CN115638832A - River slope thing source monitoring devices - Google Patents
River slope thing source monitoring devices Download PDFInfo
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- CN115638832A CN115638832A CN202211661354.1A CN202211661354A CN115638832A CN 115638832 A CN115638832 A CN 115638832A CN 202211661354 A CN202211661354 A CN 202211661354A CN 115638832 A CN115638832 A CN 115638832A
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Abstract
The application provides river course side slope thing source monitoring devices belongs to natural disasters and detects technical field, and this river course side slope thing source monitoring devices includes sliding layer monitoring devices and stress interception subassembly. In the first stage, the migration volume of each slip layer of the source is recorded by the movement of the slip layer frame, which is the initial migration volume of the slip layer. And in the second stage, when the migration amount of the sliding layer exceeds the monitoring range of the sliding layer frame, the lower wedge block moves and contacts towards the upper wedge block, the thrust of the sliding layer is decomposed into horizontal thrust and upward jacking force by a wedge surface, the whole buried cage frame overturns towards the earth surface under the limiting action of the arc rail frame, the sliding layer continues to migrate and bury the foundation pit, one side of the buried cage frame is lifted until the hydrophobic barrier frame is vertical to the sliding direction of the side slope, the conversion of the interception dam is completed, large-scale earth surface debris flow is intercepted in preparation, and meanwhile, part of the monitoring device is protected, the variety and scale of the source of the river evolution in the earthquake area are accurately monitored, and the research and analysis on the river evolution in the earthquake area are facilitated.
Description
Technical Field
The application relates to a natural disaster detection technology field, particularly relates to a river channel side slope thing source monitoring devices.
Background
In a very short time when an earthquake occurs, the constraint force of a source around the river becomes low, and under the action of short-term and medium-term heavy rainfall after the earthquake, a large-scale and concentrated debris flow event generates an obvious lifting effect on the river bed and an obvious widening effect on the river valley. The change of the transverse and longitudinal sections of the river channel is most prominent and violent. At this stage, the whole transportation process of the same-earthquake loose materials in the watershed from the slope to the main river is basically completed, and the loose materials on the slope basically keep relatively stable after the process is completed and are difficult to participate in the river evolution process of the main river.
However, remote sensing monitoring is difficult to carry out due to loosening of the slope source caused by an earthquake, the migration of different sliding layers can be influenced by the infiltration degree of short-term strong rainfall, and different sources can enter the river channel due to the sliding of different sliding layers, so that the evolution of the river channel is influenced. The existing river channel side slope evolution monitoring can only carry out remote sensing monitoring on the river channel side slope afterwards, and the species and scale of the source participating in earthquake region river channel evolution are difficult to be accurately monitored, so that quantitative research and deep analysis on the earthquake region river channel evolution are influenced.
Disclosure of Invention
The present application is directed to solving at least one of the problems in the prior art. Therefore, the river slope matter source monitoring device is provided, the migration amount of each sliding layer is accurately monitored, and the type and the proportion of each sliding layer matter source are recorded according to the migration amount; when the monitoring quantity of the device sliding layer is exceeded, the ground surface interception posture is converted, and partial monitoring devices are protected.
The application is realized as follows:
the application provides a river course side slope thing source monitoring devices includes sliding layer monitoring devices and sharp interception subassembly.
The sliding layer monitoring device comprises buried pile frames, buried cage frames, layer rails, sliding layer frames, grid racks, counting toothed shafts, water seepage brackets and water seepage flow meters, wherein the buried cage frames are rotatably connected between the buried pile frames, the layer rails are uniformly arranged on the peripheral sides of the buried cage frames, the sliding layer frames slide between the layer rails, the grid racks are arranged on the layer rails, the counting toothed shafts are rotatably connected on the sliding layer frames, the counting toothed shafts are meshed on the grid racks, the water seepage brackets are lapped on the sliding layer frames, the water seepage flow meters are communicated in the water seepage brackets, stress interception components comprise water tower frames, arc rail frames, hydrophobic blocking frames, lower wedge blocks and upper wedge blocks, the water tower frames are arranged on the buried pile frames, the arc rail frames are arranged on the water tower frames, the buried cage frames slide between the arc rail frames, the hydrophobic blocking frames are arranged on the buried cage frames, the lower wedge blocks are arranged on the sliding layer rails, the upper wedge blocks face the upper layer rails, the lower wedge blocks face the lower blocks.
In an embodiment of this application, evenly be provided with the side brace piece on the sliding layer frame, infiltration bracket bottom evenly is provided with the strutbeam, strutbeam one end rotate connect in on the side brace piece.
In an embodiment of this application, it is provided with the inserted bar to rotate on the strutbeam, it is provided with the plug bush to rotate on the collateral branch piece, the inserted bar slide run through in the plug bush, the plug bush surface with the inserted bar surface all is provided with the lockhole, the lockhole one-to-one.
In an embodiment of the application, the infiltration bracket is evenly provided with water through holes, the infiltration bracket is evenly provided with a waterproof seat, and the infiltration flowmeter is fixed on the waterproof seat.
In one embodiment of the application, a support is arranged on the sliding layer frame, the counting gear shaft is rotatably connected to the support, and a counter is arranged on the support and faces the counting gear shaft.
In one embodiment of the present application, the support is rotatably provided with a roller, and the roller slides on the surface of the layer rail.
In an embodiment of the present application, a clamping seat is disposed on the sliding layer frame, the lower wedge block is fixed on the clamping seat, and one end of the lower wedge block is attached to the surface of the sliding layer frame.
In an embodiment of the application, a support beam is arranged on the layer rail, and one end of the support beam is attached to the surface of the upper wedge block.
In an embodiment of the present application, a rib beam is disposed on the water tower frame, and the rib beam is fixed on the arc rail frame.
In one embodiment of the application, the buried pile frame is uniformly provided with angle beams.
In an embodiment of the application, the river slope source monitoring device further comprises a source pressure sensing component and a rainfall monitoring component.
The material source pressure sensing assembly comprises an intercepting frame, an induction seat, an induction column, a reset spring and a pressure sensor, wherein the intercepting frame is arranged on a water tower frame, the induction seat is uniformly arranged in the intercepting frame, the induction column slides and runs through the induction seat, the induction column is communicated with the induction seat, the reset spring is arranged in the induction seat, one end of the reset spring is laminated on the surface of the intercepting frame, the other end of the reset spring is laminated on the induction column, the pressure sensor is arranged in the induction seat, the pressure sensor faces the induction column, the rainfall monitoring assembly comprises a rainwater collecting hopper, a rainfall flowmeter, a lateral flow head and a saturated flowmeter, the rainwater collecting hopper is arranged in the upper end of the water tower frame, the rainfall flowmeter is communicated with the bottom of the rainwater collecting hopper, the lateral flow head is communicated with the induction column, the saturated flowmeter is arranged on the intercepting frame, and the saturated flowmeter is communicated with the induction seat.
In an embodiment of this application, interception board has been laid on the interception frame surface, the response post both ends are provided with the limiting plate, and one of them the limiting plate orientation in the response seat, another the limiting plate orientation interception board.
In an embodiment of the application, a lateral flow port is arranged on the lateral side of the lateral flow head, the lateral flow port faces to the inside of the induction column, a top pressure plate is arranged at one end of the lateral flow head, a screen port is arranged on the surface of the top pressure plate, and the screen port faces to the lateral flow port.
The beneficial effect of this application is: this application obtains river course side slope thing source monitoring devices through above-mentioned design, during the use, according to the reality topography and landform of seismic region river course, installs thing source monitoring devices at every other section length. And (3) driving the lower end of a pile of the buried pile frame into the immovable sliding bed, and installing a frame and a monitoring device at the upper end of the buried pile frame. Excavation buries ground between the ground pile frame and reserves the foundation ditch, will bury ground cage and hang into the foundation ditch in, will bury ground cage with bury ground pile frame and rotate the installation through the axostylus axostyle, will bury ground cage and slide through the installation with the arc rail frame through the axostylus axostyle, foundation ditch bottom degree of depth should not interfere the upset of burying ground cage, foundation ditch landslide direction lateral wall and the laminating of landing sill frame, the foundation ditch bottom should set up water drainage pipeline, reduces the influence of hole ponding to the landslide layer.
After the earthquake, the slope sources are loosened, all sliding layers are easy to migrate, and the underground sliding layers can slide in the direction of the slopes before the debris flow appears on the river slopes, so that the types and the scale of the sources carried by the debris flow are directly influenced. Each sliding layer can bulldoze the sliding layer frame of co-altitude not at the migration in-process, and sliding layer frame slides on the layer rail through the gyro wheel, and the slip in-process is accurate through count gear shaft and grid rack toothing and is slided, and the change circle of counter record count gear shaft to the current sliding distance of sliding layer of accurate record compares traditional photoelectric distance monitoring, has reduced the measurement inefficacy that device extrusion deformation arouses. Asynchronous phenomenon can appear when sliding in each thing source sliding layer, lifts each thing source sliding layer through the infiltration bracket, and audio-visual reaction river course side slope thing source sliding layer's sliding state. And analyzing the variety proportion of the erosion source of the river slope in the seismic region through the migration of each sliding layer. The riverway side slope after the earthquake does not have the energy of sliding, and the sliding layer migration can be caused only by the short-time strong rainfall infiltration. Adjust the slide position of inserted bar and plug bush to die through the bolt lock, adjust the horizontal contained angle of infiltration bracket, adjust the flow direction of infiltration in the sliding layer ground, carry out the accurate record to infiltration in each sliding layer ground through the infiltration flowmeter, research rainfall infiltration is to the influence of shock zone sliding layer migration separation and ground moisture saturation.
In the first stage, the migration volume of each slip layer of the source is recorded by the movement of the slip layer frame, which is the initial migration volume of the slip layer. And a second stage, when the migration amount of the sliding layer exceeds the monitoring range of the sliding layer frame, the lower wedge block moves and contacts towards the upper wedge block, the thrust of the sliding layer is decomposed into horizontal thrust and upward jacking force by a tapered wedge surface, the whole buried cage frame overturns towards the earth surface under the limiting effect of the arc rail frame, the sliding layer continues to migrate the landfill foundation pit, one side of the buried cage frame is lifted until the hydrophobic blocking frame stands in the sliding direction of the side slope, the transformation of the blocking dam is completed, the earth surface large-scale debris flow is blocked in preparation, and meanwhile, part of the monitoring device is protected, the variety and scale of the origin of the river course in the earthquake area are accurately monitored, and the research and analysis on the river course evolution in the earthquake area are facilitated.
Drawings
In order to more clearly explain 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 that for those skilled in the art, other related drawings can be obtained from these drawings without inventive effort.
Fig. 1 is a schematic perspective view of a river slope source monitoring device provided in an embodiment of the present application;
fig. 2 is a schematic perspective structure view of a river slope source monitoring device provided in an embodiment of the present application;
fig. 3 is a schematic partial perspective view of a slip layer monitoring device according to an embodiment of the present disclosure;
fig. 4 is a schematic perspective structure diagram of a sliding layer monitoring device and a stress intercepting component according to an embodiment of the present application;
fig. 5 is a schematic perspective view of a rainfall monitoring assembly provided in an embodiment of the present application;
fig. 6 is a schematic perspective view of a source pressure sensing assembly and a rainfall monitoring assembly according to an embodiment of the present disclosure.
In the figure: 100-slip layer monitoring device; 110-buried pile frames; 111-corner beam; 120-buried cage frame; 130-layer rail; 131-a resisting beam; 140-a slide frame; 141-side branch block; 142-a sleeve; 143-a lock hole; 144-a support; 145-a counter; 146-a roller; 147-a card holder; 150-grid rack; 160-counting gear shaft; 170-water seepage bracket; 171-corbel; 172-plunger; 173-water through holes; 174-a bump guard; 180-water seepage flow meter; 300-a stress interception component; 310-a water tower; 311-a rib beam; 320-arc rail frame; 330-hydrophobic blocking frame; 340-lower wedge; 350-upper wedge block; 500-a source pressure sensing assembly; 510-an intercepting frame; 511-interception plates; 520-an induction seat; 530-induction column; 531-limiting plate; 540-return spring; 550-a pressure sensor; 700-a rainfall monitoring component; 710-a rain collecting hopper; 720-rainfall flow meter; 730-side flow head; 731-side flow port; 732-a top pressure plate; 733-screen openings; 740-saturation flow meter.
Detailed Description
The technical solutions in the embodiments of the present application will be described below with reference to the drawings in the embodiments of the present application.
To make the objects, technical solutions and advantages of the embodiments of the present application clearer, the technical solutions of 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. All other embodiments obtained by a person of ordinary skill in the art without any inventive work based on the embodiments in the present application are within the scope of protection of the present application.
Examples
As shown in fig. 1 to 6, a river slope source monitoring device according to an embodiment of the present application includes a skid layer monitoring device 100, a stress intercepting component 300, a source pressure sensing component 500, and a rainfall monitoring component 700. The stress intercepting assembly 300 is installed on the slip layer monitoring apparatus 100, the source pressure sensing assembly 500 is installed on the stress intercepting assembly 300, and the rainfall monitoring assembly 700 is installed on the stress intercepting assembly 300. The sliding layer monitoring device 100 accurately monitors the migration volume of each sliding layer, and records the types and proportions of the sliding layer sources; when the slip layer monitoring quantity of the device is exceeded, the stress interception component 300 is converted into an earth surface interception posture to protect part of the monitoring device; the source pressure sensing assembly 500 records the circulation time and the circulation height of the earth surface large-scale debris flow, so that the scale of the river channel side slope debris flow is calculated; the rainfall monitoring assembly 700 accurately records the amount of local rainfall and seepage of surface debris flow.
As shown in fig. 2-6, remote sensing monitoring is difficult to perform due to the loosening of slope sources caused by an earthquake, the migration of different sliding layers can be influenced by the infiltration degree of a short-term heavy rainfall, and the sliding of different sliding layers can cause different sources to enter a river channel, so that the evolution of the river channel is influenced. The existing river channel side slope evolution monitoring can only carry out remote sensing monitoring on river channel side slopes afterwards, and the variety and scale of river channel evolution sources in seismic zones are difficult to monitor accurately, so that the research and analysis on the river channel evolution in seismic zones are influenced.
The sliding layer monitoring device 100 includes a buried pile frame 110, a buried cage frame 120, a layer rail 130, a sliding layer frame 140, a grid rack 150, a counting pinion 160, a seepage bracket 170, and a seepage flow meter 180. The buried cage 120 is rotatably connected between the buried pile frames 110, and the buried cage 120 is in pin connection with the buried pile frames 110. The layer rails 130 are uniformly arranged on the peripheral side of the buried cage 120, and the layer rails 130 are bolted with the buried cage 120. The sliding layer frame 140 slides between the layer rails 130, a support 144 is arranged on the sliding layer frame 140, and the support 144 is bolted with the sliding layer frame 140. The support 144 is rotatably provided with a roller 146, and the roller 146 is pin-jointed with the support 144. The roller 146 slides on the surface of the layer rail 130. The grid rack 150 is disposed on the layer rail 130, and the grid rack 150 is bolted to the layer rail 130. The counting gear shaft 160 is rotatably connected to the sliding layer frame 140, the counting gear shaft 160 is rotatably connected to the support 144, and the counting gear shaft 160 is pin-jointed with the support 144. The counting gear shaft 160 is engaged with the grid rack 150 to facilitate smooth sliding of the sliding rack 140.
Wherein, be provided with counter 145 on the support 144, counter 145 and support 144 spiro union, counter 145 is towards count pinion 160, makes things convenient for the monitoring of sliding layer frame 140 displacement, compares traditional photoelectric displacement monitoring, reduces the monitoring accuracy that deformation extrusion caused and descends. The water seepage bracket 170 is lapped on the sliding layer frame 140, the sliding layer frame 140 is uniformly provided with side supporting blocks 141, and the side supporting blocks 141 are welded with the sliding layer frame 140. The bottom of the water seepage bracket 170 is uniformly provided with support beams 171, and the support beams 171 are welded with the water seepage bracket 170. One end of the support beam 171 is rotatably connected to the side support block 141, and the support beam 171 is pin-connected to the side support block 141. The support beam 171 is rotatably provided with an inserted link 172, and the inserted link 172 is pin-connected with the support beam 171. The lateral support block 141 is rotatably provided with an insertion sleeve 142, and the insertion sleeve 142 is pin-connected with the lateral support block 141. The inserted bar 172 penetrates through the inserted sleeve 142 in a sliding mode, the surfaces of the inserted sleeve 142 and the inserted bar 172 are respectively provided with a lock hole 143, the lock holes 143 correspond to one another, and the inserted bar is specifically limited and adjusted through a bolt, so that the sliding layer frame 140 is convenient to adjust the angle, and water seepage in a soil body of a sliding layer is convenient to recover.
Wherein, the water holes 173 are uniformly arranged on the water seepage bracket 170, which is convenient for recovering the seepage water in the soil body of the sliding layer. The seepage flow meter 180 is communicated with the seepage bracket 170, the seepage bracket 170 is uniformly provided with anti-impact seats 174, and the anti-impact seats 174 are bolted with the seepage bracket 170. The seepage flow meter 180 is fixed on the anti-impact seat 174, and the seepage flow meter 180 is bolted with the anti-impact seat 174. The buried pile frame 110 is uniformly provided with the angle beams 111, and the angle beams 111 are bolted with the buried pile frame 110, so that the supporting strength of the buried pile frame 110 is increased.
The stress intercepting assembly 300 includes a water tower 310, an arc rail frame 320, a hydrophobic fence frame 330, a lower wedge 340, and an upper wedge 350. The water tower frame 310 is installed on the buried pile frame 110, and the water tower frame 310 is bolted with the buried pile frame 110. The arc rail frame 320 is arranged on the water tower frame 310, and the arc rail frame 320 is welded with the water tower frame 310. The buried cage frame 120 slides between the arc rail frames 320, a pin shaft is rotatably arranged on the buried cage frame 120, an arc groove is formed in the arc rail frame 320, and the pin shaft slides in the arc groove. The hydrophobic rail 330 is disposed on the buried cage 120, and the hydrophobic rail 330 is bolted to the buried cage 120. The lower wedge block 340 is arranged on the sliding layer frame 140, the sliding layer frame 140 is provided with a clamping seat 147, and the clamping seat 147 is bolted with the sliding layer frame 140. The lower wedge 340 is fixed to the cassette 147, and the lower wedge 340 is bolted to the cassette 147. One end of the lower wedge block 340 is attached to the surface of the sliding layer frame 140. The layer rail 130 is provided with a support beam 131, and the support beam 131 is bolted with the layer rail 130. One end of the support beam 131 is attached to the surface of the upper wedge 350.
Wherein, the upper wedge block 350 is disposed on the layer rail 130, and the upper wedge block 350 is bolted to the layer rail 130. The lower wedge 340 faces the upper wedge 350. The water tower frame 310 is provided with a rib beam 311, the rib beam 311 is fixed on the arc rail frame 320, and the rib beam 311 is respectively welded with the water tower frame 310 and the arc rail frame 320.
According to the real topography and landform of the river channel in the seismic region, the source monitoring devices are installed at intervals of a certain length. The lower end of a pile of the buried pile frame 110 is driven into a non-movable sliding bed, and the upper end of the buried pile frame 110 is provided with a frame and a monitoring device. Excavation buries ground between the pile frame 110 and reserves the foundation ditch, will bury ground cage 120 and hang into in the foundation ditch, will bury ground cage 120 and bury ground pile frame 110 and rotate the installation through the axostylus axostyle, will bury ground cage 120 and arc rail frame 320 and slide through the installation through the axostylus axostyle, the upset that buries ground cage 120 should not interfere in the foundation ditch bottom degree of depth, foundation ditch landslide direction lateral wall and sliding layer frame 140 laminating, the foundation ditch bottom should set up water drainage pipeline, reduce the influence of pot hole ponding to the landslide layer.
After the earthquake, the source of the side slope is loosened, all sliding layers are easy to migrate, the underground sliding layers can slide in the direction of the side slope before the debris flow occurs on the side slope of the river channel, and the type and the scale of the source carried by the debris flow are directly influenced. During the migration process of each sliding layer, the sliding layer frames 140 with different heights can be pushed, the sliding layer frames 140 slide on the layer rails 130 through the rollers 146, accurate sliding is achieved through meshing of the counting toothed shafts 160 and the grid racks 150 during the sliding process, the counter 145 records the rotation circle of the counting toothed shafts 160, therefore the sliding distance of the current sliding layer is accurately recorded, and compared with the traditional photoelectric distance monitoring, the measuring failure caused by extrusion deformation of the device is reduced. Asynchronous phenomenon can appear when sliding in each thing source sliding layer, lifts each thing source sliding layer through infiltration bracket 170, and audio-visual reaction river course side slope thing source sliding layer's sliding state. And analyzing the variety proportion of the erosion source of the river slope in the seismic region through the migration of each sliding layer. The riverway side slope after the earthquake does not have the energy of sliding, and the sliding layer migration can be caused only by the short-time strong rainfall infiltration. Adjust inserted bar 172 and plug bush 142's sliding position to lock through the bolt, adjust the horizontal contained angle of infiltration bracket 170, adjust the flow direction of infiltration in the sliding layer ground, carry out the accurate record to infiltration in each sliding layer ground through infiltration flowmeter 180, research rainfall infiltration under to the influence of seismic zone sliding layer slippage separation and ground moisture saturation.
In the first stage, the migration volume of each slip layer of the source is recorded by the movement of the slip layer frame 140, which is the initial migration volume of the slip layer. And in the second stage, when the migration amount of the sliding layer exceeds the monitoring range of the sliding layer frame 140, the lower wedge block 340 moves towards the upper wedge block 350 and contacts with the upper wedge block, the thrust of the sliding layer is decomposed into horizontal thrust and upward jacking force by a wedge surface, under the limiting action of the arc rail frame 320, the whole buried cage frame 120 is turned over towards the ground surface, the sliding layer continuously migrates to bury the foundation pit, one side of the buried cage frame 120 is lifted until the hydrophobic blocking frame 330 stands in the sliding direction of the side slope, the transformation of the blocking dam is completed, the large-scale earth surface debris flow is ready to be blocked, meanwhile, part of monitoring devices are protected, the type and the scale of the source of the river course evolution in the earthquake region are accurately monitored, and the research and the analysis of the river course evolution in the earthquake region are facilitated.
The source pressure sensing assembly 500 includes an intercepting frame 510, a sensing seat 520, a sensing post 530, a return spring 540, and a pressure sensor 550. The intercepting frame 510 is disposed on the water tower frame 310, and the intercepting frame 510 is bolted to the water tower frame 310. The induction seats 520 are uniformly arranged in the intercepting frame 510, and the intercepting frame 510 is bolted with the induction seats 520. The induction column 530 is slidably penetrated through the induction seat 520, the interception plate 511 is laid on the surface of the interception frame 510, and the interception plate 511 is bolted with the interception frame 510. Limiting plates 531 are arranged at two ends of the induction column 530, and the limiting plates 531 are bolted with the induction column 530. One of the limiting plates 531 faces the inside of the sensing seat 520, and the other limiting plate 531 faces the intercepting plate 511, so as to limit the sliding of the sensing column 530. The induction column 530 is communicated with the induction seat 520, so that seepage water in the debris flow can be conveniently recovered. The return spring 540 is disposed in the sensing seat 520, one end of the return spring 540 is attached to the surface of the intercepting frame 510, and the other end of the return spring 540 is attached to the sensing post 530.
Wherein, pressure sensor 550 is disposed in sensing seat 520, and pressure sensor 550 is screwed with sensing seat 520. The pressure sensor 550 faces the inductive column 530 and monitors the height of the landslide debris flow.
In the third stage, the sliding layer is migrated and broken to cause the generation of the earth surface debris flow, the hydrophobic blocking frame 330 is matched with the blocking frame 510 and the blocking plate 511 to block the earth surface debris flow, the debris flow impacts the top pressure plate 732 to drive the induction column 530 to slide and impact the pressure sensor 550, the height of the debris flow at the moment is recorded, and the induction column 530 is reset through the reset spring 540. The hydrophobic diversion effect of the hydrophobic barrier 330 and the narrow and wide design of the interception plate 511 can reduce the blockage of debris flow in front of the interception device. The method is characterized in that the circulation time and the circulation height of the earth surface debris flow are accurately recorded, the scale of the debris flow is measured and calculated, and the law of the debris flow with different source type proportions on the evolution erosion of the river channel is accurately researched by matching with the type proportions of the sliding layer source.
The mud-rock flow that the short-time heavy rainfall triggered can corrode the seismic region river course and evolve, collects local rainfall through rain collecting hopper 710, and the rainfall is accurately recorded through rainfall flowmeter 720. Collect the infiltration in the mud-rock flow through side flow head 730, through the infiltration water content of each height of saturation flowmeter 740 accurate record mud-rock flow, cooperation above-mentioned structure, the research rainfall, the looseness of earthquake side slope thing source, the kind and the proportion of skid bed thing source, the relation between the scale of landslide mud-rock flow carries out scientific data to current seismic region river course evolution and corrodes and supply, the convenient research and the analysis to seismic region river course evolution.
Specifically, this river course side slope thing source monitoring devices's theory of operation: according to the real topography and landform of the river channel in the seismic region, the source monitoring devices are installed at intervals of a certain length. The lower end of a pile of the buried pile frame 110 is driven into a non-movable sliding bed, and the upper end of the buried pile frame 110 is provided with a frame and a monitoring device. Excavation buries ground between the pile frame 110 and reserves the foundation ditch, will bury ground cage 120 and hang into in the foundation ditch, will bury ground cage 120 and bury ground pile frame 110 and rotate the installation through the axostylus axostyle, will bury ground cage 120 and arc rail frame 320 and slide through the installation through the axostylus axostyle, the upset that buries ground cage 120 should not interfere in the foundation ditch bottom degree of depth, foundation ditch landslide direction lateral wall and sliding layer frame 140 laminating, the foundation ditch bottom should set up water drainage pipeline, reduce the influence of pot hole ponding to the landslide layer.
After the earthquake, the slope sources are loosened, all sliding layers are easy to migrate, and the underground sliding layers can slide in the direction of the slopes before the debris flow appears on the river slopes, so that the types and the scale of the sources carried by the debris flow are directly influenced. During the migration process of each sliding layer, the sliding layer frames 140 with different heights can be pushed, the sliding layer frames 140 slide on the layer rails 130 through the rollers 146, accurate sliding is achieved through meshing of the counting toothed shafts 160 and the grid racks 150 during the sliding process, the counter 145 records the rotation circle of the counting toothed shafts 160, therefore the sliding distance of the current sliding layer is accurately recorded, and compared with the traditional photoelectric distance monitoring, the measuring failure caused by extrusion deformation of the device is reduced. Asynchronous phenomenon can appear when sliding in each thing source sliding layer, lifts each thing source sliding layer through infiltration bracket 170, and audio-visual reaction river course side slope thing source sliding layer's sliding state. And analyzing the variety proportion of the erosion source of the river slope in the seismic region through the migration of each sliding layer. The riverway side slope after the earthquake does not have the energy of sliding, and the sliding layer migration can be caused only by the short-time strong rainfall infiltration. Adjust inserted bar 172 and plug bush 142's sliding position to lock through the bolt, adjust the horizontal contained angle of infiltration bracket 170, adjust the flow direction of infiltration in the sliding layer ground, carry out the accurate record to infiltration in each sliding layer ground through infiltration flowmeter 180, research rainfall infiltration under to the influence of seismic zone sliding layer slippage separation and ground moisture saturation.
In the first stage, the migration volume of each slip layer of the source is recorded by the movement of the slip layer frame 140, which is the initial migration volume of the slip layer. And in the second stage, when the migration amount of the sliding layer exceeds the monitoring range of the sliding layer frame 140, the lower wedge block 340 moves towards the upper wedge block 350 and contacts with the upper wedge block, the thrust of the sliding layer is decomposed into horizontal thrust and upward jacking force by a wedge surface, under the limiting action of the arc rail frame 320, the whole buried cage frame 120 is turned over towards the ground surface, the sliding layer continuously migrates to bury the foundation pit, one side of the buried cage frame 120 is lifted until the hydrophobic blocking frame 330 stands in the sliding direction of the side slope, the transformation of the blocking dam is completed, the large-scale earth surface debris flow is ready to be blocked, meanwhile, part of monitoring devices are protected, the type and the scale of the source of the river course evolution in the earthquake region are accurately monitored, and the research and the analysis of the river course evolution in the earthquake region are facilitated.
In the third stage, the sliding layer is migrated and broken to cause the generation of the earth surface debris flow, the hydrophobic blocking frame 330 is matched with the blocking frame 510 and the blocking plate 511 to block the earth surface debris flow, the debris flow impacts the top pressure plate 732 to drive the induction column 530 to slide and impact the pressure sensor 550, the height of the debris flow at the moment is recorded, and the induction column 530 is reset through the reset spring 540. The hydrophobic diversion effect of the hydrophobic barrier 330 and the narrow and wide design of the interception plate 511 can reduce the blockage of debris flow in front of the interception device. The circulation time and the circulation height of the earth surface debris flow are accurately recorded, the scale of the debris flow is measured and calculated, and the law of the erosion of the debris flow to the river channel evolution by different source type proportions is accurately researched by matching with the type proportion of the sliding layer source.
The mud-rock flow that the short-term heavy rainfall triggered can corrode the evolution to the earthquake district river course, collects local rainfall through rain collecting bucket 710, through rainfall flowmeter 720 accurate record rainfall. Collect the infiltration in the mud-rock flow through side flow head 730, through the infiltration water content of each height of saturation flowmeter 740 accurate record mud-rock flow, cooperate above-mentioned structure, research rainfall, the relation between the loose degree of earthquake side slope thing source, the kind and the proportion of skid bed thing source and the scale of landslide mud-rock flow, carry out scientific data to current earthquake area river course evolution and corrode, the convenient research and the analysis to earthquake area river course evolution.
It should be noted that the specific model specifications of the counter 145, the pressure sensor 550, the rainfall flowmeter 720 and the saturation flowmeter 740 need to be determined by type selection according to the actual specification of the device, and the specific type selection calculation method adopts the prior art, so detailed description is omitted.
The powering of the counter 145, the pressure sensor 550, the rainfall flow meter 720 and the saturation flow meter 740, and the principles thereof, will be clear to those skilled in the art and will not be described in detail herein.
The above embodiments are merely examples of the present application and are not intended to limit the scope of the present application, and various modifications and changes may be made by those skilled in the art. Any modification, equivalent replacement, improvement, etc. made within the spirit and principle of the present application shall be included in the protection scope of the present application. It should be noted that like reference numerals and letters refer to like items in the following figures, and thus once an item is defined in one figure, it need not be further defined and explained in subsequent figures.
Claims (10)
1. River slope material source monitoring device, which is characterized by comprising
The sliding layer monitoring device (100) comprises buried pile frames (110), buried cage frames (120), layer rails (130), sliding layer frames (140), grid racks (150), counting gear shafts (160), water seepage brackets (170) and water seepage flow meters (180), wherein the buried cage frames (120) are rotatably connected among the buried pile frames (110), the layer rails (130) are uniformly arranged on the peripheral sides of the buried cage frames (120), the sliding layer frames (140) slide among the layer rails (130), the grid racks (150) are arranged on the layer rails (130), the counting gear shafts (160) are rotatably connected on the sliding layer frames (140), the counting gear shafts (160) are meshed on the grid racks (150), the water seepage brackets (170) are lapped on the sliding layer frames (140), and the flow meters (180) are communicated in the water seepage brackets (170);
stress interception subassembly (300), stress interception subassembly (300) include water tower frame (310), arc rail frame (320), hydrophobic rail frame (330), wedge piece (340) and go up wedge piece (350), water tower frame (310) is installed on buried pile frame (110), arc rail frame (320) set up in on the water tower frame (310), buried cage frame (120) slide in between arc rail frame (320), hydrophobic rail frame (330) set up in on buried cage frame (120), wedge piece (340) set up in on sliding layer frame (140), go up wedge piece (350) set up in on layer rail (130), wedge piece (340) orientation goes up wedge piece (350).
2. The riverway slope source monitoring device according to claim 1, wherein side supporting blocks (141) are uniformly arranged on the sliding layer frame (140), supporting beams (171) are uniformly arranged at the bottom of the water seepage bracket (170), and one end of each supporting beam (171) is rotatably connected to the side supporting block (141).
3. The riverway side slope matter source monitoring device according to claim 2, wherein the supporting beam (171) is rotatably provided with an inserting rod (172), the side supporting block (141) is rotatably provided with an inserting sleeve (142), the inserting rod (172) slidably penetrates through the inserting sleeve (142), the surface of the inserting sleeve (142) and the surface of the inserting rod (172) are respectively provided with a lock hole (143), and the lock holes (143) are in one-to-one correspondence.
4. The riverway slope matter source monitoring device according to claim 1, wherein the water seepage bracket (170) is uniformly provided with water through holes (173), the water seepage bracket (170) is uniformly provided with anti-flushing seats (174), and the water seepage flow meter (180) is fixed on the anti-flushing seats (174).
5. The riverway slope matter source monitoring device according to claim 1, wherein a support (144) is arranged on the sliding layer frame (140), the counting gear shaft (160) is rotatably connected to the support (144), a counter (145) is arranged on the support (144), and the counter (145) faces the counting gear shaft (160).
6. The riverway slope matter source monitoring device according to claim 5, wherein the support (144) is rotatably provided with a roller (146), and the roller (146) slides on the surface of the layer rail (130).
7. The riverway slope matter source monitoring device according to claim 1, wherein a clamping seat (147) is arranged on the sliding layer frame (140), the lower wedge block (340) is fixed on the clamping seat (147), and one end of the lower wedge block (340) is attached to the surface of the sliding layer frame (140).
8. The riverway slope source monitoring device according to claim 1, wherein the layer rail (130) is provided with a support beam (131), and one end of the support beam (131) is attached to the surface of the upper wedge block (350).
9. The riverway slope matter source monitoring device according to claim 1, wherein a rib beam (311) is arranged on the water tower frame (310), and the rib beam (311) is fixed on the arc rail frame (320).
10. The riverway slope source monitoring device according to claim 1, wherein angle beams (111) are uniformly arranged on the buried pile frames (110).
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Citations (17)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JP2000056031A (en) * | 1998-08-07 | 2000-02-25 | Hokkaido Doshitsu Shiken Kyodo Kumiai | Method for predicting breakage of bedrock, slope, soil structure and civil engineering structure in advance |
JP2012032330A (en) * | 2010-08-02 | 2012-02-16 | Japan Health Science Foundation | Penetration type pipe strain meter |
CN104762922A (en) * | 2015-03-05 | 2015-07-08 | 四川大学 | Water-force-based method for treating debris flow by removing sediment source |
CN205333624U (en) * | 2016-01-28 | 2016-06-22 | 西南石油大学 | Mud -rock flow collection river physical simulation test device |
CN106501154A (en) * | 2016-11-16 | 2017-03-15 | 华北理工大学 | The experimental provision of simulation coating precipitation leakage and method |
CN106569287A (en) * | 2016-09-14 | 2017-04-19 | 中国石油化工股份有限公司 | Fan delta front reservoir prediction method based on composite sand body configuration model |
CN206448309U (en) * | 2016-12-30 | 2017-08-29 | 温州鸿浩建设有限公司 | River bottom mud dehydration device |
CN107656312A (en) * | 2017-10-12 | 2018-02-02 | 中国石油天然气集团公司 | Based on the channel sand prediction method and device for dividing azimuth to be superimposed |
US20180238012A1 (en) * | 2015-11-16 | 2018-08-23 | Maurice Garzon | Method for forming a stable foundation ground |
CN109797717A (en) * | 2019-01-21 | 2019-05-24 | 北京通成达水务建设有限公司 | The construction method for having subway tunnel is worn on a kind of river |
CN111984914A (en) * | 2020-08-17 | 2020-11-24 | 中国科学院、水利部成都山地灾害与环境研究所 | Method for measuring and calculating height of dam body of collapsing type damming dam and application |
JP2021085166A (en) * | 2019-11-26 | 2021-06-03 | 株式会社データ・トゥ | Double sheath pipe for drain pipe installation and installation method of non-excavation drain pipe |
CN113405769A (en) * | 2021-06-18 | 2021-09-17 | 中国科学院、水利部成都山地灾害与环境研究所 | Experimental device and experimental method for simulating complete process of superlift burst disaster of tillite lake |
CN114360214A (en) * | 2022-03-18 | 2022-04-15 | 四川省公路规划勘察设计研究院有限公司 | Extra-large scale glacier debris flow early warning method |
CN114723179A (en) * | 2022-05-24 | 2022-07-08 | 浙江省环境科技有限公司 | Water environment early warning traceability system and method based on water yield and water quality combined control |
CN115077479A (en) * | 2022-07-19 | 2022-09-20 | 航天智讯新能源(山东)有限公司 | Hydraulic engineering side slope settlement monitoring facilities |
CN115110491A (en) * | 2022-08-25 | 2022-09-27 | 四川省公路规划勘察设计研究院有限公司 | Alarming device for debris flow monitoring and early warning |
-
2022
- 2022-12-23 CN CN202211661354.1A patent/CN115638832B/en active Active
Patent Citations (17)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JP2000056031A (en) * | 1998-08-07 | 2000-02-25 | Hokkaido Doshitsu Shiken Kyodo Kumiai | Method for predicting breakage of bedrock, slope, soil structure and civil engineering structure in advance |
JP2012032330A (en) * | 2010-08-02 | 2012-02-16 | Japan Health Science Foundation | Penetration type pipe strain meter |
CN104762922A (en) * | 2015-03-05 | 2015-07-08 | 四川大学 | Water-force-based method for treating debris flow by removing sediment source |
US20180238012A1 (en) * | 2015-11-16 | 2018-08-23 | Maurice Garzon | Method for forming a stable foundation ground |
CN205333624U (en) * | 2016-01-28 | 2016-06-22 | 西南石油大学 | Mud -rock flow collection river physical simulation test device |
CN106569287A (en) * | 2016-09-14 | 2017-04-19 | 中国石油化工股份有限公司 | Fan delta front reservoir prediction method based on composite sand body configuration model |
CN106501154A (en) * | 2016-11-16 | 2017-03-15 | 华北理工大学 | The experimental provision of simulation coating precipitation leakage and method |
CN206448309U (en) * | 2016-12-30 | 2017-08-29 | 温州鸿浩建设有限公司 | River bottom mud dehydration device |
CN107656312A (en) * | 2017-10-12 | 2018-02-02 | 中国石油天然气集团公司 | Based on the channel sand prediction method and device for dividing azimuth to be superimposed |
CN109797717A (en) * | 2019-01-21 | 2019-05-24 | 北京通成达水务建设有限公司 | The construction method for having subway tunnel is worn on a kind of river |
JP2021085166A (en) * | 2019-11-26 | 2021-06-03 | 株式会社データ・トゥ | Double sheath pipe for drain pipe installation and installation method of non-excavation drain pipe |
CN111984914A (en) * | 2020-08-17 | 2020-11-24 | 中国科学院、水利部成都山地灾害与环境研究所 | Method for measuring and calculating height of dam body of collapsing type damming dam and application |
CN113405769A (en) * | 2021-06-18 | 2021-09-17 | 中国科学院、水利部成都山地灾害与环境研究所 | Experimental device and experimental method for simulating complete process of superlift burst disaster of tillite lake |
CN114360214A (en) * | 2022-03-18 | 2022-04-15 | 四川省公路规划勘察设计研究院有限公司 | Extra-large scale glacier debris flow early warning method |
CN114723179A (en) * | 2022-05-24 | 2022-07-08 | 浙江省环境科技有限公司 | Water environment early warning traceability system and method based on water yield and water quality combined control |
CN115077479A (en) * | 2022-07-19 | 2022-09-20 | 航天智讯新能源(山东)有限公司 | Hydraulic engineering side slope settlement monitoring facilities |
CN115110491A (en) * | 2022-08-25 | 2022-09-27 | 四川省公路规划勘察设计研究院有限公司 | Alarming device for debris flow monitoring and early warning |
Non-Patent Citations (1)
Title |
---|
付宴菊,江耀,王姣 * |
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