2016
DOI: 10.1016/j.jenvman.2016.05.080
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Soil–air greenhouse gas fluxes influenced by farming practices in reservoir drawdown area: A case at the Three Gorges Reservoir in China

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Cited by 37 publications
(17 citation statements)
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“…It floods 489 km 2 of very diverse types of ecosystems including forest, agricultural soils and wetlands (Descloux et al, 2011). Geological formations responsible for the soil development in the NT2R area are mainly composed of more or less consolidated sedimentary rocks (Lovatt Smith et al, 1996;Smith and Stokes, 1997). The parental rocks belong to the Khorat group and Phon Hong group formations (Cretaceous) with two main lithologies: (1) late cretaceous Maha Sarakham formation (i.e.…”
Section: Study Sitementioning
confidence: 99%
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“…It floods 489 km 2 of very diverse types of ecosystems including forest, agricultural soils and wetlands (Descloux et al, 2011). Geological formations responsible for the soil development in the NT2R area are mainly composed of more or less consolidated sedimentary rocks (Lovatt Smith et al, 1996;Smith and Stokes, 1997). The parental rocks belong to the Khorat group and Phon Hong group formations (Cretaceous) with two main lithologies: (1) late cretaceous Maha Sarakham formation (i.e.…”
Section: Study Sitementioning
confidence: 99%
“…However, areal fluxes from the drawdown area are on average 2.5 times higher than the diffusive fluxes from the reservoir water surface in 2009-2010 and 6 times higher than those fluxes in 2013 making the soils in the area of influence of the reservoir a hotspot for CO 2 emissions compared to the reservoir surface waters. The total emissions of reservoirs with contrasted hydrology characterized by marked wet and dry seasons and large water-level variations of 30 % of the total surface could have been significantly underestimated as it is the case for Petit Saut (∼ 100 km 2 ), Samuel (∼ 280 km 2 ), Balbina (∼ 220 km 2 ) or The Three Gorges Reservoir (∼ 400 km 2 ) for instance (Guérin et al, 2006;Kemenes et al, 2011;Li et al, 2016). This pathway is expected to be more significant in flatbottom reservoirs than in valley-type reservoirs in mountainous regions and cannot be generalized to just the drawdown area without taking into account hydrological water management and the local topography.…”
Section: Total Co 2 Emissions From the Nam Theun 2 Reservoirmentioning
confidence: 99%
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“…This reservoir is from Chongqing (west) to Yichang of Hubei province (east), and the distance is approximately 662.9 km 1 . In the winter, water level of the TGR is 175 m, whereas water level of the TGR is only 145 m in the summer for the aim of flood control 2 . This water fluctuation every year produces an area of 400 km 2 along the upper stream of Yangtze River called water-level fluctuating zone (WLFZ).…”
Section: Introductionmentioning
confidence: 99%
“…In each plot, GHG flux were made at the row position between plants in croplands, and aboveground vegetation in each plot of grasslands was cut off before gas sampling. Sampling time was selected from 9 a.m. to 11 a.m., when transient emissions represent the mean emission of the day (Li et al, 2016). Gas samples were collected from each chamber at 0, 10, 20 and 30 min after the chamber was deployed using a polypropylene medical syringe through a triple valve.…”
Section: Field Sampling and Measurementsmentioning
confidence: 99%