Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone
Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some dep...
Ausführliche Beschreibung
Autor*in: |
Zhmur, V. V. [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2022 |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. |
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Übergeordnetes Werk: |
Enthalten in: Water resources - Pleiades Publishing, 1974, 49(2022), 2 vom: 27. März, Seite 201-211 |
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Übergeordnetes Werk: |
volume:49 ; year:2022 ; number:2 ; day:27 ; month:03 ; pages:201-211 |
Links: |
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DOI / URN: |
10.1134/S0097807822020166 |
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OLC212993661X |
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10.1134/S0097807822020166 doi (DE-627)OLC212993661X (DE-He213)S0097807822020166-p DE-627 ger DE-627 rakwb eng 690 VZ 14 ssgn Zhmur, V. V. verfasserin aut Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. Fomin, Yu. V. aut Enthalten in Water resources Pleiades Publishing, 1974 49(2022), 2 vom: 27. März, Seite 201-211 (DE-627)129431702 (DE-600)192813-2 (DE-576)014804026 0097-8078 nnns volume:49 year:2022 number:2 day:27 month:03 pages:201-211 https://doi.org/10.1134/S0097807822020166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OPC-GGO AR 49 2022 2 27 03 201-211 |
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10.1134/S0097807822020166 doi (DE-627)OLC212993661X (DE-He213)S0097807822020166-p DE-627 ger DE-627 rakwb eng 690 VZ 14 ssgn Zhmur, V. V. verfasserin aut Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. Fomin, Yu. V. aut Enthalten in Water resources Pleiades Publishing, 1974 49(2022), 2 vom: 27. März, Seite 201-211 (DE-627)129431702 (DE-600)192813-2 (DE-576)014804026 0097-8078 nnns volume:49 year:2022 number:2 day:27 month:03 pages:201-211 https://doi.org/10.1134/S0097807822020166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OPC-GGO AR 49 2022 2 27 03 201-211 |
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10.1134/S0097807822020166 doi (DE-627)OLC212993661X (DE-He213)S0097807822020166-p DE-627 ger DE-627 rakwb eng 690 VZ 14 ssgn Zhmur, V. V. verfasserin aut Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. Fomin, Yu. V. aut Enthalten in Water resources Pleiades Publishing, 1974 49(2022), 2 vom: 27. März, Seite 201-211 (DE-627)129431702 (DE-600)192813-2 (DE-576)014804026 0097-8078 nnns volume:49 year:2022 number:2 day:27 month:03 pages:201-211 https://doi.org/10.1134/S0097807822020166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OPC-GGO AR 49 2022 2 27 03 201-211 |
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10.1134/S0097807822020166 doi (DE-627)OLC212993661X (DE-He213)S0097807822020166-p DE-627 ger DE-627 rakwb eng 690 VZ 14 ssgn Zhmur, V. V. verfasserin aut Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. Fomin, Yu. V. aut Enthalten in Water resources Pleiades Publishing, 1974 49(2022), 2 vom: 27. März, Seite 201-211 (DE-627)129431702 (DE-600)192813-2 (DE-576)014804026 0097-8078 nnns volume:49 year:2022 number:2 day:27 month:03 pages:201-211 https://doi.org/10.1134/S0097807822020166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OPC-GGO AR 49 2022 2 27 03 201-211 |
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Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. |
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Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. |
abstract_unstemmed |
Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed. © Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183. |
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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">Transient Seepage of Seawater in the Coastal Zone under Freezing of This Zone</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, No. 2, pp. 201–211. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Vodnye Resursy, 2022, Vol. 49, No. 2, pp. 172–183.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract A physical model was proposed to describe the response of groundwater level in a coastal area to sea level variations. An impermeable interlayer is supposed to exist on the shore slope, simulating a layer of aufeis or frozen soil deepening into water and ending on the sloped bed at some depth under water. This interlayer hampers water exchange between the sea and the aquifer in the coastal zone. The results of this study were compared with those in similar studies with models containing no impermeable layer. New properties were revealed.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fomin, Yu. 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