The impacts of the Churchill Barriers on the coastal environment
The impacts of the Churchill Barriers on the coastal environment
This research investigated the impact of The Churchill Barriers on the coastal and marine environment through analysis of nearshore and terrestrial cores using geochemical and diatom analyses, 210Pb and 137Cs dating and field surveying. Analyses of a core taken from near barrier 1 showed that an eutrophic environment dominated throughout the sedimentary sequence. An increase in calcium carbonate, combined with increases in strontium and sodium and a small change in diatom composition, is thought to relate to barrier construction around 1940–1945. A similar pattern is revealed from a core taken near barrier 4 and also from Echna Loch (Burray). On the east side of barrier 4, a large area of sand deposition has occurred as a result of the sheltered environment offered by the barrier. Sediment has been transported northwards by longshore drift and moved onshore from offshore sand bars, forming an extensive sand dune environment. The sediment deposition can be seen to a lesser extent on the east side of the barriers 1, 2 and 3. These results suggest tentatively that barrier formation may have impacted on water flow patterns, and hence algal communities, leading to changes in floral composition. Furthermore, changes in sediment patterns, coastal geomorphology are evident from barrier emplacement.
100-118
Selby, K.A.
e9f6ac15-0ceb-424e-85c1-ee0debeb5346
Langdon, P.G.
95b97671-f9fe-4884-aca6-9aa3cd1a6d7f
14 September 2012
Selby, K.A.
e9f6ac15-0ceb-424e-85c1-ee0debeb5346
Langdon, P.G.
95b97671-f9fe-4884-aca6-9aa3cd1a6d7f
Selby, K.A. and Langdon, P.G.
(2012)
The impacts of the Churchill Barriers on the coastal environment.
Scottish Geographical Journal, 128 (2), .
(doi:10.1080/14702541.2012.716606).
Abstract
This research investigated the impact of The Churchill Barriers on the coastal and marine environment through analysis of nearshore and terrestrial cores using geochemical and diatom analyses, 210Pb and 137Cs dating and field surveying. Analyses of a core taken from near barrier 1 showed that an eutrophic environment dominated throughout the sedimentary sequence. An increase in calcium carbonate, combined with increases in strontium and sodium and a small change in diatom composition, is thought to relate to barrier construction around 1940–1945. A similar pattern is revealed from a core taken near barrier 4 and also from Echna Loch (Burray). On the east side of barrier 4, a large area of sand deposition has occurred as a result of the sheltered environment offered by the barrier. Sediment has been transported northwards by longshore drift and moved onshore from offshore sand bars, forming an extensive sand dune environment. The sediment deposition can be seen to a lesser extent on the east side of the barriers 1, 2 and 3. These results suggest tentatively that barrier formation may have impacted on water flow patterns, and hence algal communities, leading to changes in floral composition. Furthermore, changes in sediment patterns, coastal geomorphology are evident from barrier emplacement.
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Published date: 14 September 2012
Organisations:
Palaeoenvironment Laboratory (PLUS)
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Local EPrints ID: 350695
URI: http://eprints.soton.ac.uk/id/eprint/350695
ISSN: 1470-2541
PURE UUID: 30a1a1fc-eb17-43df-a09b-25e1ddef1164
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Date deposited: 28 Mar 2013 14:07
Last modified: 15 Mar 2024 02:57
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K.A. Selby
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