Info iconThis preview shows pages 1–2. Sign up to view the full content.

View Full Document Right Arrow Icon
IMPROVING THE PERFORMANCE OF A GEOPHONE THROUGH CAPACITIVE POSITION SENSING AND FEEDBACK Aaron Barzilai Dept. of Mechanical Engineering Stanford University Stanford, CA Tom VanZandt Center for Space Microelectronics Technology Jet Propulsion Laboratory Pasadena, CA Tom Kenny Dept. of Mechanical Engineering Stanford University Stanford, CA ABSTRACT This paper reports on the improved performance of a geo- phone obtained by measuring the displacement of its proof mass capacitively rather than inductively and operating the sensor as a closed loop system. A measurement of the displacement of the proof mass rather than the velocity measurement made with a conventional geophone provides better low frequency perfor- mance. As a result, a geophone can be considered for use in a broader array of applications. A capacitive geophone can operate in either an open loop or closed loop mode. This paper describes a closed loop geophone system with a frequency response similar to the state of the art Streckeisen seismometers. INTRODUCTION Seismologists and geophysicists rely on a wide variety of sen- sors to study the Earth. Historically, a popular sensor in these communities has been the geophone, a highly sensitive ground motion transducer that have been in use for decades(Sheriff & Geldart, 1995). Figure 1 shows both a schematic drawing and a cross-sectional view of a geophone, which uses the motion of a spring supported coil in the field of a permanent magnet to generate an output signal. Studies of local and regional seismic- ity often rely on geophones. However, these sensors are most commonly used as sensors for seismic reflection and refraction surveys, techniques to image the three-dimensional structure of oil and gas deposits beneath the Earth’s surface. For imaging ap- plications, large, two-dimensional arrays of sensors are deployed on the surface to record seismic waves as they propagate be- low the ground. By measuring travel times and amplitudes of various components of the waves, the underground structures encountered by the waves can be determined. The combination of attributes offered by a geophone make it a good choice for these applications and others. Riedesel et al.(1990) showed that a geophone can have a minimum instru- mental noise as low as 0.1 n g / Hz, which is quieter than the minimum seismic noise of the Earth(Peterson, 1993). The nom- inally 4.5 Hz GS-11D geophone by OYO Geospace used in this work has a minimum instrumental noise of 0.6 n g / Hz(Barzilai Magnet Cylinder Coil Geophone Housing Leaf Spring Figure 1: Schematic drawing and cross-sectional view of a geophone et al. , 1998). The total harmonic distortion(THD) of a geophone is also quite low, less than 0.2% for the GS-11D. Geophones are also expected to be robust, capable of withstanding a one meter drop onto a piece of plywood 1000 times. Perhaps most impor- tantly, geophones deliver this performance quite affordably, as one sensor costs on the order of $50 to $100.
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Image of page 2
This is the end of the preview. Sign up to access the rest of the document.

This note was uploaded on 05/09/2010 for the course EARTH SCIE APPLIED GE taught by Professor Es during the Spring '09 term at IIT Bombay.

Page1 / 8


This preview shows document pages 1 - 2. Sign up to view the full document.

View Full Document Right Arrow Icon
Ask a homework question - tutors are online