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Citation Fannin, R.J., J. Jaakkola, J.M.T. Wilkinson, and E.D. Hetherington. 2000. Hydrologic response of soils to precipitation at Carnation Creek, British Columbia, Canada: Reproduced/modified by permission of American Geophysical Union. Water Resour. Res. 36:1481-1494.
Organization UBC
URL https://www.for.gov.bc.ca/hfd/library/ffip/Fannin_RJ2000_Water_RR.pdf
Abstract/Description or Keywords The extreme hydrologic response of gravelly, sandy soils in the Carnation
Creek watershed is examined from observations at 12 standpipe piezometers. The nearly
continuous piezometric data are reported as a time series of monthly maximum readings.
Ten locations of measurement appear to exhibit an upper limit to the pore water pressure
head that is independent of rainfall intensity and duration. Two locations exhibit artesian
pressures that appear directly influenced by rainfall characteristics and may last for several
hours. We found the impact of individual storms to be highly variable. The spatial
variation in hydrologic response is attributed to the influence of preferential flow paths in
the soil matrix.
Information Type article
Regional Watershed Vancouver Island South
Sub-watershed if known Carnation Creek
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Project status complete
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