Form of presentation | Articles in international journals and collections |
Year of publication | 2011 |
Язык | русский |
|
Obnosov Yuriy Viktorovich, author
|
Bibliographic description in the original language |
Kacimov, A., Y. Obnosov, A. Al-Maktoumi, and M. Al-Balushi (2011), How much floating light nonaqueous phase liquid can a phreatic surface sustain" Riesenkampf's scheme revisited, Water Resour. Res., 47, W11521, doi:10.1029/2010WR010369 |
Annotation |
Steady, Darcian, one-phase, phreatic surface flow
of groundwater into a horizontal well with a pancake lens of LNAPL
accumulated in the water table trough is studied by the methods of
complex analysis. A sharp-interface model assumes groundwater
capped by two isobaric limbs (groundwater-vadoze zone interfaces)
of a free surface with an in-between cambered segment of an
immiscible LNAPL-water interface, along which pressure is
hydrostatically increasing with the depth of the LNAPL
``channel''. |
Keywords |
Holomorphic functions, phreatic surface, horizontal well, LNAPL |
The name of the journal |
WATER RESOUR RES
|
URL |
http://www.agu.org/pubs/crossref/2011/2010WR010369.shtml |
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=28657&p_lang=2 |
Resource files | |
|
Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Obnosov Yuriy Viktorovich |
ru_RU |
dc.date.accessioned |
2011-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2011-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2011 |
ru_RU |
dc.identifier.citation |
Kacimov, A., Y. Obnosov, A. Al-Maktoumi, and M. Al-Balushi (2011), How much floating light nonaqueous phase liquid can a phreatic surface sustain" Riesenkampf's scheme revisited, Water Resour. Res., 47, W11521, doi:10.1029/2010WR010369 |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=28657&p_lang=2 |
ru_RU |
dc.description.abstract |
WATER RESOUR RES |
ru_RU |
dc.description.abstract |
Steady, Darcian, one-phase, phreatic surface flow
of groundwater into a horizontal well with a pancake lens of LNAPL
accumulated in the water table trough is studied by the methods of
complex analysis. A sharp-interface model assumes groundwater
capped by two isobaric limbs (groundwater-vadoze zone interfaces)
of a free surface with an in-between cambered segment of an
immiscible LNAPL-water interface, along which pressure is
hydrostatically increasing with the depth of the LNAPL
``channel''. |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
Holomorphic functions |
ru_RU |
dc.subject |
phreatic surface |
ru_RU |
dc.subject |
horizontal well |
ru_RU |
dc.subject |
LNAPL |
ru_RU |
dc.title |
How much floating light nonaqueous phase liquid can a phreatic surface sustain" Riesenkampf's scheme revisited |
ru_RU |
dc.type |
Articles in international journals and collections |
ru_RU |
|