JEQ
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 PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Moffet, C. A.
Right arrow Articles by Sosebee, R. E.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Moffet, C. A.
Right arrow Articles by Sosebee, R. E.
Agricola
Right arrow Articles by Moffet, C. A.
Right arrow Articles by Sosebee, R. E.
Related Collections
Right arrow Municipal Waste
Right arrow Runoff
Right arrow Infiltration
Right arrow Soil Erosion

Surface Biosolids Application

Effects on Infiltration, Erosion, and Soil Organic Carbon in Chihuahuan Desert Grasslands and Shrublands

C. A. Moffeta,*, R. E. Zartmanb, D. B. Westerc and R. E. Sosebeec

a USDA-ARS, Northwest Watershed Research Center, 800 Park Boulevard, Plaza IV, Suite 105, Boise, ID 83712
b Department of Plant and Soil Science, Texas Tech University, Lubbock, TX 79409
c Department of Range, Wildlife and Fisheries Management, Texas Tech University, Lubbock, TX 79409



View larger version (27K):

[in a new window]
 
Fig. 1. Infiltration rate (cm h–1) during a 30-min simulated rainfall (164 mm h–1) for two Stellar soil cover conditions with 0, 7, 34, and 90 dry Mg ha–1 of biosolids: (A) bare Stellar soil and (B) vegetated Stellar soil. Steady-state infiltration values within the same level of cover labeled with the same letter are not different ({alpha} = 0.05).

 


View larger version (20K):

[in a new window]
 
Fig. 2. Cumulative infiltration (cm) during a 30-min simulated rainfall (168 mm h–1, winter; 159 mm h–1, summer) for two trial seasons with two Stellar soil cover conditions and 0, 7, 34, and 90 dry Mg ha–1 of biosolids: simulated rain applied in (A) summer and (B) winter. Points with the same level of season and cover labeled with the same letter are not different ({alpha} = 0.05).

 


View larger version (25K):

[in a new window]
 
Fig. 3. Cumulative infiltration (cm) and standard error bars during a 30-min simulated rainfall during three trials (166 mm, winter of 1994; 159 mm, summer of 1994; 167 mm, winter of 1995) for two Stellar soil cover conditions treated with 90 dry Mg ha–1 of biosolids on four different occasions (Batch 1, summer of 1993; Batch 2, winter of 1994; Batch 3, summer of 1994; and Batch 4, winter of 1995): (A) bare Stellar soil and (B) vegetated Stellar soil.

 


View larger version (20K):

[in a new window]
 
Fig. 4. Cumulative erosion (Mg ha–1) during a 30 min simulated rainfall (79 mm) from three soil–cover combinations with 0, 7, 34, and 90 dry Mg ha–1 of biosolids. The analysis was performed on log-transformed cumulative erosion estimates, but the results are presented in back-transformed units. Points with the same level of "soil" labeled with the same letter are not different ({alpha} = 0.05).

 





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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 2005 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.