W. Davison et al., PERFORMANCE-CHARACTERISTICS OF GEL PROBES USED FOR MEASURING THE CHEMISTRY OF PORE WATERS, Environmental science & technology, 28(9), 1994, pp. 1623-1632
Polyacrylamide gel probes provide a rapid, simple procedure for measur
ing iron and manganese in pore waters at sub-millimeter resolution by
diffusional equilibration in thin films (DET). Fe(II) and Mn(II) diffu
se freely within the gel matrix, and with a 0.4 mm thick gel, complete
equilibration is achieved in 6 min. Gels must be deoxygenated prior t
o deployment, and exposure to air limited to 15 s to avoid overestimat
ion of iron. Treatment with 10 mmol L(-1) NaOH or KOH quantitatively i
mmobilizes Fe and Mn as their insoluble oxyhydroxides and brings about
a diffusional transfer of Fe and Mn to the edges of the gel. The time
from removal from the sediment to fixing or slicing the gel is the gr
eatest limit to resolution. Fixing within 20 s should allow good resol
ution at a millimeter scale, but to achieve 250-mu m resolution, fixin
g within 1-2 s in a 250 mu m thick gel is required.