Patent application number | Description | Published |
20100142326 | Method For Identifying Gas Leaks Using A Stationary Seabed Placed Steered Beamformed Acoustic Antenna With Active Narrow Beam Transmitter Interrogation Capability - A method for identifying position of acoustic source proximate sediments below the bottom of a body of water includes deploying a plurality of arrays of acoustic sensors on the bottom of the body of water. Each array includes a plurality of lines of acoustic sensors disposed in a substantially radial pattern. The arrays have a center to center distance therebetween of about twice a diameter of each of the arrays. Signals are detected from each of the sensors for a selected time period. A direction of the acoustic source with respect to each of the arrays is determined by steering a response of the sensors in each array. A range of the acoustic source is determined using the determined directions. | 06-10-2010 |
20100328138 | SHORT BASELINE HELICOPTER POSITIONING RADAR FOR LOW VISIBILITY - A method for determining position and orientation of a rotating wing aircraft (e.g. helicopter) with respect to a ground station includes transmitting an electromagnetic signal from the aircraft. The signal includes a plurality of electromagnetic signals, each signal having a different selected frequency. The signal is detected at an array of sensors disposed on the ground surface in a selected pattern. The array includes at least one reference sensor and at least three spaced apart time difference determination sensors. A difference in arrival time of the signals between the reference sensor and each of the time difference determination sensors is determined and a spatial position of the aircraft is determined from the time differences. | 12-30-2010 |
20110158048 | SPIRAL SENSOR CONFIGURATION FOR SEISMIC BEAMFORMING AND FOCUSING - A seismic sensor array includes a plurality of seismic sensors disposed on a line. The line is arranged in a spiral. The seismic sensors are disposed at at least one of equal angular spacing between adjacent sensors and equal linear spacing between adjacent sensors. A recording system is in signal communication with each of the seismic sensors. The recording system includes means for beam steering a response of the sensors. | 06-30-2011 |
20110175395 | DRAG REDUCTION DEVICE FOR TRANSPORT VEHICLES HAVING RANDOMIZED IRREGULAR SHAPED EDGE VORTEX GENERATING CHANNELS - A drag reducing device for use on transport vehicles includes a delta wing having variable height and irregularly spaced undulations on an upper surface of each side of the wing. A length of each side of the delta wing is different than the length of the other wing side thereof. | 07-21-2011 |
20110188343 | Random Transmitter Placement Method For Stationary Seismic Imaging - A method for at least one of imparting seismic energy into formations below the bottom of a body of water and detecting seismic energy therefrom includes releasing a plurality of acoustic transducers into the water. The transducers move to the bottom by gravity. A geodetic position of each of the transducers on the water bottom is determined. At least one of the following is performed: actuating each of the transducers as a transmitter at least once, the actuating of each transducer occurring at a time selected to cause seismic energy to be imparted into the formations in a beam along a selected direction, the selected time related to relative positions of the transducers; and recording signals detected by each of the transducers, the recording including adding a selected time delay to cause response of the transducers to be amplified along a selected direction. | 08-04-2011 |
20110317518 | METHOD FOR COMBINED ACTIVE SOURCE AND PASSIVE SEISMIC IMAGING FOR SUBSURFACE FLUID MOVEMENT MAPPING AND FORMATION CHARACTERIZATION - A method for characterizing fluid pumping effects on a subsurface formation includes (a) during pumping of fluid into the subsurface formation, detecting passive seismic signals related to fractures created in the subsurface formation. (b) A place of origin of the passive seismic signals is determined. (c) A seismic energy source is actuated for a plurality of actuations and an output thereof is beam steered toward the place of origin. (d) At least one acoustic property is determined for the place of origin using signals detected as a result of the plurality of actuations. The detected signals are beam steered toward the place of origin and are stacked over the plurality of actuations. (a), (b), (c) and (d) are repeated until the pumping is completed. | 12-29-2011 |
20120008461 | METHOD FOR ACCENTUATING SPECULAR AND NON-SPECULAR SEISMIC EVENTS FROM WITHIN SHALLOW SUBSURFACE ROCK FORMATIONS - A method for evaluating subsurface formations includes deploying at least two intersecting seismic transducer lines above an area of the subsurface to be surveyed. Each line includes spaced apart seismic transmitters on one side of the intersection and spaced apart seismic receivers on the other side. On each line, one of the transmitters is actuated and signals are detected at one of the receivers. The foregoing is repeated for each of the remaining receivers. The foregoing is then repeated for each of the remaining transmitters on each line. The detected signals are processed to enhance both specular and non-specular seismic events in the subsurface. The enhanced events may be stored and/or displayed. | 01-12-2012 |
20130258811 | DISCRETE VOLUMETRIC SONAR METHOD AND APPARATUS FOR SUB-SEABED SURVEYING - A method for imaging formations below the bottom of a body of water includes imparting acoustic energy into the formations along a predetermined length swath at a selected geodetic position. Acoustic energy reflected from the formations is detected along a line parallel to the length of the swath. The selected geodetic position is moved a selected distance transverse to the length of the swath. The imparting acoustic energy, detecting acoustic energy and moving the geodetic position are repeated until a selected distance transverse to the length of the swath is traversed. The detected acoustic energy from all the selected geodetic positions is coherently stacked. The detected acoustic energy is beam steered to each of a plurality of depths and positions along the length of the swath to generate an image for each such depth and position. | 10-03-2013 |