Proceedings of the 6th International Conference on Information Engineering for Mechanics and Materials

Analysis of Longitudinal Deposition in Reservoir Confluence

Authors
Tao Yan, Hui Huang
Corresponding Author
Tao Yan
Available Online November 2016.
DOI
10.2991/icimm-16.2016.89How to use a DOI?
Keywords
Reservoir Confluence; Deposition Pattern; Hydrodynamic Conditions; Dual Backwater Effect
Abstract

The erosion basis in reservoir confluence, with the characteristic of dual change, resulted in special longitudinal deposition patterns. Based on field data, longitudinal deposit patterns of mainstream and tributary in reservoir confluence was studied and two special tributary deposition patterns-adverse cone and cone-adverse cone were proposed. Considering the operating mode of reservoir and backwater effect, variety of hydrodynamic conditions formed different deposition patterns of tributary and mainstream. It was revealed dual backwater effect is the internal mechanism of different deposition pattern in reservoir confluence.

Copyright
© 2016, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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Volume Title
Proceedings of the 6th International Conference on Information Engineering for Mechanics and Materials
Series
Advances in Engineering Research
Publication Date
November 2016
ISBN
10.2991/icimm-16.2016.89
ISSN
2352-5401
DOI
10.2991/icimm-16.2016.89How to use a DOI?
Copyright
© 2016, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

Cite this article

TY  - CONF
AU  - Tao Yan
AU  - Hui Huang
PY  - 2016/11
DA  - 2016/11
TI  - Analysis of Longitudinal Deposition in Reservoir Confluence
BT  - Proceedings of the 6th International Conference on Information Engineering for Mechanics and Materials
PB  - Atlantis Press
SP  - 488
EP  - 492
SN  - 2352-5401
UR  - https://doi.org/10.2991/icimm-16.2016.89
DO  - 10.2991/icimm-16.2016.89
ID  - Yan2016/11
ER  -