| 000 | 01724nas a2200325 a 4500 | ||
|---|---|---|---|
| 003 | AR-ReUNN | ||
| 005 | 20260702154116.0 | ||
| 008 | 260630c19899999ag |||||||||||||||eng | ||
| 041 | 0 | _aeng | |
| 100 | 1 |
_aJunk, Wolfgang J. _9147680 |
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| 700 | 1 |
_aBayley, Peter B. _9147681 |
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| 700 | 1 |
_aSparks, Richard e. _9147682 |
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| 245 | 1 | 4 | _aThe floop pulse concept in river-floodplain systems / Wolfgang J. Junk ; Peter B. Bayley ; Richard E. Sparks |
| 264 | 1 |
_aCanadá _bNational Research Council of Canada _c1989 |
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| 500 | _aPublication speciale canadienne des sciences halieutiques et aquatiques | ||
| 520 | _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 | ||
| 650 | 4 |
_aIchthyology _9119207 |
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| 650 | 4 |
_aIctiología _99239 |
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| 650 | 4 |
_aInundaciones _94351 |
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| 650 | 4 |
_aFlood Plains _9147683 |
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| 650 | 4 |
_aFlooding _9147684 |
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| 650 | 4 |
_aHidrology _9147027 |
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| 650 | 4 |
_aFresh Water _9121283 |
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| 650 | 4 |
_aEcology _9117438 |
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| 650 | 4 |
_aRivers _9147249 |
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| 650 | 4 |
_aCanada _95388 |
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| 942 | _cCR | ||
| 035 | _a(INICN)39662 | ||
| 001 | 234825 | ||
| 999 |
_c234825 _d234825 |
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| 040 |
_aAR-ReUNN _bspa _cAR-ReUNN _eaacr2 |
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