2010
DOI: 10.1007/s10661-010-1418-3
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Co-assessment of biomass and soil organic carbon stocks in a future reservoir area located in Southeast Asia

Abstract: An assessment of the organic carbon stock present in living or dead vegetation and in the soil on the 450 km2 of the future Nam Theun 2 hydroelectric reservoir in Lao People's Democratic Republic was made. Nine land cover types were defined on the studied area: dense, medium, light, degraded, and riparian forests; agricultural soil; swamps; water; and others (roads, construction sites, and so on). Their geographical distribution was assessed by remote sensing using two 2008 SPOT 5 images. The area is mainly co… Show more

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Cited by 30 publications
(22 citation statements)
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“…The main tributaries of the reservoir are the Nam Xot, the Nam Theun and the Nam On Rivers. The reservoir flooded almost 70% of dense to light forest, 23% of degraded forest, riparian forest and agricultural soils and the last 7% were composed of water system, swamps and villages (Descloux et al, 2011 …”
Section: Study Areamentioning
confidence: 99%
“…The main tributaries of the reservoir are the Nam Xot, the Nam Theun and the Nam On Rivers. The reservoir flooded almost 70% of dense to light forest, 23% of degraded forest, riparian forest and agricultural soils and the last 7% were composed of water system, swamps and villages (Descloux et al, 2011 …”
Section: Study Areamentioning
confidence: 99%
“…In the Nam Ngum reservoir in Laos, standing trees almost completely eliminate wind-generated turbulence and consequently reduce the extent of mixing (Baxter, 1977). It may explain why the impact of annual destratification is lower in the Nam Malou area (RES3) initially covered by forest (Descloux et al, 2011). Contrary to the Petit Saut Reservoir in French Guiana , this stratification weakened then disappeared each year during the CD season due to a drop of air temperature (Descloux et al, this issue-a).…”
Section: From a Riverine System To A Lacustrine Systemmentioning
confidence: 99%
“…The NT2 Reservoir covers a surface area of 489 km² at its full supply level and potentially decreases to a minimum of 86 km² at the end of the dry season (Descloux et al, same issue). The reservoir flooded almost 70% of dense to light forest, 23% of degraded forest, riparian forest and agricultural soils and the last 7% were composed of water system, swamps and villages (Descloux et al, 2011). The reservoir is qualified as a dendritic and is relatively shallow with an average depth of 8 m (Chanudet et al, 2012).…”
Section: Study Areamentioning
confidence: 99%