Goethite (Gt) and humic acid (HA) are important components of soil that significantly affect Cd mobility. In this study, the co-transport of Cd²⁺ and Gt with/without HA in saturated sand columns was investigated by monitoring the breakthrough curves at different pH values. A solute transport model was used to study Cd²⁺ transport and retention in the saturated sand in the presence of Gt and HA, and a colloid transport model was used to describe the Gt colloid (Gt_C) transport in the columns. Our results showed that the transport behaviors of Cd²⁺ and Gt colloids/aggregates were regulated by pH. Cadmium transport was significantly inhibited at high pH due to its adsorption on the sand and Gt. Moreover, Gt retention was gradually stabilized with increasing pH regardless of its forms, i.e., individual colloids (Gt_C) or larger assemblages of particles due to aggregation (Gt_A). This retention was obviously enhanced in the presence of HA. Thus, the superposition of increased Cd²⁺ adsorption on Gt and Gt retention (stabilization) enhanced the immobilization of Cd²⁺ at high pH. In addition to stabilizing Gt, HA further enhance Cd²⁺ adsorption on Gt, thus promoting Cd²⁺ immobilization. However, only a small amount of organicmatter-bound Cd2+ was observed in the columns with injected HA. The major fractions of retained Cd²⁺ were exchangeable Cd²⁺ and Fe-oxide-bound Cd²⁺. Our results provide new insights into the roles of Gt and HA in the transport and mobilization of Cd²⁺ in soil-groundwater systems.