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The influence of wind, fetch, and water depth on the distribution of sediments in Lake Vänern, Sweden

Håkanson, Lars·1977·Canadian Journal of Earth Sciences

Abstract

The purpose of this work is to establish an erosion–transportation–accumulation diagram for fine recent deposits on lake bottoms and to show empirically that an understanding of the bottom dynamic processes is of vital importance for a proper interpretation of sediment data.The potential maximum effective fetch (PF eff) has been used to indicate the available water energy, and the water depth has been used to indicate the effectiveness of the PF eff on the bottom. The 50% water content of surficial sediments, 0–1 cm, has been utilized as a physical sediment parameter to distinguish erosion from transportation and the 75% water content to separate transportation from accumulation.Relationships between water content, bulk density, and grain size are discussed.The distribution pattern of different elements (Be, B, V, Ni, Cu, Zn, Mo, Ag, Cd, Sn, Hg, Pb, Bi, P, and N) in the sediments of Lake Vänern is interpreted in the light of the bottom dynamic processes.

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Metadata

Authors
Håkanson, L.
Venue
Canadian Journal of Earth Sciences
Published
1977-03-01
Volume
14
Issue
3
Pages
397-412
ISSN
  • 0008-4077 (ISSN-L)
  • 1480-3313
OpenAlex
W1985131767
Cited by
293
References
0
FWCI
4.72
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The influence of wind, fetch, and water depth on the distribution of sediments in Lake Vänern, Sweden. https://app.cochat.ai/papers/10.1139/e77-040
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Håkanson, L. (1977). The influence of wind, fetch, and water depth on the distribution of sediments in Lake Vänern, Sweden. Canadian Journal of Earth Sciences. https://doi.org/10.1139/e77-040

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.