A disclosed example method includes providing, in a borehole, a transmitter (Tx) and receivers (Rxs) spaced linearly from Tx at known distances, measuring linear propagation times (LPts) for a signal to propagate from Tx to each of Rxs, determining an inline velocity (VINL) based on LPts, measuring reflection times (Rts) for a signal to propagate from Tx to each of the Rxs via a boundary, for each of Rts, providing a time-distance anisotropic velocity (TDAV) relationship depending on an effective signal velocity (ESV) in an anisotropic formation adjacent the boundary as a function of reflection angle for the reflection time signal to the boundary, VINL and orthogonal velocity, performing semblance processing to combine the TDAV relationships with VINL for a best-fit calculation of the ESVs for the different reflection angles of the reflection time signals, and calculating a distance for the corresponding receiver to the boundary on the calculation.
Drawings
Claims12
A method comprising:
providing, in a borehole, a transmitter and a series of receivers spaced linearly from the transmitter at known different distances from the transmitter;
measuring linear propagation times for a signal to propagate linearly from the transmitter to each of the receivers;
determining an inline velocity based at least in part on the linear propagation times;
measuring reflection times for a signal to propagate from the transmitter to a boundary and from the boundary to each of the receivers;
for each of the reflection times, providing a time-distance anisotropic velocity (TDAV) relationship that depends on an effective signal velocity in an anisotropic subterranean formation adjacent the boundary as a function of reflection angle for the reflection time signal with respect to the boundary, inline velocity and orthogonal velocity, orthogonal to the inline velocity;
performing semblance processing to combine the time-distance anisotropic velocity (TDAV) relationships with the inline velocity to provide for a best-fit calculation of the effective signal velocities for the different reflection angles of the reflection time signals;
and
based on the best-fit calculation, calculating for each of the effective anisotropic velocities a distance for the corresponding receiver to the boundary.
5 more elements
An apparatus to calculate distances from a borehole to a boundary of an anisotropic subterranean rock layer, the apparatus comprising:
an input receiver to receive input from equipment in a borehole that comprises a transmitter and a series of receivers spaced linearly from the transmitter at known different distances from the transmitter;
and
a processor configured to
determine an inline velocity based at least in part on received input for linear propagation times for a signal to propagate linearly from the transmitter to each of the receivers,
receive input for reflection times for a signal to propagate from the transmitter to the boundary and from the boundary to each of the receivers,
for each of the reflection times, provide a time-distance anisotropic velocity (TDAV) relationship that depends on an effective signal velocity in the anisotropic subterranean rock layer as a function of reflection angle for the reflection time signal with respect to the boundary, inline velocity and orthogonal velocity, orthogonal to the inline velocity,
perform semblance processing to combine the time-distance anisotropic velocity (TDAV) relationships with the inline velocity to provide for a best-fit calculation of the effective signal velocities for the different reflection angles of the reflection time signals,
based on the best-fit calculation, calculate for each of the effective anisotropic velocities a distance for the corresponding receiver to the boundary.
1 Sep 2030Estimated · howhide20 years from earliest known nonprovisional domestic filing plus recorded patent term adjustment, including 372 days of adjustment. Maintenance-fee lapses, terminal disclaimers and statutory extensions have not been checked. The continuity chain may be incomplete; this is not an enforceability determination.
About 3 years 10 months of term left · ends 1 Sep 2030 (estimated)
Priority25 Aug 2009
Filed17 Aug 2012
Published6 Dec 2012
Granted16 Dec 2014
Today12 Oct 2026
Term ends1 Sep 2030
Priority25 Aug 2009
Granted16 Dec 2014
Term ends1 Sep 2030
Priority claimedParent application 12/547,464
Application filedUS 13/587,931
PublishedUS 2012/0307592 A1
GrantedUS 8,913,460 B2
TodayWithin its term
Term endsEstimated, includes 372 days of adjustment
Description12,676 words
Summary629 words
#This disclosure relates generally to oil production and, more particularly, to methods and apparatus to calculate a distance from a borehole to a boundary of an anisotropic subterranean rock layer.
#Oil and gas producers typically image subterranean rock layers to determine the location and shape of the subterranean rock layers. Such imaging may also be used to identify a boundary between the subterranean rock layer and an adjacent subterranean rock layer. The imaging is often performed using an imaging tool disposed within a borehole drilled into the subterranean rock layer to be imaged.
#Identifying a boundary of a subterranean rock layer is an important aspect of oil or gas well production. For example, identifying such a boundary of a rock layer enables oil or gas producers to plan well locations to efficiently and optimally extract oil or gas. Additionally, knowing the boundary of a rock layer may prevent oil and gas producers from drilling into undesired rock layers.
Brief description of the drawings9 figures
#FIGS. 1A-1D show typical seismic-while-drilling tools with one or more transmitters located at the surface.
#FIG. 2 shows a graph representing the effect of anisotropy within a subterranean rock layer.
#FIG. 3 shows an example wellsite system including a transmitter and receivers to implement the example methods and apparatus described herein.
Detailed description11,865 words
#Certain examples are shown in the above-identified figures and described in detail below. In describing these examples, like or identical reference numbers are used to identify common or similar elements. The figures are not necessarily to scale and certain features and certain views of the figures may be shown exaggerated in scale or in schematic for clarity and/or conciseness. Although the following discloses example systems including, among other components, software or firmware executed on hardware, it should be noted that such systems are merely illustrative and should not be considered as limiting. For example, it is contemplated that any form of logic may be used to implement the systems or subsystems disclosed herein. Logic may include, for example, implementations that are made exclusively in dedicated hardware (e.g., circuits, transistors, logic gates, hard-coded processors, programmable array logic (PAL), application-specific integrated circuits (ASICs), etc.) exclusively in software, exclusively in firmware, or some combination of hardware, firmware, and/or software. Accordingly, while the following describes example systems, persons of ordinary skill in the art will readily appreciate that the examples are not the only way to implement such systems. Further, the examples may be implemented by acoustic signals that may include seismic signals, sonic signals, ultrasonic signals and/or any other shear and/or compression signals.
#Currently, oil and/or gas producers use time-indexed waveforms of a signal to image a boundary of a subterranean rock layer adjacent to a wellbore or a borehole. The frequency, amplitude, and/or energy of the signal are specified so that the signal can propagate through the rock layer being logged but reflect off a boundary of the rock layer. For example, a signal having a frequency of 8000 Hertz (Hz) may be specified to enable the signal to propagate through a first rock layer. However, a signal at this frequency may reflect off a boundary of the rock layer. The boundary may include a change in rock type from the subterranean rock layer being logged to a second type of rock in a second subterranean rock layer, a change in a lithology of the subterranean rock layer, a change in a fault of the subterranean rock layer, or a change in an unconformity within the subterranean rock layer.
#The boundary is imaged by transmitting one or more acoustic signals from a transmitter and recording when the signals are received by one or more receivers. Each receiver may include one or more sensors circumferentially located around the receiver so that each sensor may detect the transmitted signal from a specified direction. The sensors may include any type of transducer to convert a detected acoustic (e.g., seismic, sonic, ultrasonic, etc.) signal into an electrical signal and/or impulse decipherable by a microcontroller, a transistor, and/or a processor. By aligning the sensors in specified directions, oil and/or gas producers can determine the direction from which a signal was reflected. Typically, one or more transmitter(s) are located at the surface in proximity of a well site while receivers are included within a tool that is placed within a wellbore or borehole of a rock layer bring logged.