1012VOLUME II, CHAPTER 36TABLE 36.1Ecological attributes of riparian areas.General Attribute Specific Attributes ReferencesMoisture availability Shallow water table supports phrea<strong>to</strong>phytes California State Lands Commission 1993Evapotranspiration, shading increase humidityMoist environments for amphibians, reptiles Reynolds et al. 1993; Jennings 1996Structural complexityVegetation provides cover for wildlife, birdsMultiple plant canopies create multiple niches Krzysik 1990Seasonal changes in deciduous vegetation Reynolds et al. 1993Periodic disturbance Floods disrupt existing organisms, providing Resh et al. 1988; Sparks et al. 1990;opportunities for pioneer speciesJunk et al.1989Linear nature Edge effect: terrestrial-aquatic eco<strong>to</strong>ne Schimer and Zalewski 1992Riparian zones serve as wildlife migration corridors Thomas et al. 1979Food resources Diverse vegetation yields diverse foods Cross 1988Diverse habitat harbors diverse prey Raedeke et al. 1988Open water available for wildlifeMicroclimate Shaded, cool, moist in summer Raedeke et al. 1988Protected in winter: overwintering habitatInfluences on aquatic habitat Shading moderates water temperatures Brown 1969Shading moderates algal growthPlant materials and insects fall in<strong>to</strong> stream, adding Cummins et al. 1989;chemical energy and nitrogen Knight and Bot<strong>to</strong>rff 1984Riparian zone “buffers” stream from upland Erman and Mahoney 1983;Mahoney and Erman 1984Riparian vegetation stabilizes stream banks Kondolf and Curry 1986and San Francisco Bay (Gilbert 1917; Mount 1995). Along theYuba River above Marysville, the “debris plain” built of thesesediments exceeds 64 km 2 (40 mi 2 ) in area.A later phase of mining involved dredgers. These reworkedthe natural floodplains or hydraulic mining debris and leftbehind elongated mounds of tailings, which are still largelyunvegetated because their surfaces consist of open cobbles inwhich plants cannot become established. The dredgers requiredextensive, deep, relatively flat deposits <strong>to</strong> work, so theywere concentrated in the lower Central Valley reaches of western<strong>Sierra</strong> Nevada rivers.Gravel mining for construction aggregate from river channelsand floodplains results in the direct removal of riparianvegetation for the creation of process yards, haul roads, andpits. Indirect effects of in-channel extraction typically includechannel incision, which propagates both upstream and downstream,lowering the alluvial water table and inducing channelinstability.Gravel mining for construction aggregate is the largestmining industry in the state (see Diggles et al. 1996). Morethan 100 million metric <strong>to</strong>ns are produced annually, virtuallyall from river channels and floodplains. Large gravel depos-TABLE 36.2Selected geomorphic and hydrologic processes in riparian areas.Process Physical Effect Ecological Consequence ReferenceFloodingInundation Soil anoxia Selects for plants <strong>to</strong>lerant of anoxia Walters et al. 1980; Gill 1970Saturation of soilIncreases soil moistureHigh-velocity flow Scour of seedlings Prevents establishment of woodyvegetation in channelPhysical damage <strong>to</strong> plants Selects for <strong>to</strong>lerant plants Sigafoos 1964Bank erosion and undercutting of Creates new habitats for colonizationmature vegetationDeposition Burial of plants Selects for <strong>to</strong>lerant plants Sigafoos 1964Sand-gravel bar depositionSelects for plants capable ofcolonizing sandy substratesFine-grained overbank deposition Provides silty substratesStream-GroundwaterInteractionsDrainage from hill slope Maintains high water table Supports vegetation independent of streamflowBank s<strong>to</strong>rage Recharges alluvial water table Supports vegetation Kondolf et al. 1987aMaintains base flowProvides water downstream
1013Status of Riparian HabitatTABLE 36.3Human activities, physical effects, and ecological consequences in riparian areas.Activity and Potential Direct Physical Effects Potential Ecological Consequences ReferencesGold MiningFormer floodplain forests reworked by placer mining in<strong>to</strong> Riparian vegetation removed and replaced with Clark 1970unvegetated dredger tailingsunvegetated gravelRivers and streams dammed and diverted through canals Water stress in dewatered reaches, riparian vegetation Averill 1946; Pagenhart 1969established along canals and ditchesIncreased sediment from hydraulic mining debris leads <strong>to</strong> Burial of existing vegetation Gilbert 1917aggradation of sand and gravel in valley bot<strong>to</strong>msContinued erosion from hydraulic mine sites Elevated fine sediment loads affect aquatic biota Marchetti 1994Gravel MiningDirect removal of vegetation for gravel yards, processing Riparian vegetation replaced by roads and industrial Poulin et al. 1994plants, haul roads, pitsland useMining-induced channel incision lowers alluvial water Increased mortality, decreased growth rate and crown Kondolf 1994b;table volume in woody riparian vegetation Scott et al. in pressMining-induced channel instability results in increased Erosion of banks supporting riparian vegetation Todd 1989bank erosionMining <strong>to</strong>ps of gravel bars (“skimming”) lowers ground Riparian vegetation established in channel where water Kondolf and Matthews 1993surface relative <strong>to</strong> water tabletable was formerly <strong>to</strong>o deepDamsReduced flood flows lead <strong>to</strong> reduced rate of channel Reduced diversity of riparian habitats Johnson 1992, 1994;migration Ligon et al. 1995;Hesse and Sheets 1993Reduced flood flows eliminate frequent scour of active Riparian vegetation encroaches in<strong>to</strong> active channel Williams and Wolman 1984;channel Bergman and Sullivan 1963;Brothers 1984Increased base flows and raised alluvial water table Waterlogging of vegetation Parrish and Matthews 1993Base flows reduced or eliminated, stream dries up Riparian vegetation severely stressed or dies Kondolf and Vorster 1993;Stine et al. 1984Trapping of bedload sediments behind dam, release of Alluvial water table drops and overbank flooding is less Williams and Wolman 1984sediment-starved water, channel incisionfrequent due <strong>to</strong> channel incisionReservoirs drown existing vegetation, fluctuating water Longitudinal continuity of riparian corridor interrupted Hagan and Roberts 1973levels may limit establishment of new vegetationalong marginsHydroelectric GenerationRivers and streams dammed and diverted through canals Water stress in dewatered reaches, riparian vegetation Harris et al. 1987;established along canals and ditchesKondolf et al. 1987bHydroelectric dams and associated canals, pens<strong>to</strong>cks, Riparian vegetation removed and replaced with roads Federal Energy Regula<strong>to</strong>rypower-houses, and access roads constructed within and structures Commission 1986riparian zoneFlow fluctuates rapidly <strong>to</strong> generate peak hydroelectric Rapid stage changes can lead <strong>to</strong> increased bank erosionpowerIrrigationWater diverted from streams Water stress in dewatered reaches, riparian vegetation Erman 1992established along canals and ditchesIrrigation water may infiltrate, recharging groundwater Excess irrigation water may support vegetation Kondolf and Vorster 1993Land DrainageAlluvial water table lowered by land drainage Riparian plants desiccated Hughes 1934Land Clearance for AgricultureRemoval of floodplain forest Riparian vegetation removed and replaced with Katibah et al. 1984agricultural landPhrea<strong>to</strong>phyte RemovalRemoval of riparian vegetation Riparian vegetation removed, may require herbicides <strong>to</strong> Dunford and Fletcher 1947;prevent regrowth Biswell 1989NavigationChannel dredged, resulting in incision Alluvial water table drops and overbank flooding is less Brookes 1988frequent due <strong>to</strong> channel incisionChannel straightened and stabilized Length, complexity, and dynamic nature of channel Brookes 1988reducedTimber HarvestHarvest of timber in riparian areas, removal of trees for Direct loss of large trees in riparian areas, reduction in Gregory et al. 1991;logging road construction structural complexity, elimination of supply of large Maser and Sedell 1994woody debris <strong>to</strong> channelLog transport on rivers erodes banks, simplifies Habitat complexity reduced Sedell and Luchessa 1981channel geometryRemoval of timber on hill slopes, resulting in increased Bank erosion, conversion of vegetated bot<strong>to</strong>mland in<strong>to</strong> Lyons and Beschta 1983;peak runoff and erosion open gravel-bed channel Grant 1988continued
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