Re: Scouring/deposition of inter-tidal mud
- From: "Carsten Troelsgaard" <carsten.troelsgaard@xxxxxxx>
- Date: Fri, 25 Nov 2005 10:44:53 +0100
"N Cook" <diverse@xxxxxxxxx> skrev i en meddelelse
news:dm6h0g$dc0$1@xxxxxxxxxxxxxxxxxx
> There is a local site of historic interest that consists of the
> remnants of wood piles in intertidal mud of a local river.
> Recently, viewing the site, there was nothing to be seen but previous
> occassions the stumps are exposed by as much as a foot each.
> Could someone tell me what the mechanism is and whether the
> scouring/deposition is related to springs/neap tides, time of year,
> upstream
> rainfall, temperature, wind, worm activity or what ?
I have difficulties visioning your setting, but you obviously have a site at
the 'end of a river'. One thing that primarily comes to mind is the question
of the magnitude of the tidal cycle, the wave/wind-climate of the coast, the
hinterland and the shelf, but it may not alter some basic characteristics.
One characteristic scouring is related to low-tide: at high tide the total
area covered by water may act as a conduite for the flow of water. When the
area is reduced, the flow to and from is confined to smaller and smaller
areas that consequently suffers scouring. - this may evolve into a dendritic
drainage-pattern. Sedimentation happens at high tide and covers large areas,
so the scour and the sedimentation differs. The characteristics of the tidal
sediments may be the heterolithic mix of small pockets of sand draped by a
fine clay that binds the sand and gives it less resistance (smooth surface)
to erosion by subsequent return-flow.
The tidal flow happens in response to a changing gradient of the
sea-surface - if a large shelf is inundated, this gradient makes in and
out-flow different: the out-flow has to pass a volume of water under a lower
surface-height, than the inflow. This is why an 'inland' drainage-pattern
may be prolonged to cover the shelf outside the tidal zone.
I cannot tell weather your setting is so that enhanced runoff in rainy
periods makes for a fluvial (stream) sedimentation on the premises of the
river - and that the principles of this deposits later interfer with the
coastal/tidal sedimentation. The alternative is, that the river-mouth
naturally displace barres over time - which, I believe, you already have
considered, as well as weather the covering of the stumps has been related
to storm-events? The slushing to and fro of tidal waters potentially makes
it a dynamic place for moving sediments around.
I see that you write from uk, so I wonder weather your river faces an east
or a west coast. There is a large differens in tidal magnitude and
wind/wave-climate between the two.
Carsten
.
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