2009
DOI: 10.1016/j.geoderma.2009.05.028
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Fluxes of dissolved organic carbon in two tropical forest ecosystems of East Kalimantan, Indonesia

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Cited by 76 publications
(73 citation statements)
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“…The TOC and TN contents and the C/N ratios are also similar for both soils (Tables 3 and 4), and are comparable to values measured in pristine forest soils in the East Kalimantan Province, Indonesia (Fujii et al, 2009), humid tropical primary forest soils in Sumatra (van Noordwijk et al, 1997), and ferralitic soils under tropical rainforest originate from different countries around the world like Brazil, Indonesia, Zaire, … (Kauffman et al, 1998). Several inferences can be made from these results:…”
Section: Production and Evolution Of Som In Volcanic Tropical Soilssupporting
confidence: 76%
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“…The TOC and TN contents and the C/N ratios are also similar for both soils (Tables 3 and 4), and are comparable to values measured in pristine forest soils in the East Kalimantan Province, Indonesia (Fujii et al, 2009), humid tropical primary forest soils in Sumatra (van Noordwijk et al, 1997), and ferralitic soils under tropical rainforest originate from different countries around the world like Brazil, Indonesia, Zaire, … (Kauffman et al, 1998). Several inferences can be made from these results:…”
Section: Production and Evolution Of Som In Volcanic Tropical Soilssupporting
confidence: 76%
“…Taiwan, New Zealand, Guadeloupe), the majority part of the organic carbon export occurs during flood events (Hilton et al, 2008a;Fujii et al, 2009;Bass et al, 2011;Lloret et al, 2013). Accordingly, the sources of organic carbon exported from the catchments vary with the hydrological stage, in particular for small rivers (Lloret et al, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…3). Ultisols are characterized by argillic horizons (clay illuviation) due to clay migration from surface horizon to deeper horizons (lessivage), but clay destruction by acidification can also contribute to loss of clays in the surface soil horizons (Fujii et al 2009). The low concentrations of iron oxides and dominance of permanent-charged 2:1 type clay minerals lead to instability of soil structure and poor water drainage (Sollins et al 1988).…”
Section: +mentioning
confidence: 99%
“…However, inputs of dissolved organic C to the forest floor in litter leachate and throughfall are reduced during the dry season, particularly during periods of very low rainfall (e.g., January to February during the current study year, when\12 mm of rain fell in two months). Inputs of DOC from litter leaching can be considerable and can make an important contribution to organic matter in mineral soil (Fujii et al 2009(Fujii et al , 2011. For example, litter leachate contributed 277 kg C ha -1 y -1 to the soil in a tropical forest under a perudic moisture regime in Costa Rica, much of which occurred in stable high-molecular weight compounds that were retained in the soil through sorption to mineral surfaces (Schwendenmann and Veldkamp 2005).…”
Section: Seasonal Dynamics Of Soil Organic Mattermentioning
confidence: 99%