JEQ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
QUICK SEARCH:   [advanced]


     

This Article
Right arrow Abstract Freely available
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 Similar articles in ISI Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (4)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Garrido, F.
Right arrow Articles by Chendorain, M.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Garrido, F.
Right arrow Articles by Chendorain, M.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Garrido, F.
Right arrow Articles by Chendorain, M.
Related Collections
Right arrow Soil Physics
Right arrow Vadose Zone Processes and Chemical Transport
Right arrow Soil Analysis

Detailed Characterization of Solute Transport in a Heterogeneous Field Soil

Fernando Garridoa, Masoud Ghodratib, Chris G. Campbellb and Michael Chendorainb

a Centro de Ciencias Medioambientales, Consejo Superior de Investigaciones Científicas, Serrano 115-dup. E-28006-Madrid, Spain
b Ecosystem Sciences Division, Dep. of Environmental Science Policy and Management, Univ. of California, 151 Hilgard Hall, Berkeley, CA 94720-3110



View larger version (51K):

[in a new window]
  		Fig. 1. Schematic plot design and instrumentation. Fiber optic miniprobes (FOMPs) and time domain reflectometry (TDR) are identified by their respective numbers at each depth level

 


View larger version (82K):

[in a new window]
  		Fig. 2. Plot of the mass recoveries of the fiber optic miniprobes (FOMPs) at different spatial locations in the plot

 


View larger version (22K):

[in a new window]
  		Fig. 3. Breakthrough curves (BTCs) measured by the fiber optic miniprobes (FOMPs) at the 0.10-m depth for a 20-mm pulse of 4 g/L pyranine. MR = mass recovery

 


View larger version (34K):

[in a new window]
  		Fig. 4. Breakthrough curves (BTCs) measured by the fiber optic miniprobes (FOMPs) at the 0.20-m depth for a 20-mm pulse of 4 g/L pyranine. MR = mass recovery

 


View larger version (28K):

[in a new window]
  		Fig. 5. Cumulative breakthrough curves (BTCs) of conservative CaCl2 measured during the calibration of the time domain reflectometry (TDR) probes

 


View larger version (22K):

[in a new window]
  		Fig. 6. Breakthrough curves (BTCs) measured by the time domain reflectometry (TDR) probes at the 0.10-m depth for a 20-mm pulse of 4 g/L pyranine. MR = mass recovery

 


View larger version (14K):

[in a new window]
  		Fig. 7. Breakthrough curves (BTCs) measured by the time domain reflectometry (TDR) probes at the 0.20-m depth for a 20-mm pulse of 4 g/L pyranine. MR = mass recovery

 


View larger version (16K):

[in a new window]
  		Fig. 8. Response measured by the 0.05-m-long time domain reflectometry (TDR) probes inserted into the first 50 mm of the soil horizon

 


View larger version (28K):

[in a new window]
  		Fig. 9. The bimodal convective lognormal transfer function (CLT) model fitted to the four time domain reflectometry (TDR) probes at the 0.10-m depth in the soil

 




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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.