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The adsorption of Gd 3+ into sediments was studied by electron spin resonance (ESR) to investigate the uranium uptake model and the migration of harmful elements into sediments in nuclear waste repositories. The ESR signal in montmorillonite immersed in GdCl 3 solution was ascribed to Gd 3+ observed at g=2.0 with a width of 48mT. This signal saturated with the concentration...
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