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pro vyhledávání: '"M. A. Shanafield"'
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 1917-1929 (2018)
Profiles of temperature time series are commonly used to determine hyporheic flow patterns and hydraulic dynamics in the streambed sediments. Although hyporheic flows are 3-D, past research has focused on determining the magnitude of the vertical f
Externí odkaz:
https://doaj.org/article/d5bc69f57bb1453ea5f296ab7b115a57
