WO2018040592A1 - 一种微地震监测中的震源定位方法及系统 - Google Patents
一种微地震监测中的震源定位方法及系统 Download PDFInfo
- Publication number
- WO2018040592A1 WO2018040592A1 PCT/CN2017/081583 CN2017081583W WO2018040592A1 WO 2018040592 A1 WO2018040592 A1 WO 2018040592A1 CN 2017081583 W CN2017081583 W CN 2017081583W WO 2018040592 A1 WO2018040592 A1 WO 2018040592A1
- Authority
- WO
- WIPO (PCT)
- Prior art keywords
- node
- grid
- layer
- preset condition
- preset
- Prior art date
Links
- 238000012544 monitoring process Methods 0.000 title claims abstract description 172
- 238000000034 method Methods 0.000 title claims abstract description 87
- 238000004590 computer program Methods 0.000 claims description 29
- 230000004807 localization Effects 0.000 claims description 21
- 238000004364 calculation method Methods 0.000 abstract description 26
- 230000008569 process Effects 0.000 description 21
- 238000003860 storage Methods 0.000 description 14
- 238000010586 diagram Methods 0.000 description 8
- 238000012545 processing Methods 0.000 description 7
- 238000005516 engineering process Methods 0.000 description 6
- 230000006870 function Effects 0.000 description 5
- 238000004519 manufacturing process Methods 0.000 description 4
- 230000000694 effects Effects 0.000 description 3
- 230000003287 optical effect Effects 0.000 description 3
- 238000012986 modification Methods 0.000 description 2
- 230000004048 modification Effects 0.000 description 2
- 230000002085 persistent effect Effects 0.000 description 2
- 239000007787 solid Substances 0.000 description 2
- 230000008859 change Effects 0.000 description 1
- 238000004891 communication Methods 0.000 description 1
- 238000001514 detection method Methods 0.000 description 1
- 238000009826 distribution Methods 0.000 description 1
- 230000000877 morphologic effect Effects 0.000 description 1
- 230000000750 progressive effect Effects 0.000 description 1
- 230000003068 static effect Effects 0.000 description 1
Images
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. for interpretation or for event detection
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. for interpretation or for event detection
- G01V1/288—Event detection in seismic signals, e.g. microseismics
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/003—Seismic data acquisition in general, e.g. survey design
- G01V1/005—Seismic data acquisition in general, e.g. survey design with exploration systems emitting special signals, e.g. frequency swept signals, pulse sequences or slip sweep arrangements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. for interpretation or for event detection
- G01V1/30—Analysis
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/10—Aspects of acoustic signal generation or detection
- G01V2210/12—Signal generation
- G01V2210/123—Passive source, e.g. microseismics
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/60—Analysis
- G01V2210/62—Physical property of subsurface
- G01V2210/622—Velocity, density or impedance
- G01V2210/6222—Velocity; travel time
Definitions
- the present application relates to the field of geophysical exploration technology in wells, and in particular to a method and system for locating a source in microseismic monitoring.
- Microseismic monitoring technology is a geophysical technique that monitors the impacts, effects, and subsurface conditions of production activities by observing and analyzing microseismic events generated during production activities, in hydraulic fracturing crack monitoring, oilfield safety monitoring, oilfield dynamic monitoring, and Mine safety and other fields have an important role.
- the microseismic monitoring technology can not only analyze the morphological characteristics and distribution law of underground cracks, but also estimate the effective volume of reservoirs and future production trends.
- microseismic monitoring technology is to accurately determine the location of the seismic source.
- the micro-seismic source localization method based on forward modeling, the micro-seismic source location is determined by uniformly meshing the monitoring regions and searching by nodes, wherein the size of the mesh is determined by the precision.
- the speed of positioning by this method depends on the accuracy of the monitoring. The higher the monitoring accuracy, the denser the meshing required, and the amount of calculation will be very large. Although the monitoring accuracy is low, the calculation speed can be improved but the monitoring result It is often difficult to meet the needs.
- the purpose of the embodiments of the present application is to provide a method and system for locating a source in microseismic monitoring, which can achieve high precision and precise positioning and a small amount of calculation.
- the embodiment of the present application provides a method for locating a source in microseismic monitoring, and the method includes:
- the initial side length, the initial side length is not more than twice the distance between the respective observation points;
- determining and searching for a node in the i-th layer grid that satisfies the first preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location, and the first preset requirement is that a node that meets the preset condition in the i-1st layer grid is centered.
- the embodiment of the present application further provides a method for locating a source in microseismic monitoring, the method comprising:
- the initial side length, the initial side length is not more than twice the distance between the respective observation points;
- the node that meets the first preset requirement in the i-th layer grid is determined and searched, and the node that meets the preset condition is obtained, where the first preset requirement is to fall into the i-1th layer.
- the nodes in the grid that satisfy the preset condition are centered. Within the circle of radius;
- determining and searching for a node in the i-th layer grid that satisfies the second preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location
- the second preset requirement is that a node that meets the preset condition in the i-th layer grid is centered.
- Steps (3) and (4) are repeated within the circle of the radius until the determination in step (3) is YES. At this time, the node in the i-th layer mesh that satisfies the preset condition is the source point.
- the second layer of mesh is divided into the monitoring area, and the node in the second layer grid that satisfies the first preset requirement is searched.
- the node that meets the preset condition, where the first preset requirement is that a node that meets the preset condition in the i-1th layer grid is centered.
- Steps (4) and (5) searching a node in the i-th layer grid that satisfies the second preset requirement, and acquiring a node in which the preset condition is met, where the second preset requirement is that the falling into the i-th layer grid satisfies
- the node of the preset condition is a center of the circle.
- Steps (4) and (5) are repeated within the circle of the radius until the determination in step (4) is YES.
- the node in the i-th layer mesh that satisfies the preset condition is the source point.
- the embodiment of the present application provides a source location system in microseismic monitoring, the system comprising:
- a memory configured to store computer program instructions, the computer program instructions being executed by the processor, performing the following steps:
- the initial side length, the initial side length is not more than twice the distance between the respective observation points;
- determining and searching for a node in the i-th layer grid that satisfies the first preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location, and the first preset requirement is that a node that meets the preset condition in the i-1st layer grid is centered.
- a source location system for microseismic monitoring comprising:
- a memory configured to store computer program instructions, the computer program instructions being executed by the processor, performing the following steps:
- the initial side length, the initial side length is not more than twice the distance between the respective observation points;
- the node that meets the first preset requirement in the i-th layer grid is determined and searched, and the node that meets the preset condition is obtained, where the first preset requirement is to fall into the i-1th layer.
- the nodes in the grid that satisfy the preset condition are centered. Within the circle of radius;
- determining and searching for a node in the i-th layer grid that satisfies the second preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location
- the second preset requirement is that a node that meets the preset condition in the i-th layer grid is centered.
- a source location system for microseismic monitoring comprising:
- a memory configured to store computer program instructions, the computer program instructions being executed by the processor, performing the following steps:
- Steps (3) and (4) are repeated within the circle of the radius until the determination in step (3) is YES. At this time, the node in the i-th layer mesh that satisfies the preset condition is the source point.
- a source location system for microseismic monitoring comprising:
- a memory configured to store computer program instructions, the computer program instructions being executed by the processor, performing the following steps:
- the second layer of mesh is divided into the monitoring area, and the node in the second layer grid that satisfies the first preset requirement is searched.
- the node that meets the preset condition, where the first preset requirement is that a node that meets the preset condition in the i-1th layer grid is centered.
- Steps (4) and (5) searching a node in the i-th layer grid that satisfies the second preset requirement, and acquiring a node in which the preset condition is met, where the second preset requirement is that the falling into the i-th layer grid satisfies
- the node of the preset condition is a center of the circle.
- Steps (4) and (5) are repeated within the circle of the radius until the determination in step (4) is YES.
- the node in the i-th layer mesh that satisfies the preset condition is the source point.
- the monitoring area is divided into an N-layer grid according to the location accuracy of the source, and only the next layer of the grid is searched in the next layer of the grid node search process.
- the mesh node that meets the preset condition determined in the above layer grid is a node in a neighborhood circle of the center of the circle, and the search range is gradually reduced. Only one node needs to be searched for each additional search layer, including the previous one.
- the nodes in the layer grid that satisfy the preset conditions, that is, each additional search layer only the search calculation amount of 8 nodes is actually increased, and in the high-precision positioning, a small calculation amount can be realized.
- FIG. 1 is a schematic flow chart of a method for locating a source in a microseismic monitoring according to an embodiment of the present application
- FIG. 2 is a schematic diagram of a search result of a G(i-1) layer mesh node according to an embodiment of the present application
- FIG. 3 is a schematic diagram of searching for a G(i) layer mesh node according to an embodiment of the present application
- FIG. 4 is a schematic flow chart of another method for locating a source in microseismic monitoring according to an embodiment of the present application
- FIG. 5 is a schematic diagram of searching for a G(i) layer mesh node considering a two-layer neighborhood according to an embodiment of the present application
- FIG. 6 is a schematic flow chart of another method for locating a source in microseismic monitoring according to an embodiment of the present application.
- FIG. 7 is a schematic flow chart of another method for locating a source in microseismic monitoring according to an embodiment of the present application.
- FIG. 8 is a schematic structural diagram of a source localization system in microseismic monitoring according to an embodiment of the present application.
- FIG. 1 is a schematic flow chart of a source localization method in microseismic monitoring. As shown in FIG. 1, a method for locating a source in microseismic monitoring may include:
- the first preset requirement is that a node falling in a grid satisfying the preset condition in the i-1th layer grid is centered. Within the circle of the radius.
- the embodiment of the present application divides the monitoring area into an N-layer grid according to the location accuracy of the source.
- the search process of the next layer of the grid node only the next layer of the grid falls into the upper layer.
- Full in the grid The mesh node of the pre-predetermined condition is a node in a neighborhood circle of the center of the circle, and the search range is gradually reduced. Only one node needs to be searched for each additional search layer, and the preset condition is also met in the upper layer of the grid. Nodes, that is, for each additional search layer, only 8 nodes are added for search calculation. When high-precision positioning is performed, a small amount of calculation can be realized.
- the source location accuracy is P
- the monitoring area is divided into an N-layer grid according to the source location accuracy, and the source location accuracy is compared with the N-layer grid.
- the number of layers N satisfies the following relationship,
- the detection area is meshed according to the requirements of the source location accuracy, and the N-layer grid is divided to provide a basis for the subsequent stepwise search to determine the source range.
- the node search is performed according to the process described in FIG. 1, and the total number of operations required OTimes is:
- NGX indicates the number of mesh nodes in the horizontal direction of the first layer mesh
- NNG indicates the number of mesh nodes in the vertical direction of the first layer mesh
- the monitoring height is 150 meters
- the monitoring length is 2000 meters
- the observation point distance is 20 meters
- the source positioning accuracy is required to be 1 meter.
- the initial edge length of the mesh element is chosen to be 20 meters. According to the relationship between the focal location accuracy and the number of mesh layers N, it can be known that:
- the binary grid search method adopted in this embodiment is 1.6 times more accurate than the existing method, and the calculation amount is reduced by 357 times.
- the above embodiment can be seen that only one node needs to be searched for each additional search layer, and the node that satisfies the preset condition in the upper layer grid is added, that is, for each additional search layer, only 8 nodes are searched for calculation. Small calculations can be achieved with high precision positioning.
- the monitoring area is divided into N-layer grids according to source positioning accuracy, and each layer grid is respectively recorded as G(1)...G(N), wherein the i-th layer grid
- the node that satisfies the preset condition in the G(i-1) layer grid is g i-1 (j, k), as shown in Figure 2. Determining and searching for the node in the i-th layer grid that satisfies the first preset requirement, as shown in FIG. 3, the node to be searched (including the node g i-1 (j, k)), and acquiring the node record in which the preset condition is met. For g i (m,n), and so on, the final source point location is determined until the search within the N-th layer grid is completed.
- the monitoring area is divided into an N-layer grid.
- the next layer of the grid node search process only the next layer of the grid falls into the upper layer of the grid and the predetermined preset is satisfied.
- the conditional grid node is a node in a neighborhood circle of the center of the circle, and the search range is gradually reduced. Only one node needs to be searched for each additional search layer, and the node that satisfies the preset condition in the upper layer grid is also included. For each additional search layer, only 8 nodes are added for search calculation. When high-precision positioning is performed, a small amount of calculation can be realized.
- the preset condition is that the current node has the largest energy among all nodes in the search range.
- the process of calculating node energy can include:
- the velocity of the medium obtained by sonic logging is calculated point by point by ray tracing method, and the theoretical propagation path and the first arrival travel time of each mesh node to each observation point are obtained.
- the energy of each grid point can be extracted by extracting the direct wave energy in the seismic record according to the initial schedule.
- the node energy near the actual source point position should be larger than other nodes. In each search process of this embodiment, the node with the largest energy can be gradually approached to the actual source point position.
- the method before step S103, the method further includes: picking up an actual first arrival time of the micro earthquake.
- the preset condition is that the time difference of the current node is the smallest among all the nodes in the search range, and the time difference is the forward first arrival time of the node to each monitoring point in the monitoring area and the actual first arrival time. The time difference between.
- the process of calculating the time difference between the forward start time of the node and the actual first arrival time of each monitoring point in the monitoring area may include:
- n the number of observation points.
- the time difference will be smaller.
- the node with the smallest time difference is acquired, and the actual source point position can be gradually approached.
- FIG. 4 is a schematic flow chart of another method for locating a source in microseismic monitoring according to an embodiment of the present application. As shown in FIG. 4, another method for locating a source in microseismic monitoring may include:
- the first preset requirement is that a node falling in a grid satisfying the preset condition in the i-1th layer grid is centered. Within the circle of the radius.
- the second preset requirement is that a node falling in the i-2th layer grid satisfies the preset condition is a center. Within the circle of the radius, and simultaneously falling into the center of the node satisfying the preset condition in the i-1st layer grid, Within the circle of the radius.
- the present embodiment considers the neighborhood of the node satisfying the preset condition in the i-1th layer and the i-2th layer in the search process.
- the neighborhood of the conditional node further reduces the amount of calculation and improves the search speed.
- the node that satisfies the preset condition in the i-2th layer grid G(i-2) is g i-2 (j, k), and the i-th layer grid G(i) is determined.
- -1 When the node that meets the preset condition is found, it has searched for G(i-1) falling into the center of g i-2 (j, k). For all the nodes in the circle of the radius (as shown by the black solid dot in Fig. 5), the node that satisfies the preset condition in G(i-1) is finally obtained, which is denoted as g i-1 (m, n).
- the neighborhood of the node satisfying the preset condition in the i-1th layer and the neighborhood of the node satisfying the preset condition in the i-2th layer are further considered, which further reduces The amount of calculation increases the search speed.
- FIG. 6 is a schematic flow chart of a source location method in a microseismic monitoring.
- another method for locating the source in the microseismic monitoring may include:
- S602. Perform a first layer mesh division on the monitoring area according to a preset edge length D of the preset grid unit, search all the nodes therein, and obtain a node that meets the preset condition.
- the initial side length is not more than twice the distance between the respective observation points.
- the first preset requirement is that a node falling in a grid satisfying the preset condition in the i-1th layer grid is centered. Within the circle of the radius.
- the monitoring area is meshed according to the grid unit from large to small, and nodes in each layer of the grid satisfying the preset condition are searched.
- the search process only the nodes in the neighborhood circle that fall into the grid of the previous layer determined by the previous layer of the mesh that meet the preset condition are searched, and the search range is gradually reduced.
- the search layer only needs to search for 9 nodes, including the nodes in the upper layer that meet the preset conditions, that is, for each additional search layer, only 8 nodes are added for search calculation. Calculated amount.
- FIG. 7 is a flow chart of a method for locating a source in another microseismic monitoring.
- another method for locating the source in the microseismic monitoring may include:
- the initial side length is not more than twice the distance between the respective observation points.
- the first preset requirement is that a node falling in a grid satisfying the preset condition in the i-1th layer grid is centered. Within the circle of the radius.
- the second preset requirement is that a node falling in the i-2th layer grid satisfies the preset condition is a center. Within the circle of the radius, and simultaneously falling into the center of the node satisfying the preset condition in the i-1st layer grid, Within the circle of the radius.
- the monitoring area is meshed according to the grid unit from large to small, and nodes in each layer of the grid satisfying the preset condition are searched.
- the present embodiment simultaneously considers the neighborhood of the largest energy node in the i-1th layer and the neighborhood of the largest energy node in the i-2th layer in the search process, further reducing the calculation amount. Improve search speed.
- a source localization system in microseismic monitoring is also provided in the embodiment of the present application, as described in the following embodiments. Since the principle of solving the problem of the system is similar to the method of locating the source in the micro-seismic monitoring, the implementation of the system can be referred to the implementation of the focal location method in the micro-seismic monitoring, and the repetition will not be repeated.
- the system in the embodiment of the present application may include a processor, an internal bus, a memory, and a memory at a hardware level, and may of course include hardware required for other services.
- the processor reads the corresponding computer program instructions from memory into memory and then runs.
- the present application does not exclude other implementation manners, such as a logic device or a combination of software and hardware, etc., that is, the execution body of the following processing flow is not limited to each logical unit, and may be Hardware or logic device.
- the initial side length is not more than twice the distance between the respective observation points.
- determining and searching for a node in the i-th layer grid that satisfies the first preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location, and the first preset requirement is that a node that meets the preset condition in the i-1st layer grid is centered.
- the embodiment of the present application divides the monitoring area into an N-layer grid according to the location accuracy of the source.
- the grid nodes in the grid that meet the preset conditions are nodes in a neighborhood circle of the center of the circle, and the search range is gradually reduced. Only one node needs to be searched for each additional search layer, including the upper layer grid.
- the node that satisfies the preset condition, that is, the search calculation of only 8 nodes is added for each additional search layer, and the small calculation amount can be realized when the high-precision positioning is performed.
- the initial side length is not more than twice the distance between the respective observation points.
- the node that meets the first preset requirement in the i-th layer grid is determined and searched, and the node that meets the preset condition is obtained, where the first preset requirement is to fall into the i-1th layer.
- the nodes in the grid that satisfy the preset condition are centered. Within the circle of the radius.
- determining and searching for a node in the i-th layer grid that satisfies the second preset requirement acquiring a node in which the preset condition is satisfied, until completing the search of the Nth layer grid, the Nth layer
- the node that meets the preset condition obtained in the grid is a source point location
- the second preset requirement is that a node that meets the preset condition in the i-th layer grid is centered.
- the embodiment of the present application divides the monitoring area into an N-layer grid according to the location accuracy of the source.
- the mesh node determined in the grid that satisfies the preset condition is a node within a neighborhood circle of the center of the circle, and the search range is gradually reduced, each increase
- a search layer only needs to search for 9 nodes, including the nodes in the upper layer that meet the preset conditions, that is, for each additional search layer, only 8 nodes are added for search calculation, which can be realized in high-precision positioning. Small calculations.
- Steps (3) and (4) are repeated within the circle of the radius until the determination in step (3) is YES. At this time, the node in the i-th layer mesh that satisfies the preset condition is the source point.
- the embodiment of the present application searches only the mesh node that falls within the upper layer of the grid and meets the preset condition determined by the previous layer of the grid as the center of the circle.
- the node within a neighborhood circle the search range is gradually reduced.
- Each additional search layer only needs to search for 9 nodes, including the nodes in the upper layer that meet the preset conditions, that is, each additional search layer, only Adding 8 nodes of search calculations, you can achieve small calculations when positioning with high precision.
- the second layer of mesh is divided into the monitoring area, and the node in the second layer grid that satisfies the first preset requirement is searched.
- the node that meets the preset condition where the first preset requirement is that a node that meets the preset condition in the i-1th layer grid is centered. Within the circle of radius.
- Steps (4) and (5) searching a node in the i-th layer grid that satisfies the second preset requirement, and acquiring a node in which the preset condition is met, where the second preset requirement is that the falling into the i-th layer grid satisfies
- the node of the preset condition is a center of the circle.
- Steps (4) and (5) are repeated within the circle of the radius until the determination in step (4) is YES.
- the node in the i-th layer mesh that satisfies the preset condition is the source point.
- the embodiment of the present application searches only the mesh node that falls within the upper layer of the grid and meets the preset condition determined by the previous layer of the grid as the center of the circle.
- the node within a neighborhood circle the search range is gradually reduced.
- Each additional search layer only needs to search for 9 nodes, including the nodes in the upper layer that meet the preset conditions, that is, each additional search layer, only Adding 8 nodes of search calculations, you can achieve small calculations when positioning with high precision.
- embodiments of the present invention can be provided as a method, system, or computer program product. Accordingly, the present invention may take the form of an entirely hardware embodiment, an entirely software embodiment, or a combination of software and hardware. Moreover, the invention can take the form of a computer program product embodied on one or more computer-usable storage media (including but not limited to disk storage, CD-ROM, optical storage, etc.) including computer usable program code.
- computer-usable storage media including but not limited to disk storage, CD-ROM, optical storage, etc.
- the computer program instructions can also be stored in a computer readable memory that can direct a computer or other programmable data processing device to operate in a particular manner, such that the instructions stored in the computer readable memory produce an article of manufacture comprising the instruction device.
- the apparatus implements the functions specified in one or more blocks of a flow or a flow and/or block diagram of the flowchart.
- These computer program instructions can also be loaded onto a computer or other programmable data processing device such that a series of operational steps are performed on a computer or other programmable device to produce computer-implemented processing for execution on a computer or other programmable device.
- the instructions provide steps for implementing the functions specified in one or more of the flow or in a block or blocks of a flow diagram.
- a computing device includes one or more processors (CPUs), input/output interfaces, network interfaces, and memory.
- processors CPUs
- input/output interfaces network interfaces
- memory volatile and non-volatile memory
- the memory may include non-persistent memory, random access memory (RAM), and/or non-volatile memory in a computer readable medium, such as read only memory (ROM) or flash memory.
- RAM random access memory
- ROM read only memory
- Memory is an example of a computer readable medium.
- Computer readable media includes both permanent and non-persistent, removable and non-removable media.
- Information storage can be implemented by any method or technology.
- the information can be computer readable instructions, data structures, modules of programs, or other data.
- Examples of computer storage media include, but are not limited to, phase change memory (PRAM), static random access memory (SRAM), dynamic random access memory (DRAM), other types of random access memory (RAM), read only memory. (ROM), electrically erasable programmable read only memory (EEPROM), flash memory or other memory technology, compact disk read only memory (CD-ROM), digital versatile disk (DVD) or other optical storage, Magnetic tape cartridges, magnetic tape storage or other magnetic storage devices or any other non-transportable media can be used to store information that can be accessed by a computing device.
- computer readable media does not include temporary storage of computer readable media, such as modulated data signals and carrier waves.
- embodiments of the present application can be provided as a method, system, or computer program product.
- the present application can take the form of an entirely hardware embodiment, an entirely software embodiment or an embodiment in combination of software and hardware.
- the application can take the form of a computer program product embodied on one or more computer-usable storage media (including but not limited to disk storage, CD-ROM, optical storage, etc.) including computer usable program code.
- the application can be described in the general context of computer-executable instructions executed by a computer, such as a program module.
- program modules include routines, programs, objects, components, data structures, and the like that perform particular tasks or implement particular abstract data types.
- the present application can also be practiced in distributed computing environments where tasks are performed by remote processing devices that are connected through a communication network.
- program modules can be located in both local and remote computer storage media including storage devices.
Landscapes
- Engineering & Computer Science (AREA)
- Remote Sensing (AREA)
- Life Sciences & Earth Sciences (AREA)
- Physics & Mathematics (AREA)
- Environmental & Geological Engineering (AREA)
- Acoustics & Sound (AREA)
- Geology (AREA)
- General Life Sciences & Earth Sciences (AREA)
- General Physics & Mathematics (AREA)
- Geophysics (AREA)
- Business, Economics & Management (AREA)
- Emergency Management (AREA)
- Geophysics And Detection Of Objects (AREA)
- Position Fixing By Use Of Radio Waves (AREA)
Abstract
Description
Claims (18)
- 一种微地震监测中的震源定位方法,其特征在于,包括以下步骤:获取监测区域和所述监测区域内的各个观测点;根据震源定位精度,将所述监测区域划分成N层网格,其中第i层网格的网格单元的边长为D/2i-1,i=1,…N,D为网格单元的初始边长,所述初始边长不大于所述各个观测点之间距离的2倍;搜索第1层网格中所有节点,获取其中满足预设条件的节点;
- 如权利要求1所述的方法,其特征在于,所述震源定位精度与所述N层网格的层数N满足以下关系式:P≥D/2N-1且P<D/2N-2式中P表示震源定位精度。
- 如权利要求1所述的方法,其特征在于,所述预设条件为当前节点在搜索范围内的所有节点中能量最大。
- 如权利要求1所述的方法,其特征在于,在所述搜索第1层网格中所有节点,获取其中满足预设条件的节点之前还包括:拾取微地震的实际初至时间,对应的,所述预设条件为当前节点在搜索范围内的所有节点中时间差最小,所述时间差为节点到所述监测区域内各个监测点的正演初至时间与所述实际初至时间之间的时间差。
- 一种微地震监测中的震源定位方法,其特征在于,包括以下步骤:获取监测区域和所述监测区域内的各个观测点;根据震源定位精度,将所述监测区域划分成N层网格,其中第i层网格的网格单元的边长为D/2i-1,i=1,…N,D为网格单元的初始边长,所述初始边长不大于所述各个观测点之间距离的2倍;搜索第1层网格中所有节点,获取其中满足预设条件的节点;
- 如权利要求5所述的方法,其特征在于,所述震源定位精度与所述N层网格的层数N满足以下关系式:P≥D/2N-1且P<D/2N-2式中P表示震源定位精度。
- 如权利要求5所述的方法,其特征在于,所述预设条件为当前节点在搜索范围内的所有节点中能量最大。
- 如权利要求5所述的方法,其特征在于,在所述搜索第1层网格中所有节点,获取其中满足预设条件的节点之前还包括:拾取微地震的实际初至时间,对应的,所述预设条件为当前节点在搜索范围内的所有节点中时间差最小,所述时间差为节点到所述监测区域内各个监测点的正演初至时间与所述实际初至时间之间的时间差。
- 一种微地震监测中的震源定位方法,其特征在于,包括以下步骤:(1)获取监测区域和所述监测区域内的各个观测点;(2)按照预设的网格单元的初始边长D对所述监测区域进行第1层网格划分,搜索其中的所有节点,获取满足预设条件的节点,所述初始边长不大于所述各个观测点之间距离的2倍;(3)判断当前网格单元边长是否满足震源定位精度,如果判断为否,从i=2开始,按照网格单元边长为D/2i-1,其中i=2,3,4…,对所述监测区域进行第i层网格划分;
- 如权利要求9所述的方法,其特征在于,所述预设条件为当前节点在搜索范围内的所有节点中能量最大。
- 如权利要求9所述的方法,其特征在于,在所述搜索第1层网格中所有节点,获取其中满足预设条件的节点之前还包括:拾取微地震的实际初至时间,对应的,所述预设条件为当前节点在搜索范围内的所有节点中时间差最小,所述时间差为节点到所述监测区域内各个监测点的正演初至时间与所述实际初至时间之间的时间差。
- 一种微地震监测中的震源定位方法,其特征在于,包括以下步骤:(1)获取监测区域和所述监测区域内的各个观测点;(2)按照预设的网格单元的初始边长D对所述监测区域进行第1层网格划分,搜索其中的所有节点,获取满足预设条件的节点,所述初始边长不大于所述各个观测点之间距离的2倍;(3)按照网格单元边长为D/2i-1,其中i=2,对所述监测区域进行第2层网格划分,搜索第2层网格中满足第一预设要求的节点,获取其中满足所述预设条件的节点,所述第一预设要求为落入以第i-1层网格中满足所述预设条件的节点为圆心,为半径的圆内;(4)判断当前网格单元边长是否满足震源定位精度,如果判断为否,从i=3开始,按照网格单元边长为D/2i-1,其中i=3,4…,对所述监测区域进行第i层网格划分;
- 如权利要求12所述的方法,其特征在于,所述预设条件为在搜索范围内的所有节点中能量最大。
- 如权利要求12所述的方法,其特征在于,在所述搜索第1层网格中所有节点,获取其中满足预设条件的节点之前还包括:拾取微地震的实际初至时间,对应的,所述预设条件为在搜索范围内的所有节点中时间差最小,所述时间差为节 点到所述监测区域内各个监测点的正演初至时间与所述实际初至时间之间的时间差。
- 一种微地震监测中的震源定位系统,其特征在于,所述系统包括:处理器;以及存储器,所述存储器被配置为用以存储计算机程序指令,所述计算机程序指令被所述处理器执行时,执行如下步骤:获取监测区域和所述监测区域内的各个观测点;根据震源定位精度,将所述监测区域划分成N层网格,其中第i层网格的网格单元的边长为D/2i-1,i=1,…N,D为网格单元的初始边长,所述初始边长不大于所述各个观测点之间距离的2倍;搜索第1层网格中所有节点,获取其中满足预设条件的节点;
- 一种微地震监测中的震源定位系统,其特征在于,所述系统包括:处理器;以及存储器,所述存储器被配置为用以存储计算机程序指令,所述计算机程序指令被所述处理器执行时,执行如下步骤:获取监测区域和所述监测区域内的各个观测点;根据震源定位精度,将所述监测区域划分成N层网格,其中第i层网格的网格单元的边长为D/2i-1,i=1,…N,D为网格单元的初始边长,所述初始边长不大于所述各个观测点之间距离的2倍;搜索第1层网格中所有节点,获取其中满足预设条件的节点;
- 一种微地震监测中的震源定位系统,其特征在于,所述系统包括:处理器;以及存储器,所述存储器被配置为用以存储计算机程序指令,所述计算机程序指令被所述处理器执行时,执行如下步骤:(1)获取监测区域和所述监测区域内的各个观测点;(2)按照预设的网格单元的初始边长D对所述监测区域进行第1层网格划分,搜索其中的所有节点,获取满足预设条件的节点,所述初始边长不大于所述各个观测点之间距离的2倍;(3)判断当前网格单元边长是否满足震源定位精度,如果判断为否,从i=2开始,按照网格单元边长为D/2i-1,其中i=2,3,4…,对所述监测区域进行第i层网格划分;
- 一种微地震监测中的震源定位系统,其特征在于,所述系统包括:处理器;以及存储器,所述存储器被配置为用以存储计算机程序指令,所述计算机程序指令被所述处理器执行时,执行如下步骤:(1)获取监测区域和所述监测区域内的各个观测点;(2)按照预设的网格单元的初始边长D对所述监测区域进行第1层网格划分,搜索其中的所有节点,获取满足预设条件的节点,所述初始边长不大于所述各个观测点之间距离的2倍;(3)按照网格单元边长为D/2i-1,其中i=2,对所述监测区域进行第2层网格划分,搜索第2层网格中满足第一预设要求的节点,获取其中满足所述预设条件的节点,所述第一预设要求为落入以第i-1层网格中满足所述预设条件的节点为圆心,为半径的圆内;(4)判断当前网格单元边长是否满足震源定位精度,如果判断为否,从i=3开始,按照网格单元边长为D/2i-1,其中i=3,4…,对所述监测区域进行第i层网格划分;
Priority Applications (3)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
GB1901140.2A GB2567089B (en) | 2016-08-29 | 2017-04-24 | Method and system for positioning seismic source in microseism monitoring |
CA3022158A CA3022158C (en) | 2016-08-29 | 2017-04-24 | Method and system for positioning seismic source in microseism monitoring |
US16/263,118 US11125898B2 (en) | 2016-08-29 | 2019-01-31 | Method and system for positioning seismic source in microseism monitoring |
Applications Claiming Priority (2)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
CN201610750747.8 | 2016-08-29 | ||
CN201610750747.8A CN106324670B (zh) | 2016-08-29 | 2016-08-29 | 一种微地震监测系统中的震源定位的方法及装置 |
Related Child Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
US16/263,118 Continuation US11125898B2 (en) | 2016-08-29 | 2019-01-31 | Method and system for positioning seismic source in microseism monitoring |
Publications (1)
Publication Number | Publication Date |
---|---|
WO2018040592A1 true WO2018040592A1 (zh) | 2018-03-08 |
Family
ID=57788750
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
PCT/CN2017/081583 WO2018040592A1 (zh) | 2016-08-29 | 2017-04-24 | 一种微地震监测中的震源定位方法及系统 |
Country Status (5)
Country | Link |
---|---|
US (1) | US11125898B2 (zh) |
CN (1) | CN106324670B (zh) |
CA (1) | CA3022158C (zh) |
GB (1) | GB2567089B (zh) |
WO (1) | WO2018040592A1 (zh) |
Families Citing this family (4)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN106324670B (zh) * | 2016-08-29 | 2018-09-04 | 中国石油天然气集团公司 | 一种微地震监测系统中的震源定位的方法及装置 |
CN106772591B (zh) * | 2017-04-05 | 2018-08-14 | 吉林大学 | 一种适用于提高微地震定位可靠性的联合定位方法 |
CN110795452B (zh) * | 2019-10-11 | 2020-12-25 | 天聚地合(苏州)数据股份有限公司 | 一种基于通信运营商位置核验技术的迭代搜索定位方法 |
CN113281806B (zh) * | 2021-05-19 | 2022-10-25 | 中南大学 | 一种用于矿山越界越层开采微震监测方法及系统 |
Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102129063A (zh) * | 2010-12-23 | 2011-07-20 | 中南大学 | 一种微震源或声发射源的定位方法 |
WO2013169937A1 (en) * | 2012-05-08 | 2013-11-14 | Octave Reservoir Technologies, Inc. | Microseismic event localization using both direct-path and head-wave arrivals |
CN104076392A (zh) * | 2014-05-28 | 2014-10-01 | 中国矿业大学(北京) | 基于网格搜索和牛顿迭代的微震震源定位联合反演方法 |
CN105022031A (zh) * | 2015-07-03 | 2015-11-04 | 四川大学 | 一种区域岩体微震震源的分层速度定位方法 |
CN105549077A (zh) * | 2015-12-16 | 2016-05-04 | 中国矿业大学(北京) | 基于多级多尺度网格相似性系数计算的微震震源定位方法 |
CN105842735A (zh) * | 2016-05-20 | 2016-08-10 | 四川大学 | 具有复杂速度分布的区域岩体微震震源定位方法 |
CN106324670A (zh) * | 2016-08-29 | 2017-01-11 | 中国石油天然气集团公司 | 一种微地震监测系统中的震源定位的方法 |
Family Cites Families (10)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
US8995224B2 (en) * | 2003-08-22 | 2015-03-31 | Schlumberger Technology Corporation | Real-time velocity and pore-pressure prediction ahead of drill bit |
GB2409722A (en) | 2003-12-29 | 2005-07-06 | Westerngeco Ltd | Microseismic determination of location and origin time of a fracture generated by fracturing operation in a hydrocarbon well |
US8209125B2 (en) * | 2007-03-12 | 2012-06-26 | Geomage (2003) Ltd. | Method for identifying and analyzing faults/fractures using reflected and diffracted waves |
US20120116680A1 (en) * | 2010-11-08 | 2012-05-10 | Saudi Arabian Oil Company | Microseismic source location estimation method with high resolution using green's functions |
CN103105622B (zh) | 2011-11-11 | 2015-08-12 | 中国石油集团川庆钻探工程有限公司地球物理勘探公司 | 基于数据库技术的同型波时差定位方法 |
GB2503507B (en) * | 2012-06-29 | 2015-04-15 | Foster Findlay Ass Ltd | Adaptive fault tracking |
US20150006082A1 (en) * | 2013-06-26 | 2015-01-01 | Baker Hughes Incorporated | Method and apparatus for microseismic attribute mapping for stimulated reservoir volume evaluation |
CN105093274B (zh) * | 2014-05-07 | 2017-10-20 | 中国石油化工股份有限公司 | 一种水力压裂裂缝震源机制的反演方法及系统 |
CN105093298B (zh) * | 2015-07-10 | 2017-06-13 | 北京派特森科技股份有限公司 | 一种微地震数据四维搜索逆时叠加的快速计算方法 |
CN105277971A (zh) * | 2015-10-16 | 2016-01-27 | 中国石油天然气集团公司 | 一种微地震监测系统及方法 |
-
2016
- 2016-08-29 CN CN201610750747.8A patent/CN106324670B/zh active Active
-
2017
- 2017-04-24 CA CA3022158A patent/CA3022158C/en active Active
- 2017-04-24 WO PCT/CN2017/081583 patent/WO2018040592A1/zh active Application Filing
- 2017-04-24 GB GB1901140.2A patent/GB2567089B/en active Active
-
2019
- 2019-01-31 US US16/263,118 patent/US11125898B2/en active Active
Patent Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102129063A (zh) * | 2010-12-23 | 2011-07-20 | 中南大学 | 一种微震源或声发射源的定位方法 |
WO2013169937A1 (en) * | 2012-05-08 | 2013-11-14 | Octave Reservoir Technologies, Inc. | Microseismic event localization using both direct-path and head-wave arrivals |
CN104076392A (zh) * | 2014-05-28 | 2014-10-01 | 中国矿业大学(北京) | 基于网格搜索和牛顿迭代的微震震源定位联合反演方法 |
CN105022031A (zh) * | 2015-07-03 | 2015-11-04 | 四川大学 | 一种区域岩体微震震源的分层速度定位方法 |
CN105549077A (zh) * | 2015-12-16 | 2016-05-04 | 中国矿业大学(北京) | 基于多级多尺度网格相似性系数计算的微震震源定位方法 |
CN105842735A (zh) * | 2016-05-20 | 2016-08-10 | 四川大学 | 具有复杂速度分布的区域岩体微震震源定位方法 |
CN106324670A (zh) * | 2016-08-29 | 2017-01-11 | 中国石油天然气集团公司 | 一种微地震监测系统中的震源定位的方法 |
Also Published As
Publication number | Publication date |
---|---|
US11125898B2 (en) | 2021-09-21 |
GB2567089B (en) | 2022-01-26 |
CA3022158A1 (en) | 2018-03-08 |
GB201901140D0 (en) | 2019-03-20 |
CA3022158C (en) | 2021-02-23 |
CN106324670B (zh) | 2018-09-04 |
GB2567089A (en) | 2019-04-03 |
US20190162867A1 (en) | 2019-05-30 |
CN106324670A (zh) | 2017-01-11 |
Similar Documents
Publication | Publication Date | Title |
---|---|---|
Zhang et al. | Locating induced earthquakes with a network of seismic stations in Oklahoma via a deep learning method | |
WO2018040592A1 (zh) | 一种微地震监测中的震源定位方法及系统 | |
CN103105624B (zh) | 基于数据库技术的纵横波时差定位方法 | |
CN102692644B (zh) | 生成深度域成像道集的方法 | |
CN105549077B (zh) | 基于多级多尺度网格相似性系数计算的微震震源定位方法 | |
CN105093274A (zh) | 一种水力压裂裂缝震源机制的反演方法及系统 | |
CN105301639A (zh) | 基于vsp旅行时双加权层析反演速度场的方法及其装置 | |
US20150241582A1 (en) | Methods and systems for using known source events in seismic data processing | |
WO2023098441A1 (zh) | 基于地层记录沉降反演被动陆缘地壳结构的方法及装置 | |
CN104730574A (zh) | 构建近地表结构模型的方法 | |
CN109991658A (zh) | 一种基于“震源-台站”速度模型的微地震事件定位方法 | |
CN107045141B (zh) | 基于反时到时差数据库的微地震/地震震源快速定位方法 | |
CN108845350A (zh) | 反演二维速度模型的方法及装置 | |
CN106405644A (zh) | 裂缝确定方法和装置 | |
RU2011148308A (ru) | Способ комплексной обработки геофизических данных и технологическая система "литоскан" для его осуществления | |
CN111413741A (zh) | 一种砂岩型铀矿资源量计算方法和装置 | |
CN103513279B (zh) | 一种基于地震波波动方程的照明分析计算方法及计算装置 | |
CN105301638A (zh) | 一种提取风化层底界面的方法和装置 | |
WO2019054905A1 (ru) | Способ и система анализа скважины с помощью пассивного акустического каротажа | |
CN104111476B (zh) | 构建地层速度场的方法及装置 | |
CN109001804B (zh) | 一种基于三维地震数据确定有效应力的方法、装置及系统 | |
Hsu et al. | Improving location of offshore earthquakes in earthquake early warning system | |
US20220091292A1 (en) | Automated extraction of horizon patches from seismic data | |
CN104570091B (zh) | 一种获得初至波射线的方法和装置 | |
Zhang et al. | Improvement of microseismic source location during cavern excavation in faulted rock mass using fast marching method |
Legal Events
Date | Code | Title | Description |
---|---|---|---|
ENP | Entry into the national phase |
Ref document number: 3022158 Country of ref document: CA |
|
121 | Ep: the epo has been informed by wipo that ep was designated in this application |
Ref document number: 17844900 Country of ref document: EP Kind code of ref document: A1 |
|
ENP | Entry into the national phase |
Ref document number: 201901140 Country of ref document: GB Kind code of ref document: A Free format text: PCT FILING DATE = 20170424 |
|
NENP | Non-entry into the national phase |
Ref country code: DE |
|
122 | Ep: pct application non-entry in european phase |
Ref document number: 17844900 Country of ref document: EP Kind code of ref document: A1 |