Abstract
Water samples were obtained from a number of mountain lakes and irrigation reservoirs in the Okanagan Valley, and from streams emptying them. It was found that in any one drainage basin, the water had a higher pH and salt content at low elevation than at high elevation.A more detailed investigation was conducted in the Mission Creek watershed. With decreasing elevation the following relationships were found: (a) increasing pH, electrical conductivity, and contents of calcium, potassium and sodium in the stream water; (b) increasing pH and conductivity in seepage water; (c) increasing pH and conductivity in the soil. Relationships between elevation and pH were similar with stream water, seepage water and soil, as also were relationships between elevation and conductivity values.
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