Groundwater contribution to river flows – using hydrograph separation, hydrological and hydrogeological models in a southern Quebec aquifer
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2010
- handle: 10670/1.fv4gmu
- Larocque, M.; Fortin, V.; Pharand, M. C. et Rivard, C. (2010). « Groundwater contribution to river flows – using hydrograph separation, hydrological and hydrogeological models in a southern Quebec aquifer ». Hydrology and Earth System Sciences Discussions, 7(5), pp. 7809-7838.
Ce document est lié à :
http://archipel.uqam.ca/7769/
Ce document est lié à :
http://dx.doi.org/10.5194/hessd-7-7809-2010
Ce document est lié à :
doi:10.5194/hessd-7-7809-2010
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Groundwater river QuébecCiter ce document
M. Larocque et al., « Groundwater contribution to river flows – using hydrograph separation, hydrological and hydrogeological models in a southern Quebec aquifer », UQAM Archipel : articles scientifiques, ID : 10670/1.fv4gmu
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Groundwater contribution to river flows, generally called base flows, often accounts for a significant proportion of total flow rate, especially during the dry season. The objective of this work is to test simple approaches requiring limited data to understand groundwater contribution to river flows. The Noire river basin in southern Quebec is used as a case study. A lumped conceptual hydrological model (the MOHYSE model), a groundwater flow model (MODFLOW) and hydrograph separation are used to provide estimates of base flow for the study area. Results show that the methods are complementary. Hydrograph separation and the MOHYSE surface flow model provide similar annual estimates for the groundwater contribution to river flow, but monthly base flows can vary significantly between the two methods. Both methods have the advantage of being easily implemented. However, the distinction between aquifer contribution and shallow subsurface contribution to base flow can only be made with a groundwater flow model. The aquifer renewal rate estimated with the MODFLOW model for the Noire River is 30% of the recharge estimated from base flow values. This is a significantly difference which can be crucial for regional-scale water management.