Relationship of Water and Nitrogen Inputs to Occurrence of Arsenic and
Uranium in the Deep Unsaturated Zone and Local Groundwater
Abstract
The unsaturated zone serves as reservoir for geogenic and anthropogenic
contaminants to local groundwater. Biogeochemical processes in this zone
can be affected by nitrogen and water infiltration mobilizing
contaminants, ultimately affecting groundwater quality. In this
large-scale study, we evaluated the effects of estimated water and
nitrogen inputs to the unsaturated zone of a public water supply
wellhead protection (WHP) area with respect to subsurface occurrence and
transport of nitrate, ammonium, arsenic, and uranium. Thirty-two coring
sites were sampled and grouped by water application volume, irrigated –
sprinkler (n=20), gravity (n=4) and non-irrigated land use. Unsaturated
zone sediments were evaluated for the potential to mobilize arsenic and
uranium in relation to nitrogen and water use. Sediment nitrate and
ammonium had strong significant (p<0.05) correlation
under all water application. Nitrate concentrations were lower beneath
sprinkler-irrigated sites but had statistically higher ammonium
concentrations than gravity-irrigated. Sediment nitrate concentrations
were significantly (p<0.05) different among water
application types, suggesting a strong effect of water volume on the
changing nitrate concentration. Sediment arsenic presumably attenuated
by iron (r=0.32 p<0.05). Uranium in sediments of
unsaturated zone was negatively correlated to increase in sediment
nitrate (r=-0.23 p<0.05) and ammonium
(r=-0.19 p<0.05). Water application types were
found to significantly influence sediment arsenic and uranium. While the
groundwater arsenic and uranium concentration were below maximum
contaminant levels, the highest uranium concentrations were observed in
samples from WHP area. The study suggests that irrigation has an impact
on unsaturated zone geochemistry with the potential to ultimately affect
groundwater quality.