The present invention relates to an underground infrastructure and method for transporting water from an abundant source of water such as the sea or a lake and exposing it to deep lying sources of geothermal heat, and further for transporting heated water to facilities on the surface and/or at depth where the thermal energy is used for desalination, electrical energy generation or other purposes. More generally it relates to an underground hydraulic system.
A first aspect of the invention is an underground hydraulic system arranged in a landmass, comprising an intake tunnel connected to a body of water with a surface, where the intake tunnel comprises an intake opening at one end and inclines towards an outlet opening at the other end, where the intake opening provides access to the intake tunnel for water from the body of water. The system further comprises a control unit arranged to control flow of water from the body of water into the intake tunnel, a distribution tunnel connected to the intake tunnel at the outlet opening, and arranged at an average depth h1 below the surface of the body of water which is greater than that of the intake opening, where the distribution tunnel is arranged at least partially in a geological layer with a temperature in a range of 40° C. and above, geothermally heating water in the distribution tunnel, and at least one riser tunnel connected at a lower end to the distribution tunnel and extending towards the surface of the landmass, where the at least one riser tunnel is arranged for receiving water from the distribution tunnel, where water in the riser tunnel is pumped up by the hydrostatic pressure at the lower end of the at least one riser tunnel (6), generated by the cumulative head of water through the body of water (1), the intake tunnel (2) and the distribution tunnel (5), and in addition one or more of the following: the gas lift effect, and the thermally generated density differential effect.
Optionally, h1 is larger than 1 km.
Optionally, the underground hydraulic system further comprising the following:
a user unit connected to the riser tunnel, allowing water in the riser tunnel entering the user unit; and
a riser control unit arranged related to the riser tunnel, the riser control unit controlling water flow into the user unit above.
Optionally, the underground hydraulic system comprises a mechanical pump arranged for assisting in pumping water upwards in the riser tunnel.
Optionally, the control unit comprises at least one of the following: filtration systems and sensors for parameters. The parameters can comprise at least one of the following: salinity, temperature, turbidity and pressure.
Optionally, the underground hydraulic system further comprises a turbine unit arranged related to one of the tunnels for producing hydroelectric energy from water flow in the tunnel.
Optionally, the underground hydraulic system further comprises:
a second distribution tunnel essentially parallel to the first distribution channel, but at less depth h2, below the surface of the body of water transporting water under hydrostatic pressure from the body of water, and connected at branching off points to one or more of the riser control units.
Optionally, the underground hydraulic system further comprises at least one water transport loop comprising at least one user unit being connected to a turbine tunnel where water from the riser tunnel is redirected from the user unit and through a water turbine located in the turbine tunnel, and where a lower part of the turbine tunnel connects with a distribution tunnel which delivers water to a second water transport loop in a chain of two or more loops, in which the last user unit in the chain drains water from the chain by transporting the received water away or by re-injecting the water into the first user unit in the chain.
Embodiments of the present invention will now be described, by way of example only, with reference to the following diagrams wherein:
The present invention employs gradients in water temperatures and pressures in a deep underground hydraulic system to transport water from an abundant source such as the sea or a lake across large distances to remote inland locations, to heat the water in deep geological structures, and to pump steam and hot water to facilities on the surface. Temperatures of the steam and water entering the surface facilities are typically in the range 150-250° C., suitable for desalination, electric energy production, or other applications. The system is driven by geothermal heat extracted from the underground in conjunction with gravity-driven transport.
The major parts of the hydraulic system are the following:
i) An intake tunnel (2) connects the body of water (1) with the underground hydraulic system. A control unit (3) controls the flow of water and incorporates technical equipment, including filtration systems and sensors for parameters such as salinity and temperature. A turbine unit (4) produces hydroelectric energy from the water flow.
ii) An essentially horizontal distribution tunnel (5) transports the water to locations inland. The distribution tunnel typically has a large cross section and a length L which may extend across large distances. It is located at a depth h1 below the surface of the body of water (1).
iii) Riser tunnels (6) that receive water from the distribution tunnel. Four riser tunnels are shown in
The distribution channel (5) is located at considerable depth, typically up to several kilometers, in a geological structure (12) which is characterized by high geothermal heat content. In operation, water from the intake tunnel (2) flows through the tunnel system in the geological structure and heats up, typically to 150-250 degrees C. Due to the high hydrostatic pressure at this depth, the water does not boil, but will experience buoyancy relative to the colder water in the riser tunnels as long as it maintains a high temperature. When a control unit (11) is activated, it opens for a flow of water from the riser tunnel and into the user unit above. The flow may be initiated by pumps that draw water from the riser tunnel and lift it into the user unit. This imbalances the water column in the riser tunnel, which is replenished from below by gravity-fed hot water from the distribution channel (5). This water is subject to the hydrostatic pressure generated by the water column in the body of water (1) and the intake tunnel (2), which is at ambient temperatures and therefore more dense than the water in the riser tunnels. This generates an imbalance which favors the water in the riser tunnel to be lifted by the thermally generated density differential, or hot water buoyancy effect. As the hot water rises in the riser channel, it experiences a lower hydrostatic pressure, and ultimately starts boiling. The bubbles float up through the riser tunnel, providing a pumping action. This pumping effect, which has variously been termed as the “Gas lift” or “Geyser” or “Bubble pump” effect, is well known and has been explained by entrainment of water by rising bubbles in a column of liquid and/or by reduced density of a gas bubble admixed liquid in hydrostatic contact with a column of non bubble admixed liquid (cf. e.g. Wikipedia “Gas lift”: https://en.wikipedia.orq/wiki/Gas_lift and A. Benhmidene et al.: “A Review of Bubble Pump Technologies”, Journal of Applied Sciences 10 (16): 1806-1813, 2010). Recently it has been proposed to exploit the effect in connection with large scale geothermal systems (cf.: K. Heller et al.: “A New Deep Geothermal Concept Based on the Geyser Principle”, PROCEEDINGS, Thirty-Ninth Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, Calif., Feb. 24-26, 2014, SGP-TR-202).
The system shown in
In the case where the user unit on the surface is a desalination plant, the hot water delivered from the riser tunnel may be flash evaporated without further heating and condensed. Thermal desalination technology is mature and commercially available in many variants.
Generally, thermally driven processes shall require a cold sink to provide high efficiency.
In
Water temperatures in each turbine tunnel can be adjusted in the user units by making use of the heat content for purposes as described above. Hot water may also be returned down the turbine tunnels, as long as this does not damage the turbines.
This may be done to maintain adequate temperatures in the riser tunnels further down the chain.
Number | Date | Country | Kind |
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1917778.1 | Dec 2019 | GB | national |
Filing Document | Filing Date | Country | Kind |
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PCT/NO2020/050296 | 12/2/2020 | WO |