Simultaneous removal of low concentrations of ammonium and humic acid from simulated groundwater by vermiculite/palygorskite columns

Abstract Vermiculite and palygorskite are common clay minerals having large surface area and high cation exchange capacities. They have different affinities for ammonium (NH 4 + ) and humic acid (HA), and hence were combined to remove NH 4 + and HA simultaneously from simulated groundwater in column tests. Three columns were assembled by filling the columns with the same amount of vermiculite and palygorskite but in different arrangements. The simulated groundwater containing NH 4 + and HA was pumped to the columns in an upward direction. The concentrations of N-NH 4 + and HA at different height of the columns were measured over time. No significant differences on HA removal among the three column settings were observed. However, the NH 4 + removal efficiencies were significantly different among the three column settings. For the column filled with separate vermiculite and palygorskite layers, NH 4 + was mainly adsorbed on the vermiculite layer. In contrast, when mixture of vermiculite and palygorskite was packed at the ratio of 1:1, NH 4 + was mainly accumulated at the bottom of the column.