The mass curve method for determination of storage capacity of a reservoir uses
water inflow data and water demand data
The mass curve method is a vital graphical tool used in hydrology and water resource engineering to determine the necessary storage capacity for a reservoir. It helps engineers understand how much water storage is needed to reliably meet water demands over time, even during periods of low water availability.
This method involves plotting the cumulative values of water inflow and water outflow (demand) against time on a graph. The cumulative inflow curve shows the total amount of water that has entered the reservoir up to any given point in time. The cumulative demand represents the total amount of water required to be released from the reservoir up to the same point in time.
To accurately apply the mass curve method for determining storage capacity, the following types of data are crucial:
The process works as follows:
The core principle of the mass curve method is to reconcile the variability of water supply (inflow) with the consistency or variability of water requirements (demand). Therefore, having accurate data for both water inflow and water demand is fundamental for the method's success.
Considering the data requirements explained above:
Isohyet is a line joining points having
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