“…Infrared and X-ray techniques have generally required that the clays have high organic cation contents and could not be used to study clay-water systems at equilibrium. However, recent investigations have shown that electron spin resonance (ESR) spectroscopy of clays containing small quantities of adsorbed organic radical cations provides insight into clay--organic interactions in water and various other solvents (McBride, 1976(McBride, , 1977a(McBride, , 1977b. The advantages of this approach are (1) a very small fraction of the total exchange sites can be occupied by the organic cation, resulting in little effect of the adsorption upon the hydration and expanding properties of the clay, (2) adsorption can be studied over a wide range of organic cation concentrations because of the sensitivity of the ESR technique, and (3) studies can be made of aqueous suspensions as well as dry powders and films.…”