CN113377255A - Geological disaster slippage azimuth angle processing method and device and electronic equipment - Google Patents
Geological disaster slippage azimuth angle processing method and device and electronic equipment Download PDFInfo
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Abstract
The application provides a geological disaster slippage azimuth angle processing method and device and electronic equipment, and relates to the technical field of geological disaster monitoring. The method comprises the following steps: responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point; determining a slip azimuth angle of the disaster point according to the slip line of the disaster point; and adding the slippage azimuth angle of the disaster point as an azimuth attribute into a file corresponding to the disaster point. According to the geological disaster sliding method and device, the sliding azimuth angle of the geological disaster is obtained through automatic processing of the sliding direction based on the disaster point, the sliding azimuth angle is automatically added to the file corresponding to the disaster point through spatial correlation, and therefore the working efficiency and the data accuracy are greatly improved.
Description
Technical Field
The application relates to the technical field of geological disaster monitoring, in particular to a geological disaster slippage azimuth angle processing method and device and electronic equipment.
Background
When the investigation and research work of gravity-type geological disasters such as collapse, landslide, debris flow and the like is carried out, the sliding direction of a disaster body is one of basic elements for representing the characteristics of the geological disasters.
At present, when geological disaster remote sensing interpretation is carried out, after an attribute field of a slip direction is generally established, technical personnel estimate an azimuth angle of a disaster body by visually sensing a remote sensing image and manually fill the azimuth angle into the field of the slip direction.
However, when the number of geological disasters is large, the azimuth angles of the disasters are visually estimated one by one, and manual filling causes time and labor waste of the work, certain errors exist in the visually estimated azimuth angles, and the risk of wrong filling exists in the manual filling attributes.
Disclosure of Invention
An object of the present application is to provide a method and an apparatus for processing a sliding azimuth angle of a geological disaster, and an electronic device, so as to solve the problem that the work is time-consuming and labor-consuming and has a risk of misfilling due to the fact that the azimuth angle of a disaster body is estimated visually and the disaster body is filled manually in the prior art.
In order to achieve the above purpose, the technical solutions adopted in the embodiments of the present application are as follows:
in a first aspect, an embodiment of the present application provides a geological disaster slippage azimuth processing method, where the method includes:
responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point;
determining a slip azimuth angle of the disaster point according to the slip line of the disaster point;
and adding the slippage azimuth angle of the disaster point as an azimuth attribute into a file corresponding to the disaster point.
Optionally, the determining the slip azimuth angle of the disaster point according to the slip line of the disaster point includes:
and determining the slip azimuth angle of the disaster point according to the slip line of the disaster point and a preset azimuth scale.
Optionally, the determining a slip azimuth angle of the disaster point according to the slip line of the disaster point and a preset azimuth scale includes:
the initial position of the slip line of the disaster point is coincided with the central point of the preset azimuth scale;
and taking the included angle between the slip line and the reference line in the preset azimuth scale as the slip azimuth of the disaster point.
Optionally, the determining the slip azimuth angle of the disaster point according to the slip line of the disaster point includes:
and responding to the triggering operation of a user for generating a control for the azimuth, and determining the slippage azimuth of the disaster point according to the slippage line of the disaster point.
Optionally, the responding to an operation that the user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface includes:
and responding to the operation that a user inputs a plurality of disaster points and the slip lines of the disaster points, and displaying icons of the disaster points and the slip lines of the disaster points on an interface.
Optionally, the determining the slip azimuth angle of the disaster point according to the slip line of the disaster point includes:
responding to the selection operation of a user, and determining at least one target disaster point;
and determining the slip azimuth angle of each target disaster point according to the slip line of each target disaster point.
Optionally, after the adding the slip azimuth of the disaster point as the azimuth attribute to the file corresponding to the disaster point, the method further includes:
and displaying the identification of the disaster point and at least one attribute of the disaster point, wherein the at least one attribute comprises the azimuth attribute.
In a second aspect, an embodiment of the present application further provides a geological disaster slippage azimuth processing apparatus, where the apparatus includes:
the response module is used for responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point;
the determining module is used for determining the slippage azimuth angle of the disaster point according to the slippage line of the disaster point;
and the adding module is used for adding the slippage azimuth angle of the disaster point into a file corresponding to the disaster point as an azimuth attribute.
Optionally, the determining module is specifically configured to determine the slip azimuth of the disaster point according to the slip line of the disaster point and a preset azimuth scale.
Optionally, the determining module is specifically configured to coincide an initial position of the slip line of the disaster point with a central point of the preset azimuth scale; and taking the included angle between the slip line and the reference line in the preset azimuth scale as the slip azimuth of the disaster point.
Optionally, the determining module is specifically configured to determine, according to the slip line of the disaster point, the slip azimuth of the disaster point in response to a triggering operation of a user for an azimuth generation control.
Optionally, the response module is specifically configured to respond to an operation that a user inputs a plurality of disaster points and the slip lines of each disaster point, and display an icon of each disaster point and the slip lines of each disaster point on the interface.
Optionally, the determining module is specifically configured to determine at least one target disaster point in response to a selection operation of a user; and determining the slip azimuth angle of each target disaster point according to the slip line of each target disaster point.
Optionally, the adding module is specifically configured to display the identifier of the disaster point and at least one attribute of the disaster point, where the at least one attribute includes the azimuth attribute.
In a third aspect, an embodiment of the present application further provides an electronic device, including a processor, a communication interface, a memory, and a communication bus, where the processor, the communication interface, and the memory complete mutual communication through the communication bus;
the memory is used for storing a computer program;
the processor is configured to implement the steps of the optimized region planning method according to the first aspect when executing the program stored in the memory.
In a fourth aspect, an embodiment of the present application further provides a computer-readable storage medium, where a computer program is stored in the computer-readable storage medium, and when the computer program is executed by a processor, the steps of the optimized region planning method according to the first aspect are implemented.
The beneficial effect of this application is: the application provides a geological disaster slippage azimuth processing method, which comprises the following steps: responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point; determining a slip azimuth angle of the disaster point according to the slip line of the disaster point; and adding the slippage azimuth angle of the disaster point as an azimuth attribute into a file corresponding to the disaster point. According to the geological disaster sliding method and device, the sliding azimuth angle of the geological disaster is obtained through automatic processing of the sliding direction based on the disaster point, the sliding azimuth angle is automatically added to the file corresponding to the disaster point through spatial correlation, and therefore the working efficiency and the data accuracy are greatly improved.
Drawings
In order to more clearly illustrate the technical solutions of the embodiments of the present application, the drawings that are required to be used in the embodiments will be briefly described below, it should be understood that the following drawings only illustrate some embodiments of the present application and therefore should not be considered as limiting the scope, and for those skilled in the art, other related drawings can be obtained from the drawings without inventive effort.
Fig. 1 is a schematic view of a slip azimuth provided in an embodiment of the present application;
fig. 2 is a schematic flow chart of a geological disaster slippage azimuth processing method according to an embodiment of the present disclosure;
fig. 3 is a schematic view of a debris flow remote sensing image according to an embodiment of the present disclosure;
fig. 4 is a schematic view of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 5 is a schematic diagram of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 6 is a schematic diagram of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 7 is a schematic diagram of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 8 is a schematic diagram of a geological disaster glide azimuth processing interface fifth provided in the embodiment of the present application;
fig. 9 is a schematic diagram six of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 10 is a schematic diagram seven of a geological disaster glide azimuth processing interface provided in the embodiment of the present application;
fig. 11 is a schematic structural diagram of a geologic hazard slippage azimuth processing apparatus according to an embodiment of the present application;
fig. 12 is a schematic structural diagram of an electronic device according to an embodiment of the present application.
Detailed Description
In order to make the objects, technical solutions and advantages of the embodiments of the present application clearer, the technical solutions in the embodiments of the present application will be clearly and completely described below with reference to the drawings in the embodiments of the present application, and it is obvious that the described embodiments are some embodiments of the present application, but not all embodiments.
The slip direction is one of the basic elements characterizing geological disasters, and can be represented by a slip azimuth angle. The slip azimuth angle is a horizontal included angle from a north arrow of a certain point to a slip direction line along a clockwise direction. FIG. 1 is an exemplary view of slip azimuth.
For disaster points where slippage occurs in the remote sensing image, for example, gravity-type geological disasters such as landslide, collapse, debris flow and the like occur in a certain place or a plurality of places, the slippage azimuth angles of the disaster points can be calculated in a specific mode. In the outdoor remote sensing interpretation work, the slippage azimuth angle can be used as the reference direction of slippage of the disaster point, so that the outdoor remote sensing interpretation work can quickly find the place where the slippage of the disaster point occurs. At present, when geological disaster remote sensing interpretation is carried out, after an attribute field of a slip direction is established, a technician estimates the slip azimuth angle of a disaster point by visually sensing an image and manually fills the slip azimuth angle into the field of the slip direction. However, with the current technical solution, when the number of geological disasters is large, the slip azimuth of the disaster point is visually estimated one by one, and manual filling is performed, so that the work is time-consuming and labor-consuming, the visually estimated azimuth has a certain error, and the manual filling attribute also has a risk of misfilling.
Based on the problems, the method for processing the sliding azimuth angle of the geological disaster is provided, the sliding azimuth angle of the disaster point is automatically determined based on the sliding line aiming at the disaster point input by a user, and the sliding azimuth angle of the disaster point is automatically added to the attribute file corresponding to the disaster point in a correlated manner, so that the sliding azimuth angle of the geological disaster does not need to be estimated and manually filled, and the working efficiency and the accuracy are greatly improved.
Fig. 2 is a flowchart of a geological disaster glide azimuth processing method according to an embodiment of the present application, where the method may be applied to an electronic device, and the electronic device may be any device with computer processing capability, such as a desktop computer, a server, and the like. As shown in fig. 2, the method includes:
s201, responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point.
The disaster point may be an area where a geological disaster occurs, for example, a side where a certain mountain collapses is regarded as a disaster point, and a hill slope where a debris flow occurs is regarded as a disaster point.
In a specific implementation process, a user can check a remote sensing image map in advance, fig. 3 is an example of the remote sensing image map of the debris flow, and as shown in fig. 3, the remote sensing image map of the debris flow comprises a typical debris flow area, wherein an area I is a debris flow forming area, an area II is a debris flow circulation area, and an area III is a debris accumulation area. The area I can be used as a disaster point, and the slip direction of the debris flow in the area II is the slip direction of the disaster point of the area I. The sliding direction of the disaster point of the area I can be judged by visually observing the remote sensing image map, and further the sliding azimuth angle of the disaster point can be automatically generated by utilizing the method.
Optionally, the electronic device may display an operation interface, and the user may input the disaster point and the slip line of the disaster point on the interface based on the visual observation result. Fig. 4 is a schematic view of an operation interface, and as shown in fig. 4, a user draws an icon of a disaster point and a slip line of the disaster point on the operation interface. The disaster point icon may be a circle, a rectangle, a polygon, or other icons capable of representing the disaster point, the slip line may be a solid line or a dotted line with an arrow, a solid line or a dotted line without an arrow, or other lines capable of representing the slip direction of the disaster point, and the slip direction may be any direction of 360 °. In fig. 4, the diagram of the disaster point and the slip line of the disaster point are illustrated by a circle and a solid line without an arrow. One disaster point can be drawn, or a plurality of disaster points can be drawn, and when a plurality of disaster points are drawn, the slip azimuth angles of the disaster points can be calculated respectively at the back.
Specifically, the electronic device responds to a user operation to create a file, and the file is used for storing the disaster point and the slip line input by the user through the following processes, and is specifically used for storing the name attribute of the disaster point and the azimuth angle of the slip line. And the name of the file is displayed on the interface of the file according to the name of the file by the user, for example, "xian", as shown in fig. 4. And then, displaying the icon at the clicked position of the interface according to the shape of the icon clicked by the user and the position of the interface, and displaying the line at the slid position and direction of the interface according to the shape of the line clicked by the user and the position and direction of sliding on the interface. The size of the icon displayed on the interface and the length of the sliding line are determined according to the distance of the user sliding on the interface, namely the distance between the starting position and the ending position of the user clicking on the interface.
It should be noted that, when the user draws a sliding line on the icon, a connection point for prompting to connect one end of the sliding line to the center of the icon is displayed at the center position of the icon, so that the user places one end of the sliding line on the connection point according to the prompted connection point. When the user does not completely place the sliding line on the connecting point, the position coordinate of one end of the sliding line is automatically changed to be consistent with the center coordinate of the nearest icon, so that one end of the sliding line is coincided with the center of the icon. The method aims to establish a one-to-one correspondence relationship between disaster points and slip lines, and when a plurality of disaster points exist on an interface at the same time, the one-to-one correspondence relationship can be established to rapidly and clearly distinguish the slip direction of each disaster point, wherein each disaster point has a unique name attribute and is used for distinguishing other disaster points.
S202, determining a slippage azimuth angle of the disaster point according to the slippage line of the disaster point.
Referring to the foregoing embodiment, the slip azimuth refers to a horizontal included angle from a north-pointing direction line of a certain point to a slip direction line along a clockwise direction.
Optionally, the calculation may be performed according to a preset algorithm based on the coordinates of the starting point position of the slip line and the coordinates of the ending point position of the slip line, so as to obtain the slip azimuth of the disaster point.
For example, referring to the interface coordinate system shown in fig. 5, the coordinates of the disaster point and the coordinates of the end point of the slip line are obtained according to the disaster point and the slip line on the interface shown in fig. 4, for example, the coordinates of the disaster point are (3,5), the coordinates of the end point of the slip line are (4,6), and the direction of the y-axis is the true north direction, the slip azimuth angle can be calculated by the pythagorean theorem. The specific calculation process is as follows: subtracting the coordinate of the disaster point from the terminal coordinate of the slip line to obtain the height a of the slip line in the y direction and the width b of the slip line in the x direction, and then using the height a2+b2＝c2Calculating the length c of the slip line, and then using the following formula: sin theta, b/ccos theta, a/c, tan theta, a/b, and calculating the slip azimuth angle theta. From the coordinates of the slip lines shown in fig. 5, a is calculated as 1, b is calculated as 1,
therefore, the temperature of the molten metal is controlled,
since tan θ is 1, the slip azimuth is 45 °.
It should be noted that there are 4 cases in which the value of the coordinate of the end point of the slip line minus the coordinate of the end point of the icon is (x, y), (x, -y), (-x, -y), (-x, y), where the minus sign indicates that the coordinate value of the end point of the slip line is smaller than the coordinate value of the icon. If the value is (x, y), the sin theta value, the cos theta value and the tan theta value are all positive, the slip azimuth angle is theta; if the value is (x, -y), the value of sin theta is positive, the value of cos theta and the value of tan theta is negative, the slip azimuth angle is 180-theta; if the value is (-x, -y), the value of sin theta, the value of cos theta are negative, and the value of tan theta is positive, the slip azimuth angle is 180 degrees + theta; if (-x, y), the sin theta value is negative, the cos theta value is positive, and the tan theta value is negative, the slip azimuth angle is 360-theta.
According to the above description, the slip azimuth is calculated by inputting slip lines in the electronic device. Compared with the prior art, when the number of geological disasters is large, the method can quickly and accurately obtain the slip azimuth angle of the disaster point.
And S203, adding the slippage azimuth angle of the disaster point as an azimuth attribute into a file corresponding to the disaster point.
Optionally, the file corresponding to the disaster point may be a file which is created by a user and is specially used for storing attributes of the disaster point, for example, attributes such as a name of the disaster point, rainfall, a slope gradient, and a flow rate are stored. The file corresponding to the disaster point may be named "Join _ Output". And the slip azimuth angle of the disaster point is one of important attributes in geological disaster remote sensing interpretation, and can be stored in a file corresponding to the disaster point as an azimuth attribute.
In this step, the azimuth attribute may be added to the file corresponding to the disaster point in combination with the operation of the user, and the addition is realized by spatial association. Spatial association is the addition of a field stored in one file to another file, and the following is an exemplary process for spatial association.
For example, after obtaining the slip azimuth of the disaster point, the slip azimuth is stored as an azimuth attribute in a slip azimuth file "xian", and specifically, the name of each disaster point and the slip azimuth corresponding to the disaster point are stored as a field in the file. Further, referring to fig. 6, by selecting a connection function by a user, and selecting a file "Join _ Output" storing the calculated slip azimuth file "xian" and a file "Join _ Output" corresponding to the disaster point stored in the D disk, respectively, the electronic device reads fields in the file "xian", where the fields may include: and then opening a 'Join _ Output' file according to the storage address of the 'Join _ Output' file, building a table for storing azimuth attributes in the 'Join _ Output' file, and writing the slip azimuth of the disaster point in the 'xian' file into the azimuth attribute table corresponding to the disaster point name in the 'Join _ Output' file. As shown in fig. 7, the "xian" file stores names and slip azimuth angles of a plurality of disaster points, and the "Join _ Output" file stores names of disaster points, and then adds the slip azimuth angle in the "xian" file to the "Join _ Output" file through a connection function.
And directly and spatially associating the obtained field of the slip azimuth of the disaster point into another file specially used for storing the attribute of the disaster point. Compared with the prior art, the result is stored to the position to be stored through spatial correlation without manual filling, so that the risk of misfilling is avoided, and the accuracy of the data is improved.
In summary, the embodiment of the present application provides a geological disaster slippage azimuth processing method, which displays an icon of a disaster point and shapes and sizes of a slip line on an interface according to a shape of the disaster point icon and a shape of the slip line selected by a user and starting and ending positions of sliding of the user on the interface, calculates a slippage azimuth of the disaster point according to a direction of the slip line of the disaster point, and adds the calculated slippage azimuth of the disaster point to a file of a storage attribute corresponding to the disaster point by using spatial correlation. The method and the device have the advantages that the sliding azimuth angle of the geological disaster is obtained through the sliding direction processing based on the disaster point, the sliding azimuth angle is added to the file corresponding to the disaster point through spatial association, and the working efficiency and the data accuracy are greatly improved.
As described above, when the slip azimuth of the disaster point is determined in step S202, the slip azimuth can be determined by using the pythagorean theorem. As another alternative, the determination may be performed based on an orientation scale as follows. Optionally, the determining the slip azimuth of the disaster point according to the slip line of the disaster point in step S202 may include:
and determining the slip azimuth angle of the disaster point according to the slip line of the disaster point and a preset azimuth scale.
The azimuth scale is a scale with angle scale lines and angle scale values, and the angle scale value on each angle scale line is the included angle between the angle scale line and a zero reference line, so that the azimuth scale can be used for measuring the included angle between the two lines.
Optionally, the preset azimuth scale may be an azimuth scale with coordinate values, the length and width of each square is unit 1, the position coordinates of the line segment are obtained by counting the squares, and then the azimuth angle of the line segment is calculated by the pythagorean theorem, and the specific implementation manner is shown in step S202. The reference line of the azimuth scale is coincided with one line of the two crossed line segments, and the angle scale value corresponding to the angle scale line coincided with the other line is read from the azimuth scale, namely the included angle of the two crossed lines. The preset orientation scale can be one fixed at the center of the whole interface, and the slip line azimuth angle is read by translating the coordinate value of the slip line, and the orientation scale can be called as a fixed orientation scale; or countless small scales, namely, each coordinate is a small azimuth scale at the position and is directly used for reading the azimuth angle; it may also be a movable azimuth scale, which is called a movable azimuth scale, and which is moved to the slip line to read the azimuth angle. The orientation scale may or may not be displayed in the interface and may be determined by the user.
As shown in fig. 8, referring to fig. 8, for the above-mentioned exemplary diagram of the movable azimuth scale, the center point of the azimuth scale may be moved to any position in the interface according to actual needs, and meanwhile, the due north direction is 0 °, where the zero reference line may be any other direction besides the due north direction, and may be an increasing direction with an angle in the counterclockwise direction besides the clockwise direction, and the increasing direction is an angle in the clockwise direction.
Illustratively, taking the disaster point and the slip line thereof as illustrated in fig. 4 as an example, an azimuth scale with an angle scale line is movable on the interface, and further, as shown in fig. 8, on the basis of fig. 4, when calculating the azimuth angle of the slip line, the electronic device moves the center of the azimuth scale to the center of the disaster point, that is, the azimuth scale of the solid line moves to the position of the dotted line in the figure, and then reads the azimuth angle of the slip line directly from the azimuth scale. As shown in fig. 8, the slip azimuth for reading the disaster point is 45 °.
As shown in fig. 9, referring to fig. 9, for the above-mentioned exemplary diagram of fixing the azimuth scale, the central point of the azimuth scale is fixed at any position of the interface, and meanwhile, the due north direction is a zero reference line 0 °, wherein the zero reference line may be any other direction besides the due north direction, and may be an increasing direction with an angle in the clockwise direction and an increasing direction with an angle in the counterclockwise direction besides the clockwise direction, and the user may set the direction according to his own actual requirements, which is not limited herein.
Illustratively, taking the disaster point and the slip line thereof illustrated in fig. 4 as an example, an azimuth scale with an angle scale line is fixed on the interface, and further, as shown in fig. 9, on the basis of fig. 4, when calculating the azimuth angle of the slip line, the electronic device translates the center of the icon of the disaster point to the center position of the azimuth scale, and the slip line moves according to the trajectory of the icon, i.e., the implemented circle and the slip line move to the position of the dashed line in the figure, and then directly reads the azimuth angle of the slip line from the azimuth scale.
By setting the azimuth scale, the azimuth angle of the slip line can be quickly obtained by reading the scale value on the azimuth scale, so that the implementation process of calculating the slip azimuth angle of the disaster point is simple, accurate and quick.
Optionally, determining the slip azimuth angle of the disaster point according to the slip line of the disaster point and a preset azimuth scale may include:
the initial position of the slip line of the disaster point is coincided with the central point of a preset azimuth scale;
and taking the included angle between the slip line and a reference line in a preset azimuth scale as the slip azimuth of the disaster point.
Alternatively, the starting position of the slip line of the disaster point may be a position where the slip line of the disaster point is connected with the icon of the disaster point. Taking the azimuth scale shown in fig. 9 as an example, the center point of the preset azimuth scale may be a cross point as shown in fig. 9. The reference line in the preset azimuth scale may be, for example, a 0 ° line of the azimuth scale, but is not limited thereto, and may be set according to a user's requirement, and is not limited herein.
Specifically, referring to fig. 4, a fixed azimuth scale is provided at the center of the interface, as shown in fig. 9, where the circle and line of the solid line are a disaster point and a slip line input by the user, when the azimuth angle of the slip line is read according to the slip line of the disaster point and the preset azimuth scale, the coordinates of the connection point of the slip line and the icon, the coordinates of the terminal of the slip line and the coordinates of the center point of the azimuth scale are first read, for example, the coordinates of the connection point of the slip line and the icon are (-1, -0.05), the coordinates of the terminal of the slip line are (3,2), the coordinates of the center point of the azimuth scale are (0,0), the position of the connection point of the slip line and the icon is first moved to the coordinates (0,0), that is, moved rightward and moved 1 upward, then the slip line is moved rightward and moved 1 upward according to the moving manner of the connection point, and the coordinates of the terminal of the slip line are changed to (3.05,3) and enabling the connecting point of the slip line and the icon to coincide with the center of the azimuth scale, and obtaining the slip azimuth angle of the disaster point by reading the included angle between the dotted line and the 0-degree line, such as the circle and the line of the dotted line. As shown in fig. 9, the slip azimuth for reading the disaster point is 45 °.
The function of directly reading the slippage azimuth angle of the disaster point on the azimuth scale can be realized by the coincidence of the initial position of the slippage line of the movable disaster point and the central point of the preset azimuth scale.
Optionally, determining the slip azimuth of the disaster point according to the slip line of the disaster point in step S202 may further include:
and responding to the triggering operation of a user for generating a control for the azimuth, and determining the slippage azimuth of the disaster point according to the slippage line of the disaster point.
Optionally, a plurality of controls may be displayed on the interface, including the azimuth generating control, where the azimuth generating control may be a button, a menu, a link, and the like, and after the user triggers, the electronic device executes the step S202. The electronic equipment starts to execute the step of generating the azimuth angle through the control triggering operation, so that the electronic equipment definitely receives an instruction to start the algorithm to calculate the slip azimuth angle, and the risk that the electronic equipment does not know when the algorithm is started to cause non-calculation or starts to calculate under the condition that a user does not input the algorithm is effectively avoided.
Optionally, the step S201 includes displaying an icon of the disaster point and the slip line of the disaster point on the interface in response to the operation of inputting the disaster point and the slip line of the disaster point by the user, including:
and responding to the operation that a user inputs a plurality of disaster points and the slip lines of the disaster points, and displaying icons of the disaster points and the slip lines of the disaster points on an interface.
Optionally, a plurality of disaster points and slip lines corresponding to the disaster points may be displayed on the interface. And displaying the icon at the clicked position of the interface according to the shape of the icon clicked by the user and the position of the interface, and displaying the line at the slid position and direction of the interface according to the shape of the line clicked by the user and the position and direction of sliding on the interface. The size of the icon displayed on the interface and the length of the sliding line are determined according to the distance of the user sliding on the interface, namely the distance between the starting position and the ending position of the user clicking on the interface. And the starting point of the sliding line is connected with the central point of the icon. As shown in fig. 10, the icons of the disaster points displayed on the interface are circular, and the directions of the slip lines are different.
By inputting a plurality of disaster points and slip lines on the interface, the slip azimuth angles of the disaster points can be simultaneously calculated when the slip azimuth angles of the disaster points are calculated, and compared with the technology that only one disaster point can be input in one interface, the time spent on calculating the slip azimuth angles is greatly reduced.
Optionally, the determining the slip azimuth of the disaster point according to the slip line of the disaster point in step S202 may include:
and responding to the selection operation of the user, and determining at least one target disaster point.
And determining the slip azimuth angle of each target disaster point according to the slip line of each target disaster point.
Optionally, after the triggering operation of the azimuth generating control is triggered, coordinates of connection points of icons of all disaster points and a slip line on the interface, coordinates of a slip line terminal and coordinates of a center point of the azimuth scale are obtained, then, as shown in fig. 9, the connection points of the icons of the disaster points and the slip line and the slip lines are translated up and down, left and right, so that the coordinates of the connection points of the icons of the disaster points and the slip line are consistent with the coordinates of the center point of the azimuth scale, and then, a slip azimuth of each disaster point is read.
Optionally, by obtaining coordinates of the disaster points displayed on the interface, and then translating the icons and the slip lines of the disaster points to the center of the azimuth scale, the azimuth can be directly read through the above steps under the condition that there are many disaster points, and the working efficiency is greatly improved.
Optionally, after the adding the slip azimuth of the disaster point as the azimuth attribute to the file corresponding to the disaster point in step S203, the method may further include:
and displaying the identification of the disaster point and at least one attribute of the disaster point, wherein the at least one attribute comprises a position attribute.
Optionally, the identifier of the disaster point may be a name attribute of the disaster point, and when there are a large number of disaster points in the interface, the identifier of the disaster point may be used to distinguish the disaster points, and in the spatial association process, the slip azimuth of each disaster point may be correspondingly added to the azimuth attribute of each disaster point in another file through the identifier of the disaster point.
Fig. 11 further provides a geological disaster glide azimuth processing device for the embodiment of the present application, the device includes:
a response module 1101, configured to respond to an operation that a user inputs a disaster point and a slip line of the disaster point, and display an icon of the disaster point and the slip line of the disaster point on an interface, where the slip line is used to identify a slip direction of the disaster point, and the slip line uses a position of the disaster point as a starting point;
a determining module 1102, configured to determine a slip azimuth of the disaster point according to the slip line of the disaster point;
an adding module 1103, configured to add the slippage azimuth of the disaster point to a file corresponding to the disaster point as an azimuth attribute.
Optionally, the determining module 1102 is specifically configured to determine the slip azimuth of the disaster point according to the slip line of the disaster point and a preset azimuth scale.
Optionally, the determining module 1102 is specifically configured to coincide an initial position of the slip line of the disaster point with a central point of the preset azimuth scale; and taking the included angle between the slip line and the reference line in the preset azimuth scale as the slip azimuth of the disaster point.
Optionally, the determining module 1102 is specifically configured to determine, according to the slip line of the disaster point, the slip azimuth of the disaster point in response to a triggering operation of a user for an azimuth generating control.
Optionally, the response module 1101 is specifically configured to respond to an operation that a user inputs a plurality of disaster points and the slip lines of each disaster point, and display an icon of each disaster point and the slip lines of each disaster point on the interface.
Optionally, the determining module 1102 is specifically configured to determine at least one target disaster point in response to a selection operation of a user; and determining the slip azimuth angle of each target disaster point according to the slip line of each target disaster point.
Optionally, the adding module 1103 is specifically configured to display the identifier of the disaster point and at least one attribute of the disaster point, where the at least one attribute includes the azimuth attribute.
The above-mentioned apparatus is used for executing the method provided by the foregoing embodiment, and the implementation principle and technical effect are similar, which are not described herein again.
These above modules may be one or more integrated circuits configured to implement the above methods, such as: one or more Application Specific Integrated Circuits (ASICs), or one or more microprocessors, or one or more Field Programmable Gate Arrays (FPGAs), etc. For another example, when one of the above modules is implemented in the form of a Processing element scheduler code, the Processing element may be a general-purpose processor, such as a Central Processing Unit (CPU) or other processor capable of calling program code. For another example, these modules may be integrated together and implemented in the form of a system-on-a-chip (SOC).
Fig. 12 is a schematic structural diagram of an electronic device according to an embodiment of the present application, where the apparatus may be integrated in a terminal device or a chip of the terminal device, and the terminal may be a computing device with a data processing function;
the electronic device includes: a processor 1201 and a memory 1202.
The memory 1202 is used for storing programs, and the processor 1201 calls the programs stored in the memory 1202 to execute the above-mentioned method embodiments. The specific implementation and technical effects are similar, and are not described herein again.
Optionally, the present application also provides a program product, such as a computer readable storage medium, comprising a program which, when being executed by a processor, is adapted to carry out the above-mentioned method embodiments.
In the several embodiments provided in the present application, it should be understood that the disclosed apparatus and method may be implemented in other ways. For example, the above-described apparatus embodiments are merely illustrative, and for example, the division of the units is only one logical division, and other divisions may be realized in practice, for example, a plurality of units or components may be combined or integrated into another system, or some features may be omitted, or not executed. In addition, the shown or discussed mutual coupling or direct coupling or communication connection may be an indirect coupling or communication connection through some interfaces, devices or units, and may be in an electrical, mechanical or other form.
The units described as separate parts may or may not be physically separate, and parts displayed as units may or may not be physical units, may be located in one place, or may be distributed on a plurality of network units. Some or all of the units can be selected according to actual needs to achieve the purpose of the solution of the embodiment.
In addition, functional units in the embodiments of the present application may be integrated into one processing unit, or each unit may exist alone physically, or two or more units are integrated into one unit. The integrated unit can be realized in a form of hardware, or in a form of hardware plus a software functional unit.
The integrated unit implemented in the form of a software functional unit may be stored in a computer readable storage medium. The software functional unit is stored in a storage medium and includes several instructions for enabling a computer device (which may be a personal computer, a server, or a network device) or a processor (processor) to perform some steps of the methods according to the embodiments of the present application. And the aforementioned storage medium includes: a U disk, a removable hard disk, a Read-Only Memory (ROM), a Random Access Memory (RAM), a magnetic disk or an optical disk, and other various media capable of storing program codes.
Claims (10)
1. A geological disaster glide azimuth processing method, characterized in that the method comprises:
responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point;
determining a slip azimuth angle of the disaster point according to the slip line of the disaster point;
and adding the slippage azimuth angle of the disaster point as an azimuth attribute into a file corresponding to the disaster point.
2. The method of claim 1, wherein said determining a slip azimuth for said disaster point based on said slip lines for said disaster point comprises:
and determining the slip azimuth angle of the disaster point according to the slip line of the disaster point and a preset azimuth scale.
3. The method of claim 2, wherein said determining a slip azimuth angle of said disaster point based on said slip line of said disaster point and a predetermined azimuth scale comprises:
the initial position of the slip line of the disaster point is coincided with the central point of the preset azimuth scale;
and taking the included angle between the slip line and the reference line in the preset azimuth scale as the slip azimuth of the disaster point.
4. The method according to any one of claims 1-3, wherein said determining a slip azimuth angle of said disaster point from a slip line of said disaster point comprises:
and responding to the triggering operation of a user for generating a control for the azimuth, and determining the slippage azimuth of the disaster point according to the slippage line of the disaster point.
5. The method according to any one of claims 1 to 3, wherein said displaying an icon of a disaster point and a slip line of the disaster point on an interface in response to a user input of the disaster point and the slip line of the disaster point comprises:
and responding to the operation that a user inputs a plurality of disaster points and the slip lines of the disaster points, and displaying icons of the disaster points and the slip lines of the disaster points on an interface.
6. The method of claim 5, wherein said determining a slip azimuth for said disaster point based on said slip lines for said disaster point comprises:
responding to the selection operation of a user, and determining at least one target disaster point;
and determining the slip azimuth angle of each target disaster point according to the slip line of each target disaster point.
7. The method according to any one of claims 1 to 3, wherein after adding the slip azimuth of the disaster point as an azimuth attribute to the file corresponding to the disaster point, the method further comprises:
and displaying the identification of the disaster point and at least one attribute of the disaster point, wherein the at least one attribute comprises the azimuth attribute.
8. A geological disaster glide azimuth processing apparatus, characterized in that the apparatus comprises:
the response module is used for responding to the operation that a user inputs a disaster point and a slip line of the disaster point, and displaying an icon of the disaster point and the slip line of the disaster point on an interface, wherein the slip line is used for identifying the slip direction of the disaster point, and the slip line takes the position of the disaster point as a starting point;
the determining module is used for determining the slippage azimuth angle of the disaster point according to the slippage line of the disaster point;
and the adding module is used for adding the slippage azimuth angle of the disaster point into a file corresponding to the disaster point as an azimuth attribute.
9. An electronic device, comprising a processor, a communication interface, a memory and a communication bus, wherein the processor, the communication interface and the memory complete communication with each other through the communication bus;
the memory is used for storing a computer program;
the processor, when executing the program stored in the memory, implementing the steps of the method of any of claims 1-7.
10. A computer-readable storage medium, in which a computer program is stored which, when being executed by a processor, carries out the steps of the method according to any one of claims 1 to 7.
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