VZJ Download to Citation Manager
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Sisson, J. B.
Right arrow Articles by Caldwell, T. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Sisson, J. B.
Right arrow Articles by Caldwell, T. G.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Sisson, J. B.
Right arrow Articles by Caldwell, T. G.
Related Collections
Right arrow Soil Physics
Right arrow Soil Hydrology
Right arrow Soil Methods/Instrumentation
Vadose Zone Journal 1:310-315 (2002)
© 2002 Soil Science Society of America

Notes

Advances in Tensiometry for Long-term Monitoring of Soil Water Pressures

J. B. Sissona, G. W. Gee*,b, J. M. Hubbella, W. L. Brattonc, J. C. Ritterb, A. L. Wardb and T. G. Caldwelld

a Geosciences Research Department, Idaho National Engineering and Environmental Laboratory, Bechtel Idaho, Incorporated, Idaho Falls, ID 83415
b Hydrology Group, Environmental Technology Division, Pacific Northwest National Laboratory, Richland, WA 99352
c Applied Research Associates, Inc., Richland, WA 99352
d Desert Research Institute, Reno, NV 89512

* Corresponding author (glendon.gee{at}pnl.gov)

Received 17 July 2001.

Soil water pressures, measured over space and time, are needed to predict the direction of water flow and chemical transport in the vadose zone. Advanced tensiometers (ATs), which utilize a water-filled porous cup connected directly to a pressure transducer, can be installed at almost any location and depth using standard drilling techniques such as auger drilling, but these methods can significantly disturb the site. For sites where minimal disturbance is desired, alternate approaches for tensiometer placement have been sought. To test installation techniques and performance longevity, advanced tensiometers were placed into the ground at a test site near Richland, WA using two different installation methods, auger drilling and a drive-cone push technique. The tensiometers were subsequently monitored for nearly 2 yr without refilling or recalibration. The data indicated that tensiometers placed by the auger technique took several months to equilibrate, while the cone push units came to equilibrium within 24 h following their installation. Soil water pressures always remained above -90 cm pressure head (-90 mbar) at depths >90 cm. At the greatest depth (730 cm), positive then negative pressures were observed as the water table was lowered and the soil drained. The results suggest that for our test conditions (coarse sandy soil, no vegetation), soil water pressures stay well within the tensiometer range and unit gradient conditions persist, indicating a draining profile. Advanced tensiometers, placed either by auger or cone penetrometer, provide a robust and reliable method for long-term monitoring of soil water pressure profiles.

Abbreviations: AT, advanced tensiometer • BGS, below ground surface • CPT, cone-penetrometer technology • DCT, drive-cone tensiometer • PVC, polyvinyl chloride




This article has been cited by other articles:


Home page
Vadose Zone JHome page
J. C. Seaman, B. B. Looney, and M. K. Harris
Research in Support of Remediation Activities at the Savannah River Site
Vadose Zone J., May 17, 2007; 6(2): 316 - 326.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
G. W. Gee, J. M. Keller, and A. L. Ward
Measurement and Prediction of Deep Drainage from Bare Sediments at a Semiarid Site
Vadose Zone J., February 1, 2005; 4(1): 32 - 40.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
G. W. Gee, Z. F. Zhang, S. W. Tyler, W. H. Albright, and M. J. Singleton
Chloride Mass Balance: Cautions in Predicting Increased Recharge Rates
Vadose Zone J., February 1, 2005; 4(1): 72 - 78.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
M. J. Singleton, E. L. Sonnenthal, M. E. Conrad, D. J. DePaolo, and G. W. Gee
Multiphase Reactive Transport Modeling of Seasonal Infiltration Events and Stable Isotope Fractionation in Unsaturated Zone Pore Water and Vapor at the Hanford Site
Vadose Zone J., August 1, 2004; 3(3): 775 - 785.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
J. M. Hubbell and J. B. Sisson
Comments on "Tensiometer modification for diminishing errors due to the fluctuating inner water column"
Soil Sci. Soc. Am. J., March 1, 2004; 68(2): 709 - 710.
[Full Text] [PDF]


Home page
Vadose Zone JHome page
D. L. McElroy and J. M. Hubbell
Evaluation of the Conceptual Flow Model for a Deep Vadose Zone System Using Advanced Tensiometers
Vadose Zone J., February 1, 2004; 3(1): 170 - 182.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
J. M. Hutchison, J. M. Hutchison, J. C. Seaman, S. A. Aburime, and D. E. Radcliffe
Chromate Transport and Retention in Variably Saturated Soil Columns
Vadose Zone J., November 1, 2003; 2(4): 702 - 714.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2002 by the Soil Science Society of America.