Seismosedimentation and Lives of Reservoirs
1988
- 30Usage
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Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
Citation Benchmarking is provided by Scopus and SciVal and is different from the metrics context provided by PlumX Metrics.
Metrics Details
- Usage30
- Downloads26
- Abstract Views4
Conference Paper Description
When moderate to major earthquakes, usually of magnitude more than or equal to 6. 0 on Richter Scale, occur in catchment area of river, additional amount of geological materials is generated, which is called as Seismosediments and the process is known as Seismosedimentation. River flow mechanism carries it down to reservoir. This amount of seismosediment is quantified by a mathematical relation. A specific case of seismosedimentation with reference to sediments in Bhakra reservoir has been discussed. It is observed that seismosedimentation could reduce the economic life of reservoir and adversely affects the utility of reservoir. Re-examination of lives of large reservoirs in active seismic zones is recommended.
Bibliographic Details
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