Agronomy Journal
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 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 Web of Science (5)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bremer, D. J.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Bremer, D. J.
Agricola
Right arrow Articles by Bremer, D. J.
Related Collections
Right arrow Agroclimatology
Right arrow Turfgrass Management
Right arrow Water Use
Right arrow Soil Methods/Instrumentation
Right arrow Evapotranspiration
Right arrow Lysimeter/Rhizosphere Studies
Right arrow Turfgrass
Right arrow Maize Management

Evaluation of Microlysimeters Used in Turfgrass Evapotranspiration Studies Using the Dual-Probe Heat-Pulse Technique

Dale J. Bremer*

Dep. of Horticulture, Forestry & Recreation Resources, 2021 Throckmorton Hall, Kansas State Univ., Manhattan, KS 66506



View larger version (31K):

[in a new window]
 
Fig. 1. Comparisons of volumetric soil water content from DPHP sensors: A) among MSL and PSL containers and the Ambient soil [average 5, 15, and 25 cm (0- to 30-cm profile)]; and B) between MSNL and the Ambient soil [average 5 and 15 cm (0- to 20-cm profile)]. Vertical dashed lines highlight irrigation dates. Symbols (x) along the abscissa of each graph indicate significant differences between MSL and ambient soil (P < 0.05), and plus (+) indicates significant differences between both MSL and PSL and the ambient soil on a given day (at 1800 h).

 


View larger version (39K):

[in a new window]
 
Fig. 2. Green leaf area index (A) and aboveground biomass (B) in MSL, PSL, MSNL, MFCL, and WPSL microlysimeters and in the surrounding turfgrass. Means in each plot (A and B) with the same letter are not significantly different (P < 0.05).

 


View larger version (40K):

[in a new window]
 
Fig. 3. Comparisons of volumetric water content from DPHP sensors at 5 (A) and 15 cm (B) among MSL, PSL, MSNL, and Ambient soil, and at 25 cm (C) among MSL, PSL, and Ambient soil. Vertical dashed lines highlight irrigation dates. Symbols (plus-x) along abscissa of each graph indicate significant differences among three treatments (P < 0.05), and x indicates significant differences between two treatments on a given day (at 1800 h).

 


View larger version (28K):

[in a new window]
 
Fig. 4. Comparisons of volumetric water content from DPHP sensors: A) among MSL and PSL containers and the Ambient soil [average 5, 15, and 25 cm (0- to 30-cm profile)]; and B) between MSNL and the Ambient soil [average 5 and 15 cm (0- to 20-cm profile)]. Vertical dashed lines highlight irrigation date. Symbols (x) along the abscissa of each graph indicate significant differences between MSL and ambient soil (P < 0.05), and plus (+) indicates significant differences between both MSL and PSL and the ambient soil on a given day (at 1800 h).

 


View larger version (36K):

[in a new window]
 
Fig. 5. Comparisons of volumetric water content from DPHP sensors at 5 (A) and 15 cm (B) among MSL, PSL, MSNL, and Ambient soil, and at 25 cm (C) among MSL, PSL, and Ambient soil. Vertical dashed lines highlight irrigation date. Symbols (x) along abscissa of each graph indicate significant differences between MSL and Ambient soil (P < 0.05), diamond-x indicates significant differences between MSL and both Ambient soil and MSNL, and plus (+) indicates significant differences between both MSL and PSL and the Ambient soil on a given day (at 1800 h).

 


View larger version (18K):

[in a new window]
 
Fig. 6. Comparison of volumetric water content ({theta}v) as determined by DPHP sensors and gravimetric (Lysimeter) methods for MSL (A), PSL (B), and MSNL (C) microlysimeters.

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Crop Science Vadose Zone Journal
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 © 2003 by the American Society of Agronomy.