2009
DOI: 10.1016/j.foreco.2009.02.011
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Estimation of annual suspended sediment yield from a Japanese cypress (Chamaecyparis obtusa) plantation considering antecedent rainfalls

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Cited by 39 publications
(26 citation statements)
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“…The exceptionally high TSS concentrations observed during the peak flow periods of some of the intensive rainfall events we monitored suggest that soil erosion in steep mountainous watersheds can be vulnerable to extreme rainfall events, even without any disturbances over recent years. Similar high rates of sediment export during intense storm events have been observed in steep mountainous watersheds in Japan [12,48,49]. In a Korean natural forest dominated by 80-200-year old trees of similar species to the study site, Kim et al [50] also observed high export rates of suspended sediment (measured as POC) during intense storm events.…”
Section: Discussionsupporting
confidence: 79%
“…The exceptionally high TSS concentrations observed during the peak flow periods of some of the intensive rainfall events we monitored suggest that soil erosion in steep mountainous watersheds can be vulnerable to extreme rainfall events, even without any disturbances over recent years. Similar high rates of sediment export during intense storm events have been observed in steep mountainous watersheds in Japan [12,48,49]. In a Korean natural forest dominated by 80-200-year old trees of similar species to the study site, Kim et al [50] also observed high export rates of suspended sediment (measured as POC) during intense storm events.…”
Section: Discussionsupporting
confidence: 79%
“…As a result, except in areas where the forest floor has been removed by fire or other disturbances or soils have been severely compacted, both overland flow and soil erosion have very low observed rates in forested watersheds (Ice and Stednick, 2004). Where soil erosion rates are higher, such as from recently constructed roads or skid trails, the forest litter layer and other forest floor components such as coarse wood and understory vegetation play important roles in filtering and trapping suspended sediments (Swift and Burns, 1999;Ide et al, 2009, Fukuyama et al, 2010. Thus, management practices that ensure that areas (such as riparian buffers) that receive suspended sediment are of sufficient size and capacity to effectively trap, filter, and retain sediment are key in influencing overland flow, soil erosion, and sediment loading in streams.…”
Section: Soil Protection and Sediment Trapping And Filteringmentioning
confidence: 99%
“…The nutrient loads during the storm flow periods were calculated using the ∑L-∑Q equation derived from the concentration and discharge data obtained during storm events (Chiwa et al 2010a;Ebise 1984;Ebise and Goda 1985;Ide et al 2009). The ∑L-∑Q equation calculates the cumulative nutrient load per storm event and is expressed as follows:…”
Section: Calculation Of Annual Loadsmentioning
confidence: 99%