沉积物
水文学(农业)
腐蚀
环境科学
流域
沉积预算
示踪剂
地质学
泥沙输移
地貌学
地理
地图学
物理
核物理学
岩土工程
作者
J. A. Motha,Peter Wallbrink,Peter B. Hairsine,Rodger B. Grayson
摘要
Knowledge is scarce regarding the relative contributions from harvested areas and unsealed roads to sediments in forested catchments. We investigate the source composition of suspended sediment using sediment tracers and an improved multivariate mixing model. Sediment samples were collected during six rainfall events. Geochemical and radiometric tracer properties were corrected for particle size and organic content as well as conservativeness during erosion and sediment delivery. The mixing model incorporates variability of the tracer properties, using a Monte Carlo simulation technique. Mean sediment contribution from the undisturbed forest was 50–70%; harvested areas, gravel‐surfaced roads, and ungravelled roads contributed 5–15%, 6–14%, and 12–25%, respectively. The unsealed roads contribute 20 to 60 times more sediment than the undisturbed forest and about 10 times more sediment than the harvested areas on a per unit area basis. Harvested areas contribute 1 to 5 times greater sediment than the undisturbed forest. These results support other studies that identify unsealed roads as important sediment sources in forested catchments.
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