We describe a new method suitable for the precise and accurate determination of 226Ra in porewater and sediment samples using a single-collector sector field ICP-MS (ThermoFisher Element XR) equipped with an Apex-Q desolvation device and a high-sensitivity Jet-X interface. In combination with 230Th measurements in parallel sediment samples, this method allows precise and accurate quantification of the 226Ra/230Th disequilibria in surface sediment cores, thereby enabling the use of this isotope pair as a tracer of solute transfer across the sediment-water interface in the deep ocean. The method integrates a step of isotope dilution with 228Ra as an internal spike, a pre-concentration of Ra and Ba by MnO2 precipitation, and an efficient separation of Ra from other undesirable elements using a cation exchange resin and a Triskem Sr-spec resin. With the inclusion of one or two additional cation resin columns and the use of up to 16 bed-volumes of a lower molarity (1.7 M) HCl eluent, our procedure eliminates the complicated matrix effects persistently encountered in previous studies, and provides a highly purified solution suitable for 226Ra measurement using an Element XR ICP-MS apparatus. Consequently, we are able to determine the activity of 226Ra in ∼20–50 ml of porewater or 100 mg of sediment with an internal precision of ∼1.0% and an accuracy of ∼99.2%. The precise measurements of porewater and solid phase 226Ra in a sediment core from the North Pacific Ocean allowed the distribution coefficient (Kd) of 226Ra to be constrained tightly within a range of 4700–11,600 ml g−1. Moreover, with the aid of a one-dimensional exchange model, the combination of the 226Ra and 230Th measurements allowed us to estimate a 226Ra flux of 1140 ± 20 dpm m−2 y−1 from the sediment core.