| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2017 |
| Язык | английский |
|
Обносов Юрий Викторович, автор
|
|
Al-Maktoumi Ali , автор
Kacimov Anvar Rashidovich, автор
|
| Библиографическое описание на языке оригинала |
A.R.Kacimov, A.Al-Maktoumi, Yu.V.Obnosov. Phreatic/Confined Flows in Polygons: Dupuit-Forchheimer Model Versus Potential Solutions. European Water, V.57, 2017, pp.489-496. |
| Аннотация |
European Water |
| Ключевые слова |
Seepage refraction, hodograph, leaky layer, infiltration, numerical simulations |
| Название журнала |
European Water
|
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=169848 |
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Обносов Юрий Викторович |
ru_RU |
| dc.contributor.author |
Al-Maktoumi Ali |
ru_RU |
| dc.contributor.author |
Kacimov Anvar Rashidovich |
ru_RU |
| dc.date.accessioned |
2017-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2017-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2017 |
ru_RU |
| dc.identifier.citation |
A.R.Kacimov, A.Al-Maktoumi, Yu.V.Obnosov. Phreatic/Confined Flows in Polygons: Dupuit-Forchheimer Model Versus Potential Solutions. European Water, V.57, 2017, pp.489-496. |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=169848 |
ru_RU |
| dc.description.abstract |
European Water |
ru_RU |
| dc.description.abstract |
Analytical and numerical (HYDRUS2D and MODFLOW) solutions for steady unconfined Darcian flows with accretion and leakage in a single aquifer is obtained for domains bounded by trigons (in particular common triangles)
and polygons that allows modeling catchment-scale groundwater flows. Strack's comprehensive potential obeys the
2-D Poisson equations, which assumes the Dupuit-Forchheimer vertical averaging of the head. Along the lateral boundaries in 2-D flows and leaky layer in 1-D flow, Robin's condition models clogging of river/wadi banks and
beds. In a layered aquifer, confined flows are decoupled into two types of analytic elements: highly-low permeable strata with 1-D and essentially 2-D seepage, correspondingly. |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
Seepage refraction |
ru_RU |
| dc.subject |
hodograph |
ru_RU |
| dc.subject |
leaky layer |
ru_RU |
| dc.subject |
infiltration |
ru_RU |
| dc.subject |
numerical simulations |
ru_RU |
| dc.title |
Phreatic/Confined Flows in Polygons: Dupuit-Forchheimer Model Versus Potential Solutions |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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