2015
DOI: 10.1007/s10750-015-2410-2
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Different hydrodynamic conditions on the deposition of organic carbon in sediment of two reservoirs

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Cited by 23 publications
(4 citation statements)
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“…Burial rates smaller than that of CUN were observed in in some reservoirs located in colder climate zones (boreal Eastmain reservoir: 32.9 g C m -2 yr -1 , Canada, Teodoru et al, 2012); temperate Xinanjiang reservoir: 43.4 g C m -2 yr -1 , China, (Wang et al, 2017); temperate Huairou water supply reservoir: 62.3 g C m -2 yr -1 , China, (Luo et al, 2016). However, some higher rates 20 than in CUN were also registered (temperate Shisanling hydroelectric reservoir: 100 g C m -2 yr -1 , China, (Luo et al, 2016); US reservoirs: range 149 to 363 g C m −2 yr −1 , (Clow et al, 2015); temperate Lake Wohlen: 1,113 ± 482 g C m -2 yr -1 , Switzerland, (Sobek et al, 2012). According to the latest global estimate, an OC burial rate of 1,418 ± 2,761 g C m −2 yr −1 was reported for reservoirs (Mendonça et al, 2017).…”
Section: Sediment Accumulation and Organic Carbon Burial Ratesmentioning
confidence: 93%
“…Burial rates smaller than that of CUN were observed in in some reservoirs located in colder climate zones (boreal Eastmain reservoir: 32.9 g C m -2 yr -1 , Canada, Teodoru et al, 2012); temperate Xinanjiang reservoir: 43.4 g C m -2 yr -1 , China, (Wang et al, 2017); temperate Huairou water supply reservoir: 62.3 g C m -2 yr -1 , China, (Luo et al, 2016). However, some higher rates 20 than in CUN were also registered (temperate Shisanling hydroelectric reservoir: 100 g C m -2 yr -1 , China, (Luo et al, 2016); US reservoirs: range 149 to 363 g C m −2 yr −1 , (Clow et al, 2015); temperate Lake Wohlen: 1,113 ± 482 g C m -2 yr -1 , Switzerland, (Sobek et al, 2012). According to the latest global estimate, an OC burial rate of 1,418 ± 2,761 g C m −2 yr −1 was reported for reservoirs (Mendonça et al, 2017).…”
Section: Sediment Accumulation and Organic Carbon Burial Ratesmentioning
confidence: 93%
“…Organic matter is a major component of suspended particles and fine sediment particles that determine many biogeochemical processes in marine environments (Bernasconi et al, 1997;Chen et al, 2012). Two natural sources of organic matter are generally considered in coastal ecosystems: allochthonous inputs and autochthonous production (Antonio and Richoux, 2014;Luo et al, 2016). Major sources of autochthonous organic matter include phytoplankton and aquatic macrophytes (Dalu and Froneman, 2016;Pearson et al, 2015).…”
Section: Fish Isotopic Nichesmentioning
confidence: 99%
“…Additionally, dam construction promotes the intensive water-level fluctuations to cause landslides and debris flows and indirectly influence land types, which may increase the terrestrial POC in the reservoir (Yao et al, 2006;Luo et al, 2016;Iqbal et al, 2018;Zorzal-Almeida et al, 2018).…”
Section: Cascade Damming Effect On Input and Accumulation Of Pocmentioning
confidence: 99%