Transformation of sand formations in deltas of major tributaries due to lake Baikal level fluctuations


Дәйексөз келтіру

Толық мәтін

Аннотация

In the work, it is studied the state dynamics of sand formations, connected with Lake Baikal level increase, in deltas of the main tributaries. It is observed a significant decrease in the length and area of islands, peninsulas, and sand bars in the lacustrine parts of deltas. In some places, the islands configuration has changed, and braid bars have formed.

Негізгі сөздер

Авторлар туралы

Alexander Ukraintsev

N.L. Dobretsov Geological Institute of the Siberian Branch of the Russian Academy of Sciences

Email: ukraintsev87@bk.ru
ORCID iD: 0000-0001-6919-0736

Cand. Sc., Scientific Researcher

Ресей, 6а, Sakhyanova street, Ulan-Ude, 670047

A. Plyusnin

Dobretsov Geological Institute, Siberian Branch, Russian Academy of Sciences (GIN SB RAS), 670047, Ulan-Ude, Russia

Хат алмасуға жауапты Автор.
Email: plyusnin@ginst.ru
ORCID iD: 0000-0001-9380-7281
Россия, 670047, Улан-Удэ, ул. Сахьяновой, 6а

Әдебиет тізімі

  1. Peryazeva E.G., Plyusnin A.M., Ukraintsev A.V. Transformation of Accumulative Landforms in the Area of the Selenga River Delta Under the Influence of Changes in Baikal Level. Geografiya i prirodnye resursy, 2022, vol. 43, no. S5, pp. 115–123. (In Russ.). doi: 10.15372/GIPR20220512.
  2. Peryazeva E.G., Plyusnin A.M., Ukrainsev A.V. Changes in the Configuration of the Еastern Coast of Baikal Lake Due to the Rise in its Level, in Ehvolyutsiya biosfery i tekhnogenez: materialy Vseros. konf. s mezhdunar. uchastiem (The evolution of the biosphere and technogenesis: proceedings of the All-Russian Conference with the International participation). Chita, 2022, pp. 299–303. doi: 10.57245/978_5_9293_3064_3_2022_2_299. (In Russ.).
  3. Potemkina T.G., Potemkin V.L., Guseva E.A, Nosyreva E.V. Dynamics of Sediment Run off in the Lake Baikal Basin. Vestnik Irkutskogo gosudarstvennogo tekhnicheskogo universiteta, 2012, no. 4 (63), pp. 53–61. (In Russ.).

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© Украинцев А.В., Плюснин А.М., 2024

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