2020
DOI: 10.1016/j.ecss.2020.106718
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Effects of an estuarine dam on sediment flux mechanisms in a shallow, macrotidal estuary

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Cited by 19 publications
(14 citation statements)
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“…Other human activities including upstream dam construction, farmland reclamation, and tourism activities may increase landscape fragmentation and have a negative impact on vegetation and related ecosystems. Simultaneously, dam protection [ 55 , 56 ] and appropriate protection management [ 33 ] can respond to the change of ecological vulnerability by implementing different strategies to natural disasters and man-made disturbances. Finally, 17 indicators were selected from three subsystems ( Table 1 ).…”
Section: Methodsmentioning
confidence: 99%
“…Other human activities including upstream dam construction, farmland reclamation, and tourism activities may increase landscape fragmentation and have a negative impact on vegetation and related ecosystems. Simultaneously, dam protection [ 55 , 56 ] and appropriate protection management [ 33 ] can respond to the change of ecological vulnerability by implementing different strategies to natural disasters and man-made disturbances. Finally, 17 indicators were selected from three subsystems ( Table 1 ).…”
Section: Methodsmentioning
confidence: 99%
“…In the GRE, the sediment was sandy-silt and d 50 was 14-58 µm (Ministry of Oceans and Fisheries, 2019). The mean current velocity reached approximately 0.5 m s −1 during the spring tide (Figueroa et al, 2020). The optical backscattering sensor and LISST-Holo were profiled at intervals of 30 min for 12 h on September 2, 2016, to collect the particle information.…”
Section: Study Sites and Data Collectionmentioning
confidence: 99%
“…Available case studies indicate that these estuarine dams can result in tidal amplification due to reflection of the tidal wave (Díez‐Minguito et al., 2012; Kang, 1999; Kwon & Lee, 1999), reduction of tidal currents due to loss of the tidal prism, and change in the magnitude of tidal asymmetry due to altered tidal and river forcing (Kang, 1999; Kim et al., 2006; Traini et al., 2015). In turn, altered tidal and river forcing has been inferred to change the salinity structure and estuarine type (Shin et al., 2019), including the potential to develop periodic stratification (Figueroa et al., 2019; Figueroa, Lee, & Shin, 2020). Furthermore, the reduced tidal currents and estuarine dam discharge have been observed to result in lower suspended sediment concentration (SSC; Kim et al., 2006; Traini et al., 2015), increasing fluvial sediment abundance (Williams et al., 2014), and enhanced deposition of fine sediment in the remnant estuary (Kim et al., 2006; Lee & Lee, 2007; Tilai et al., 2019; van Proosdij et al., 2009; Williams et al., 2013, 2014; Zhu et al., 2017).…”
Section: Introductionmentioning
confidence: 99%
“…For example, in a microtidal estuary with relatively large freshwater discharge, sediment flux convergence can occur due to a negative gradient in the seaward advective sediment flux driven by river runoff (Chang et al., 2020; Williams et al., 2015). In contrast, in a macrotidal estuary with moderate freshwater discharge, sediment flux convergence can occur due to a negative gradient in the landward tidal pumping sediment flux driven by tidal asymmetry (Figueroa, Lee, Chang, et al., 2020; Figueroa, Lee, & Shin, 2020; Zhu et al., 2017).…”
Section: Introductionmentioning
confidence: 99%