Exploring the kinetic adsorption and desorption of Americium (Am(III)) on sediments and natural colloids can effectively predict its solid–liquid distribution behavior in the environment. In this study, we used batch and stirred flow-through experiments to describe the kinetic adsorption and desorption process of Am(III) on Am(III)-sediments (AS) system and Am(III)-sediments-natural colloids (ASN) system under different conditions (such as solution pH, background electrolyte concentration, and solution injection velocity). The retention and desorption behavior of Am(III) was analyzed through adsorption distribution coefficients and breakthrough curves. The kinetic adsorption process was described using reaction and transport control models. The results showed that in the batch adsorption experiment, the presence of natural colloids significantly increased the adsorption distribution coefficient of the ASN system (249.11—2512.74 mL/g) compared to the AS system (233.05—447.29 mL/g). The retention of Am(III) in the stirred flow-through reactor in AS (70.26% - 73.64%) and ASN (74.13% - 76.25%) systems is relatively high under neutral and low flow rate conditions, which is attributed to the strong adsorption ability of dispersed and stable natural colloids and the sufficient adsorption time provided by low velocity. According to the fitted results of the models, it can be seen that physical reactions such as surface precipitation or surface complexation, as well as diffusion of the liquid surrounding the solid-phase adsorbent, dominate the kinetic adsorption process, which is time-dependent or non-equilibrium.