Monitoring Tc Dynamics
in a Bioreduced Sediment: An
Investigation with Gamma Camera Imaging of <sup>99m</sup>Tc-Pertechnetate
and <sup>99m</sup>Tc-DTPA
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Abstract
We demonstrate the utility of nuclear medical imaging
technologies
and a readily available radiotracer, [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup>, for the noninvasive monitoring of Fe(II) production
in acetate-stimulated sediments from Old Rifle, CO, USA. Microcosms
consisting of sediment in artificial groundwater media amended with
acetate were probed by repeated injection of radiotracer over three
weeks. Gamma camera imaging was used to noninvasively quantify the
rate and extent of [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup> partitioning from solution to sediment. Aqueous Fe(II) and sediment-associated
Fe(II) were also measured and correlated with the observed tracer
behavior. For each injection of tracer, curves of <sup>99m</sup>Tc
concentration in solution vs time were fitted to an analytic function
that accounts for both the observed rate of sedimentation as well
as the rate of <sup>99m</sup>Tc association with the sediment. The
rate and extent of <sup>99m</sup>Tc association with the biostimulated
sediment correlated well with the production of Fe(II), and a mechanism
of [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup> reduction
via reaction with surface-bound Fe(II) to form an immobile Tc(IV)
species was inferred. After three weeks of bioreduction, a subset
of microcosms was aerated in order to reoxidize the Fe(II) to Fe(III),
which also destroyed the affinity of the [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup> for the sediments. However, within 3 days
postoxidation, the rate of Tc(VII) reduction was faster than immediately
before oxidation implying a rapid return to more extensive bioreduction.
Furthermore, aeration soon after a tracer injection showed that sediment-bound
Tc(IV) is rapidly resolubilized to Tc(VII). In contrast to the [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup>, a second commercially
available tracer, <sup>99m</sup>Tc-DTPA (diethylenetriaminepentaacetic
acid), had minimal association with sediment in both controls and
biostimulated sediments. These experiments show the promise of [<sup>99m</sup>Tc]TcO<sub>4</sub><sup>–</sup> and <sup>99m</sup>Tc-DTPA as noninvasive imaging probes for a redox-sensitive radiotracer
and a conservative flow tracer, respectively