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 ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wuest, S. B.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wuest, S. B.
Agricola
Right arrow Articles by Wuest, S. B.
Related Collections
Right arrow Crop Growth and Development
Right arrow Seed Establishment
Right arrow Hydraulic Conductivity

Water Transfer from Soil to Seed

The Role of Vapor Transport

Stewart B. Wuest*

USDA-ARS, Columbia Plateau Conservation Research Center, P.O. Box 370, Pendleton, OR 97801



View larger version (134K):

[in a new window]
 
Fig. 1. Apparatus used to produce different amounts of seed-soil distance. Two of the ten seed positions had no hole, resulting in the seed being pressed directly into the soil. Wheat seed was glued to the plastic dowel.

 


View larger version (19K):

[in a new window]
 
Fig. 2. Water gain and dye coverage of wheat seed suspended in holes of different diameter for 24 h. Error bars, where large enough to be seen, show standard error of the mean (n = 42). There were two zero diameter (no hole) positions in each soil block. Dotted lines indicate averages for the five runs with the greatest soil water potential (-0.07 MPa) and for the four driest (-1.3 MPa). Average soil water potential for all 42 runs was -0.16 MPa.

 


View larger version (19K):

[in a new window]
 
Fig. 3. Comparison of water gain and germination for wheat seed in good seed-soil contact and for seed suspended in 11-mm holes. Individual seed weights were used to calculate water gain on a dry weight basis. (a) Oven-dried (105°C) seed. At 64 h, water gain was 18.1 mg for soil contact and 17.5 mg for 11-mm holes. (b) Normal seed. The large increase in water gain at 55 h by seeds in soil contact is probably due to root growth, averaging 7 mm. Error bars, where large enough to be seen, show standard error of the mean: (a) n = 3, (b) n = 5.

 





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 © 2002 by the Soil Science Society of America.