
Right arrow Articles by Rasmussen, T. C.

Neutron Probe Calibration in Unsaturated Tuff

A. N. Elder

Tucson Water, 310 W. Alameda St., Tucson, AZ 85701

Todd C. Rasmussen*

Warnell School of Forest Resources, University of Georgia, Athens, GA 30602

*Corresponding author (trasmuss{at}uga.cc.uga.edu).

ABSTRACT

The measurement of water content in unsaturated media using neutron moisture probes requires a calibration relationship between neutron counts and water contents. Techniques for obtaining the relationship in unconsolidated geologic media may be unsuitable for consolidated media due to the difficulty of extracting undisturbed samples for water content analysis. The calibration relationship, {theta} = {alpha}0 + ({alpha}1 + {alpha}2{rho}b)C = {alpha}3{rho}b, with C = neutron counts, and {rho}b = dry bulk density, provided a good predictor of volumetric water content, {theta}, for consolidated media at the Apache Leap Tuff Site. Four techniques were employed to obtain data necessary to construct this relationship. Two methods employed a neutron transport code to predict neutron counts from scattering and absorption neutron cross sections. The first method calculated cross sections from elemental compositions, while the second used cross sections obtained from rock samples placed in a graphite pile containing a neutron source. The third method used in situ neutron counts measured in two access holes constructed in unsaturated rock with known water contents estimated from rock fragments excavated surrounding the access holes using a pneumatic hammer. The fourth technique used neutron counts from crushed rock packed into containers and maintained at prescribed water contents. Neutron cross sections obtained from elemental analyses were smaller than graphite-pile values, although the differences were insignificant at the 95% confidence level and the difference in rock water content predictions was small. The neutron transport model provided neutron count estimates consistent with in situ counts and counts from saturated crushed rock in containers.


NOTES

Work was performed at Dep. of Hydrology and Water Resources, Univ. of Arizona, Tucson.

Received for publication June 21, 1993.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1994 by the Soil Science Society of America.