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GROUND WATER OF THE ISLAND OF MONTREAL, CANADA 1
Author(s) -
Grice R. H.,
Eggboro M. D.
Publication year - 1978
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.1978.tb02297.x
Subject(s) - groundwater recharge , geology , shore , groundwater , water well , glacial period , hydrology (agriculture) , carbonate , bay , geological survey , igneous rock , geochemistry , aquifer , oceanography , geomorphology , paleontology , materials science , geotechnical engineering , metallurgy
The geochemistry and nature of the flow of ground water not only control the supply potential but constitute clues to the whole geology of an area. A study has been made of the largest available assemblage of data from 161 wells for the Island of Montreal collected by the Geological Survey of Canada in 1951–53. Data indicated that the system is generally subartesian, flowing from the principal topographically high areas towards the shores of the Island. As the probable use is about 13% of the estimated recharge of 140 million liters per day, most wells could be supplied by local recharge. The study has confirmed the predominance of calcium bicarbonate ground water from the carbonate sequence. The waters appeared to be saturated with respect to CaCO 3 in all but 10 wells. The presence of other types of waters suggests the effects of the igneous intrusions of the area, the post‐glacial marine submergence and the upward movement of waters from deep sources through fault and other structural zones. Confirmation of the significant variations in chemical composition in some neighboring wells indicated the future need for repetitive sampling from specific horizons for chemical and isotopic analyses.