Evaluation of plain river channel deformation in the absenceof observation data

Podrobná bibliografie
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 24 : Scientific and Technical Challenges in the Well Drilling Progress, 24–27 November 2014, Tomsk, Russia.— 2015.— [012027, 6 p.]
Korporace: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ), Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра иностранных языков (ИЯПР)
Další autoři: Savitshev O. G. Oleg Gennadiewich, Reshetko M. V. Margarita Viktorovna, Matveenko I. A. Irina Alekseevna, Ivanova Ye. V.
Shrnutí:Title screen
Evaluation and long-term forecast techniques for plain river channel deformation has been developed in the absence of observation data. Their testing was performed by the example of medium rivers (with catchment area from 2000 to 50000 km{2}) in taiga zone of Western Siberia (the Ob river basin on the section of its midstream). The technique is based on determination of flow parameters, at which the maximum river bed deformations are observed. Standard data of hydrometric observations obtained at the state hydrological network are used for calculation.
Режим доступа: по договору с организацией-держателем ресурса
Vydáno: 2015
Témata:
On-line přístup:http://dx.doi.org/10.1088/1755-1315/24/1/012027
Médium: Elektronický zdroj Kapitola
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=639711
Popis
Shrnutí:Title screen
Evaluation and long-term forecast techniques for plain river channel deformation has been developed in the absence of observation data. Their testing was performed by the example of medium rivers (with catchment area from 2000 to 50000 km{2}) in taiga zone of Western Siberia (the Ob river basin on the section of its midstream). The technique is based on determination of flow parameters, at which the maximum river bed deformations are observed. Standard data of hydrometric observations obtained at the state hydrological network are used for calculation.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1088/1755-1315/24/1/012027