2023
DOI: 10.1016/j.catena.2023.106976
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Factors and thresholds determining sediment delivery pathways between forest road and stream in mountainous watershed

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Cited by 4 publications
(9 citation statements)
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“…However, due to the spatiotemporal variability of factors governing sediment transport and storage, it is inaccurate to proportionally convert forest road-induced soil erosion into watershed sediment discharge [76]. Generally, the transport processes of forest road-eroded sediment can be decomposed into three distinct phases: the road surface transport process [77], the road-stream slope trans-port process [16], and the stream transport process upon entering the stream network [65]. Therefore, we delve into the specific mechanisms and inherent interconnections of these three transport processes (Figure 4).…”
Section: Transport Process Of Eroded Sediment On Forest Road Surfacesmentioning
confidence: 99%
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“…However, due to the spatiotemporal variability of factors governing sediment transport and storage, it is inaccurate to proportionally convert forest road-induced soil erosion into watershed sediment discharge [76]. Generally, the transport processes of forest road-eroded sediment can be decomposed into three distinct phases: the road surface transport process [77], the road-stream slope trans-port process [16], and the stream transport process upon entering the stream network [65]. Therefore, we delve into the specific mechanisms and inherent interconnections of these three transport processes (Figure 4).…”
Section: Transport Process Of Eroded Sediment On Forest Road Surfacesmentioning
confidence: 99%
“…Once discharged from the road surface, sediment-laden runoff proceeds downhill toward the stream, initiating slope erosion and the creation of sediment transport routes connecting the road to the stream [15]. Typically, these established sediment transport pathways can be classified into three main categories: diffuse pathways, gully pathways, and partially gullied pathways (Figure 5) [16]. The diffuse pathways are generally found on lower hillslopes that have not been significantly eroded by road runoff.…”
Section: Sediment Transport Mechanismsmentioning
confidence: 99%
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