Theoretical reserve evaluation method for ocean current energy

Abstract

A theoretical reserve evaluation method for ocean current energy includes steps of: 1) selecting a target region, and extracting a coordinate range of the target region; 2) obtaining a seabed water depth of the target region; 3) obtaining hydrological data of flow velocities and seawater densities of a target region space; 4) calculating a theoretical reserve of the ocean current energy per unit area of the target region according to the hydrological data, 5) calculating an area of the target region; and 6) calculating the theoretical reserves of the ocean current energy within a spatial range of the target region according to the hydrological data of the flow velocities and the seawater densities obtained in the step 3), the seabed water depth of the target region obtained in the step 2), and the area of the target region obtained in the step 5).

Claims

1. A theoretical reserve evaluation method for ocean current energy, comprising steps of: 1) selecting a target region for theoretical reserve evaluation of the ocean current energy, and extracting a coordinate range of the target region; wherein the coordinate range of the target region is a sequence of longitudes and latitudes of boundary inflection points, or a description of spatial geometric scales by using a coordinate point as a reference; 2) obtaining a seabed water depth of the target region selected in the step 1); 3) obtaining hydrological data of flow velocities and seawater densities of a target region space obtained in the step 2); wherein the hydrological data of the flow velocities and the seawater densities are measured data at one or more discrete points, or calculated data at one or more discrete points according to a numerical simulation model; after the hydrological data of the flow velocities and the seawater densities at multiple discrete points are obtained, the target region is divided into grids; a maximum grid step size is less than or equal to 1/10 of a distance from a nearest data point; the hydrological data of the flow velocities and the seawater densities of the discrete points, together with water depth data, are interpolated to grid center points; 4) calculating a theoretical reserve of the ocean current energy per unit area of the target region according to the hydrological data obtained in the step 3); 5) calculating an area of the target region; wherein the area of the target region is calculated based on an equal-area projection, a geometric figure area calculation method, or a polygon area calculation method, or based on AutoCAD, ArcGis, MapGis and Mapinfor geographic information systems; and 6) calculating the theoretical reserves of the ocean current energy within a spatial range of the target region according to the hydrological data of the flow velocities and the seawater densities obtained in the step 3), the seabed water depth of the target region obtained in the step 2), and the area of the target region obtained in the step 5).

2. The theoretical reserve evaluation method for the ocean current energy, as recited in claim 1, wherein in the step 4), the theoretical reserve of the ocean current energy per unit area is calculated with the following formula:
E.sub.D=∫(½ρV.sup.2)dz wherein: E.sub.D is the theoretical reserve of the ocean current energy per unit area, V is the flow velocity, ρ is the seawater density, and dz is a height of a vertical space.

3. The theoretical reserve evaluation method for the ocean current energy, as recited in claim 2, wherein in the step 6), the theoretical reserves of the ocean current energy within the spatial range of the target region are calculated according to a regional ocean current energy theoretical reserve calculating formula; the regional ocean current energy theoretical reserve calculating formula is:
E.sub.R=∫∫∫(½ρV.sup.2)dxdydz wherein: E.sub.R is a regional ocean current energy theoretical reserve, V is a height-related flow velocity; ρ is the seawater density; dz is a step size of a vertical space, which is determined according to a vertical distribution of the hydrological data; ∫∫dxdy is the area of the target region selected for the theoretical reserve evaluation of the ocean current energy; dxdy is a space step size, which is determined by a plane location of the hydrological data and a meteorological complexity of the target region.

Description

BRIEF DESCRIPTION OF THE DRAWINGS

[0023] FIG. 1 is a basic flow chart of a theoretical reserve evaluation method for ocean current energy according to an embodiment of the present invention;

[0024] FIG. 2 is a sketch diagram of selecting a target region according to the embodiment of the present invention;

[0025] FIG. 3 illustrates water depth distribution within a selected target region according to the embodiment of the present invention;

[0026] FIG. 4 illustrates flow velocity data distribution according to the embodiment of the present invention;

[0027] FIG. 5 is a grid diagram of target region division according to the embodiment of the present invention; and

[0028] FIG. 6 is a distribution diagram of the theoretical reserve of ocean current energy per unit area according to the embodiment of the present invention.

DETAILED DESCRIPTION OF THE PREFERRED EMBODIMENT

[0029] Referring to the drawings, the present invention will be further illustrated.

Embodiment 1

[0030] Referring to FIGS. 1-6, A theoretical reserve evaluation method for ocean current energy, comprising steps as follows.

[0031] 1) Selecting a target region for theoretical reserve evaluation of the ocean current energy, and extracting a coordinate range of the target region;

[0032] wherein the coordinate range of the target region is a sequence of longitudes and latitudes of boundary inflection points (or projected plane Cartesian coordinates).

[0033] According to this embodiment, Zhanjiang Bay is selected as the target region, and the specific area coordinate range is the sequence of longitudes, latitudes, and identification points of the range coordinate points (or projected plane Cartesian coordinates). Specifically, FIG. 2 is a sketch diagram of selecting the target region according to this embodiment of the present invention, wherein the coordinate range is Cartesian coordinates under UTM49 projection:

TABLE-US-00001 longitude latitude description 530834.80 2375561.11 boundary inflection point 1 529889.66 2375904.30 boundary inflection point 2 529208.04 2376643.67 boundary inflection point 3 528421.81 2377271.27 boundary inflection point 4 . . . . . . . . . 532235.03 2272310.26 boundary inflection point 908 530834.80 2375561.11 boundary inflection point 1

[0034] 2) Obtaining a seabed water depth of the target region selected in the step 1).

[0035] According to this embodiment, the seabed water depth of the target region means seabed water depth within the target region. FIG. 3 illustrates water depth distribution within the selected target region according to this embodiment of the present invention.

[0036] 3) Obtaining hydrological data of flow velocities and seawater densities of a target region space obtained in the step 2);

[0037] wherein the hydrological data of the flow velocities and the seawater densities are measured data at one or more discrete points, or calculated data at one or more discrete points according to a numerical simulation model;

[0038] according to this embodiment, the calculation result data of the spatial distribution is obtained by the numerical simulation method, and FIG. 4 illustrates flow velocity data distribution according to this embodiment of the present invention.

[0039] After the hydrological data of the flow velocities and the seawater densities at multiple discrete points are obtained, the target region is divided into grids; FIG. 5 is a grid diagram of target region division according to this embodiment of the present invention; a maximum grid step size is less than or equal to 1/10 of a distance from the nearest data point; the hydrological data of the flow velocities and the seawater densities of the discrete points, together with water depth data, are interpolated to grid center points.

[0040] In this embodiment, the seawater density is a constant. The seawater density is generally 1.02-1.07 g/cm.sup.3, and this embodiment takes 1.05 g/cm.sup.3 as the constant.

[0041] 4) Calculating a theoretical reserve of the ocean current energy per unit area of the target region according to the hydrological data obtained in the step 3);

[0042] wherein the theoretical reserve of the ocean current energy per unit area is calculated with the following formula:

E.sub.D=∫(½ρV.sup.2)dz

[0043] wherein: E.sub.D is the theoretical reserve of the ocean current energy per unit area, V is the flow velocity, ρ is the seawater density, and dz is the height of vertical space.

[0044] The calculated results can be displayed by using surfer, AutoCAD, ArcGis, MapGis, Mapinfor and other geographic information system software, so as to display a distribution diagram of the theoretical reserves of the ocean current energy per unit area. FIG. 6 is the distribution diagram of the theoretical reserve of the ocean current energy per unit area according to this embodiment of the present invention. The ocean current energy resources are evaluated by the level of the theoretical reserves of the ocean current energy per unit area in the distribution diagram.

[0045] 5) Calculating an area of the target region;

[0046] wherein the area of the target region is calculated based on an equal-area projection, a geometric figure area calculation method, or a polygon area calculation method, or based on AutoCAD, ArcGis, MapGis and Mapinfor geographic information systems;

[0047] in order to accurately calculate the theoretical reserves of the ocean current energy in the target region, this embodiment uses the projection of Equal Area to calculate the grid areas of the target region; the calculated grid area gradually increases from 130371 m.sup.2 to 1054440 m.sup.2; by summing up the area of each grid in the target region, the area of the target region is obtained as 8448904058 m.sup.2.

[0048] 6) Calculating the theoretical reserves of the ocean current energy within a spatial range of the target region according to the hydrological data of the flow velocities and the seawater densities obtained in the step 3), the seabed water depth of the target region obtained in the step 2), and the area of the target region obtained in the step 5).

[0049] The regional ocean current energy theoretical reserve calculating formula is:

E.sub.R=∫∫∫(½ρV.sup.2)dxdydz

[0050] wherein: E.sub.R is a regional ocean current energy theoretical reserve, V is a height-related flow velocity; ρ is the seawater density; dz is a step size of a vertical space, which is determined according to the vertical distribution of the hydrological data; ∫∫dxdy is the area of the target region selected for the theoretical reserve evaluation of the ocean current energy; dxdy is a space step size, which is determined by a plane location of the hydrological data and a meteorological complexity of the target region.

[0051] According to this embodiment, the theoretical reserve of the ocean current energy in the selected target region, Zhanjiang Bay, is calculated to be 1.01×10.sup.13 joules.

Embodiment 2

[0052] Referring to FIGS. 1-6, A theoretical reserve evaluation method for ocean current energy, comprising steps as follows.

[0053] 1) Selecting a target region for theoretical reserve evaluation of the ocean current energy, and extracting a coordinate range of the target region;

[0054] wherein the coordinate range of the target region is a description of spatial geometric scales by using a coordinate point as a reference.

[0055] In this embodiment, a certain ocean current energy generator is selected as an example: its geographical coordinates are 110.5374° E, 21.08145° N, and the specific regional coordinate range is a circle with a radius of 20 m centered on a base of the ocean current energy generator.

[0056] 2) Obtaining a seabed water depth of the target region selected in the step 1).

[0057] The seabed water depth of the target region in this embodiment is located in a cylindrical space with a height of 30 m.

[0058] 3) Obtaining hydrological data of flow velocities and seawater densities of a target region space obtained in the step 2);

[0059] wherein the hydrological data of the flow velocities and the seawater densities are measured data of one or more discrete points, or calculated data of one or more discrete points according to a numerical simulation method;

[0060] according to this embodiment, average measured vertical stratified flow velocity data of a station in 2019 are selected, and specific data are as follows:

TABLE-US-00002 Depth (m) Velocity (m/s) Direction (°) 2 1.65 96 8 1.43 94 18 1.38 88 28 1.25 85

[0061] In this embodiment, the seawater density according to empirical data is 1.05 g/cm.sup.3.

[0062] 4) Calculating a theoretical reserve of the ocean current energy per unit area of the target region according to the hydrological data obtained in the step 3);

[0063] wherein the theoretical reserve of the ocean current energy per unit area is calculated with the following formula:

E.sub.D=∫(½ρV.sup.2)dz

[0064] wherein: E.sub.D is the theoretical reserve of the ocean current energy per unit area, V is the flow velocity, ρ is the seawater density, and dz is the height of vertical space.

[0065] In this embodiment, the obtained vertical stratification of the flow velocities is used for stratification with an intermediate stratification method, and specific layer thicknesses are (5 m, 8 m, 10 m, 7 m), and a water depth of the space in this embodiment is 30 m.

[0066] In this embodiment, the theoretical reserves of the ocean current energy per unit area of space in the selected target region are calculated according to the above formula near the ocean current energy generator, and the calculated result is about 31475 joules/m.sup.2.

[0067] 5) Calculating an area of the target region;

[0068] wherein the target region is a regular cylinder, whose circular bottom has a radius of 20 m. The area is calculated to be 1256 m.sup.2 according to the geometric figure area (circle area) calculation method.

[0069] 6) Calculating the theoretical reserves of the ocean current energy within a spatial range of the target region according to the hydrological data of the flow velocities and the seawater densities obtained in the step 3), the seabed water depth of the target region obtained in the step 2), and the area of the target region obtained in the step 5).

[0070] The regional ocean current energy theoretical reserve calculating formula is:

E.sub.R=∫∫∫(½ρV.sup.2)dxdydz

[0071] wherein: E.sub.R is a regional ocean current energy theoretical reserve, V is a height-related flow velocity; ρ is the seawater density; dz is a step size of a vertical space, which is determined according to the vertical distribution of the hydrological data; ∫∫dxdy is the area of the target region selected for the theoretical reserve evaluation of the ocean current energy; dxdy is a space step size, which is determined by a plane location of the hydrological data and a meteorological complexity of the target region.

[0072] In this embodiment, the seawater density according to empirical data is 1.05 g/cm.sup.3. The obtained vertical stratification of the flow velocities is used for stratification with an intermediate stratification method, and the specific layer thicknesses are (5 m, 8 m, 10 m, 7 m), and a water depth of the space in this embodiment is 20 m. ∫∫dxdy is the area, which is the area obtained in the step 4).

[0073] In this embodiment, the theoretical reserve of the ocean current energy in the selected target region near the ocean current energy generator is calculated according to the above formula. The cylindrical space near the ocean current energy generator has a circular bottom with a radius of 20 m and a depth of 30 m. The theoretical reserve of ocean current energy within such space is 3.95×10.sup.7 joules.

[0074] The above are only preferred embodiments of the present invention, and are not intended to be limiting. Those skilled in the art may make changes and modification according to the technical content disclosed above to obtain equivalent embodiments. However, any simple changes and modifications made to the above embodiments without departing from the content of the technical solutions of the present invention still belong to the protection scope of the present invention.