The mountain reservoirs are an accumulator of the processing products of river banks and sediments. These elements form the silting prism and its bench, which are located in the reservoir and the riverbeds of the tributaries. As a result, there is increased riverbeds and there are a number of catastrophic flooding risk and deficit of the beach-forming sediment on the sea coast. The aim of our research is the estimation of accumulation of solid material in the reservoirs and tributaries, as well as a change of channel processes. In order to study the sedimentation prism-formation and equilibrium bad processes, the method of field experiment is proposed, which was used in the mountain reservoirs of Georgia. For analysis of obtained results were used the methods of mathematical statistics - least square method and differential calculus. The experiment showed that the final result of the reservoirs' silting is an accumulative terrace, which produced an equilibrium alluvial bed. Fractional distribution of sediments in silting prism is determined by reservoir control type and intra-annual distribution of fluvial sediments. The network of sediment extraction quarries has to be located along the reservoir taking into account this principle.
Published in | Journal of Water Resources and Ocean Science (Volume 5, Issue 2) |
DOI | 10.11648/j.wros.20160502.11 |
Page(s) | 22-27 |
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
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Copyright © The Author(s), 2016. Published by Science Publishing Group |
Accumulate Terrace, Caucasus, Mountain Reservoir, Silting
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APA Style
Giorgi Metreveli, Lia Matchavariani. (2016). Research Method of Silting the Mountain Reservoirs Under the Current Climate Change. Journal of Water Resources and Ocean Science, 5(2), 22-27. https://doi.org/10.11648/j.wros.20160502.11
ACS Style
Giorgi Metreveli; Lia Matchavariani. Research Method of Silting the Mountain Reservoirs Under the Current Climate Change. J. Water Resour. Ocean Sci. 2016, 5(2), 22-27. doi: 10.11648/j.wros.20160502.11
AMA Style
Giorgi Metreveli, Lia Matchavariani. Research Method of Silting the Mountain Reservoirs Under the Current Climate Change. J Water Resour Ocean Sci. 2016;5(2):22-27. doi: 10.11648/j.wros.20160502.11
@article{10.11648/j.wros.20160502.11, author = {Giorgi Metreveli and Lia Matchavariani}, title = {Research Method of Silting the Mountain Reservoirs Under the Current Climate Change}, journal = {Journal of Water Resources and Ocean Science}, volume = {5}, number = {2}, pages = {22-27}, doi = {10.11648/j.wros.20160502.11}, url = {https://doi.org/10.11648/j.wros.20160502.11}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.wros.20160502.11}, abstract = {The mountain reservoirs are an accumulator of the processing products of river banks and sediments. These elements form the silting prism and its bench, which are located in the reservoir and the riverbeds of the tributaries. As a result, there is increased riverbeds and there are a number of catastrophic flooding risk and deficit of the beach-forming sediment on the sea coast. The aim of our research is the estimation of accumulation of solid material in the reservoirs and tributaries, as well as a change of channel processes. In order to study the sedimentation prism-formation and equilibrium bad processes, the method of field experiment is proposed, which was used in the mountain reservoirs of Georgia. For analysis of obtained results were used the methods of mathematical statistics - least square method and differential calculus. The experiment showed that the final result of the reservoirs' silting is an accumulative terrace, which produced an equilibrium alluvial bed. Fractional distribution of sediments in silting prism is determined by reservoir control type and intra-annual distribution of fluvial sediments. The network of sediment extraction quarries has to be located along the reservoir taking into account this principle.}, year = {2016} }
TY - JOUR T1 - Research Method of Silting the Mountain Reservoirs Under the Current Climate Change AU - Giorgi Metreveli AU - Lia Matchavariani Y1 - 2016/04/01 PY - 2016 N1 - https://doi.org/10.11648/j.wros.20160502.11 DO - 10.11648/j.wros.20160502.11 T2 - Journal of Water Resources and Ocean Science JF - Journal of Water Resources and Ocean Science JO - Journal of Water Resources and Ocean Science SP - 22 EP - 27 PB - Science Publishing Group SN - 2328-7993 UR - https://doi.org/10.11648/j.wros.20160502.11 AB - The mountain reservoirs are an accumulator of the processing products of river banks and sediments. These elements form the silting prism and its bench, which are located in the reservoir and the riverbeds of the tributaries. As a result, there is increased riverbeds and there are a number of catastrophic flooding risk and deficit of the beach-forming sediment on the sea coast. The aim of our research is the estimation of accumulation of solid material in the reservoirs and tributaries, as well as a change of channel processes. In order to study the sedimentation prism-formation and equilibrium bad processes, the method of field experiment is proposed, which was used in the mountain reservoirs of Georgia. For analysis of obtained results were used the methods of mathematical statistics - least square method and differential calculus. The experiment showed that the final result of the reservoirs' silting is an accumulative terrace, which produced an equilibrium alluvial bed. Fractional distribution of sediments in silting prism is determined by reservoir control type and intra-annual distribution of fluvial sediments. The network of sediment extraction quarries has to be located along the reservoir taking into account this principle. VL - 5 IS - 2 ER -