The range and distribution of mercury in soils at a decommissioned gas plan
t near Turner Valley, Alberta were investigated in order to facilitate risk
assessment and the remediation and development of the site into a tourism
area. Although high levels of Hg were thought to be present in some areas o
n the site, it was unclear whether the source of the Hg was industrial proc
esses or from river deposition of HgS impurities after erosion of upstream
sulfide deposits. Background Hg concentrations in undisturbed soils and sur
ficial bedrock near the gas plant were also unknown. Mercury concentrations
in surface soil material on the gas plant site were found to range up to 2
30 mg Hg kg(-1) soil, with the highest concentrations found next to process
building doorways. Investigation of Hg distribution with soil depth showed
that levels were generally highest at the surface, dropping rapidly with d
epth to near background levels of 0.07 mg Hg kg(-1) soil or lower. The high
est Hg concentrations were associated with the clay fraction, which contain
ed up to 2300 mg Hg kg(-1) soil. The results are consistent with an anthrop
ogenic source from spillage of elemental Hg contained in manometers and pre
ssure monitoring devices used in plant buildings. Mercury concentrations at
depth and in uncontaminated surface soils were similar to those reported b
y Dudas and Pawluk (1976) for surface soils formed in glacial and fluvial d
eposits elsewhere in Alberta.