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Please be aware that this old REACH registration data factsheet is no longer maintained; it remains frozen as of 19th May 2023.

The new ECHA CHEM database has been released by ECHA, and it now contains all REACH registration data. There are more details on the transition of ECHA's published data to ECHA CHEM here.

Diss Factsheets

Environmental fate & pathways

Adsorption / desorption

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Description of key information

Ammonia is strongly adsorbed on soil, sediment particles and colloids in water.  Ammonia is strongly adsorbed on soil, sediment particles and colloids in water.

Key value for chemical safety assessment

Additional information

Ammonia is strongly adsorbed on soil, sediment particles and colloids in water.  In clay, ammonium tends to be absorbed on the negative adsorption sites of clay colloids. Ammonia may substitute for potassium in the lattice structure of a clay mineral. Ammonia is bound in soil by the attraction of the positive charge on the ammonium ion to the negatively charged soil micelles. In soil, ammonium is adsorbed primarily by four mechanisms: chemical (exchangeable), fixation (non-exchangeable), reaction with organic matter and physical attractive forces. The behaviour of fluoride in water is dependent on pH and mineral content. Fluoride is deposited to sediment as insoluble complexes and is essentially immobile in soil due to its incorporation into insoluble complexes.