CN206627477U - Low-and high-frequency sediment parameter measurement instrument - Google Patents

Low-and high-frequency sediment parameter measurement instrument Download PDF

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Publication number
CN206627477U
CN206627477U CN201720195232.6U CN201720195232U CN206627477U CN 206627477 U CN206627477 U CN 206627477U CN 201720195232 U CN201720195232 U CN 201720195232U CN 206627477 U CN206627477 U CN 206627477U
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low
frequency
module
measuring instrument
parameter measurement
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CN201720195232.6U
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韩宝坤
卢涛
秦敏
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Shandong University of Science and Technology
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Shandong University of Science and Technology
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Abstract

The utility model discloses a kind of low-and high-frequency sediment parameter measurement instrument, including measuring instrument body and host computer, the top of the measuring instrument body is provided with release binding mechanism, and the bottom of measuring instrument body is provided with pressure switch, underwater sound acoustic velocity measutement module, reflecting plate, high frequency transceiver transducer and low frequency transceiver transducer;Processor circuit plate module, wire and velocity sensor are provided with measuring instrument body, data storage cell is provided with processor circuit plate module, pressure switch, underwater sound acoustic velocity measutement module, high frequency transceiver transducer, low frequency transceiver transducer and velocity sensor are connected by wire with processor circuit plate module respectively, data storage cell completes data transfer by wireline cable or radio communication with host computer, and host computer internal memory contains ground acoustic model storehouse.The continuity of gathered data can be realized using the utility model, improves the accuracy of measurement.

Description

Low-and high-frequency sediment parameter measurement instrument
Technical field
The utility model belongs to sediment Research of Acoustic technical field, more particularly to a kind of low-and high-frequency sediment Parameter measurement instrument.
Background technology
In the means for the various detection oceans that the mankind have grasped, acoustic method is still one and most effectively detects hand Section.The lower boundary that seabed is propagated in the seawater as sound wave, the influence to sound field is huge, therefore, understands and obtains sediment Acoustic characteristic be solve underwateracoustic propagation problem key factor.
Current more methods using remote sensing obtain the topography and geomorphology and sediment parameter in seabed, but remote sensing technology obtains Data be historical data, the data not measured in real time are significant and convincingness.Currently to the real-time survey of sediment parameter Amount is usually to use submarine sampling, and is measured in laboratory, and lab measurements are then adapted to in-site measurement value Method.The sample length of wherein submarine sampling is usually no more than 30cm, and is typically obtained using gravity core, and as much as possible Reduce error caused by sampling disturbance.There are many shortcomings in this method measured in real time, for example, the company in seabed can not be obtained Continuous data, the data of discrete point can only be obtained;Sample is easily washed away by seawater and loses original appearance, while is lost original Pressure, the environmental condition such as temperature;This method wastes time and energy, and is limited by sea conditions, (the Ru Huagang when sediment is very hard Rock and basalt substrate) it is not easy to obtain sample.
As can be seen here, prior art is up for further improving.
Utility model content
The utility model is to avoid above-mentioned the shortcomings of the prior art part, there is provided a kind of low-and high-frequency sediment ginseng Number measuring instrument, to realize the continuity of gathered data, improves the accuracy of measurement.
Technical scheme is used by the utility model:
Low-and high-frequency sediment parameter measurement instrument, including measuring instrument body and host computer, the top of the measuring instrument body Release binding mechanism is provided with, the bottom of measuring instrument body is provided with pressure switch, underwater sound acoustic velocity measutement module, reflecting plate, height Frequency transceiver transducer and low frequency transceiver transducer, underwater sound acoustic velocity measutement module are used to launch and receive sound wave, instead Penetrate plate be used for reflect from underwater sound acoustic velocity measutement module sound wave, high frequency transceiver transducer is for launching high frequency sound wave and connect High frequency sound wave of the reflection from substrate is received, low frequency transceiver transducer is used to launch low-frequency sound wave and receives reflection from the low of substrate Frequency sound wave;Processor circuit plate module, wire and velocity sensor are provided with measuring instrument body, in processor circuit plate module It is provided with data storage cell, pressure switch, underwater sound acoustic velocity measutement module, high frequency transceiver transducer, low frequency transceiver Transducer and velocity sensor are connected by wire with processor circuit plate module respectively, and data storage cell passes through wired line Cable or radio communication complete data transfer with host computer, and host computer internal memory contains ground acoustic model storehouse.
The low-and high-frequency sediment parameter measurement instrument is recovery type low-and high-frequency sediment parameter measurement instrument, the recovery type Low-and high-frequency sediment parameter measurement instrument includes ship and the spooling gear being arranged on ship, and the release binding mechanism passes through Hawser is connected with spooling gear.
The low-and high-frequency sediment parameter measurement instrument is deserted low-and high-frequency sediment parameter measurement instrument, and this is deserted Low-and high-frequency sediment parameter measurement instrument includes floating body, and floating body is connected with release binding mechanism, and data are provided with the floating body Memory module, data memory module and processor circuit plate module communicate to connect, and data memory module by wireline cable with Host computer completes data transfer.
Battery module is additionally provided with the measuring instrument body, the processor circuit plate module is connected with battery module.
The bottom of the measuring instrument body is additionally provided with polylith skirtboard.
The release binding mechanism includes the release, motor and the underwater acoustic transducer that are sequentially connected, motor respectively with release Device, underwater acoustic transducer are connected, and underwater acoustic transducer is connected with processor circuit plate module, the action of motor control release.
The top of the measuring instrument body is additionally provided with external cabling mouth, and external cabling mouth passes through wire and processor circuit Plate module is connected, and measuring instrument body completes the order between host computer or the transmission of data by external cabling port transmission.
Bluetooth module is additionally provided with the measuring instrument body, bluetooth module passes through wire and the processor circuit template die Block is connected, and measuring instrument body completes the order between host computer or the biography of data by bluetooth module wireless communication transmission It is defeated.
Ground acoustic model storehouse in the host computer includes Hamilton viscoelastic modes, Biot-stoll models, Buckingham VGS models and Chotiros-Isakson BICSQS models.
By adopting the above-described technical solution, having the beneficial effect that acquired by the utility model:
1st, each parameter of sediment in tested marine site can be measured in real time using the utility model, overcome traditional remote sensing The shortcomings that measurement and collection sediment sample method and deficiency, can obtain the continuous data in seabed, obtain continuous data, Reliability is high.
2nd, the measuring instrument body in the utility model can both calculate the base of sediment in real time according to the data measured This parameter, the data collected can also be imported in host computer the analysis and processing for carrying out data, obtained at careful analysis Manage result and more vivid visual image result.
3rd, the utility model occupation mode is flexible and changeable, can use recovery type or use deserted, Ke Yiman The various demands of sufficient different application.
4th, the utility model uses two kinds of communication functions, to meet the needs of different.In recovery type occupation mode, both may be used So that by there is cable connection, the transmission of data and order can also be carried out by bluetooth connection host computer and measuring instrument body;Throwing When abandoning formula occupation mode, measuring instrument body can cable connects measuring instrument body and floating body carries out data transmission by having.This practicality New communication function fully meet it is various under the conditions of use demand.
5th, the host computer in the utility model is powerful, can utilize existing ground acoustic mode according to the data that measurement obtains Type carries out the analysis and processing of data, can also be according to actual conditions from the analysis for editing ground acoustic model or formula progress data Reason, finally export man-machine interface interactivity preferably visualization result.
Brief description of the drawings
Fig. 1 is the structure diagram of measuring instrument body in the utility model.
Fig. 2 is the structure letter of recovery type low-and high-frequency sediment parameter measurement instrument (removing host computer) in the utility model Figure.
Fig. 3 is the structure letter of deserted low-and high-frequency sediment parameter measurement instrument (removing host computer) in the utility model Figure.
Fig. 4 is that sediment parameter is measured using the low-and high-frequency sediment parameter measurement instrument in the utility model Schematic diagram.
Wherein,
1st, measuring instrument body 2, external cabling mouth 3, wire 4, release binding mechanism 5, motor 6, underwater acoustic transducer 7th, processor circuit plate module 8, battery module 9, underwater sound acoustic velocity measutement module 10, reflecting plate 11, bluetooth communication module 12nd, pressure switch 13, high frequency transceiver transducer 14, low frequency transceiver transducer 15, skirtboard 16, spooling gear 17th, hawser 18, fixed pulley 19, wheel disc 20, fixed support 21, floating body 22, data memory module
Embodiment
The utility model is described in further detail with specific embodiment below in conjunction with the accompanying drawings, but the utility model It is not limited to these embodiments.
As shown in figure 1, low-and high-frequency sediment parameter measurement instrument, including measuring instrument body 1 and host computer, the measuring instrument The top of body 1 is provided with release binding mechanism 4.It is described release binding mechanism 4 include be sequentially connected release, motor 5 and Underwater acoustic transducer 6, motor 5 are connected with release, underwater acoustic transducer 6 respectively, underwater acoustic transducer 6 and following processor circuit template dies Block 7 is connected, the action of the control release device of motor 5.
The bottom of the measuring instrument body 1 is provided with pressure switch 12, underwater sound acoustic velocity measutement module 9, reflecting plate 10, high frequency Transceiver transducer 13 and low frequency transceiver transducer 14, underwater sound acoustic velocity measutement module 9 are used to launch and receive sound wave, Reflecting plate 10 is used to reflect the sound wave from underwater sound acoustic velocity measutement module 9, and high frequency transceiver transducer 13 is used to launch high frequency Sound wave simultaneously receives high frequency sound wave of the reflection from substrate, and low frequency transceiver ring energy device 14 is used to launch low-frequency sound wave and receives reflection From the low-frequency sound wave of substrate.
The high frequency transceiver transducer 13 is in same height with low frequency transceiver transducer 14 on locus Opening position is spent, i.e., both are equal apart from the vertical range of each layer substrate in seabed.
Processor circuit plate module 7, wire 3 and velocity sensor, processor circuit are provided with the measuring instrument body 1 Data storage cell, pressure switch 12, underwater sound acoustic velocity measutement module 9, high frequency transceiver transducer are provided with plate module 7 13rd, low frequency transceiver transducer 14 and velocity sensor are connected by wire 3 with processor circuit plate module 7 respectively, number Data transfer is completed with host computer by wireline cable or radio communication according to memory cell.
Battery module 8, the processor circuit plate module 7 and the phase of battery module 8 are additionally provided with the measuring instrument body 1 Even.
The top of the measuring instrument body 1 is additionally provided with external cabling mouth 2, and external cabling mouth 2 passes through wire 3 and processor Circuit board module 7 is connected, and measuring instrument body 1 is transmitted order or data between host computer by external cabling mouth 2 Transmission.
In addition, being additionally provided with bluetooth module 11 in the measuring instrument body 1, bluetooth module 11 passes through wire 3 and the place Manage device circuit board module 7 to be connected, measuring instrument body 1 is transmitted order or number between host computer by bluetooth module 11 According to transmission.
The bottom of the measuring instrument body 1 is additionally provided with polylith skirtboard 15, to ensure the center of gravity of whole measuring instrument body 1 Downwards.
The host computer internal memory contains ground acoustic model storehouse.Ground acoustic model storehouse in the host computer includes Hamilton viscoelastics Model, Biot-stoll models, Buckingham VGS models and Chotiros-Isakson BICSQS models.
On the earth's crust in seabed, the sedimentary of one layer or the non-nodule state of multilayer, seawater and submarine sedimentary strata are covered with Interface shows, generally, shallow sea continental shelf belongs to the high velocity of sound there is a seabed interface according to existing historical data Seabed (the substrate velocity of sound>Sound velocity in seawater), absmal deposit layer belongs to fast seabed (the substrate velocity of sound in a low voice<Sound velocity in seawater).
The utility model is using propagation attenuation of the acoustic propagation in measurement process and passes through experiment or historical data determines Acoustic propagation decay and substrate composition correspond to form, to calculate analysis sediment parameter, (substrate composition forms and substrate layer It is thick), and can import data in host computer and utilize existing ripe ground acoustic model or user can be according to actual measurement The situation in marine site is come to carry out further refinement analysis to sediment and delamination from editor's self-defined ground acoustic model or formula Processing, and show visual result.Wherein, high frequency transceiver transducer 13 is together with removing low frequency transceiver in measuring instrument Each part beyond transducer 14 together, mainly carries out accurately measurement (height to several meters of the superiors of deposit in sediment Frequency is decayed seriously, the main upper strata for measuring sediment layering).Low frequency transceiver transducer 14 removes high frequency together with measuring instrument Together, substantially measurement is carried out to sediment, and (low cut is slow, and fathom ratio for each part beyond transceiver transducer 13 High frequency is deep).
As shown in Fig. 2 Fig. 2 shows one of embodiment of the present utility model, the low-and high-frequency seabed in the embodiment Substrate parameter measurement instrument is recovery type low-and high-frequency sediment parameter measurement instrument, the recovery type low-and high-frequency sediment parameter measurement Instrument includes ship and the spooling gear 16 being arranged on ship, and the release binding mechanism 4 passes through hawser 17 and spooling gear 16 It is connected.
The spooling gear 16 includes hawser 17, fixed pulley 18, wheel disc 19 and for wheel disc 19 to be fixed on ship Whole spooling gear 16 is fixed on ship by fixed support 20, fixed support 20.Release binding mechanism 4 is connected with hawser 17, Changed course of the hawser 17 successively through multiple fixed pulleys 18 carries out the folding and unfolding of hawser 17 by wheel disc 19, wheel disc 19 is logical around to wheel disc 19 Cross folding and unfolding hawser 17 and control fathoming for measuring instrument body.
In use, measuring instrument body 1 is connected on ship by spooling gear 16, measuring instrument body 1 is discharged into and leaned on Near Sea Bottom it is underwater, after pressure switch 12 bears certain pressure under water, pressure switch 12 is opened, measuring instrument body 1 start into Row measurement, measuring instrument body 1 move with ship, the sediment parameter below surveying vessel ship motion and record data.Survey After amount terminates, measuring instrument body 1 is withdrawn by spooling gear 16, measuring instrument body 1 is passed through into wire cable or wireless blue tooth Transmit data, import data in host computer using or be further processed.
As shown in figure 3, Fig. 3 shows another embodiment of the present utility model, the low-and high-frequency seabed in the embodiment Substrate parameter measurement instrument is deserted low-and high-frequency sediment parameter measurement instrument, the deserted low-and high-frequency sediment parameter measurement Instrument includes floating body 21, and floating body 21 is connected with release binding mechanism 4, and data memory module 22, data are provided with the floating body 21 Memory module 22 communicates to connect with processor circuit plate module 7, and data memory module 22 is complete with host computer by wireline cable Into data transfer.
The deserted low-and high-frequency sediment parameter measurement instrument is mainly severe in sea conditions, can not complete measuring instrument sheet Used during the recovery operation of body 1, measuring instrument body 1 can coordinate floating body 21 to carry out deserted effect.
In use, the floating body 21 with data memory module 22 is connected to measuring instrument body 1 by discharging binding mechanism 4 On, and row data communication is entered by the external cabling mouth 2 of wire cable connection floating body 21 and measuring instrument body 1.In application process, Directly the measuring instrument body 1 with floating body 21 can be put into the sea area for needing to measure, measuring instrument body 1 sinks, Pressure switch 12 is opened in the presence of outside static pressure, when velocity sensor detects that the subsidence velocity of measuring instrument body 1 is When zero, it may be determined that measuring instrument body 1 bottoms out, and measuring instrument body 1 starts measurement and the data for recording completion are passed through into wired line Cable is transferred in the data memory module 22 of floating body 21, and triggering release binding mechanism 4 discharges floating body 21, floating body 21 after being transmitted Rise in the presence of buoyancy, and depart from the external cabling mouth 2 on measuring instrument body 1, floating body 21 is risen to after sea, is made User can set by color eye-catching on floating body 21 (being easily at sea found as red) or on floating body 21 and can dodge Bright warning lamp is timely salvaged to floating body 21.Floating body 21 can be connected upper by wireline cable after the completion of salvaging Machine, the data collected are imported in host computer to the analyzing and processing for using or carrying out next step.
As shown in figure 4, below to being surveyed using the low-and high-frequency sediment parameter in the utility model by taking Tipple Bottom matter as an example The substantially process of amount instrument measurement sediment parameter illustrates:
One is established as shown in following table by historical data or experimental data, marine field propagation loss TL, The corresponding table of substrate composition and substrate velocity of sound cpr, each substrate composition in ocean, the historical data or experiment number are determined to follow-up It is customized from editing according to the situation that can measure marine site according to reality by existing ground acoustic model in host computer or user Ground acoustic model or formula are analyzed and processed to obtain to sediment composition.
Bottom type rho cpr cpi csr csi TL
Mud 1.4 0.99*Cw -0.002*Cw 0.1*cpr -0.004*Cw -0.006*Cw
It is husky 2.0 1.2*Cw -0.005*Cw 0.3*cpr -0.07*Cw -0.075*Cw
Limestone 2.4 2.7*Cw -0.004*Cw 0.6*cpr -0.003*Cw -0.007*Cw
Basalt 2.7 3.4*Cw -0.006*Cw 0.6*cpr -0.006*Cw -0.012*Cw
Certainly, there is density ratio rho (rhos of the propagation loss TL with corresponding substrate composition in above-mentioned corresponding table>0), squeeze Pressure decay cpi is (meter per second, cpi<0) speed of sound csr (meter per second, csr, are sheared>0, typically<0.6), shearing decay csi (meter per second, csi<0) corresponding relation between, so as to which after each layer substrate composition is subsequently determined, each layer substrate can be obtained by tabling look-up Relevant parameter.
Measuring instrument body 1 is put into marine site to be measured, pressure switch 12 is opened in the presence of outside static pressure under water, when When the subsidence velocity for the measuring instrument body 1 that velocity sensor detects is zero, measuring instrument body 1 starts measurement and record data.
Using time leap technology measurement underwater sound velocity of sound Cw, i.e. matching somebody with somebody using underwater sound acoustic velocity measutement module 9 and reflecting plate 10 Close measurement velocity of sound Cw, calculation formula is:
Wherein, LWater is surveyedThe distance between refer to from underwater sound acoustic velocity measutement module 9 to reflecting plate 10, tWater is surveyedRefer to from the underwater sound Acoustic velocity measutement module 9 sends sound wave and started to the time for receiving reflecting plate 10 for the first time and reflecting sound wave.
The distance between the upper interface of high and low frequency transceiver transducer and first layer substrate L0 waterCalculating:Because high and low The distance between upper interface of frequency transceiver transducer and first layer substrate is not very big, so the propagation in the segment distance Loss is ignored, L0 waterCalculation formula be:
L0 water=(Cw×t0 water)/2
Wherein, CwFor the above-mentioned velocity of sound measured, t0 waterFor high frequency transceiver transducer 13 or low frequency transceiver transducing Device 14 is from sound wave is sent to the time for receiving the sound wave returned by the upper bound surface launching of first layer substrate for the first time.
The determination of first layer substrate composition:The sound source level intensity sent from high and low frequency transceiver transducer is Xdb, sound Ripple is from being issued to through first layer substrate upper surface, run into original route after first layer substrate lower surface and return to high and low frequency transmitting-receiving Integral transducer, the intensity received are Y1Db, then the propagation loss TL in first layer substrate1=(X-Y1)/2, calculate propagation Lose TL1Afterwards, first layer substrate is determined according to above-mentioned propagation loss TL, substrate composition and the substrate velocity of sound cpr corresponding table Composition, and obtain the substrate velocity of sound cpr of first layer substrate1 bottom
Assuming that the propagation loss TL being calculated1For -0.006Cw+ threshold value≤TL1≤-0.006Cw- threshold value, according to above-mentioned Form can determine that first layer substrate composition is mud, corresponding substrate velocity of sound cpr1 bottomFor 0.99Cw
The principle that above-mentioned substrate composition determines is:According to sonar equation SL-2TL+TS-NL+DI=DT, wherein, SL is Sound source level (is launched, therefore known to its intensity) by high and low frequency transceiver transducer, and TS- target strengths (are ignored), NL- noises Level (ignoring), DI- receive directive property (ignoring), and DT refers to the detection that high and low frequency transceiver transducer n-th receives direct wave Value.Therefore above-mentioned sonar equation can be reduced to:SL-2TL=DT, so as to obtain
The calculating of first layer substrate thickness:The distance between interface and lower interface are L on first layer substrate1 bottom, i.e. first layer The thickness of substrate is L1 bottom, in measurement high and low frequency transceiver transducer to the distance at interface under first layer substrate be L0 water+L1 bottom, Then have:
Wherein, t1 bottomFor high and low frequency transceiver transducer receive from sound wave is sent, pass through first layer substrate to sound wave Upper interface, to the time for running into interface under first layer substrate and being reflected back high and low frequency transceiver transducer.
The determination of second layer substrate composition:The sound source level intensity sent from high and low frequency transceiver transducer is Xdb, sound Ripple continues across interface on the second layer from being issued to through first layer substrate upper surface, lower interface, runs into second layer substrate following table Original route returns to high and low frequency transceiver transducer after face, and the intensity received is Y2Db, the then propagation in second layer substrate LossCalculate propagation loss TL in the second layer2Afterwards, according to above-mentioned propagation loss TL, substrate composition with And substrate velocity of sound cpr corresponding table determines the composition of second layer substrate, and obtain the substrate velocity of sound cpr of second layer substrate2 bottoms
Assuming that the propagation loss TL being calculated2For -0.075Cw+ threshold value≤TL2≤-0.075Cw- threshold value, according to above-mentioned Form can determine second layer substrate composition for sand, corresponding second layer substrate velocity of sound cpr2 bottomsFor 1.2Cw
The calculating of second layer substrate thickness:The distance between interface and lower interface are L on second layer substrate2 bottoms, i.e. the second layer Substrate thickness is L2 bottoms, in measurement high and low frequency transceiver transducer to the distance at interface under second layer substrate be L0 water+L1 bottom+ L2 bottoms, then have:
Wherein, t2 bottomsFor high and low frequency transceiver transducer receive from sound wave is sent, pass through first layer substrate to sound wave Interface under upper interface, first layer substrate, interface on second layer substrate, run into interface original route under second layer substrate be reflected back it is high, The time of low frequency transceiver transducer.
The determination of third layer substrate composition:The sound source level intensity sent from high and low frequency transceiver transducer is Xdb, sound Ripple interface, lower interface on second layer substrate, continues across third layer from being issued to through first layer substrate upper surface, lower interface Interface on substrate, original route returns to high and low frequency transceiver transducer after running into third layer substrate lower surface, and what is received is strong Spend for Y3Db, the then propagation loss in third layer substrateCalculate propagation loss in third layer TL3Afterwards, the composition of third layer substrate is determined according to above-mentioned propagation loss TL, substrate composition and the substrate velocity of sound cpr corresponding table, And obtain the substrate velocity of sound cpr of third layer substrate3 bottoms
Assuming that the propagation loss TL being calculated3For -0.007Cw+ threshold value≤TL2≤-0.007Cw- threshold value, according to above-mentioned Form can determine that third layer substrate composition is limestone, corresponding third layer substrate velocity of sound cpr3 bottomsFor 2.7Cw
The calculating of third layer substrate thickness:The distance between interface and lower interface are L on third layer substrate3 bottoms, i.e. third layer Substrate thickness is L3 bottoms, in measurement high and low frequency transceiver transducer to the distance at interface under third layer substrate be L0 water+L1 bottom+ L2 bottoms+L3 bottoms, then have:
Wherein, t3 bottomsFor high and low frequency transceiver transducer receive from sound wave is sent, pass through first layer substrate to sound wave Interface under upper interface, first layer substrate, interface under interface, second of substrate, interface on third layer substrate on second layer substrate, meet The time of high and low frequency transceiver transducer is reflected back to interface original route under third layer substrate.
Only the composition of Tipple Bottom matter is determined for said process and thickness is enumerated, certainly, the utility model and not only The calculating of Tipple Bottom matter is limited only to, can also be four layers, five layers, six layers ... N layers.
The determination of n-th layer substrate composition:The sound source level intensity sent from high and low frequency transceiver transducer is Xdb, sound wave From being issued to through interface, lower interface ... on first layer substrate upper surface, lower interface, second layer substrate up through n-th layer Upper interface, original route returns to high and low frequency transceiver transducer after running into n-th layer substrate lower surface, and the intensity received is YnDb, the then propagation loss in n-th layer substrateCalculate propagation loss TLnAfterwards, the composition of n-th layer substrate is determined according to above-mentioned propagation loss TL, substrate composition and the substrate velocity of sound cpr corresponding table, And obtain the substrate velocity of sound cpr of n-th layer substrateN bottoms
The calculating of n-th layer substrate thickness:The distance between interface and lower interface are L on n-th layer substrateN bottoms, i.e. n-th layer bottom Matter thickness is LN bottoms, in measurement high and low frequency transceiver transducer to the distance at interface under n-th layer substrate be L0 water+L1 bottom+L2 bottoms +…+LN bottoms, then have:
Wherein, tN-1 bottomsFor high and low frequency transceiver transducer receive from sound wave is sent, pass through first layer substrate to sound wave Interface under upper interface, first layer substrate, interface on the N-1 layer substrates of interface ... on second layer substrate, run into N-1 layer substrates Lower interface original route is reflected back the time of high and low frequency transceiver transducer;tN bottomsReceived for high and low frequency transceiver transducer From sending sound wave, to sound wave through interface ... on interface under interface, first layer substrate on first layer substrate, second layer substrate Interface on N layer substrates, run into the time that interface original route under n-th layer substrate is reflected back high and low frequency transceiver transducer.
The part do not addressed in the utility model uses or used for reference prior art and can be achieved.
Specific embodiment described herein is only to spiritual example explanation of the present utility model.This practicality New person of ordinary skill in the field can make various modifications or supplement or adopt to described specific embodiment Substituted with similar mode, but without departing from spirit of the present utility model or surmount model defined in appended claims Enclose.

Claims (9)

1. low-and high-frequency sediment parameter measurement instrument, it is characterised in that including measuring instrument body and host computer, the measuring instrument sheet The top of body is provided with release binding mechanism, and the bottom of measuring instrument body is provided with pressure switch, underwater sound acoustic velocity measutement module, anti- Plate, high frequency transceiver transducer and low frequency transceiver transducer are penetrated, underwater sound acoustic velocity measutement module is used to launch and receive Sound wave, reflecting plate are used to reflect the sound wave from underwater sound acoustic velocity measutement module, and high frequency transceiver transducer is used to launch high frequency Sound wave simultaneously receives high frequency sound wave of the reflection from seabed different layers substrate, and low frequency transceiver transducer is used to launch low-frequency sound wave simultaneously Receive low-frequency sound wave of the reflection from seabed different layers substrate;Be provided with measuring instrument body processor circuit plate module, wire and Velocity sensor, data storage cell, pressure switch, underwater sound acoustic velocity measutement module, height are provided with processor circuit plate module Frequency transceiver transducer, low frequency transceiver transducer and velocity sensor pass through wire and processor circuit template die respectively Block is connected, and data storage cell completes data transfer by wireline cable or radio communication with host computer, and host computer internal memory contains A variety of ground acoustic model.
2. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that low-and high-frequency seabed bottom Matter parameter measurement instrument is recovery type low-and high-frequency sediment parameter measurement instrument, the recovery type low-and high-frequency sediment parameter measurement instrument Including ship and the spooling gear being arranged on ship, the release binding mechanism is connected by hawser with spooling gear.
3. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that low-and high-frequency seabed bottom Matter parameter measurement instrument is deserted low-and high-frequency sediment parameter measurement instrument, the deserted low-and high-frequency sediment parameter measurement instrument Including floating body, floating body is connected with release binding mechanism, and data memory module, data memory module and place are provided with the floating body The communication connection of device circuit board module is managed, and data memory module completes data transfer by wireline cable and host computer.
4. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that in the measuring instrument body Battery module is additionally provided with, the processor circuit plate module is connected with battery module.
5. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that the measuring instrument body Bottom is additionally provided with polylith skirtboard.
6. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that the release binding mechanism Including the release, motor and underwater acoustic transducer being sequentially connected, motor is connected with release, underwater acoustic transducer respectively, and the underwater sound changes Energy device is connected with processor circuit plate module, the action of motor control release.
7. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that the measuring instrument body Top is additionally provided with external cabling mouth, and external cabling mouth is connected by wire with processor circuit plate module, and measuring instrument body leads to Cross external cabling port transmission and complete the order between host computer or the transmission of data.
8. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that in the measuring instrument body Bluetooth module is additionally provided with, bluetooth module is connected by wire with the processor circuit plate module, and measuring instrument body passes through indigo plant Tooth module wireless communication transmission completes the order between host computer or the transmission of data.
9. low-and high-frequency sediment parameter measurement instrument according to claim 1, it is characterised in that the ground in the host computer Acoustic model includes Hamilton viscoelastic modes, Biot-stoll models, Buckingham VGS models and Chotiros- IsaksonBICSQS models.
CN201720195232.6U 2017-03-02 2017-03-02 Low-and high-frequency sediment parameter measurement instrument Expired - Fee Related CN206627477U (en)

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CN113588797A (en) * 2020-04-30 2021-11-02 中国石油化工股份有限公司 Shaft salt deposition monitoring device and method for gas storage
CN115598217A (en) * 2022-12-13 2023-01-13 自然资源部第二海洋研究所(Cn) Device and method for in-situ measurement of low-frequency acoustic characteristics of seabed sediment layer

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* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN113588797A (en) * 2020-04-30 2021-11-02 中国石油化工股份有限公司 Shaft salt deposition monitoring device and method for gas storage
CN115598217A (en) * 2022-12-13 2023-01-13 自然资源部第二海洋研究所(Cn) Device and method for in-situ measurement of low-frequency acoustic characteristics of seabed sediment layer
CN115598217B (en) * 2022-12-13 2023-03-31 自然资源部第二海洋研究所 Device and method for in-situ measurement of low-frequency acoustic characteristics of seabed sediment layer

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