Iron minerals are important soil
components; however, little information
is available for the transformation of antibiotics on iron mineral
surfaces, especially under limited moisture conditions. In this study,
we investigated the catalytic performance of four iron minerals (maghemite,
hematite, goethite, and siderite) for the hydrolysis of chloramphenicol
(CAP) antibiotic at different moisture conditions. All the iron oxides
could efficiently catalyze CAP hydrolysis with the half-lives <6
days when the surface water content was limited, which was controlled
by the atmospheric relative humidity of 33–76%. Different minerals
exhibited distinctive catalytic processes, depending on the surface
properties. H-bonding or Lewis acid catalysis was proposed for surface
hydrolytic reaction on iron oxides, which however was almost completely
inhibited when the surface water content was >10 wt % due to the
competition
of water molecules for surface reactive sites. For siderite, the CAP
hydrolysis was resistant to excessive surface water. A bidentate H-bonding
interaction mechanism would account for CAP hydrolysis on siderite.
The results of this study highlight the importance of surface moisture
on the catalytic performance of iron minerals. The current study also
reveals a potential degradation pathway for antibiotics in natural
soil, which has been neglected before.