My Account: Log In | Join | Renew
Search
Author
Title
Vol.
Issue
Year
1st Page

Abstract

 

This article in SSSAJ

  1. Vol. 63 No. 4, p. 955-961
     
    Received: Apr 17, 1998
    Published: July, 1999


    * Corresponding author(s): hlin@uwsp.edu
 View
 Download
 Alerts
 Permissions

doi:10.2136/sssaj1999.634955x

Effects of Soil Morphology on Hydraulic Properties II. Hydraulic Pedotransfer Functions

  1. H. S. Lin *a,
  2. K. J. McInnesb,
  3. L. P. Wildingb and
  4. C. T. Hallmarkb
  1. a College of Natural Resources, Univ. of Wisconsin, Stevens Point, WI 54481 USA
    b Dep. of Soil and Crop Sciences, Texas A&M Univ., College Station, TX 77843-2474 USA

Abstract

Pedotransfer functions (PTFs) have gained recognition in recent years as an approach to translate simple soil characteristics found in soil surveys into more complicated model input parameters. However, existing pedotransfer functions have not yet incorporated critical soil structural information. This study showed that soil hydraulic properties could be estimated from morphological features determined in situ (including texture, initial moisture state, pedality, macroporosity, and root density) through a morphology quantification system. Comparison between the class and continuous PTFs developed in this study indicated that the use of quantified morphological properties yielded predictive power similar to that of physical properties in estimating hydraulic conductivity at zero potential; water flow rates in macro-, meso-, and micropores; and a soil structure and texture parameter αmacro The results confirmed that soil structure was crucial in characterizing hydraulic behavior in macropore flow region; whereas texture had major impact on those hydraulic properties controlled by micropores. Depending on the flow domain to be included, estimation of hydraulic properties required the use of different combinations of morphometric indices or physical properties. The PTFs established may be used as starting points for estimating model input parameters.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © 1999. Soil Science SocietySoil Science Society of America

Facebook   Twitter