JEQ Grow Your Career With ASA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 14:224-228 (1985)
© 1985 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
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 Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Goldberg, B. S.
Right arrow Articles by Angle, J. S.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Goldberg, B. S.
Right arrow Articles by Angle, J. S.
Agricola
Right arrow Articles by Goldberg, B. S.
Right arrow Articles by Angle, J. S.

Aflatoxin Movement in Soil1

B. S. Goldberg and J. S. Angle2

ABSTRACT

Crops contaminated with > 20 µg kg–1 aflatoxin cannot be transported across state lines. Contaminated preharvest crops are often disposed of by plowing the crop into the soil, thereby creating the potential for aflatoxin contamination of groundwater. The objective of this study was thus to determine the leaching and adsorption potential of aflatoxin in soils.

Leaching and adsorption studies were conducted with a silt loam, clay loam, sandy loam, and silty clay loam soil. Soil columns were utilized in the leaching experiment. The length of the column and the volume of soil used were 30.54 cm and 1234 cm3, respectively. A total of 2.5 mg aflatoxin B1 was applied to the soil surface and the column was leached with 1 L of water under saturated conditions for 24 h. The results demonstrate that aflatoxin B1 or its derivatives, aflatoxin B2 and G2, were retained within the upper 20 cm of all soil types. Between 80 and 92% of the total amount of aflatoxin applied was retained in the upper 2.5 cm of the soil columns. No aflatoxin was found in the leachate from any of the soils.

Freundlichs isotherm was used to establish adsorption coefficients for the soils by the slurry technique. The concentrations of aflatoxin used to establish the constants were 0.1, 1.0, 5.0, and 10 mg L–1. The resulting adsorption coefficients were 238, 76, 46, and 17 mg kg–1 for the silty clay loam, silt loam, clay loam, and sandy loam, respectively. As a result of the two experiments, aflatoxin contamination of groundwater would not be expected to occur unless the soils were extremely sandy or shallow.

Key Words: adsorption • groundwater contamination • mycotoxin


NOTES

1 Scientific Article no. A-3831 and Contribution no. 6811 of the Maryland Agric. Exp. Stn., Dep. of Agron., Univ. of Maryland, College Park, MD 20742.

2 Graduate research assistant and assistant professor, Dep. of Agron., Univ. of Maryland.

Received for publication May 14, 1984.





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
Soil Science Society of America Journal
Copyright © 1985 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.