Evaluation of 3C sensor coupling using ambient noise measurements Summary

Similar documents
Th ELI1 08 Efficient Land Seismic Acquisition Sampling Using Rotational Data

The Hodogram as an AVO Attribute

MEMS-based 3C accelerometers for land seismic acquisition: Is it time?

UNIT Explain the radiation from two-wire. Ans: Radiation from Two wire

Improvement of signal to noise ratio by Group Array Stack of single sensor data

Auto-levelling geophone development and testing

Field Tests of 3-Component geophones Don C. Lawton and Malcolm B. Bertram

GAIN COMPARISON MEASUREMENTS IN SPHERICAL NEAR-FIELD SCANNING

CDP noise attenuation using local linear models

Multicomponent seismic polarization analysis

Circuit Analysis-II. Circuit Analysis-II Lecture # 2 Wednesday 28 th Mar, 18

Acoustic Emission Linear Location Cluster Analysis on Seam Welded Hot Reheat Piping

I = I 0 cos 2 θ (1.1)

Seismic acquisition projects 2010

Keywords: cylindrical near-field acquisition, mechanical and electrical errors, uncertainty, directivity.

The introduction and background in the previous chapters provided context in

South Africa CO2 Seismic Program

Comparisons between data recorded by several 3-component coil geophones and a MEMS sensor at the Violet Grove monitor seismic survey

Lecture # 7 Coordinate systems and georeferencing

Seismic Reflection Method

The fast marching method in Spherical coordinates: SEG/EAGE salt-dome model

Survey results obtained in a complex geological environment with Midwater Stationary Cable Luc Haumonté*, Kietta; Weizhong Wang, Geotomo

Bird Model 7022 Statistical Power Sensor Applications and Benefits

AVO processing of walkaway VSP data at Ross Lake heavy oilfield, Saskatchewan

Antenna Measurement Software Features and Specifications

Practical Considerations for Radiated Immunities Measurement using ETS-Lindgren EMC Probes

Millimetre Spherical Wave Antenna Pattern Measurements at NPL. Philip Miller May 2009

AN5129 Application note

An Efficient Color Image Segmentation using Edge Detection and Thresholding Methods

Structural Correction of a Spherical Near-Field Scanner for mm-wave Applications

CX896-MT inch Coaxial Loudspeaker, 70 V. product specification SERIES. Performance Specifications 1

Groundwave Propagation, Part One

How to Check the Quality of your Seismic Data Conditioning in Hampson-Russell Software. HRS9 Houston, Texas 2011

Nonuniform multi level crossing for signal reconstruction

Sub-millimeter Wave Planar Near-field Antenna Testing

ANECHOIC CHAMBER DIAGNOSTIC IMAGING

Dr. John S. Seybold. November 9, IEEE Melbourne COM/SP AP/MTT Chapters

DEEP FLAW DETECTION WITH GIANT MAGNETORESISTIVE (GMR) BASED SELF-NULLING PROBE

A multi-window algorithm for real-time automatic detection and picking of P-phases of microseismic events

Accuracy Estimation of Microwave Holography from Planar Near-Field Measurements

RECOMMENDATION ITU-R F *

Characteristics of HF Coastal Radars

The case for longer sweeps in vibrator acquisition Malcolm Lansley, Sercel, John Gibson, Forest Lin, Alexandre Egreteau and Julien Meunier, CGGVeritas

Numerical Study of Stirring Effects in a Mode-Stirred Reverberation Chamber by using the Finite Difference Time Domain Simulation

I017 Digital Noise Attenuation of Particle Motion Data in a Multicomponent 4C Towed Streamer

Borehole Seismic Processing Summary Checkshot Vertical Seismic Profile

Antenna & Propagation. Antenna Parameters

Effect of data sampling on the location accuracy of high frequency microseismic events

Single-photon excitation of morphology dependent resonance

Summary. Theory. Introduction

THE SINUSOIDAL WAVEFORM

CX inch Coaxial Loudspeaker. product specification SERIES. Performance Specifications 1

Noise generators. Spatial Combining of Multiple Microwave Noise Radiators NOISE ARRAY. This article reports on. experiments to increase the

Optimize Full Waveform Sonic Processing

Studying the Sensitivity of Remote-Field Testing Signals when Faced with Pulling Speed Variations

STATISTICAL DISTRIBUTION OF INCIDENT WAVES TO MOBILE ANTENNA IN MICROCELLULAR ENVIRONMENT AT 2.15 GHz

Ǥ CONFERENCE ABSTRACTS 161

CHAPTER 4 IMPLEMENTATION OF ADALINE IN MATLAB

UNIVERSITY OF UTAH ELECTRICAL ENGINEERING DEPARTMENT LABORATORY PROJECT NO. 3 DESIGN OF A MICROMOTOR DRIVER CIRCUIT

USE OF BASIC ELECTRONIC MEASURING INSTRUMENTS Part II, & ANALYSIS OF MEASUREMENT ERROR 1

Developments in Electromagnetic Inspection Methods II

Polarization Experiments Using Jones Calculus

DSU3-428 DIGITAL SENSOR UNITS

The Basics of Patch Antennas, Updated

Antenna Fundamentals

Technical Notes Volume 1, N u m b e r 6. JBL High-frequency Directional Data in Isobar Form. 1. Introduction: 3. The Isobars:

Effects on phased arrays radiation pattern due to phase error distribution in the phase shifter operation

Th N Broadband Processing of Variable-depth Streamer Data

DOPPLER RADAR. Doppler Velocities - The Doppler shift. if φ 0 = 0, then φ = 4π. where

CLAUDIO TALARICO Department of Electrical and Computer Engineering Gonzaga University Spokane, WA ITALY

ANTENNA INTRODUCTION / BASICS

DISPLAY metrology measurement

GX inch Coaxial Loudspeaker. product specification SERIES. Performance Specifications 1

Making sense of electrical signals

The Impact of Very High Frequency Surface Reverberation on Coherent Acoustic Propagation and Modeling

2012 SEG SEG Las Vegas 2012 Annual Meeting Page 1

In-Situ Damage Detection of Composites Structures using Lamb Wave Methods

Repeatability Measure for Broadband 4D Seismic

360 inches (915 cm) 240 inches (610 cm) 120 inches (305 cm) 240 inches is the recommended pole length, 360 inches is the recommended free space area

Eric V. Gallant, Malcolm B. Bertram, Don C. Lawton, R. James Brown, and Robert R. Stewart

ABSTRACT INTRODUCTION. different curvatures at different times (see figure 1a and 1b).

UNIT-3. Ans: Arrays of two point sources with equal amplitude and opposite phase:

Figure 4.1 Vector representation of magnetic field.

Chapter 41 Deep Space Station 13: Venus

DISTANCE CODING AND PERFORMANCE OF THE MARK 5 AND ST350 SOUNDFIELD MICROPHONES AND THEIR SUITABILITY FOR AMBISONIC REPRODUCTION

A COMPOSITE NEAR-FIELD SCANNING ANTENNA RANGE FOR MILLIMETER-WAVE BANDS

Introduction Antenna Ranges Radiation Patterns Gain Measurements Directivity Measurements Impedance Measurements Polarization Measurements Scale

THE ELECTROMAGNETIC FIELD THEORY. Dr. A. Bhattacharya

Update of the compatibility study between RLAN 5 GHz and EESS (active) in the band MHz

Module 2 WAVE PROPAGATION (Lectures 7 to 9)

There is growing interest in the oil and gas industry to

Broadband Temporal Coherence Results From the June 2003 Panama City Coherence Experiments

Radial Polarization Converter With LC Driver USER MANUAL

Strong Noise Removal and Replacement on Seismic Data

Processing the Teal South 4C-4D seismic survey

Lab S-3: Beamforming with Phasors. N r k. is the time shift applied to r k

Line Arrays. ρav = time averaged power. Line Arrays History and Theory

ACTUAL POLARIZERS AND METHODS OF LIGHT MICROSCOPY

28th Seismic Research Review: Ground-Based Nuclear Explosion Monitoring Technologies

Processing the Blackfoot broad-band 3-C seismic data

Transcription:

Evaluation of 3C sensor coupling using ambient noise measurements Howard Watt, John Gibson, Bruce Mattocks, Mark Cartwright, Roy Burnett, and Shuki Ronen Veritas Geophysical Corporation Summary Good vector fidelity is crucial for various multicomponent applications and can be adversely impacted by poor sensor coupling during data acquisition. We present a method to evaluate the ground coupling quality of three-component (3C) sensors during field deployment using ambient seismic noise data. The method utilizes the directional nature of the noise on the three sensor components for coupling assessment. This is believed to be the first method developed to evaluate in situ sensor coupling from ambient noise measurements.

Introduction Achieving good vector fidelity is crucial for various three-component (3C) applications including AVO studies, azimuthal anisotropy analysis and polarization filtering. Vector fidelity may be compromised by variations in sensor element sensitivity, deviations from element orthogonality and particularly by poor sensor coupling. 3C MEMS (Micro Electro Mechanical System) sensor manufacturers report vector fidelity exceeding 40 db as determined from laboratory tests. It is our assertion that the quality of sensor coupling is the primary factor ensuring good vector fidelity. It is standard practice to acquire passive noise records prior to seismic production recording to establish whether ambient noise is below an acceptable level. In evaluating ambient noise records from a 3C project with poor ground coupling conditions, we observed that ambient noise levels on the two horizontal components were often 6-12 db higher than noise on the vertical component. Comparative behavior of the RMS amplitudes of various sensor components are shown for an area with typical sensor planting conditions (Figure 1a) and an area with locally poor sensor planting conditions (Figure 1b). Note the large distribution of H1 (inline horizontal) and H2 (crossline horizontal) values in Figure 1b relative to Figure 1a. Such behavior is inconsistent with typical field noise observations. As a result, controlled field tests were conducted to compare 3C ambient noise levels on the three sensor components under various coupling conditions. Figure 1. Crossplot of vertical (V), inline horizontal (H1) and crossline horizontal (H2) component RMS noise versus vertical RMS noise. a) Typical sensor planting conditions. b) Locally poor sensor coupling conditions. Note the anomalously high values of the H1 and H2 elements relative to the vertical components in b). Field Test Methodology Figure 2 shows a schematic using three qualitative descriptions standard, tight but elevated, and loose to describe variations in sensor planting quality that have been observed in practice. Standard (Figure 2a) refers to the normal deployment method of drilling a hole with a slightly smaller diameter than the sensor body and placing the sensor body in the hole, up to its base. Tight but elevated (Figure 2b) refers to a sensor planted with its base approximately 1.5 inches above the ground surface and loose (Figure 2c) refers to a situation where it is easy to rotate or wobble the sensor. Such variations can result from frozen or rocky ground, gravelly or sandy soil conditions and the presence of scree and loose sand. To test whether sensor coupling quality can be determined from 3C ambient noise records, we conducted experiments in three USA locations, two in Texas and one in Utah. Figure 3

illustrates one such experiment. During each test a significant number of ambient noise measurements were taken using 64 to 100 3C sensors. These measurements were taken over an extended period of time ranging from two hours to two days. Such measurements included the presence of both random and coherent noise. Strong coherent (and directional) noise will unduly influence amplitude measurements on the various elements and will need to be appropriately addressed in the analysis. c) Standard Tight but elevated Loose Figure 2. Schematic diagram of sensor deployment situations. a) Standard deployment, b) Tight but elevated deployment. c) Loose deployment. Standard Standard Loose Loose Tight but elevated Figure 3. Typical test layout showing the various deployment types. Inset shows an example of a Tight but elevated sensor. Data Analysis An initial analysis was based on comparing Root-Mean-Square (RMS) levels of ambient noise for the three sensor components hereafter referenced as V (vertical), H1 (inline horizontal) and H2 (crossline horizontal). For isotropic ambient noise and well-coupled sensors, we expected the ambient noise levels on the three components to be comparable. Noise records from well-coupled receivers, however, often show that ambient noise on the horizontal elements tends to be mildly reduced relative to that on the vertical element. Figure 1a) illustrates typical results from this approach. Early in the initial analysis it became clear that the results were sensitive to the presence of coherent noise and noise bursts and therefore to the choice of data analysis window. Effective field implementation will not allow the seismic observer overseeing production operations to experiment with data windows. As a result, a decision was made to abandon the windowed- RMS approach and look at ambient noise data distributions as a means of mitigating the impact of coherent noise.

Each 3C ambient noise data sample can be viewed as a three-dimensional vector with components (H1, H2 and V) as shown in Figure 4(a). Following vector normalization by the magnitude as depicted in Figure 4(b), each sample unit vector can be described by its polar (φ) and azimuthal (θ) angles. This normalization has the benefit of reducing the impact of vectors with anomalous amplitudes. Figure 4. a) Three-dimensional vector representation (Cartesian coordinates) of a 3C trace sample. b) Normalized 3C trace sample in spherical coordinates. Applying this representation to synthetic data having Gaussian distributions for each of the vector coordinates yields the spherical and angular plots shown in Figure 5. Note the uniform distribution of data points on the unit sphere (Figure 5a) and for the angular display (Figure 5b). This simply shows the two modes of display to be employed. Figure 5. a) Spherical and b) angular representations using synthetic data having Gaussian distributions for each vector coordinate. Figure 6 shows spherical displays for a field data comparison between standard and loose sensors for two different loose deployments. Note the rather uniform distribution of data points on the unit sphere for the standard (Figure 6a) case in contrast with the clustering of data points about the equator in the loose cases (Figures 6b and 6c). The situation in Figure 6c is quite extreme as the sensor is known to be very loose. Though no figure is shown for it, the tight but elevated case proves to be very similar to the standard case using spherical representations.

c) Figure 6. Field data comparison of a) Standard, b) Loose and c) Very loose deployment types using spherical representations. Figure 7 shows comparative angular representations for standard, tight but elevated, loose and very loose deployments. In this view, the angular representations of standard (Figure 7a) and tight but elevated (Figure 7b) are more distinguishable than when using spherical representations. a) b) c) d) Figure 7. Field data comparison of a) Standard, b) Tight but elevated, c) Loose and d) Very loose deployment types using angular representations. Conclusions Sensor coupling is a critical issue for preserving vector fidelity which is important for a number of multicomponent applications. Ambient noise measurements taken prior to any production recording can be analyzed to evaluate sensor coupling and to effect the necessary remediation. A methodology for field application has been developed.