Properties of suspended sediment in the estuarine turbidity maximum of the highly turbid Humber Estuary system, UK

Abstract

Measurements are presented of the properties of suspended particulate matter (SPM) in the estuarine turbidity maximum (ETM) of the upper Humber and Ouse estuaries during transient, relatively low freshwater inflow conditions of September 1995. Very high concentrations of near-bed SPM (more than 100 g l −1 ) were observed in the low-salinity (less than 1), upper reaches. SPM within the ETM consisted largely of fine sediment (silt and clay) that existed as microfloc and macrofloc aggregates and individual particles. Primary sediment particles were very fine grained, and typically, about 20-30% was clay-sized at high water. The clay mineralogy was dominated by chlorite and illite. There was a pronounced increase in particle size in the tidal river, up-estuary of the ETM. The mean specific surface area (SSA) of near-bed SPM within the ETM was 22 m 2 g −1 on a spring tide and 24 m 2 g −1 on a neap tide. A tidal cycle of measurements within a near-bed, high concentration SPM layer during a very small neap tide gave a mean SSA of 26 m 2 g −1 . The percentage of silt and clay in surficial bed sediments along the main channel of the estuary varied strongly. The relatively low silt and clay percentage of surficial bed sediments (about 10-35%) within the ETM's region of highest near-bed SPM concentrations and their low SSA values were in marked contrast to the overlying SPM. The loss on ignition (LOI) of near-bed SPM in the turbid reaches of the estuary was about 10%, compared with about 12% for surface SPM and more than 40% in the very low turbidity waters up-estuary of the ETM. Settling velocities of Humber-Ouse SPM, sampled in situ and measured using a settling column, maximized at 1.5 mm s −1 and exhibited hindered settling at higher SPM concentrations.

On the separation between inorganic and organic fractions of suspended matter in a marine coastal environment

“…grain-size, helped consolidating mass inventories. Likewise, origin and fate of matter in estuarine turbidity maximum zones can be better identified by measuring the quality of TSM, as done for example in the Humber-Ouse estuary (Uncles et al, 2006) or Elbe estuary (Van Beusekom and Brockmann, 1998). The portion of particulate organic matter (POM) of TSM is of particular interest, e.g.…”

Sedimentological and Rheological Properties of the Water–Solid Bed Interface in the Weser and Ems Estuaries, North Sea, Germany: Implications for Fluid Mud Classification

“…The classification and terminology of the constituent layers vary in the literature. The upper layer in the three-layer models is often termed low to highly concentrated suspension (Winterwerp and van Kesteren, 2004) or mobile suspension (Ross, Lin, and Mehta, 1987;Ross and Mehta, 1989;Uncles, Stephens, and Harris, 2006). In this fluid-supported layer, particles settle freely in SSCs of a few milligrams to grams per liter (Ross, Lin, and Mehta, 1987).…”

Evaluation of the Role of Silt Content on the Flocculation Behavior of Clay‐Silt Mixtures

“…Additional complications arise from the effects of sediment composition on flocculation processes. In many coastal environments, clay and silt sediments are often dominant (Carniello et al, 2012;Hill et al, 2013;Safak et al, 2013;Uncles et al, 2006). Previous studies have mostly focused on mud-sand mixtures (Amy et al, 2006;Cuthbertson et al, 2018;Le Hir et al, 2011), and the results have indicated that different compositions of sediments will influence the average floc size and floc formation rates (Cuthbertson et al, 2010(Cuthbertson et al, , 2018.…”