The present disclosure generally relates to a seismic data acquisition apparatus, and in particular, a multiple-coil, multiple-terminal geophone accelerometer.
1. Field of the Invention
This invention relates generally to the field accelerometers, and in particular to methods and closed loop accelerometers, and more specifically to an accelerometer used in a seismic data acquisition system, micro seismic monitoring/acquisition system.
2. Description of the Prior Art
It is well known that the current conventional geophones are still widely used in seismic exploration to acquire/measure the vibration signal from the ground, primarily due to low cost, lack of reliance on power and high reliability. However, current conventional geophones are still unsatisfactory due to their narrow frequency bandwidth, and high total harmonic distortion (THD). As seismic acquisition systems have rapidly been developed to service high-resolution seismic exploration, higher performance geophones are needed to match such exploration requirements. In recent years, the micro-electromechanical systems (MEMS) digital sensors, in which more improvements have been developed, have been used in many seismic exploration projects. These closed-loop MEMS sensors have 3 to 375 Hz bandwidth and lower THD of approximately 0.001% dB. However, these sensors are still not widely used, as they are both expensive and fragile. Therefore, a geophone with lower cost, broadband frequency and small THD is highly desired by the exploration market. From U.S. Pat. No. 5,172,345, Jacobus W. P. van der Poel disclosed a geophone system for measuring mechanical vibrations. This geophone system has a sensing coil, a driving coil and a compensation coil wound into 3 recesses of its bobbin separated. The sensing coil is wound in top recess of its bobbin and the compensation coil is wound in the bottom recess of its bobbin. The sensing coil is in series with the compensation coil. The sensing coil and compensation coil of the first coil set is connected with the input of the electronic processing device. The driving coil of the second coil set is wound in the middle recess of its bobbin and also connected with the electronic processing device. Both of the two coil sets are connected to two outside electronic processing devices separated. To manage the moving coil of the first coil set, the electronic processing device has been used as a feedback control module by sending a current to the driving coil of the second coil set. The magnet field magnitude of each of these three coil sets are not even and this can make big differences when using Faraday's Law and Lorentz's law. This is not easy to make in real world. In US20140293752A1, Zhentang Fu, Chunhua Gao and Du Chen disclosed a multi-coil multi-terminal closed-loop geophone accelerometer. Comparing with Jacobus's method, Zhentang Fu et. al. use only 2 recesses and put the middle driving coil overlapped with sensing coils. This makes the geophone easier to be practiced in real world and will have better performances than before. However, the magnet field magnitude of each of their coil sets are not even and this can still make big differences when using Faraday's Law and Lorentz's law. In U.S. Pat. No. 8,139,439, Masahiro Kamata presented a seismic sensor calibration method by injecting a current into a moving coil of a seismic sensor and measuring the voltage across the moving coil. In U.S. Pat. No. 6,101,864, Michael L. Abrams et. al disclosed a high performance method and apparatus for testing a closed loop transducer. By using ΣΔ and analog-to-digital converter (ADC) technologies, a closed loop feedback circuit is attached to a sensor. This invention includes a method and apparatus for combining with the one-bit ΣΔ modulated feedback signal a special purpose one-bit modulated test signal which acts as a precision forcing signal on the mass of the sensor. When such test bitstream is inserted into the feedback circuit, the transducer forward circuit senses the test signal as an external force applied to the transducer, which must be zeroed by the transducer feedback loop. Recording of the sensor ADC output provides a signal which may be compared with the test signal for evaluation of the transducer. From U.S. Pat. No. 5,469,408, Daniel M. Woo presented a high resolution geophone. The amount of harmonic distortion is reduced by making pole pieces longer than coil frame length to provide a uniform magnetic field in which the two coil portions of single coil set move.
Larger energy reserves across the globe have been discovered. The oil and gas industry now focuses on narrow, deeper energy reserve places. Therefore, new technologies are required to match such requirements. This underlies the need for high density and high-resolution seismic acquisition technologies. Broadband geophones, such as those down to 1 or 2 Hz frequency, available at lower cost and higher reliability are needed to support the exploration industry in discovering. This step change in geophone technology is required and will be welcomed by the oil and gas exploration industry.
The principles of this disclosure are directed to the technologies for highly improving the performances of current moving coil geophones, such as wider bandwidth (from 0.1 to 500 Hz) and lower THD (can be less than 0.001%). The current moving coil geophones measure the mechanical vibration based on Faraday's Law and it is expressed as follows:
{right arrow over (E)}={right arrow over (B)}*L*{right arrow over (V)} (1)
Where, the {right arrow over (E)} represents the voltage across the moving coil, {right arrow over (B)} is the magnet field magnitude, {right arrow over (V)} is the velocity of moving coil and the L is the length of the coil wire. Measuring the voltage of the output signal, the mechanical vibration can be calculated by using the equation (1), because both {right arrow over (B)} and L are considering known parameters. Here {right arrow over (B)} is the magnet field magnitude in the space which the moving coil is moving around. However, lots of researchers (for example in U.S. Pat. No. 5,469,408) have already concluded that the magnet field magnitude {right arrow over (B)} of the space between the magnetic block and the inner wall of geophone sensor housing is not uniform. In this magnetic field, the magnet field magnitudes {right arrow over (B)} in some area are not equal to each other, because they might have different values or different direction. Only the magnet field magnitude of the area, where it is close to the shoulder face of the bobbin, could be considered as uniform. Therefore, in the coil's moving area, it is not accurate to put the magnet field magnitude {right arrow over (B)} as a constant by using equation (1). This could be the reason that the current moving coil geophone has higher THD. In the disclosure, coils are assembled separated in different recesses of the bobbin and the measuring coils are located in the most well distributed magnet field (or uniformed field). For example, the sensing coil is strictly assembled in the space of which they have the well distributed magnet field magnitude {right arrow over (B)}. The moving coil's height along the geophone housing's cylindrical axis is designed to match the height of magnetic boot shoulder face. And the sensing coil's moving path is controlled by driving coil (described below) and less than +/−0.0002 mm (the current most moving coil geophones have +/−2 mm). These will highly improve the performances of geophones.
As the moving coil geophone matches the conditions for closed-loop control, another coil set is added as a feedback controller. According to Lorentz's law, it is expressed as the follows:
{right arrow over (F)}={right arrow over (I)}*L*{right arrow over (B)} (2)
By injecting a current {right arrow over (I)} to a coil, a force is generated using equation (2). The direction of the force is determined by the direction of the current. Therefore, a close loop system can be set up by putting one coil as measuring component and the other coil as the controller. For the purpose of minimizing the geophone dimensions and putting the measuring coil in the uniformed magnet field, both of the first coil set and the second coil set are wound to the bobbin separately. The first coil set (or the sensing coil) is wound to recesses which will have the most well distributed magnet field magnitude; the second coil set (or driving coil) is wound to recesses which will have the less well distributed magnet field magnitude. Therefore, the bobbin is designed to have four (4) recesses. The top recess and the bottom recess will be wound for sensing coil set and are assembled in the area of well-distributed magnet field magnitude. The middle two recesses are wound by two coils of the driving coil set. Located in separated recesses of the bobbin, each coil portion of these coil sets has an individual magnet field magnitude by using faraday's law (or equation (1)) and Lorentz's law (or equation (2)). By this mathematic method, the performances of the sensor are highly improved. Both the two coil sets are connected to an electronic device which processes the measuring signal and feedbacks the signal as a precision digital forcing signal to sensing coil as a reference position. The same methods also apply to magnetic block moving sensors which their coils and bobbin is stably assembled with housing.
The magnetic field 153A corresponds to cylindrical surface 213 (shoulder face of magnetic boot) of magnetic boot 126. Similarly, magnetic field 154A mainly corresponds to plane 214 of magnetic boot 126; magnetic 155A corresponds plane 210, cylindrical surface 211 and plane 212 of magnetic boot 126. By using the same method, 153B, 154B and 155B can be determined. Also,
For having the sensing coil sets totally located in the well uniformed magnetic field, the length of coil portion 121A is matching the length of top magnetic boot shoulder face 213 along cylindrical axis of magnetic block. For example, the length of coil portion 121A is equal to or smaller than the length of the length of magnetic boot shoulder face 213. Also, the working distance of the sensing coil is within 0.0002 mm while the conventional geophone is within +/−2 mm. By using the same method, the length of coil 121B is made equal to or smaller than the length of bottom magnetic boot shoulder face 222 and will be symmetric to 121A under the symmetric plane 144.
This application claims the benefit of U.S. Provisional Application Ser. No. 62/110,542, filed on Feb. 1, 2015.