Erosion and sediment delivery following removal of forest roads

Erosion control treatments were applied to abandoned logging roads in California, with the goal of reducing road-related sediment input to streams and restoring natural hydrologic patterns on the landscape. Treatment of stream crossings involved excavating culverts and associated road fill and reshaping streambanks. A variety of techniques were applied to road benches, which included decompacting the road surface, placing unstable road fill in more stable locations, and reestablishing natural surface drainage patterns. Following treatment and a 12-year recurrence-interval storm, some road reaches and excavated stream crossings showed evidence of mass movement failures, gullying, bank erosion and channel incision. Post-treatment erosion from excavated stream crossings was related to two variables: a surrogate for stream power (drainage area channel gradient) and the volume of fill excavated from the channel. Post-treatment erosion on road reaches was related to four explanatory variables: method of treatment, hillslope position (upper, mid-slope or lower), date of treatment, and an interaction term (hillslope position method of treatment). Sediment delivery from treated roads in upper, middle and lower hillslope positions was 10, 135 and 550 m 3 of sediment per kilometre of treated roads, respectively. In contrast, inventories of almost 500 km of forest roads in adjacent catchments indicate that untreated roads produced 1500 to 4700 m 3 of sediment per kilometre of road length. Erosion from 300 km of treated roads contributed less than 2 per cent of the total sediment load of Redwood Creek during the period 1978 to 1998. Although road removal treatments do not completely eliminate erosion associated with forest roads, they do substantially reduce sediment yields from abandoned logging roads. Published in 2001 by John Wiley & Sons, Ltd.

[1]  M. Gordon Wolman,et al.  Fluvial Processes in Geomorphology , 1965 .

[2]  W. Megahan,et al.  Effects of Logging and Logging Roads on Erosion and Sediment Deposition from Steep Terrain , 1972 .

[3]  S. Colman,et al.  Watershed conditions in the drainage basin of Redwood Creek, Humboldt County, California, as of 1973 , 1975 .

[4]  K. Richards The morphology of riffle‐pool sequences , 1976 .

[5]  T. Lisle Effects of aggradation and degradation on riffle-pool morphology in natural gravel channels, northwestern California , 1982 .

[6]  R. M. Rice,et al.  Erosion on logging roads in northwestern California: How much is avoidable? , 1983 .

[7]  R. Beschta,et al.  Influences of Increased Sand Delivery on the Morphology of Sand and Gravel Channels , 1984 .

[8]  M. O'Neill,et al.  Objective Identification of Pools and Riffles , 1984 .

[9]  T. Lisle Stabilization of a gravel channel by large streamside obstructions and bedrock bends , 1986 .

[10]  Forested block slides in the lower Redwood Creek basin, northwest California , 1987 .

[11]  H. Kelsey Formation of inner gorges , 1988 .

[12]  André Robert,et al.  Statistical properties of sediment bed profiles in alluvial channels , 1988 .

[13]  On the modelling of sand bedforms using the semivariogram , 1988 .

[14]  Michael Church,et al.  Hydraulic Geometry in Small, Coastal Streams: Progress Toward Quantification of Salmonid Habitat , 1989 .

[15]  Jonathan M. Nelson,et al.  The initial instability and finite-amplitude stability of alternate bars in straight channels , 1990 .

[16]  D. Helsel,et al.  Statistical methods in water resources , 2020, Techniques and Methods.

[17]  D. Montgomery,et al.  Pool Spacing in Forest Channels , 1995 .

[18]  H. Kelsey,et al.  Geomorphic processes and aquatic habitat in the Redwood Creek basin, northwestern California , 1995 .

[19]  T. Lisle Effects of coarse woody debris and its removal on a channel affected by the 1980 eruption of Mount St. Helens, Washington , 1995 .

[20]  M. Madej,et al.  CHANNEL RESPONSE TO SEDIMENT WAVE PROPAGATION AND MOVEMENT, REDWOOD CREEK, CALIFORNIA, USA , 1996 .

[21]  A. Brad Murray,et al.  A new quantitative test of geomorphic models, applied to a model of braided streams , 1996 .

[22]  C. Luce Effectiveness of Road Ripping in Restoring Infiltration Capacity of Forest Roads , 1997 .

[23]  Stuart N. Lane,et al.  Linking River Channel Form and Process: Time, Space and Causality Revisited , 1997 .

[24]  D. Montgomery,et al.  Channel-reach morphology in mountain drainage basins , 1997 .

[25]  Beverley C. Wemple,et al.  Investigations of runoff production and sedimentation on forest roads , 1998 .

[26]  R. M. Rice,et al.  EROSION ON LOGGING ROADS IN REDWOOD CREEK, NORTHWESTERN CALIFORNIA 1 , 1999 .

[27]  Patterns of hillslope and channel recovery following disturbances in steep, forested basins , 1999 .