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2003
DOI: 10.1023/a:1023225419111
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Cited by 58 publications
(13 citation statements)
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References 46 publications
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“…1 Landscape context of ecological succession on landslides including disturbances that cause landslides, landscape inputs and outputs and interactions of developing soils and plant communities through succession. Modified from Walker et al (1996) weathering and soil infilling (Sidle and Ochiai 2006), impact regional carbon cycles (Stallard 1998;Restrepo et al 2003), reduce vegetative cover (Tang et al 1997) and shape landscape features such as altitudinal tree limits in Chile (Veblen et al 1977). In turn, the landscape context influences light conditions , the amount and impact of precipitation (Larsen and Simon 1993) and the amount and type of atmospheric deposition (McDowell et al 1990).…”
Section: The Landscape Contextmentioning
confidence: 99%
“…1 Landscape context of ecological succession on landslides including disturbances that cause landslides, landscape inputs and outputs and interactions of developing soils and plant communities through succession. Modified from Walker et al (1996) weathering and soil infilling (Sidle and Ochiai 2006), impact regional carbon cycles (Stallard 1998;Restrepo et al 2003), reduce vegetative cover (Tang et al 1997) and shape landscape features such as altitudinal tree limits in Chile (Veblen et al 1977). In turn, the landscape context influences light conditions , the amount and impact of precipitation (Larsen and Simon 1993) and the amount and type of atmospheric deposition (McDowell et al 1990).…”
Section: The Landscape Contextmentioning
confidence: 99%
“…The summation of above and below ground biomass was done to obtain total tree biomass. The total tree biomass was then converted to tons of CO 2 equivalent as given by Pearson et al (2007). The total tree biomass lost due to landslide was then obtained indirectly.…”
Section: Methodsmentioning
confidence: 99%
“…A study by Chambers et al (2007) on carbon footprint due to hurricane Katrina on Gulf coast forest showed that a total biomass loss of 105 TgC (1,05,000,000 tons) was incurred. Similarly, Restrepo et al (2003)'s research about influence of landslide on distribution of biomass in Hawaii, showed irreversible transformation of Ninole ecosystem within last 430 years with landslide disturbance rate, 15% per century, equivalent to 53 ton ha -1 biomass per century to exit through the system. In Nepal, the nationwide landslide inventory of 2015 had reported 5,003 landslides with total area of 126.34 km 2 (CDES-TU, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…Lithological units greatly influence the landslide occurrence [77]. The lithologic units were divided into five groups ( Figure 3n, Table 1): the first group is quaternary (loess, silt), the second group is tertiary (mudstone, conglomerate), the third group is cretaceous (arkose), the fourth group is Jurassic (shale, sandstone, mudstone, conglomerate), and the fifth group is Triassic (mudstone, sandstone, conglomerate).…”
Section: Data Preparationmentioning
confidence: 99%