M. Gascoyne et Da. Thomas, IMPACT OF BLASTING ON GROUNDWATER COMPOSITION IN A FRACTURE IN CANADAUNDERGROUND RESEARCH LABORATORY, J GEO R-SOL, 102(B1), 1997, pp. 573-584
Groundwater composition in a discrete, water-bearing fracture in grani
tic lock at the Underground Research Laboratory, Manitoba, was monitor
ed during a period of underground excavation of adjacent rock to. dete
rmine the impact of conventional blasting techniques and rock fracturi
ng on the concentration of dissolved constituents. This work has relev
ance to the study of hydrogeochemical anomalies associated with seismi
c activity. Short-lived anomalies such as decreases in dissolved anion
(Cl, F, Br, SO4) and gas (He, Rn) concentrations and concurrent incre
ases in NO3 and O-2 concentrations were seen shortly after two blasts
located opposite the groundwater sampling site. A third blast downstre
am of the site resulted in variability in dissolved gases concentratio
ns but showed no impact on dissolved anion concentrations. The results
are compared with various models used to account for hydrogeochemical
fluctuations associated with earthquakes. The data best fit a general
form of the aquifer breaching/fluid mixing model in which hydrochemic
al responses are caused by localized changes in hydraulic conductivity
along the plane of a fracture which, in turn, cause changes in mixing
ratio of groundwater at the monitoring site.