1993
DOI: 10.1016/0022-1694(93)90122-p
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The effect of steep slope logging on fine sediment infiltration into the beds of ephemeral and perennial streams of the Dazzler Range, Tasmania, Australia

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Cited by 42 publications
(33 citation statements)
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“…The width of the riparian forest 'buffer' strip was a dominant factor in determining the degree of impact, with little effect of coupe slope or soil type. Time after logging has been shown to have a significant impact on changes to catchment yield and stream hydrology (Cornish 1993) and to yield of sediment (Grayson et al 1993) and infiltration of sediment into stream beds (Davies and Nelson 1993). Time was not, however, a significant factor or covariate in the present study, suggesting that significant recovery from logging impacts did not occur within a period of three to five years.…”
Section: Discussioncontrasting
confidence: 60%
“…The width of the riparian forest 'buffer' strip was a dominant factor in determining the degree of impact, with little effect of coupe slope or soil type. Time after logging has been shown to have a significant impact on changes to catchment yield and stream hydrology (Cornish 1993) and to yield of sediment (Grayson et al 1993) and infiltration of sediment into stream beds (Davies and Nelson 1993). Time was not, however, a significant factor or covariate in the present study, suggesting that significant recovery from logging impacts did not occur within a period of three to five years.…”
Section: Discussioncontrasting
confidence: 60%
“…Megahan & Kidd 1972, Doeg & Koehn 1990, Fahey & Coker 1992, Davies & Nelson 1993, Grayson et al 1993). Fine sediments which are removed from the land in this way may find their way to coastal areas within hours/ minutes (Fahey & Coker 1992), particularly in association with flood events (Nichols 1977, Wheatcroft et al 1997, Wheatcroft 2000.…”
Section: Abstract: Sedimentation · Intertidal Soft-sediments · Terrementioning
confidence: 99%
“…Impacts of forestry activities on Australasian streams include changes in stream hydrology (Vertessey 1999), alteration of stream bank stability and sediment retention (Davies and Nelson 1994;Bunce et al 2001), reduction in shading and increased water temperatures (Lake and Marchant 1990;Webster et al 1992), modification of organic debris and channel morphology (Davies and Nelson 1994;Bunce et al 2001), changes to stream sediment particle size distributions (Scrivener 1987;Davies and Nelson 1993;Bunce et al 2001) and changes in aquatic macroinvertebrate and fish assemblages and populations (Davies and Nelson 1994;Growns and Davis 1994). Despite these known changes to habitat, platypuses have been recorded in streams downstream from areas subject to logging (Grant 1991;Turnbull 1998).…”
Section: Introductionmentioning
confidence: 99%