|
|
||||||||
ABSTRACT
Adsorption of 3-amino-1,2,4-triazole by soil organic matter is greatly reduced by increasing pH. The main adsorped species is the aminotriazolium cation formed by protonation of the adsorbed molecule, but some direct physical adsorption of the latter also occurs. The aminotriazolium cations are adsorbed more strongly than sodium ions, and can be fully displaced by exchange with calcium ions.
1 Contribution from the US Soils Laboratory, Soil & Water Conservation Research Division, USDA, Beltsville, Md.
2 Research Soil Scientist (Chemistry).
Received for publication September 19, 1968. Accepted for publication February 14, 1969.
| 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 | |||