Laserfiche WebLink
<br />61 <br /> <br />TAble 1. <br /> <br />Function of riparian &on~ veaHltion III it relit", to the Iqu.u it &onfl!. <br /><.odified fro. Huh.n et 11. 1979). <br /> <br />Site <br /> <br />Component <br /> <br />Function <br /> <br />ABOVE GROUHD- <br />ABOVI!: CHANNEL <br /> <br />CANOPy 6. STEMS <br /> <br />1. Shade-contrail tempel'.ture , <br />in .trellll prillllry production <br /> <br />2. Sou'tee of largE' and rine plant <br />det,titu. <br /> <br />3. SOu'tee of terre.tri.1 irllP-ctll <br /> <br />IN CHANNEL <br /> <br />LARGE OF.BRIS <br />DERIVED FROM <br />RIPARIAN VEC. <br /> <br />I. Conl:rol routing of v~lter Ind <br />.editu,nt <br /> <br />2. Shape l'llbit4lt-poollJ, nffte. <br />..nd I:over <br /> <br />1, Sublltrate (or biol()gical <br />let \, ,,~t Y <br /> <br />STREAHBANKS <br /> <br />ROOTS <br /> <br />L Incn~.lIe. bank Itabitity <br /> <br />2. Crelltes oveThllnginll bank cover <br /> <br />FLOODPLAIN <br /> <br />STEMS AND LOW <br />LYlNG CANOPY <br /> <br />I. Retllrd 1n:)velllent of ledilllent. <br />WalE"" and floated organic <br />debl"i.. in flood f10.. <br /> <br />and (2) create overhanding banks which provide wildlife cover (shelter). <br />Stems and low lying canopy located on floodplains retard movement of <br />sediment, water and floated or suspended otl~anic debris during flood flows <br />both in a linear (longitudinal) and lateral (or horizontal) directions. <br /> <br />Phreatophyte,!. <br /> <br />A large number of plants that are chancteristic of riparian <br />ecosystelllS and tend to dominate streambank ,areas have been collectively <br />termed "phreatophytes." The term "phreatophrEe" was clreated from two Greek <br />words meaning -well plant" to identify plants whose roots tap the <br />groundwater table or the wet soil just above it (Meinz,ar 1923). The <br />phreatophyte zone, however, also includes the deeper alluvium beyond the <br />riparian zone where roots penetrate to the groundwater table for additional <br />water (Horton 1974). The continuous availability of ground water to <br />riparian phreatophytic vegetation results in large transpiration losses to <br />the atmosphere. These losses are most sign:lficant dur:lng the warmer months <br />when evapotransporation rates are high. <br /> <br />Over 70 phreatophytic plants have been classified in the western <br />United States (Robinson 1958). These include the more common forms such as <br />willow (Salix sp.), cottonwood (Populus sp.), alder (Mlnus sp.), greasewood <br />Sarcobatus sp.), mesquite (Proso is sp.), Ollk (Quercus'liji':"), quaking aspen <br />(Populus sp.), Russian olive Elaeagnus sp.), salt cedar (Tamar1x sp.), <br />