| 序号 | 专利名 | 申请号 | 申请日 | 公开（公告）号 | 公开（公告）日 | 发明人 |
|---|---|---|---|---|---|---|
| 21 | Wind Detector Devices and Methods of Detecting Wind | US12718287 | 2010-03-05 | US20100224119A1 | 2010-09-09 | Duane Sheldon Morris |
| This invention is directed to an exemplary wind detector device. The device includes a container having an interior and a nozzle in fluid communication with the interior. The device further includes powder in the interior of the container and a strip of material having first and second ends. The first end is secured to the container and the second end is configured to be secured to a support structure such as clothing. | ||||||
| 22 | Display fountain, system, array and wind detector | US10537273 | 2003-11-26 | US07735749B2 | 2010-06-15 | John Tippetts |
| A fountain (50) comprises a supply of water under pressure, a primary fluidic diverter (10) having an input (12) for said supply, and first and second outputs (16a, b) diverging from said input. Two control ports (20a, b) are provided with control flow to direct input flow to one or other of the two outputs that lead to the two inputs of a vortex amplifier (40). This comprises a vortex chamber (54), a radial port (50), a vortex inducing port (60) and an axial output port (58). One (16a) of the diverter outputs is connected to the vortex inducing port, the other (16b) to the radial port, so that supply to said axial output port is modulated by formation of a vortex in the chamber when flow is to the vortex inducing port. The axial port leads to a nozzle whereby a vortex spray or axial jet is produced, depending on which diverter output (16a, b) is active. A wind detector (100) has a vertical jet (102) and a catcher (104) which fails to catch water from the jet in high wind conditions. The catcher feeds the control port (20a) of a diverter 101, or such other pressure or flow detector as may be convenient. A fountain array of elements may comprise a number of diverters, the outputs of which have branches supplying the control ports of others in the array, whereby internal control is provided. | ||||||
| 23 | Method for measuring the flow of fluids | US708906 | 1996-09-05 | US6118519A | 2000-09-12 | Masamichi Ipponmatsu; Masashi Nishigaki; Akira Hirano; Tsuyoshi Nakajima; Yuji Ikeda; Minoru Suzuki; Tsuyoshi Tsurutani |
| The disclosed method of measuring the flow of a fluid with a porous particulate ceramic tracer and an optical instrument is characterized in that spherical particles having diameters in the range of 0.5 to 150 .mu.m are used as the tracer. Inasmuch as the tracer particles for flow measurement are spherical, the sectional area of scattered light to be detected by an optical sensor means is constant regardless of the orientation of particles. Furthermore, spherical particles have no surface irregularities that might cause concatenation so that individual particles are not agglomerated in tracking a fluid flow, thus contributing to improved measurement accuracy. | ||||||
| 24 | Method and apparatus for measuring flow-speed of gases | US42663073 | 1973-12-12 | US3875797A | 1975-04-08 | ZWENG JOSEF |
| A main stream of gas is advanced in the path, and an auxiliary stream of gas is directed across the path from one to an opposite side thereof where it impinges against a pair of separated apertures which are spaced from one another in the direction of elongation of the path. This creates differential pressures in the apertures since the auxiliary stream is deflected to some extent by the main stream and does not uniformly impinge upon both apertures. The differential pressures are measured and the auxiliary stream is moved longitudinally of the path until the pressures created in both of the apertures are identical. The extent to which the auxiliary stream has had to be moved in order to produce uniform pressure in both of the apertures is an indicator of the flow speed of the main stream.
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| 25 | Fluid flow measuring device | US3785206D | 1972-04-26 | US3785206A | 1974-01-15 | BENSON J; BAKER W |
| Apparatus for measuring the velocity of fluid flow includes a form of pitot tube having orifices that develop a differential pressure related to the stream velocity and a means of directing an auxiliary stream of gas at or near one of the orifices. The auxiliary stream is arranged to be deflected by the main stream so that in the range of low velocities of the main stream, wherein pitot tubes are insensitive, the sensitivity of the apparatus is enhanced. In a preferred form of the device, a purged thermal flowmeter connected to the two orifices senses the velocity of the main stream.
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| 26 | Air momentum anemometer | US3719079D | 1971-04-05 | US3719079A | 1973-03-06 | HOWELL W |
| A device for the measurement of horizontal wind velocity, especially low wind velocity. The horizontal component of momentum of the airstream is displaced from its normal flow. This is accomplished by either injecting an air jet into the airstream to displace the horizontal component of momentum, or withdrawing from the airstream the horizontal component of momentum by passing the airstream over an inlet into which inlet is drawn the horizontal component of the momentum flux of the airstream. The momentum of the air is converted to a force which is thus sensed and measured by a transducer, and since the force transduced is proportional to the first power of wind speed, large forces which may be accurately measured at low wind speeds are achieved.
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| 27 | Fluidic direction and velocity detection apparatus | US3686937D | 1970-06-10 | US3686937A | 1972-08-29 | COREY VICTOR B |
| Fluidic detection apparatus for determining the direction and velocity of flow of an incident fluid flow stream. A jet stream producing means is disposed in axial spaced relation to a jet stream detector and initially disposed such that the common axis lies generally in the direction of flow of the incident fluid flow stream. Any deflection of the jet stream from its normal path, caused by the intersection therewith of the incident fluid flow stream, is detected by the jet stream detector and a servomechanism responsive thereto rotates the apparatus until the jet stream is aligned with the direction of the incident fluid flow stream. A second jet stream producing means and axially spaced jet stream detector are positioned 90* to the direction apparatus and are mounted for lateral translation by the servomechanism to detect the velocity of the same incident fluid flow stream.
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| 28 | Measuring system for a fluid flow stream | US3677086D | 1970-06-10 | US3677086A | 1972-07-18 | COREY VICTOR B |
| An apparatus for determining a characteristic, as velocity or direction, of a fluid flow stream. Fluid sensors generate signals which are differentially compared to produce an error signal representative of the amount of movement, for the sensors or for a fluid stream generator, which is necessary to null the system. A servomechanism produces the nulling movement in response to the error signal. The amount of movement also generates a positional signal indicating the low frequency component or steady state characteristic of the fluid flow stream. A signal adder combines the positional signal with the error signal, containing a high frequency component, to provide an indication of the instantaneous fluid characteristic.
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| 29 | Flow sensor assembly | US15291692 | 2016-10-12 | US10072470B2 | 2018-09-11 | Kim André Henriksen; Kenneth Torjussen |
| A flow sensor assembly including a housing configured to couple to a fluid line, wherein the housing includes an inlet for receiving a flow of a first fluid, and a sensor coupled to the housing and configured to measure a flow level of a second fluid passing through the fluid line. | ||||||
| 30 | Simplified anemoscope | US12081555 | 2008-04-17 | US07721597B2 | 2010-05-25 | Yuji Onishi |
| The present invention provides a simplified anemoscope that allows the direction and intensity of the wind to be relatively accurately confirmed in a simple manner, and that is superior in portability and design. A simplified anemoscope according to the present invention allows the direction and/or intensity of the wind to be confirmed by squirting out a powder or liquid material. The simplified anemoscope includes: a hollow section loaded with the powder or liquid material, and having at least one pore sized to allow the powder or liquid material to be squirted out; and a push-out section for pushing out the air in the hollow section. | ||||||
| 31 | Simplified anemoscope | US12081555 | 2008-04-17 | US20090217751A1 | 2009-09-03 | Yuji Onishi |
| The present invention provides a simplified anemoscope that allows the direction and intensity of the wind to be relatively accurately confirmed in a simple manner, and that is superior in portability and design. A simplified anemoscope according to the present invention allows the direction and/or intensity of the wind to be confirmed by squirting out a powder or liquid material. The simplified anemoscope includes: a hollow section loaded with the powder or liquid material, and having at least one pore sized to allow the powder or liquid material to be squirted out; and a push-out section for pushing out the air in the hollow section. | ||||||
| 32 | Display fountain, system, array and wind detector | US10537273 | 2003-11-26 | US20060157596A1 | 2006-07-20 | John Tippetts |
| A fountain (50) comprises a supply of water under pressure, a primary fluidic diverter (10) having an input (12) for said supply, and first and second outputs (16a, b) diverging from said input. Two control ports (20a, b) are provided with control flow to direct input flow to one or other of the two outputs that lead to the two inputs of a vortex amplifier (40). This comprises a vortex chamber (54), a radial port (50), a vortex inducing port (60) and an axial output port (58). One (16a) of the diverter outputs is connected to the vortex inducing port, the other (16b) to the radial port, so that supply to said axial output port is modulated by formation of a vortex in the chamber when flow is to the vortex inducing port. The axial port leads to a nozzle whereby a vortex spray or axial jet is produced, depending on which diverter output (16a, b) is active. A wind detector (100) has a vertical jet (102) and a catcher (104) which fails to catch water from the jet in high wind conditions. The catcher feeds the control port (20a) of a diverter 101, or such other pressure or flow detector as may be convenient. A fountain array of elements may comprise a number of diverters, the outputs of which have branches supplying the control ports of others in the array, whereby internal control is provided. | ||||||
| 33 | Method for measuring the flow of fluids | US11139067 | 2005-05-26 | US20050219507A1 | 2005-10-06 | Masamichi Ipponmatsu; Masashi Nishigaki; Akira Hirano; Tsuyoshi Nakajima; Yuji Ikeda; Minoru Suzuki; Tsuyoshi Tsurutani |
| The disclosed method of measuring the flow of a fluid with a porous particulate ceramic tracer and an optical instrument is characterized in that spherical particles having diameters in the range of 0.5 to 150 μm are used as the tracer. Inasmuch as the tracer particles for flow measurement are spherical, the sectional area of scattered light to be detected by an optical sensor means is constant regardless of the orientation of particles. Furthermore, spherical particles have no surface irregularities that might cause concatenation so that individual particles are not agglomerated in tracking a fluid flow, thus contributing to improved measurement accuracy. | ||||||
| 34 | Method for measuring the flow of fluids | US09568866 | 2000-05-09 | US06414748B1 | 2002-07-02 | Masamichi Ipponmatsu; Masashi Nishigaki; Akira Hirano; Tsuyoshi Nakajima; Yuji Ikeda; Minoru Suzuki; Tsuyoshi Tsurutani |
| The disclosed method of measuring the flow of a fluid with a porous particulate ceramic tracer and an optical instrument is characterized in that spherical particles having diameters in the range of 0.5 to 150 &mgr;m are used as the tracer. Inasmuch as the tracer particles for flow measurement are spherical, the sectional area of scattered light to be detected by an optical sensor means is constant regardless of the orientation of particles. Furthermore, spherical particles have no surface irregularities that might cause concatenation so that individual particles are not agglomerated in tracking a fluid flow, thus contributing to improved measurement accuracy. | ||||||
| 35 | Apparatus for measuring the velocity of a fluid | US437758 | 1974-01-28 | US4026149A | 1977-05-31 | John W. Tanney |
| A fluid stream velocity measuring apparatus and its method of use wherein a fluid jet is directed from a nozzle along a portion of the flow path of a fluid stream whose velocity is to be measured, towards the open end of one or more receiver tubes. The nozzle and receiver tube or tubes are mounted by mounting means to have a jet forming space, extending between them a distance of at least five times the minimum distance across the nozzle orifice, with the fluid stream having a substantially unobstructed flow path along a surface of the mounting means extending past the nozzle and receiver tube or tubes. The fluid pressure in the receiver tube or tubes is measured to determine the velocity of the fluid stream into which the jet is directed. The internal geometry of the fluid jet nozzle is derived from the jet Reynolds number which is in excess of 1700 and the external geometry of the nozzle and/or receiver is defined to provide a substantially unobstructed flow path past the nozzle and receiver and substantially unrestrained interaction of the fluid stream with the jet. | ||||||
| 36 | Air momentum anemometer | US31955172 | 1972-12-29 | US3848465A | 1974-11-19 | HOWELL W |
| A device for the measurement of horizontal wind velocity, especially low wind velocity. The horizontal component of momentum of the airstream is displaced from its normal flow. This is accomplished by either injecting an air jet into the airstream to displace the horizontal component of momentum, or withdrawing from the airstream, over an inlet, into which inlet is drawn the horizontal component of the momentum of the airstream. The horizontal momentum flux of the air is converted to a horizontal force which is thus sensed and measured by a transducer, and since the force transduced is proportional to the first power of wind speed, large forces which may be accurately measured are achieved at low wind speeds. The force which is sensed and measured is converted to a pulsing variable superimposed on a null signal or on a signal of constant magnitude. The conversion of the pulsing or oscillating signal in this manner overcomes the problem of zero drift.
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| 37 | Device for measuring the rate of flow of dust-laden gases | US29014772 | 1972-09-18 | US3803911A | 1974-04-16 | SHKATOV E; ZHUKOV J; KOZLOV A |
| A device for measuring the rate of flow of dust-laden gases in which the primary transducer comprises two hollow tubes. The tubes are provided with holes in their external surfaces intended to feed compressed air or an inert gas into the measured dustladen gas flow. The holes in one tube are arranged co-axially with the holes in the other tube and are directed opposite to each other so that the flow of compressed air or inert gas from the holes of both tubes takes place in a direction at right angles to the direction of the measured dust-laden gas flow.
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| 38 | Simple anemoscope | JP2008048320 | 2008-02-28 | JP2009204520A | 2009-09-10 | ONISHI YUJI |
| <P>PROBLEM TO BE SOLVED: To provide a simple anemoscope which can determine the direction and velocity of the wind easily and accurately and has superior portability and design. <P>SOLUTION: The simple anemoscope 100 can determine the direction and/or velocity of the wind by ejecting a powdery material or a liquid material. The simple anemoscope 100 comprises a hollow part 1d which accommodates the powdery material or the liquid material and has at least one fine opening 4a with a size allowing the powdery material or the liquid material to be ejected and an extruding part 3 for extruding air in the hollow part 1d. <P>COPYRIGHT: (C)2009,JPO&INPIT | ||||||
| 39 | Optical flow speed sensor | JP1290882 | 1982-01-28 | JPS58129263A | 1983-08-02 | OOMAE YOSHINOBU; SHIMADA YOSHIO |
| PURPOSE:To measure the flow speed optically, quickly and accurately by simple signal processing in accordance with large random signals by running air foam out into fluid, and measuring the flow speed by the random signal of the light scattered by the air foam. CONSTITUTION:Air foam 5 is run out into the fluid of a flow pipe 7 by an air pump 12 and an air foam injecting pipe 14. A photosensor 1 provided with optical fibers 8, 9 for light projection and photodetection detects optically large random signals by the light scattered by the air foam 5. Thus, even with the fluid contg. less dust and suspended solids, the large random signals are detected easily, and the flow speed over a wide range is measured optically, quickly and accurately by the simple signal processing. | ||||||
| 40 | Measuring method for flow of ground water | JP16549381 | 1981-10-16 | JPS5866856A | 1983-04-21 | HINO TSUTOMU |
| PURPOSE:To make the properties of soil coincident with those of ground water strata and to measure the flow of the ground water with high accuracy by providing measuring electrodes and an electrolyte injecting pipe of double construction in an observing part, injecting pressure water, burying the observing part and detecting the flowing of an electroyte with the electrodes. CONSTITUTION:An electrolyte injecting pipe 12 and measuring electrodes 13-28 of double construction are provided in the observing part 11 of a probe 4 and are so designed as to deliver pressure water. The electrodes 13-28 consist of 8 sets of inside and outside electrodes which are disposed concentrically. In the stage of measurement, the probe 4 is brought downward and pressure water is injected near the holes of the bottoms whereby the part 11 is buried into ground water strata. Then an electrolyte is run from the pipe 12. When the electroyte arrives at the electrode group on account of flowing of the ground water, a change in the resistance value is detected with the change in voltage. The flowing direction is known from the electrode direction of the set by which the peak of said voltage is detected, and from the time when the same arrives at the electrode, the velocity of flow is detected. Therefore roughly the same flow as that of the ground water is obtained and the flow is measured with high accuracy. | ||||||
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