01968nas a2200361 a 4500003000900000005001700009008004100026041000800067100003000075700002900105700003100134245011300165264005600278500007600334520072300410650002401133650002301157650002301180650002501203650002101228650002201249650002401271650002001295650001901315650001701334942000701351035001701358001000701375952008501382999001901467040003501486952008501521AR-ReUNN20260702154116.0260630c19899999ag |||||||||||||||eng    0 aeng1 aJunk, Wolfgang J.91476801 aBayley, Peter B.91476811 aSparks, Richard e.914768214aThe floop pulse concept in river-floodplain systems / Wolfgang J. Junk ; Peter B. Bayley ; Richard E. Sparks 1aCanadábNational Research Council of Canadac1989  aPublication speciale canadienne des sciences halieutiques et aquatiques  aThe principal driving force responsible for the existence, productivity, and interactions of the major biota in river-floodplain systems is the flood pulse. A spectrum of geomorphological and hydrological conditions produces flood pulses, which range from unpredictable to predictable and from short to long duration. The flood pulse is a "batch" process and is distinct from concepts that emphasize the continuous processes in flowing water environments, such as the river continuum concept. Floodplains are distinct because they do not depend on upstream processing inefficiencies of organic matter, although their nutrient pool is influenced by periodic lateral exchange of water and sediments with the main channel 4aIchthyology9119207 4aIctiología99239 4aInundaciones94351 4aFlood Plains9147683 4aFlooding9147684 4aHidrology9147027 4aFresh Water9121283 4aEcology9117438 4aRivers9147249 4aCanada95388  cCR  a(INICN)39662234825  00104070aINICNbINICNcGENd2007-08-01l0o16 [40] WOL ej.1p61.01-001595yCR  c234825d234825  aAR-ReUNNbspacAR-ReUNNeaacr2  00104070aINICNbINICNcGENd2007-08-01l0o16 [40] WOL ej.1p61.01-001595yCR