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Rates of trace metal release due to mineral weathering (Sources)
Objectives being Investigated
The determination of rates of release of trace metals resulting from the breakdown of primary minerals, which naturally contain trace metals, in soils. This process is a natural source of trace metals to the surface environment that needs to be quantified so its magnitude can be compared with anthropogenic releases.
Study/Sampling Design
Study sites (3) were established along each of two transects following decreasing gradients of soil metal concentrations near Sudbury, Ontario, and Rouyn-Noranda, Quebec. At each site soil samples were collected from soil profiles so that the trace metal bearing minerals could be identified. These two transects are also the subject of studies under projects led by Hale (B1) and Courchesne (B5).
Location of Field Site(s)
Sudbury, Ontario, field sites
1. 46º 35.8´ N 80º 49.9´ W
2. 46º 35.9´ N 80º 37.4´ W
3. 46º 33.2´ N 80º 15.6´ W
Rouyn-Noranda, Quebec, field sites
1. 48º 17.0´ N 78º 54.2´ W
2. 48º 18.5´ N 78º 51.2´ W
3. 48º 32.3´ N 78º 39.4´ W
Biota Studied
Species
--- none provided ---
Metals, etc. Quantified
--- none provided ---
Biological Endpoint(s)
--- none provided ---
Physical Material(s) Studied
Medium/Media
Mineral soil
Metals, etc. Quantified
Cu, Ni, Pb, Zn
Bibliographic References on-file with Secretariat: No
Data Available: No
Data Archived with MITHE-SN: No
Collaborators
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