Deepwater reservoir water temperature layering intelligent self-adjustment and improvement device and method
A self-adjusting and water temperature technology, applied in river regulation and other directions, can solve problems such as difficulty in accurately controlling the space and time point of the stirring device, high requirements for the fluctuation range of water level and scheduling period, and limited strength and scope of aeration methods. Achieve great practical value, wide range of use, and the effect of improving water environment
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Embodiment 1
[0042] Embodiment 1: It is used to improve the intelligent self-regulation device of water temperature stratification in deep water reservoirs, such as figure 1 As shown, the device includes a housing 1 and an underwater locator attached to the housing 1, a depth measuring instrument, a density measuring instrument, a data processor 18 and a variable displacement propulsion device.
[0043] The shell 1 is made of aluminum alloy material, the top of the shell 1 is provided with a pull hook 2, the upper part is ellipsoid streamlined, the middle and lower part is cylindrical, the outer diameter is 1.0m, and the thickness is 0.05m. Smoothly connected, the end is embedded with a solid load-bearing disc 3, which is made of iron and has a density of 7.0×10 3 kg / m 3 , the diameter is 0.9m, and the vertical thickness is 0.25m, which can ensure that the center of gravity of the whole device is at the bottom, and 17 small water-permeable holes with a diameter of 3cm are symmetrically di...
Embodiment 2
[0048] Embodiment 2: Using the device in Embodiment 1 to improve the process of water temperature stratification in deep water reservoirs.
[0049] A reservoir is located in the mid-latitude subtropical zone. When it reaches the normal storage level, the average width of the water surface is 1000m, the longitudinal length is 600km, and the maximum water depth is 120m. It is a typical narrow and deep subtropical reservoir. Stratification occurs in spring and summer and lasts for 2-3 months. Along with the stratification of reservoir water temperature, the water quality in the reservoir area also stratifies. The temperature of the discharged water is lower than the natural water temperature, causing varying degrees of damage to downstream aquatic organisms and crops influences. From top to bottom, stratified reservoirs are thermocline layer, thermocline layer and thermostagnation layer. The thermocline layer is relatively low and is below 40m of the water surface, so it is diffi...
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