Abstracts
IAH_CNC_WEB2
IAH_CNC_WEB2
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168 - Deep groundwater systems in southern Ontario: Base of<br />
fresh water, water types, and flow directions<br />
Terry Carter 1 , Dejie Wang 2 , Jordan Clark 3 , Arthur Castillo 4 , & Lee Fortner 4<br />
1<br />
Consulting Geologist, London, Ontario, Canada<br />
2<br />
Ministry of Land and Resources, Beijing, People’s Republic of China<br />
3<br />
Ontario Oil, Gas and Salt Resources Library, London, Ontario, Canada<br />
4<br />
Ministry of Natural Resources and Forestry, London, Ontario, Canada<br />
Between 2008 and 2014 the Petroleum Operations Section of the Ministry of Natural<br />
Resources and Forestry (MNRF) completed a project to identify and map the principal<br />
water-bearing intervals in the Paleozoic bedrock of southern Ontario. After extensive and<br />
prolonged quality control edits, GIS queries of water records in the MNRF petroleum<br />
well database were used to create two map groupings: 17 maps of the static level of water<br />
in selected water-bearing geological formations in the Paleozoic bedrock, and 89 maps of<br />
water types and their geologic and geographic distribution in the bedrock.<br />
In all cases the water contained in Paleozoic bedrock formations and the overlying unconsolidated<br />
sediments in southern Ontario exhibits increasing salinity with depth. There is a<br />
down-dip gradation from fresh water at or near the surface in the drift and shallow bedrock<br />
(