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 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 Web of Science (6)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lapen, D. R.
Right arrow Articles by Wang, C.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Lapen, D. R.
Right arrow Articles by Wang, C.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Lapen, D. R.
Right arrow Articles by Wang, C.

Placic and Ortstein Horizon Genesis and Peatland Development, Southeastern Newfoundland

David R. Lapena and Chang Wanga

a Eastern Cereal and Oilseed Research Centre, Agriculture Canada, Ottawa, ON, Canada K1A 0C6



View larger version (46K):

[in a new window]
 
Fig. 1 Study site location, Pedons 1 through 8 (P1 to P8), and locations of 14C dates of organic soils (yr BP). Pedon 2* is located in the upland poor fen in a better drained topographic position SW of P2. See Table 1 and 3 for pedon descriptions

 


View larger version (31K):

[in a new window]
 
Fig. 2 Average daily soil temperatures (point graph), total daily rain depths (bar graph), and water table depths at selected locations in the peatland complexes (point graph) during the study period. Symbol legends for soil temperature and water table depth indicate measurement depths below surface and well locations, respectively. Note: water tables were recorded in soils above the sesquioxide pans

 


View larger version (35K):

[in a new window]
 
Fig. 3 Physical properties of pedon mineral soil horizons. Pedon number is given in small box in upper left hand corner of graph sets. Grain size (GS) on bar graph: clay = black, silt = white, sand = diagonal stripes; horizontal hydraulic conductivity Kz = {square}, vertical hydraulic conductivity Kx = {blacktriangledown}; bulk density Db = • (averages of at least 5 samples). Saturated hydraulic conductivity Ksat values are geometric averages of at least 3 samples

 


View larger version (36K):

[in a new window]
 
Fig. 4 Average daily relative saturation S ({triangledown}) and redox potential (•) profiles for selected pedons on Days 193, 194, 196, and 204. Dotted S and redox lines are for Pedon 2*. Dashed lines indicate standing water level in the soil pits. Redox and {theta} measurements were taken after the soil pits were pumped free of standing water. Redox potentials are averages of three measurements

 





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 © 1999 by the Soil Science Society of America.