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volume of the downstream reservoir.
The water time delay is the time required for discharging water from upstream reservoir to its downstream reservoir.
During flow, the electrical potential differences between each electrode and a reference located in the downstream reservoir were recorded.
Elevated winter releases of water into the downstream reservoir Kapshagai has been undertaken to cover peak loads in the power of the region, causing a sharp rise in the levels in the Ile delta and extensive flooding of the territory.
However, if the downstream reservoir is infinite (i.e. the pore fluid is allowed to vent to the atmosphere), the pore fluid compressibility varies significantly as it approaches atmospheric pressure.
Applying Eq. (7) to the interface between the upstream reservoir and the sample ((x = 0)), assuming that the upstream reservoir evacuates to an infinite downstream reservoir across the sample, and integrating along L yields k_{D} = frac{2Lmu }{A}frac{{V_{u} }}{{P_{u}^{2} - P_{d}^{2} }}frac{{dP_{u} }}{dt}.
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And contrary to your editorial, the system's other downstream reservoirs can't store this water either.
These elevated sediment yields will likely impact downstream reservoirs, which were designed under conditions of historically lower sediment yield.
In cascaded hydro systems, water delay time is a very important factor that requires coordination between upstream and downstream reservoirs.
In addition to the on-site impacts which occur across the Ethiopian Highlands, siltation of downstream reservoirs is experienced in Sudan and Egypt.
However, most reported literature focuses on the relationship between upstream and downstream reservoirs [13, 14], and considerations of correlation among natural inflows are limited.
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