Abstract
The proposed 4 laws of soil chemistry are: ions react with charged surfaces;
soil surfaces are heterogeneous; an initial adsorption reaction is followed by
a penetration of the adsorbed ions into the interior of the reacting
particles; and it is impossible to re-apply fertiliser to the same soil
because the soil has changed. These laws can explain the observed behaviour of
the reactions of cations and anions with soil. These include the effects of
the level of application, period of reaction, effects of temperature,
interactions between pH and salt concentration, desorption, and the isotopic
exchangeability.
Subject
Earth-Surface Processes,Soil Science,Environmental Science (miscellaneous)
Cited by
124 articles.
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