HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Abstract Full Text Free Full Text (PDF) Free Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Zhou, M. Articles by O'Hair, S. K. Search for Related Content PubMed Articles by Zhou, M. Articles by O'Hair, S. K. GeoRef GeoRef Citation Agricola Articles by Zhou, M. Articles by O'Hair, S. K. Related Collections Agricultural Pesticides Pesticides Organic Compounds

Endosulfan Losses through Runoff and Leaching from Calcareous Gravelly or Marl Soils

^a Department of Soil and Water Science and Department of Horticultural Sciences, University of Florida's Institute of Food and Agricultural Sciences, at the Tropical Research and Education Center, Homestead, FL 33031
^b Soil and Science Department, University of Florida's Institute of Food and Agricultural Sciences, Gainesville, FL 33611

View larger version (20K): [in a new window]   Fig. 1. The effect of rainfall intensity on sediment concentrations in runoff and cumulative runoff sediment mass as a function of cumulative rainfall for the Biscayne marl soil.

View larger version (25K): [in a new window]   Fig. 2. The effect of water table depth (WTD) on sediment concentrations in runoff and cumulative runoff sediment mass as a function of cumulative rainfall for the Krome soil.

View larger version (19K): [in a new window]   Fig. 3. The effect of soil type on sediment concentrations in runoff and cumulative runoff sediment as a function of cumulative rainfall.

View larger version (11K): [in a new window]   Fig. 4. The concentrations of endosulfan (filled symbols) and ß (open symbols) in leachates as a function of cumulative rainfall mass for the Krome soil at 150 mm h-1 rainfall intensity.

View larger version (13K): [in a new window]   Fig. 5. Measured and calculated endosulfan concentrations in runoff water vs. the sum of cumulative rainfall depth and apparent runoff sediment depths for Krome soil at all water table depths.

View larger version (13K): [in a new window]   Fig. 6. Measured and calculated endosulfan ß concentrations in runoff water vs. the sum of cumulative rainfall depth and apparent runoff sediment depth for Krome soil at all water table depths.

View larger version (16K): [in a new window]   Fig. 7. Measured and calculated endosulfan concentrations in runoff water vs. the sum of cumulative rainfall depth and apparent runoff sediment depth for Biscayne marl soil. Endosulfan at 150 mm h-1 rainfall (open squares), endosulfan at 75 mm h-1 rainfall (filled squares), endosulfan ß at 150 mm h-1 rainfall (open circles), endosulfan ß at 75 mm h-1 rainfall (filled circles).