SSSAJ
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 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 ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hwang, S. I.
Right arrow Articles by Powers, S. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Hwang, S. I.
Right arrow Articles by Powers, S. E.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Hwang, S. I.
Right arrow Articles by Powers, S. E.
Related Collections
Right arrow Hydraulic Conductivity/Relative Permeability
Right arrow Water Retention/Capillary Pressure
Right arrow Variably Saturated Fluid Flow

Using Particle-Size Distribution Models to Estimate Soil Hydraulic Properties

Sang Il Hwang and Susan E. Powers*

Dep. of Civil and Environmental Engineering, Clarkson Univ., 8 Clarkson Ave., Potsdam, NY 13699-5710



View larger version (22K):

[in a new window]
 
Fig. 1. Box plot for Akaike's information criterion (AIC) percentiles as the goodness-of-fit of four PSD models for all 24 soils.

 


View larger version (20K):

[in a new window]
 
Fig. 2. Comparative fit of (a) the PSD and (b) h({theta}) curves using four PSD models for a sand (UNSODA No. 3132).

 


View larger version (30K):

[in a new window]
 
Fig. 3. An illustration of experimental and predicted h({theta}) curves using four PSD models for each textural class, (a) sand (UNSODA 4650), (b) sandy loam (UNSODA 3310), (c) silt loam (UNSODA 1341), and (d) clay soils (UNSODA 1400).

 


View larger version (31K):

[in a new window]
 
Fig. 4. An illustration of experimental and predicted K({theta}) curves using four PSD models for each textural class, (a) sand (UNSODA 4650), (b) sandy loam (UNSODA 4160), (c) loam (UNSODA 2531), and (d) clay soils (UNSODA 1400).

 


View larger version (44K):

[in a new window]
 
Fig. 5. Comparison of experimental and predicted (a) pressure heads and (b) hydraulic conductivities for four PSD models. The 24 soils are pooled for pressure heads and 12 soils for hydraulic conductivities.

 


View larger version (33K):

[in a new window]
 
Fig. 6. Examples of the PSD and the VSD of two soils as affected by the PSD models: (a1) the PSD and (a2) the VSD of a sand soil (UNSODA No. 4650), and (b1) the PSD and (b2) the VSD of a silt loam soil (UNSODA No. 1341).

 


View larger version (20K):

[in a new window]
 
Fig. 7. An example of ri vs. Qi plot for a sand soil (UNSODA No. 4650).

 


View larger version (72K):

[in a new window]
 
Fig. 8. Variation of AIC and root mean squared errors (RMSEs) associated with estimates of (a) h({theta}) curve and (b) K({theta}) curve for each textural class.

 





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 © 2003 by the Soil Science Society of America.