Isotope hydrology of precipitation, surface and ground waters in the Okanagan Valley, British Columbia, Canada

• Published in: Journal of hydrology (Amsterdam) 2011-12, Vol.411 (1), p.37-48
• Main Authors: Wassenaar, L.I., Athanasopoulos, P., Hendry, M.J.
• Format: Article
• Language: English
• Subjects: British Columbia; Earth sciences; Earth, ocean, space; Exact sciences and technology; Freshwater; Geochemistry; Groundwater; Hydrology; Hydrology. Hydrogeology; Isotope geochemistry; Isotope geochemistry. Geochronology; Isotope hydrology; Isotopes; Lakes; Mineralogy; Okanagan Valley; Precipitation; Rivers; Silicates; Surface water; Valleys; Water balance; Water geochemistry; Water isotopes
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2011.09.032

► Relationships between water resources of the Okanagan Valley remain poorly defined. ► Stable isotopes were used to characterize rainfall, rivers and lakes, and ground water resources. ► Precipitation isotopes resulted in a local meteoric water line of δD = 6.6 ( δ 18O) − 22.7 for the Okanagan. ► Isotopic mass-balance modeling suggested ∼35% of precipitation falling upon the watershed is lost to evaporation. ► Ground water in the valley aquifers is anthropogenically recharged by irrigation water from the Okanagan River. Rapid population growth in the intermontane, semi-arid, Okanagan Valley of Western Canada has led to water shortages with increasing debate over competing water interests. Nevertheless, the relationships between the various water resources of the Okanagan remain poorly defined. Stable isotopes of hydrogen ( δ 2H) and oxygen ( δ 18O) were used to assess rainfall importance and the sources and flux of water to and from rivers and lakes in watersheds, and to evaluate the origin of ground water resources. Precipitation isotopes resulted in a meteoric water line of δ 2H = 6.6 ( δ 18O) − 22.7 for the Okanagan Valley. Isotopic seasonality in precipitation was evident, with summer precipitation clearly affected by local recycling of water vapor. The 2H and 18O of surface waters were more positive than mean annual precipitation, indicative of basin-scale evaporation of surface waters; however, Okanagan Lake and its downstream river and lake system were isotopically synchronous, indicating that they behaved as a single well-mixed hydrologic unit. Isotopic mass-balance modeling revealed ∼35% of inflow to the Lake Okanagan watershed was lost to evaporation, validating a meteorological water balance model for the region. Highland bedrock was recharged with snow-melt and early spring rains, with the isotopic composition dependent on elevation. Ground waters in the Valley bottom aquifers west of Osoyoos were recharged by irrigation water obtained from the Okanagan River system, with no evidence of recharge connections from the highland bedrock.