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http://online.sfsu.edu/jerry/geog810/2005/Hoorn/madej2.pdf
Sediment delivery from treated roads in upper,middleandlowerhillslopepositionswas10,135and550 m 3 ofsedimentperkilometreoftreatedroads,respectively. Incontrast,inventoriesofalmost500 kmofforestroadsinadjacentcatchmentsindicatethatuntreatedroadsproduced1500
https://www.krisweb.com/biblio/redwood_usgs_madej_2001_erosionandsediment.pdf
Sediment delivery from treated roads in upper, middle and lower hillslope positions was 10, 135, and 550 m of sediment/kilometer of3 treated roads, respectively. In contrast, inventories of almost 500 km of forest roads in adjacent catchments indicate that untreated roads …
https://www.researchgate.net/publication/253385321_Erosion_and_Sediment_Delivery_Following_Removal_of_Forest_Roads
Madej (2001) reported reduced sediment delivery to streams after removal and treatment of 300 km of roads in Redwood National Park, California.Switalski et al. (2004)reviewed published evaluations...Author: Maryann Madej
https://pubs.er.usgs.gov/publication/1008202
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.Author: Mary Ann Madej
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.630.1694
Sediment delivery from treated roads in upper, middle and lower hillslope positions was 10, 135 and 550 m3 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 m3 of sediment per kilometre of road length.
https://www.sciencedirect.com/science/article/pii/S1364815209001832
Most models of surface erosion and sediment delivery from unsealed roads can be categorised as empirical and physics-based models. Empirical models generally have lower parameter requirements than physics-based models but are limited in their widespread application as they only represent a rather restricted set of conditions.Author: Baihua Fu, Lachlan T. H. Newham, C. E. Ramos-Scharrón
https://www.fs.fed.us/biology/nsaec/assets/sosaperezmacdonald2017reductionroadsedimentproductiondecommissioning.pdf
The delivery of road runoff and sediment depends on the hydro- logic connectivity, where connectivity refers to the linkage or con nection between a runoff source …
https://efotg.sc.egov.usda.gov/references/public/IA/Erosion_and_Sediment_Delivery.pdf
Erosion and Sediment Delivery Introduction Soil erosion consists of a series of natural processes that move earth and rock material. The land surface is worn away through the detachment and transport of soil and rock by moving water, wind, and other geologic agents.File Size: 314KB
https://www.fs.fed.us/rm/pubs_other/rmrs_2012_goode_j001.pdf
sediment delivery, climate-driven variation in both wild fire and hydroclimate are likely to produce changes in sediment yields. Enhanced sediment delivery in a changing climate in semi-arid mountain basins: Implications for water resource management and aquatic habitat in the northern Rocky MountainsAuthor: Jaime R. Goode, Charles H. Luce, John M. Buffington
https://www.sciencedirect.com/topics/earth-and-planetary-sciences/sediment-transport
Sediment transport rates by fluvial processes are proportional to the product of flow depth and the energy gradient, or water surface slope (Richards, 1982 ). Hence, sediment transport increases with either deeper flow or steeper slopes, and conversely sediment transport rates decrease in shallower flow or on gentler slopes.
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