Multibeam sonar backscatter lineaments and anthropogenic organic components in lacustrine silty clay, evidence of shipping in western Lake Ontario

C. F.M. Lewis, L. A. Mayer, P. K. Mukhopadhyay, Michael Kruge, J. P. Coakley, M. D. Smith

Research output: Contribution to journalConference article

9 Citations (Scopus)

Abstract

A multibeam sonar survey (95 kHz) covering more than 500 km2 of western Lake Ontario revealed anomalous lineaments of relatively high backscatter. The lineaments did not align with or parallel the most prominent structural zones beneath the lake as expected. Instead, the principal lineaments lay on lines between ports on opposite sides of the lake, especially between Toronto and Welland Canal, and Toronto and Niagara River mouth. As the lineaments underlie current and historical shipping routes used during the steamship era, they are interpreted as an acoustic response to shipping debris cumulated in the near-surface bottom sediment. An exploratory study of the organic components in the silty clay surface sediment, using geochemical and petrological techniques, shows that the upper 10 cm commonly contains silt-sized particles of anthropogenic origin, especially combustion residues. Combustion residues are more abundant on or near the lineaments, consistent with an origin related to shipping. Enhanced acoustic backscatter is evident where silt-sized combustion particles are hosted in dominantly clay-sized sediment. The coarser-grained anthropogenic particles increase the acoustic impedance of the lakebed relative to the bottom water as well as the roughness and volume scattering contributions to lakebed backscatter. (C) 2000 Elsevier Science B.V. All rights reserved.

Original languageEnglish
Pages (from-to)307-324
Number of pages18
JournalInternational Journal of Coal Geology
Volume43
Issue number1-4
DOIs
StatePublished - 1 May 2000
EventTSOP - Halifax'98, 15th Annual Meeting of The Society for Organic Petrology: Sailing into the New Millennium - Halifax, NS, Can
Duration: 27 Jul 199828 Jul 1998

Fingerprint

multibeam sonar
silty clay
Sonar
Freight transportation
lineament
shipping
backscatter
Lakes
Sediments
Clay
Silt
lake
Steamships
Acoustics
Acoustic impedance
Canals
silt
Debris
acoustics
sediment

Keywords

  • Acoustic backscatter
  • Lake Ontario
  • Multibeam sonar mapping
  • Neotectonics
  • Sediment organic components
  • Seismic hazard
  • Shipping

Cite this

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title = "Multibeam sonar backscatter lineaments and anthropogenic organic components in lacustrine silty clay, evidence of shipping in western Lake Ontario",
abstract = "A multibeam sonar survey (95 kHz) covering more than 500 km2 of western Lake Ontario revealed anomalous lineaments of relatively high backscatter. The lineaments did not align with or parallel the most prominent structural zones beneath the lake as expected. Instead, the principal lineaments lay on lines between ports on opposite sides of the lake, especially between Toronto and Welland Canal, and Toronto and Niagara River mouth. As the lineaments underlie current and historical shipping routes used during the steamship era, they are interpreted as an acoustic response to shipping debris cumulated in the near-surface bottom sediment. An exploratory study of the organic components in the silty clay surface sediment, using geochemical and petrological techniques, shows that the upper 10 cm commonly contains silt-sized particles of anthropogenic origin, especially combustion residues. Combustion residues are more abundant on or near the lineaments, consistent with an origin related to shipping. Enhanced acoustic backscatter is evident where silt-sized combustion particles are hosted in dominantly clay-sized sediment. The coarser-grained anthropogenic particles increase the acoustic impedance of the lakebed relative to the bottom water as well as the roughness and volume scattering contributions to lakebed backscatter. (C) 2000 Elsevier Science B.V. All rights reserved.",
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Multibeam sonar backscatter lineaments and anthropogenic organic components in lacustrine silty clay, evidence of shipping in western Lake Ontario. / Lewis, C. F.M.; Mayer, L. A.; Mukhopadhyay, P. K.; Kruge, Michael; Coakley, J. P.; Smith, M. D.

In: International Journal of Coal Geology, Vol. 43, No. 1-4, 01.05.2000, p. 307-324.

Research output: Contribution to journalConference article

TY - JOUR

T1 - Multibeam sonar backscatter lineaments and anthropogenic organic components in lacustrine silty clay, evidence of shipping in western Lake Ontario

AU - Lewis, C. F.M.

AU - Mayer, L. A.

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AU - Coakley, J. P.

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N2 - A multibeam sonar survey (95 kHz) covering more than 500 km2 of western Lake Ontario revealed anomalous lineaments of relatively high backscatter. The lineaments did not align with or parallel the most prominent structural zones beneath the lake as expected. Instead, the principal lineaments lay on lines between ports on opposite sides of the lake, especially between Toronto and Welland Canal, and Toronto and Niagara River mouth. As the lineaments underlie current and historical shipping routes used during the steamship era, they are interpreted as an acoustic response to shipping debris cumulated in the near-surface bottom sediment. An exploratory study of the organic components in the silty clay surface sediment, using geochemical and petrological techniques, shows that the upper 10 cm commonly contains silt-sized particles of anthropogenic origin, especially combustion residues. Combustion residues are more abundant on or near the lineaments, consistent with an origin related to shipping. Enhanced acoustic backscatter is evident where silt-sized combustion particles are hosted in dominantly clay-sized sediment. The coarser-grained anthropogenic particles increase the acoustic impedance of the lakebed relative to the bottom water as well as the roughness and volume scattering contributions to lakebed backscatter. (C) 2000 Elsevier Science B.V. All rights reserved.

AB - A multibeam sonar survey (95 kHz) covering more than 500 km2 of western Lake Ontario revealed anomalous lineaments of relatively high backscatter. The lineaments did not align with or parallel the most prominent structural zones beneath the lake as expected. Instead, the principal lineaments lay on lines between ports on opposite sides of the lake, especially between Toronto and Welland Canal, and Toronto and Niagara River mouth. As the lineaments underlie current and historical shipping routes used during the steamship era, they are interpreted as an acoustic response to shipping debris cumulated in the near-surface bottom sediment. An exploratory study of the organic components in the silty clay surface sediment, using geochemical and petrological techniques, shows that the upper 10 cm commonly contains silt-sized particles of anthropogenic origin, especially combustion residues. Combustion residues are more abundant on or near the lineaments, consistent with an origin related to shipping. Enhanced acoustic backscatter is evident where silt-sized combustion particles are hosted in dominantly clay-sized sediment. The coarser-grained anthropogenic particles increase the acoustic impedance of the lakebed relative to the bottom water as well as the roughness and volume scattering contributions to lakebed backscatter. (C) 2000 Elsevier Science B.V. All rights reserved.

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