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204 results about "Surface velocity" patented technology

Methods and apparatus for intermittent rotary ultrasonic bonding system

This invention relates to apparatus and methods for intermittently bonding a substrate web in fabricating a blank subassembly for an absorbent article. The invention comprises ultrasonic bonding apparatus including an anvil roll, a substrate web thereon, and at least one rotary ultrasonic horn. The substrate web can comprise at least first and second layers of material. The rotary ultrasonic horn, in combination with the anvil roll, ultrasonically bonds intermittent segments of the first and second layers of the substrate web to each other. Such intermittent bonds can comprise end seals for the absorbent articles. The ultrasonic horn and anvil roll are periodically separated from each other to provide the intermittent bonding of the substrate web. An actuator apparatus periodically moves the anvil roll and ultrasonic horn from engaging contact with each other preventing bond formation. The actuator apparatus can include a cam mechanism moving one of the anvil roll and ultrasonic horn from engaging contact with the other during rotation of the rotary ultrasonic horn. The cam mechanism can create a physical gap between the ultrasonic horn and the anvil roll. The cam mechanism moves either the ultrasonic horn and the anvil roll toward the other of the ultrasonic horn and anvil roll at a velocity of no more than about 80 millimeters/second to prevent bounce or impact loading when the horn and anvil roll are in engaging contact. The anvil roll comprises a substrate-receiving surface generally moving the substrate web through the nip at a surface speed of at least 300 meters per minute. The ultrasonic system generally creates bonds between the first and second layers of the substrate web at least about 600 times per minute.
Owner:DUKANE IAS LLC

Near-surface modeling method using tomography inversion of two-step method

InactiveCN102590864ASolve detailed modeling challengesImprove image qualitySeismic signal processingGeophoneOffset distance
The invention relates to a near-surface modeling method using tomography inversion of a two-step method. The near-surface modeling method specifically comprises the following steps of: (1) picking and inputting short-refraction first-break; (2) carrying out tomography inversion on the short-refraction first-break and outputting explanation results capable of reflecting fine velocity change in an extremely shallow stratum as shown in picture 2; (3) picking a big shot and recording first-break time; (4) interpolating short-refraction inversion results in combination with explanation results of a microlog in a work area by using a kriging method and building near-surface velocity body of the extremely shadow stratum; (5) meshing and constraining inversion initial-velocity modeling, replacing a near-surface velocity body at the extremely shallow stratum obtained in the last step into the shallow stratum part of the initial model generated at the big-shot first-break, replenishing the velocity loss of the extremely shallow stratum resulting from the excessive minimum offset distance of the big shot; (6) constraining generation of a weight field; and (7) inversing the near-surface velocity model by using a constrained chromatography method, picking the top interface of a high-speed layer on the basis of a velocity-depth model obtained by tomography inversion, and calculating static correcting values of a shot point and a geophone position.
Owner:中国石油集团西北地质研究所有限公司

Method for establishing near-surface velocity model in high-density seismic static correction processing

ActiveCN101980054ASolve the statics problemReduce memory usageSeismic signal processingGeophoneHigh density
The invention belongs to seismic data processing in petroleum geophysical exploration and geological engineering survey, and relates to near-surface velocity modeling and static correction in seismic exploration aiming at research and development of a shallow velocity model required for combined post static correction in a detector chamber of single-point high-density seism. A method for establishing a near-surface velocity model in high-density seismic static correction processing comprises the following steps of: supposing that the near-surface velocity is linearly increased along with the depth, calculating refracted wave velocity of different geophone offset from the travel time difference of primary waves of adjacent detection points of the high-density seism according to the physical property of the primary wave of the near-surface velocity field, establishing a near-surface ramp velocity field parameter according to the relationship between the geophone offset and the refracted wave, and further establishing the near-surface velocity model which can be directly used for static correction quantity calculation in seismic processing and also can be used as an initial model for tomographic inversion of near-surface velocity. The method has high calculation speed, and does not depend on the change of the initial position caused by a seismic focus.
Owner:CHINA PETROLEUM & CHEM CORP +1

Direct prestack time migration method for three-dimensional seismic data acquired from irregular surfaces

The invention discloses a direct prestack time migration method for three-dimensional seismic data acquired from irregular surfaces, and the method is applied to the processing on reflected seismic information in seismic exploration. The method can be used for directly carrying out three-dimensional seismic data migration imaging (at different elevations) on shot points and geophone points acquired from irregular surfaces without statically correcting a processing process. In the method, no vertical emergence and incidence assumption is performed on nearsurface seismic wave propagation, therefore, the method can adapt to the situations which have no obvious low velocity region and velocity-reduction region such as high-velocity rock outcropping, and the like. In the method, the seismic wave propagation in near surfaces or stratums is described by using two equivalent speed parameters; and the two equivalent speed parameters can be determined according to the straightness of lineups inmigrated gathers, thereby avoiding the difficulties in near-surface velocity modeling. By using the method disclosed by the invention, the gathers subjected to migration can be subjected to remainingstatic correction, thereby effectively compensating the inherent errors existing in a land acquisition technology. The method has important application value in oil, gas and mineral resource exploration in complex surface areas.
Owner:INST OF GEOLOGY & GEOPHYSICS CHINESE ACAD OF SCI

Method for inverting near-surface velocity model by utilizing preliminary waveforms

The invention discloses a method for inverting a near-surface velocity model by utilizing preliminary waveforms. The method comprises acoustic wave equation-based wave field forward modeling and steepest descent-based waveform inversion technologies, and comprises the following steps of 1, extracting time-domain preliminary waveform records and an initial model; 2, calculating a simulated wave field and a wave field residual by utilizing acoustic wave equation staggered grid finite-difference forward modeling simulation; 3, reversely propagating the wave field residual to obtain a retransmission wave field; 4, calculating a gradient of a target function by utilizing the retransmission wave field and a forward propagation wave field, and calculating an updating step length; 5, updating a speed model; 6, inspecting whether the speed model is consistent with an iteration stopping condition, outputting the speed model if the speed model is consistent with the iteration stopping condition, otherwise returning to the step 2, and continuing iterative updating. According to the method, a wave equation theory-based full-waveform inversion technology is used as reference, and preliminary waves with higher energy and more stable waveforms are used for inversion, so that the multiplicity of solutions of full-waveform inversion is reduced, and the inversion stability and the calculation efficiency are improved; the accuracy of static correction and shallow depth imaging is improved.
Owner:中国石油集团西北地质研究所有限公司

Prestack depth migration method under condition of undulating surface

ActiveCN102890290AImproving Prestack Depth Migration AccuracyImprove image qualitySeismic signal processingHigh elevationImaging condition
The invention discloses a prestack depth migration method under a condition of an undulating surface. The prestack depth migration method under the condition of the undulating surface comprises the follows: a step 1 of filling a near-surface velocity between a reference surface and the undulating surface by regarding the highest elevation as a reference surface zbeg=0; a step 2 of adding a corresponding when the wave field zbeg=z=0 into an initial wave field providing that the initial reference surface zbeg=0; a step 3 of dividing the wave field in a range of a single-shot migration aperture into multiple small wave beam windows, converting the multiple wave beam windows to small wave beam regions, and respectively extending a downlink wave field and an uplink wave field to a depth z+deltaz along a depth direction; a step 4 of performing filtration treatnmetn on the extended wave fields; a step 5 of performing cross-correlation imaging by applying the downlink wave field and the uplink wave field based on the cross-correlation imaging condition to obtain an imaging result of the depth layer z+deltaz; a step 6 of judging if a wave field exists in the depth layer z+deltaz, if so, adding a corresponding wave field to the extended wave field to generate an initial extension wave field of the depth layer z+deltaz; and a step 7 of repeating the step 3 to step 6 and gradually extending and imaging until reaching a maximum depth layer zmax so as to obtain an imaging result of the single shot.
Owner:PETROCHINA CO LTD

Method and device for researching near-surface three-dimensional velocity field of physical geography

The invention provides a method and device for researching a near-surface three-dimensional velocity field of physical geography. The method comprises the steps of obtaining geological information of a research area according to the areal geology of the research area and research content; establishing a three-dimensional geological element conceptual model according to collected data; determining the preliminary survey position of a near-surface survey and a near-surface preliminary survey scheme, carrying out construction according to the determined preliminary survey position of the near-surface survey and the determined near-surface preliminary survey scheme, and obtaining site construction data; adjusting the three-dimensional geological element conceptual model according to the obtained site construction data until the geological elements in the three-dimensional geological element conceptual model are adaptive to wave velocity; establishing a geology and speed field model with the surficial geology coordinated with wave velocity layers on the basis of the three-dimensional geological element conceptual model with the geological elements adaptive to the wave velocity. According to the method and device for researching the near-surface three-dimensional velocity field of physical geography, the technical problem that in the prior art, a near-surface velocity model is not accurate is solved, and the effect of effectively improving the accuracy of the near-surface velocity model is achieved.
Owner:PETROCHINA CO LTD

Automatic lap changing winder

The invention provides an automatic lap changing winder which comprises a frame, a drawing mechanism, a cross cutting mechanism, an air expanding shaft assembly, a large roller synchronous winding mechanism, a turnover mechanism, a pressing claw mechanism and a swing arm mechanism. The automatic lap changing winder is characterized in that the linear surface velocity of the drawing mechanism is equal to that of a large roller when the drawing mechanism and the large roller synchronous winding mechanism are under the action of a main driving motor and a sprocket pair, rotatable air expanding shaft guide wheels are mounted at two ends of an air expanding shaft, guide rails are arranged on the frame, a U-shaped groove in a turnover seat can function in guiding, the air expanding shaft can linearly move in winding, a gear is fixed onto the turnover seat, the turnover seat is supported on the large roller and can turn over around the large roller, the pressing claw mechanism is arranged on the turnover seat to automatically change laps, an arc-shaped head is arranged above a swing arm, and the air expanding shaft guide wheels can be tightly pressed to realize winding and can also be pushed away to discharge coiled materials. The automatic lap changing winder is reasonable in structure and simple to operate, manual lap changing is omitted, continuous production of winding is realized, and production efficiency is improved.
Owner:JIANGSU KUNTAI MACHINERY

Non-contact flow measurement method for measuring high flood based on flow velocity of representative vertical line points

The invention discloses a non-contact flow measurement method for measuring a high flood based on the flow velocity of representative vertical line points. The method includes the following steps of (1) determining the positions of one or more vertical lines according to river section data, and using a radar flow velocity meter to measure the flow velocity of a river surface point below a measured vertical line; (2) calculating the flow velocities V1-Vp (the surface point flow velocity of P vertical lines) of the surface points of multiple vertical lines according to the surface point flow velocity of the measured vertical line; (3) conducting arithmetic average on the section surface point flow velocity of the multiple vertical lines, and obtaining the average flow velocity Vsur of the river surface; according to the empirical formula of hydraulics, making the average flow velocity of the river surface multiplied by the surface velocity coefficient lambda to obtain the average flow velocity Vave of the section; (4) according to the river section data, obtaining the river water passing section area corresponding to the set water depth, and making the area multiplied by the average flow velocity of the section to obtain a river flow value. The method can calculate the flow of artificial and natural rivers quickly, conveniently and accurately, and is especially suitable for unattended heavy rain, high flood and other complex disastrous environments.
Owner:HOHAI UNIV

NMR MAS inflow bernoulli bearing

An improved axial gas bearing for a gas-driven NMR MAS sample rotor is disclosed that utilizes inward flow with a low rotational component over a rotor conical end. A conical flow region is formed between the rotor conical end and a conical stator bearing surface such that the included angle defining the stator surface is not less than the included angle defining the rotor conical end. Gas is injected radially inward with a significant axial rearward component from a number of small holes at high velocity from the periphery into the conical flow region. Compared to the radial velocity components, the tangential flow components of the injected gas are small and preferably opposed to the direction of the rotor rotation. The high and accelerating negative radial velocities may result in significant Bernoulli effect, such that the mean axial pressure over the conical rotor end may be less than atmospheric pressure for a given axial clearance, but as the clearance decreases, the hydrostatic effects exceed the Bernoulli effects and the mean axial pressure over the conical rotor end may then exceed atmospheric pressure by a substantial amount. Thus, a self-stabilizing axial bearing is formed with improved stability and stiffness for rotor surface speeds up to at least 80% of the speed of sound. Motive power required to spin the rotor may be provided by a radial-inflow microturbine at the opposite end of the rotor in a way that is readily compatible with automatic sample change.
Owner:DOTY SCI

Seismic data processing method and device for keeping kinematics characteristics of seismic wave field

The invention provides a seismic data processing method and a device for keeping kinematics characteristics of a seismic wave field. The method comprises the steps as follows: carrying out inversion on a near-surface velocity model according to preliminary wave data; calculating matching static correction values of shot detection points according to fluctuation corresponding relation of the preliminary wave data and field measurement ground surface elevation; carrying out smoothing on the field measurement ground surface elevation and establishing a smooth ground surface elevation model; calculating corresponding terrain static correction values of the shot detection points when the field measurement ground elevation is changed into the smooth ground surface elevation, and combining the terrain static correction values of the shot detection points to carry out small disturbance time shifting processing on seismic data; embedding the near-surface velocity model into a whole velocity model to obtain a shallow velocity model; carrying out depth domain medium-deep velocity modeling based on the smooth ground surface elevation model and the shallow velocity model; establishing a new common imaging point or a common reflection angle set; establishing iteration of the common imaging point or the common reflection angle set to obtain the whole velocity model including shallow and medium-deep velocities; and carrying out prestack depth migration imaging through a prestack depth migration algorithm from the smooth ground surface elevation.
Owner:PETROCHINA CO LTD
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