Wandering channel: различия между версиями
(создание новой страницы) |
м (редакция) |
||
| Строка 5: | Строка 5: | ||
==Определение на английском== | ==Определение на английском== | ||
| − | '''Wandering channels''' - singlethread or multithread channels characterised by the processes of thalweg migration between channel banks.<ref>Leopold, L.B., Wolman, M.G. 1957. River channel patterns – braided, meandering and straight. U.S. Geol. Surv. Paper. 282-B. P. 39-85. </ref> | + | '''Wandering channels''' - singlethread or multithread channels characterised by the processes of thalweg migration between channel banks.<ref>''Leopold, L.B., Wolman, M.G.'' 1957. River channel patterns – braided, meandering and straight. U.S. Geol. Surv. Paper. 282-B. P. 39-85. DOI: 10.3133/pp282B </ref> |
| − | In contrast to anastomosing rivers, '''wandering rivers''' are laterally active, gravel-dominated rivers.<ref name=":0">Nanson, G.C., Knighton, A.D. 1996. Anabranching rivers: Their cause, character and classification. Earth Surface Processes and Landforms, 21: 217-239. DOI:10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U</ref> | + | In contrast to anastomosing rivers, '''wandering rivers''' are laterally active, gravel-dominated rivers.<ref name=":0">''Nanson, G.C., Knighton, A.D.'' 1996. Anabranching rivers: Their cause, character and classification. Earth Surface Processes and Landforms, 21: 217-239. DOI:10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U</ref> |
==Пример использования термина на английском языке== | ==Пример использования термина на английском языке== | ||
| − | '''Wandering channels''' are regarded as transitional from single channels to fully braided channels and not as a separate channel planform category.<ref>Carling P., Jansen J., Meshkova L. 2014. Multichannel rivers: their definition and classification. Earth Surface Processes and Landforms 39(1), Pp. 26-37. DOI:10.1002/esp.3419</ref> | + | '''Wandering channels''' are regarded as transitional from single channels to fully braided channels and not as a separate channel planform category.<ref>''Carling P., Jansen J., Meshkova L.'' 2014. Multichannel rivers: their definition and classification. Earth Surface Processes and Landforms 39(1), Pp. 26-37. DOI:10.1002/esp.3419</ref> |
'''Wandering rivers''' are largely discriminated from other anabranching types by greater specific stream power, larger sediment size and less cohesive banks.<ref name=":0" /> | '''Wandering rivers''' are largely discriminated from other anabranching types by greater specific stream power, larger sediment size and less cohesive banks.<ref name=":0" /> | ||
Текущая версия на 01:50, 9 ноября 2021
Блуждающее (разбросанное) русло
Разбросанные русла характеризуются беспорядочным расположением островов разных размеров и рукавов, по которым рассредотачивается расход воды в реке.[1]
Определение на английском
Wandering channels - singlethread or multithread channels characterised by the processes of thalweg migration between channel banks.[2]
In contrast to anastomosing rivers, wandering rivers are laterally active, gravel-dominated rivers.[3]
Пример использования термина на английском языке
Wandering channels are regarded as transitional from single channels to fully braided channels and not as a separate channel planform category.[4]
Wandering rivers are largely discriminated from other anabranching types by greater specific stream power, larger sediment size and less cohesive banks.[3]
Перевод использования на русском языке
Блуждающие русла могут рассматриваться как переходный тип между однорукавными и многорукавными руслами и не образуют отдельный морфологический тип.
Блуждающие реки в значительной степени отличаются от других типов многорукавных рек большей мощностью потока, большим размером наносов и менее устойчивыми к размыву берегами.
Список литературы
- ↑ Чалов Р.С. 2011. Русловедение: теория, география, практика. Том 2. Морфодинамика речных русел. М.: КРАСАНД. 960 с. ISBN: 978-5-396-00325-5.
- ↑ Leopold, L.B., Wolman, M.G. 1957. River channel patterns – braided, meandering and straight. U.S. Geol. Surv. Paper. 282-B. P. 39-85. DOI: 10.3133/pp282B
- ↑ 3,0 3,1 Nanson, G.C., Knighton, A.D. 1996. Anabranching rivers: Their cause, character and classification. Earth Surface Processes and Landforms, 21: 217-239. DOI:10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U
- ↑ Carling P., Jansen J., Meshkova L. 2014. Multichannel rivers: their definition and classification. Earth Surface Processes and Landforms 39(1), Pp. 26-37. DOI:10.1002/esp.3419