The live storage requirement for a reservoir is to be determined by
mass curve analysis
Live storage in a reservoir is the volume of water that can be withdrawn and utilized, excluding the dead storage which is unusable. Calculating the live storage requirement is fundamental for designing reservoirs that can consistently meet water demands (like irrigation, domestic supply, or industrial use) despite variations in natural water availability (inflow).
The primary method used to determine the live storage requirement for a reservoir is mass curve analysis. This technique involves plotting the cumulative inflow into the reservoir against time. It's a graphical method that helps visualize the balance between water supply and demand over extended periods.
The steps typically involved are:
The maximum deficit identified through mass curve analysis directly corresponds to the minimum reservoir capacity needed to ensure that demand can always be met. This required capacity is the live storage requirement. This method accounts for the sequential nature of inflows and demands, making it superior to methods that only consider total amounts.
Let's consider why the other options are less suitable for determining the requirement:
In summary, mass curve analysis is the appropriate technique for calculating the necessary live storage requirement because it directly addresses the temporal variations between water supply and demand.
The percentage of fresh water available as polar ice/glaciers compared to total fresh water is:-
An isohyet is a line joining points of
Engineering hydrology does NOT deal with:
For one-dimensional flow without recharge in an unconfined aquifer between two water bodies, the steady water table profile is
The water balance equation for a catchment area in terms of rainfall (P), runoff (R), evaporation (E) and storage (S) is written as