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2020
DOI: 10.1016/j.ecss.2019.106525
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Suspended particulate matter concentration in response to tidal hydrodynamics in a long mesotidal floodway

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Cited by 8 publications
(5 citation statements)
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References 38 publications
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“…Our results for the total flux between Stations A, B, and C indicated the existence of a turbidity maximum zone in the Ota Diversion Channel. Figure 9f shows the convergence of the total flux near Station B at mid-depth during spring tide, supporting the findings of Xiao et al [29]. Our findings suggest that the existence of a convergence zone in the Ota Diversion Channel is more likely to be caused by the total subtidal flux, which is strongly affected by baroclinic flow, rather than simply by river and tidal forcing.…”
Section: Discussionsupporting
confidence: 89%
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“…Our results for the total flux between Stations A, B, and C indicated the existence of a turbidity maximum zone in the Ota Diversion Channel. Figure 9f shows the convergence of the total flux near Station B at mid-depth during spring tide, supporting the findings of Xiao et al [29]. Our findings suggest that the existence of a convergence zone in the Ota Diversion Channel is more likely to be caused by the total subtidal flux, which is strongly affected by baroclinic flow, rather than simply by river and tidal forcing.…”
Section: Discussionsupporting
confidence: 89%
“…The compound cross-sectional channel spans 6 km downstream of the Gion Floodgate, and a single cross-sectional channel spans 3 km downstream of the compound channel. Generally, the bed materials in the Ota Diversion Channels are dominated by silt and clay, with an increasing proportion of finer particles closer to the river mouth [28,29]. Additionally, under normal conditions, the suspended sediment concentration in the Ota Diversion Channel does not exceed 100 g/m 3 [23].…”
Section: Field Sitementioning
confidence: 99%
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“…The tidal range is up to 2-3.5 in the semi-diurnal tidal regime. The gate controls the discharge, with the normal discharge being around 20-100 m3/s (Danial et al, 2019;Xiao et al, 2020). The average bottom topography is approximately 3 m. Moreover, the Ota River is a branching delta.…”
Section: Observation Location and Datamentioning
confidence: 99%
“…Sementara di stasiun 1 (badan sungai) dengan kondisi aliran air sungai yang lebih tenang (penelitian dilakukan saat musim kemarau) memungkinkan suspensi terendapkan ke dasar perairan, sehingga nilai konsentrasi TSS diketahui rendah di stasiun 1. Hal ini sesuai dengan Xiao et al, (2020) yang menyatakan, bahwa distribusi TSS atau MPT di kolom air merupakan hasil dari kombinasi proses-proses erosi, pengendapan atau deposisi dan transportasi. Konsentrasinya dapat bervariasi berdasarkan skala waktu dan tempat.…”
Section: Hasil Dan Pembahasanunclassified