On the factors affecting the settling velocity of fine suspended sediments in a shallow estuary

Verfasser / Beitragende:
[K. Priya, P. Jegathambal, E. James]
Ort, Verlag, Jahr:
2015
Enthalten in:
Journal of Oceanography, 71/2(2015-04-01), 163-175
Format:
Artikel (online)
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024 7 0 |a 10.1007/s10872-014-0269-x  |2 doi 
035 |a (NATIONALLICENCE)springer-10.1007/s10872-014-0269-x 
245 0 0 |a On the factors affecting the settling velocity of fine suspended sediments in a shallow estuary  |h [Elektronische Daten]  |c [K. Priya, P. Jegathambal, E. James] 
520 3 |a Of the factors that affect settling velocity (w s), the concentration of suspended sediments (SSC), C, and turbulence (root-mean-square velocity gradient), G, have been identified as being of major importance. This work reveals the important effect on w s of the vertical salinity gradient, s, (defined as the difference between surface and bottom salinity divided by water depth). w s was obtained by use of the Rouse equation, and ranged between 0.1 and 2.47mm/s. w s was found to have an exponential relationship with SSC for low SSC; an inverse relationship was observed for high SSC, because of hindered settling. The study revealed that w s was inversely related to s and its effect was observed only for high values of s. A new model is proposed in which w s is explained in terms of C, G, and s. Two scenarios were considered on the basis of the stratification parameter ∂S/S 0 (the ratio of the difference between the surface and bottom salinity divided by the mean salinity): ∂S/S 0>0.1 and ∂S/S 0<0.1. The effect of s on w s was negligible when ∂S/S 0<0.1. Regression analysis was performed on observed w s (using the Rouse equation) and calculated w s using three approaches: (1) $$w_\text{s} \propto \,C^{x}$$ w s ∝ C x , (2) $$w_\text{s} \propto \,C^{x} G^{y}$$ w s ∝ C x G y , and (3) the new model $$w_\text{s} \propto \,C^{x} G^{y} s^{ - z} , {\text{for}}$$ w s ∝ C x G y s - z , for ∂S/S 0>0.1, and coefficients of determination of 0.59, 0.65, and 0.86 respectively were obtained. The new model has the advantage that it is dimensionally stable and the empirical coefficient is dimensionless. 
540 |a The Oceanographic Society of Japan and Springer Japan, 2015 
690 7 |a Settling velocity  |2 nationallicence 
690 7 |a SS concentration  |2 nationallicence 
690 7 |a Turbulence  |2 nationallicence 
690 7 |a Salinity gradient  |2 nationallicence 
690 7 |a Stratification parameter  |2 nationallicence 
690 7 |a Muthupet estuary, India  |2 nationallicence 
700 1 |a Priya  |D K.  |u School of Civil Engineering, Karunya University, Coimbatore, India  |4 aut 
700 1 |a Jegathambal  |D P.  |u Water Institute, Karunya University, Coimbatore, India  |4 aut 
700 1 |a James  |D E.  |u Water Institute, Karunya University, Coimbatore, India  |4 aut 
773 0 |t Journal of Oceanography  |d Springer Japan  |g 71/2(2015-04-01), 163-175  |x 0916-8370  |q 71:2<163  |1 2015  |2 71  |o 10872 
856 4 0 |u https://doi.org/10.1007/s10872-014-0269-x  |q text/html  |z Onlinezugriff via DOI 
898 |a BK010053  |b XK010053  |c XK010000 
900 7 |a Metadata rights reserved  |b Springer special CC-BY-NC licence  |2 nationallicence 
908 |D 1  |a research-article  |2 jats 
949 |B NATIONALLICENCE  |F NATIONALLICENCE  |b NL-springer 
950 |B NATIONALLICENCE  |P 856  |E 40  |u https://doi.org/10.1007/s10872-014-0269-x  |q text/html  |z Onlinezugriff via DOI 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Priya  |D K.  |u School of Civil Engineering, Karunya University, Coimbatore, India  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Jegathambal  |D P.  |u Water Institute, Karunya University, Coimbatore, India  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a James  |D E.  |u Water Institute, Karunya University, Coimbatore, India  |4 aut 
950 |B NATIONALLICENCE  |P 773  |E 0-  |t Journal of Oceanography  |d Springer Japan  |g 71/2(2015-04-01), 163-175  |x 0916-8370  |q 71:2<163  |1 2015  |2 71  |o 10872