1995
DOI: 10.1007/bf02471956
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Riparian buffers and potentially unstable ground

Abstract: The spatial coincidence between riparian buffers of various widths and extents and potentially unstable ground was quantified using a physically based model for shallow landslide initiation and GIS for two watersheds on the Olympic Peninsula, Washington, USA. The proportion of the potentially unstable ground in each watershed within riparian buffers is a function of both buffer width and the extent of the stream channel network being buffered. While current buffers required by Washington State cover less than … Show more

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Cited by 13 publications
(5 citation statements)
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“…Riparian zones (the fringes of rivers or streams) are the interface between aquatic and terrestrial ecosystems. They are affected by fluvial processes such as flooding and deposition of alluvial soil, and typically support a distinctive flora that differs in structure and function from adjacent terrestrial vegetation (Gregory et al ., 1991; Naiman et al ., 1993, 2005; Tang & Montgomery, 1995; Prach et al ., 1996; Naiman & Décamps, 1997). Riparian vegetation fulfils or influences various important ecological functions in relation to aquatic habitats, including the provision of food, moderation of stream water temperature via evapotranspiration and shading, providing a buffer zone that filters sediments and controls nutrients, and stabilization of stream banks (Barling & Moore, 1994; Hood & Naiman, 2000).…”
Section: Introductionmentioning
confidence: 99%
“…Riparian zones (the fringes of rivers or streams) are the interface between aquatic and terrestrial ecosystems. They are affected by fluvial processes such as flooding and deposition of alluvial soil, and typically support a distinctive flora that differs in structure and function from adjacent terrestrial vegetation (Gregory et al ., 1991; Naiman et al ., 1993, 2005; Tang & Montgomery, 1995; Prach et al ., 1996; Naiman & Décamps, 1997). Riparian vegetation fulfils or influences various important ecological functions in relation to aquatic habitats, including the provision of food, moderation of stream water temperature via evapotranspiration and shading, providing a buffer zone that filters sediments and controls nutrients, and stabilization of stream banks (Barling & Moore, 1994; Hood & Naiman, 2000).…”
Section: Introductionmentioning
confidence: 99%
“…It is apparent that the riparian zone ecotone, operating across a broad range of spatiotemporal scales, plays an important role relating biodiversity, bioproduction and nutrient transformation (Ward and Wiens, ). They typically support a distinctive flora and vegetation communities that differ in structure and function from adjacent terrestrial vegetation (Gregory et al ., ; Naiman et al ., ; ; Tang and Montgomery, ; Prach et al ., ; Naiman and Décamps, ) in response to hydrological, geomorphological and disturbance regime (Naiman et al ., ; Décamps et al ., ; Shafroth et al ., ; Cooper et al ., ). Therefore, riparian vegetation is characterized by vertical and mainly transverse gradients (Gregory et al ., , Steiger et al ., ), reflecting the flow variability (considered as the principal process in structuring the riparian zones, Décamps et al ., ) with its critical components that affect the biodiversity of riparian communities: magnitude, frequency, duration, timing and the rate of change (Poff et al ., ).…”
Section: Introductionmentioning
confidence: 99%
“…Diversos procesos fluviales, tales como crecidas y deposición del suelo aluvial, modelan la zona ribereña. Estos factores determinan, a su vez, la formación de una flora característica, típicamente diferente en estructura y función de la vegetación terrestre adyacente (Gregory et al 1991, Naiman et al 1993, Tang & Montgomery 1995, Prach & Straskrabová 1996, Naiman & Décamps 1997. Su función como proveedoras de alimento para organismos acuáticos, moderadoras de la temperatura del agua, filtradoras de nutrientes y contaminantes (Naiman et al 1993), estabilizadoras de los bancos de los ríos (Barling & Moore 1994, Hood & Naiman 2000 y como corredores para el movimiento de organismos (Naiman & Décamps 1997), las convierten en zonas de vital importancia para el mantenimiento de la biodiversidad.…”
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