Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Matthew G. Tiedemann"'
Publikováno v:
Geomorphology. 250:147-158
Canyon river systems are laterally constrained by steep walls, strath terraces, and bedrock intrusions; however, semialluvial reaches are nested within these environments as discontinuous floodplains along the river margins. These semialluvial floodp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc3873c65a8ea415683d2487da537133
https://doi.org/10.1016/j.geomorph.2015.09.001
https://doi.org/10.1016/j.geomorph.2015.09.001
Publikováno v:
Journal of Hydrology. 519:1997-2011
Summary The hyporheic zone is the volume of the streambed sediment mostly saturated with stream water. It is the transitional zone between stream and shallow-ground waters and an important ecotone for benthic species, including macro-invertebrates, m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b894c19a43d182ee9326421373f4097
https://doi.org/10.1016/j.jhydrol.2014.09.076
https://doi.org/10.1016/j.jhydrol.2014.09.076