Modelling acoustic scattering by suspended flocculating sediments
The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this prob...
Ausführliche Beschreibung
Autor*in: |
Thorne, Peter D. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2014transfer abstract |
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Schlagwörter: |
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Umfang: |
11 |
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Übergeordnetes Werk: |
Enthalten in: A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies - Chandra', S. ELSEVIER, 2020, Amsterdam [u.a.] |
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Übergeordnetes Werk: |
volume:88 ; year:2014 ; day:1 ; month:10 ; pages:81-91 ; extent:11 |
Links: |
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DOI / URN: |
10.1016/j.csr.2014.07.003 |
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Katalog-ID: |
ELV039323447 |
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520 | |a The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. | ||
520 | |a The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. | ||
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10.1016/j.csr.2014.07.003 doi GBVA2014009000018.pica (DE-627)ELV039323447 (ELSEVIER)S0278-4343(14)00229-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Thorne, Peter D. verfasserin aut Modelling acoustic scattering by suspended flocculating sediments 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. Flocculation Elsevier Acoustic scattering Elsevier Modelling Elsevier Suspended cohesive sediments Elsevier Sediment transport Elsevier MacDonald, Iain T. oth Vincent, Christopher E. oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 https://doi.org/10.1016/j.csr.2014.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 88 2014 1 1001 81-91 11 045F 550 |
spelling |
10.1016/j.csr.2014.07.003 doi GBVA2014009000018.pica (DE-627)ELV039323447 (ELSEVIER)S0278-4343(14)00229-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Thorne, Peter D. verfasserin aut Modelling acoustic scattering by suspended flocculating sediments 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. Flocculation Elsevier Acoustic scattering Elsevier Modelling Elsevier Suspended cohesive sediments Elsevier Sediment transport Elsevier MacDonald, Iain T. oth Vincent, Christopher E. oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 https://doi.org/10.1016/j.csr.2014.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 88 2014 1 1001 81-91 11 045F 550 |
allfields_unstemmed |
10.1016/j.csr.2014.07.003 doi GBVA2014009000018.pica (DE-627)ELV039323447 (ELSEVIER)S0278-4343(14)00229-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Thorne, Peter D. verfasserin aut Modelling acoustic scattering by suspended flocculating sediments 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. Flocculation Elsevier Acoustic scattering Elsevier Modelling Elsevier Suspended cohesive sediments Elsevier Sediment transport Elsevier MacDonald, Iain T. oth Vincent, Christopher E. oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 https://doi.org/10.1016/j.csr.2014.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 88 2014 1 1001 81-91 11 045F 550 |
allfieldsGer |
10.1016/j.csr.2014.07.003 doi GBVA2014009000018.pica (DE-627)ELV039323447 (ELSEVIER)S0278-4343(14)00229-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Thorne, Peter D. verfasserin aut Modelling acoustic scattering by suspended flocculating sediments 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. Flocculation Elsevier Acoustic scattering Elsevier Modelling Elsevier Suspended cohesive sediments Elsevier Sediment transport Elsevier MacDonald, Iain T. oth Vincent, Christopher E. oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 https://doi.org/10.1016/j.csr.2014.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 88 2014 1 1001 81-91 11 045F 550 |
allfieldsSound |
10.1016/j.csr.2014.07.003 doi GBVA2014009000018.pica (DE-627)ELV039323447 (ELSEVIER)S0278-4343(14)00229-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 570 610 VZ 44.09 bkl Thorne, Peter D. verfasserin aut Modelling acoustic scattering by suspended flocculating sediments 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. Flocculation Elsevier Acoustic scattering Elsevier Modelling Elsevier Suspended cohesive sediments Elsevier Sediment transport Elsevier MacDonald, Iain T. oth Vincent, Christopher E. oth Enthalten in Elsevier Science Chandra', S. ELSEVIER A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies 2020 Amsterdam [u.a.] (DE-627)ELV006306659 volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 https://doi.org/10.1016/j.csr.2014.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.09 Medizintechnik VZ AR 88 2014 1 1001 81-91 11 045F 550 |
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English |
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Enthalten in A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies Amsterdam [u.a.] volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 |
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Enthalten in A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies Amsterdam [u.a.] volume:88 year:2014 day:1 month:10 pages:81-91 extent:11 |
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A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies |
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A Comparative Analysis of Performance of Several Wavelet Based ECG Data Compression Methodologies |
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modelling acoustic scattering by suspended flocculating sediments |
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Modelling acoustic scattering by suspended flocculating sediments |
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The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. |
abstractGer |
The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. |
abstract_unstemmed |
The development of a theoretical description of how sound interacts with flocculating sediments has been lacking and this deficiency has impeded sound being used to extract quantitative suspended sediment parameters in suspensions containing flocs. As a step towards theoretically examining this problem a relatively simple heuristic approach has been adopted to provide a description of the interaction of sound with suspensions that undergo flocculation. A model is presented for the interpretation of acoustic scattering from suspensions of fine sediments as they transition from primary particles, through an intermediate regime, to the case where low density flocs dominate the acoustic scattering. The approach is based on modified spherical elastic solid and elastic fluid scatterers and a combination of both. To evaluate the model the variation of density and compressional velocity within the flocs as they form and grow in size is required. The density can be estimated from previous studies; however, the velocity is unknown and is formulated here using a fluid mixture approach. Uncertainties in these parameters can have a significant effect on the predicted scattering characteristics and are therefore investigated in the present study. Furthermore, to assess the proposed model, outputs are compared with recently published laboratory observations of acoustic scattering by flocculating cohesive suspensions. |
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Modelling acoustic scattering by suspended flocculating sediments |
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