Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov
Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspens...
Ausführliche Beschreibung
Autor*in: |
Arkhipov, B. V. [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2010 |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2010 |
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Übergeordnetes Werk: |
Enthalten in: Computational mathematics and mathematical physics - SP MAIK Nauka/Interperiodica, 1992, 50(2010), 4 vom: Apr., Seite 711-720 |
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Übergeordnetes Werk: |
volume:50 ; year:2010 ; number:4 ; month:04 ; pages:711-720 |
Links: |
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DOI / URN: |
10.1134/S0965542510040123 |
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OLC2037346972 |
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520 | |a Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. | ||
700 | 1 | |a Koterov, V. N. |4 aut | |
700 | 1 | |a Solbakov, V. V. |4 aut | |
700 | 1 | |a Yurezanskaya, Yu. S. |4 aut | |
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10.1134/S0965542510040123 doi (DE-627)OLC2037346972 (DE-He213)S0965542510040123-p DE-627 ger DE-627 rakwb eng 510 VZ Arkhipov, B. V. verfasserin aut Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. Koterov, V. N. aut Solbakov, V. V. aut Yurezanskaya, Yu. S. aut Enthalten in Computational mathematics and mathematical physics SP MAIK Nauka/Interperiodica, 1992 50(2010), 4 vom: Apr., Seite 711-720 (DE-627)131059181 (DE-600)1106328-2 (DE-576)029158060 0965-5425 nnns volume:50 year:2010 number:4 month:04 pages:711-720 https://doi.org/10.1134/S0965542510040123 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-MAT SSG-OPC-MAT GBV_ILN_70 AR 50 2010 4 04 711-720 |
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10.1134/S0965542510040123 doi (DE-627)OLC2037346972 (DE-He213)S0965542510040123-p DE-627 ger DE-627 rakwb eng 510 VZ Arkhipov, B. V. verfasserin aut Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. Koterov, V. N. aut Solbakov, V. V. aut Yurezanskaya, Yu. S. aut Enthalten in Computational mathematics and mathematical physics SP MAIK Nauka/Interperiodica, 1992 50(2010), 4 vom: Apr., Seite 711-720 (DE-627)131059181 (DE-600)1106328-2 (DE-576)029158060 0965-5425 nnns volume:50 year:2010 number:4 month:04 pages:711-720 https://doi.org/10.1134/S0965542510040123 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-MAT SSG-OPC-MAT GBV_ILN_70 AR 50 2010 4 04 711-720 |
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10.1134/S0965542510040123 doi (DE-627)OLC2037346972 (DE-He213)S0965542510040123-p DE-627 ger DE-627 rakwb eng 510 VZ Arkhipov, B. V. verfasserin aut Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. Koterov, V. N. aut Solbakov, V. V. aut Yurezanskaya, Yu. S. aut Enthalten in Computational mathematics and mathematical physics SP MAIK Nauka/Interperiodica, 1992 50(2010), 4 vom: Apr., Seite 711-720 (DE-627)131059181 (DE-600)1106328-2 (DE-576)029158060 0965-5425 nnns volume:50 year:2010 number:4 month:04 pages:711-720 https://doi.org/10.1134/S0965542510040123 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-MAT SSG-OPC-MAT GBV_ILN_70 AR 50 2010 4 04 711-720 |
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10.1134/S0965542510040123 doi (DE-627)OLC2037346972 (DE-He213)S0965542510040123-p DE-627 ger DE-627 rakwb eng 510 VZ Arkhipov, B. V. verfasserin aut Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. Koterov, V. N. aut Solbakov, V. V. aut Yurezanskaya, Yu. S. aut Enthalten in Computational mathematics and mathematical physics SP MAIK Nauka/Interperiodica, 1992 50(2010), 4 vom: Apr., Seite 711-720 (DE-627)131059181 (DE-600)1106328-2 (DE-576)029158060 0965-5425 nnns volume:50 year:2010 number:4 month:04 pages:711-720 https://doi.org/10.1134/S0965542510040123 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-MAT SSG-OPC-MAT GBV_ILN_70 AR 50 2010 4 04 711-720 |
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10.1134/S0965542510040123 doi (DE-627)OLC2037346972 (DE-He213)S0965542510040123-p DE-627 ger DE-627 rakwb eng 510 VZ Arkhipov, B. V. verfasserin aut Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. Koterov, V. N. aut Solbakov, V. V. aut Yurezanskaya, Yu. S. aut Enthalten in Computational mathematics and mathematical physics SP MAIK Nauka/Interperiodica, 1992 50(2010), 4 vom: Apr., Seite 711-720 (DE-627)131059181 (DE-600)1106328-2 (DE-576)029158060 0965-5425 nnns volume:50 year:2010 number:4 month:04 pages:711-720 https://doi.org/10.1134/S0965542510040123 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-MAT SSG-OPC-MAT GBV_ILN_70 AR 50 2010 4 04 711-720 |
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Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov |
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Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. © Pleiades Publishing, Ltd. 2010 |
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Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. © Pleiades Publishing, Ltd. 2010 |
abstract_unstemmed |
Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique. © Pleiades Publishing, Ltd. 2010 |
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V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Simulation of suspended substance transport on the continental shelf: Computation of soil dumping in the Sea of Azov</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2010</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Suspended substance dispersion in a water body is simulated in the case when the spread area is considerably larger than the depth of the water body. The performance and features of a previously proposed computational technique are demonstrated by computing the dispersion of mineral suspension clouds generated in the southern Sea of Azov in the course of soil dumping associated with repair work in the port of Temryuk. The results presented were obtained primarily in test computations aimed at the validation of the computational technique.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Koterov, V. N.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Solbakov, V. V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yurezanskaya, Yu. S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Computational mathematics and mathematical physics</subfield><subfield code="d">SP MAIK Nauka/Interperiodica, 1992</subfield><subfield code="g">50(2010), 4 vom: Apr., Seite 711-720</subfield><subfield code="w">(DE-627)131059181</subfield><subfield code="w">(DE-600)1106328-2</subfield><subfield code="w">(DE-576)029158060</subfield><subfield code="x">0965-5425</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:50</subfield><subfield code="g">year:2010</subfield><subfield code="g">number:4</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:711-720</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0965542510040123</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">50</subfield><subfield code="j">2010</subfield><subfield code="e">4</subfield><subfield code="c">04</subfield><subfield code="h">711-720</subfield></datafield></record></collection>
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