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There are two major thermal outlets in Kamchatka, the Uzon caldera and the Geyser Valley.
A metagenomic study of integral water and sediment samples collected from two thermal outlets of the Uzon caldera, Arkashin Shurf and Zavarzin thermal spring, has been performed [ 17].
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The major specifications are 600 MW thermal output, 950 °C outlet coolant temperature, prismatic core type, enriched uranium fuel.
The proposed thermal model estimates the outlet air temperature of the nodes to predict cooling costs.
To obtain the higher thermal power and appropriate outlet temperature, there is a critical value for flow rate.
It is designed to have a 600-MW thermal power at an outlet coolant temperature of 850°C and a 275-MW electric power.
This study expands the investigation of optimising the RPSC system based on four tested parameters (pipe diameter, pipe depth, water velocity and water temperature) comparing the system performance in terms of Delta T of inlet-outlet, potential thermal collection (PTC) and surface temperature reduction (STR).
A case study of numerical modeling and physical experiment was carried out to search for best design of the new condenser effluent outlet of a thermal power plant that minimizes the amount of foam emitted from the outlet.
This deep circulation is causing a considerable part of the basin's elevated heat to be transported to the LYG outlets, preventing shallow thermal expression at the GH.
Sensitivity analysis of the trained models indicates that the thermal enrichment of the pond outlet runoff is inversely proportional to pond length-to-width ratio, pond outlet depth, and directly proportional to event runoff volume, event mean pond inflow runoff temperature, and pond initial water temperature.
The main outputs are the fluid outlet temperature, the thermal efficiency, the exergy efficiency, the thermal losses and the receiver mean temperature.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com