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Relationships Between Particle Size and Potassium Release From Biotite and Its Analogues
Author(s) -
Mortland M. M.,
Lawton K.
Publication year - 1961
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1961.03615995002500060017x
Subject(s) - biotite , chemistry , particle size , particle (ecology) , potassium , diffusion , ion , leaching (pedology) , mineralogy , analytical chemistry (journal) , chromatography , materials science , geology , thermodynamics , physics , soil water , soil science , metallurgy , organic chemistry , quartz , oceanography
The relationships of particle size of biotite to K release, oxidation state of iron, cation‐exchange capacity, and total charge of the mineral were studied. The first stage of alteration, accomplished by leaching 15 minutes with 0.1 N NaCl, showed a marked relationship to particle size. At this point, the only K removed was that on the external surfaces of the particles, and consequently the fine particles lost a larger percentage of their total K at this stage than did the larger particles. However, by the last stage where 50% of the total K had been removed, the large particles generally had lost as much as the fine. Once the initially exchangeable K has been removed, the release of matrix K from the particles is suggested to be controlled by the concentration gradient and the geometry of the diffusion path available for the exchanging ions, Na and K. The equilibrium concentration of K in 0.1 N NaCl was shown to be proportional to the total K content of biotite which had been altered to different levels of total K. The oxidation state of iron in the biotite was shown to be a function of particle size and extent of alteration.