Correlations between sound velocity and related properties of glacio-marine sediments : barents sea
Statistical analysis of laboratory-measured compressional wave (sound) velocity, porosity, wet bulk density, and selected textural parameters of surface sediments from the Barents Sea reveals that clay content and mean grain size are the best indices to sound velocity. These parameters are followed...
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| Veröffentlicht in: | Geo-marine letters 1991-01, Vol.11 (2), p.79-83 |
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| creator | ORSI, T. H DUNN, D. A |
| description | Statistical analysis of laboratory-measured compressional wave (sound) velocity, porosity, wet bulk density, and selected textural parameters of surface sediments from the Barents Sea reveals that clay content and mean grain size are the best indices to sound velocity. These parameters are followed closely by porosity and wet bulk density, while sand content provides the weakest index. Although Barents Sea surface sediments are characterized by fairly high variability, the results of the present study are in general agreement with studies of similar sediment types in other continental shelf environments. |
| doi_str_mv | 10.1007/BF02431033 |
| format | Article |
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| ispartof | Geo-marine letters, 1991-01, Vol.11 (2), p.79-83 |
| issn | 0276-0460 1432-1157 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_15976761 |
| source | SpringerNature Journals |
| subjects | Earth sciences Earth, ocean, space Exact sciences and technology Marine Marine geology |
| title | Correlations between sound velocity and related properties of glacio-marine sediments : barents sea |
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