3D Microseismic Source Location via Offset Well DAS Cable

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Solution Overview

Problem

Fiber optic distributed acoustic sensing (DAS) cables used for microseismic monitoring in the hydrocarbon production industry lack broadside sensitivity, resulting in non-unique source-location determination of microseismic events, which limits the interpretive value of fracture geometry parameters.

Innovation Solution

A method utilizing a single acoustic sensing cable to infer three-dimensional locations of microseismic events and calculate fracture geometry parameters by correlating microseismic events with fracture planes, employing a catch percentage parameter and intersecting locus rings with assumed fracture planes to reduce ambiguity in source-location determination.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Measurement precision

If a DAS cable is used for microseismic monitoring, then cost and operational advantages are achieved along with longer sensing aperture and denser spatial sampling, but broadside sensitivity is lost resulting in non-unique source-location determination

Engineering Contradiction:
Improvesource-location determination accuracyVSAvoiddirectional polarization information
Core Design Contradiction:
Measurement precisionVSLoss of information

Solution Approach 1:

The patent uses an offset well as an intermediary structure to deploy the DAS cable at a location separated from the treatment well. This geometric arrangement allows the DAS cable to detect microseismic events from multiple angles, effectively using the offset well as a mediator to overcome the single-directional sensitivity limitation of DAS technology.

Inventive Principle:
Principle #24Intermediary (Mediator)

Solution Approach 2:

The patent transitions from two-dimensional source location (horizontal plane only) to three-dimensional source location by incorporating vertical depth information. This is achieved by using arrival time differences at multiple sensor locations along the DAS cable and applying wave propagation models to calculate depth, thereby adding the vertical dimension to resolve the non-unique source location problem.

Inventive Principle:
Principle #17Another dimension (Dimensionality change)

2Ease of operation

If a single straight portion of DAS cable is available, then deployment simplicity is maintained, but the exact source-location of microseismic events becomes undefined

Engineering Contradiction:
Improvedeployment simplicityVSAvoidsource-location accuracy
Core Design Contradiction:
Ease of operationVSMeasurement precision

Solution Approach 1:

The patent divides the monitoring system into two independent but complementary components: (1) a DAS cable deployed in an offset well for detecting microseismic events, and (2) a separate fracture detection system that uses the detected events to characterize fracture geometry. This segmentation allows each component to be optimized independently while achieving the overall goal of accurate fracture characterization.

Inventive Principle:
Principle #1Segmentation

Solution Approach 2:

The patent resolves the source location ambiguity by adding the vertical depth dimension. Instead of attempting to improve horizontal resolution alone, the system uses arrival time analysis and wave propagation modeling to calculate the vertical position of microseismic events, transforming the problem from 2D to 3D space and enabling unique source location determination.

Inventive Principle:
Principle #17Another dimension (Dimensionality change)

3Device complexity

If DAS cable lacks directional polarization sensing, then device complexity is reduced, but interpretive value of microseismic results is significantly reduced

Engineering Contradiction:
Improvesensor system complexityVSAvoidinterpretive value of results
Core Design Contradiction:
Device complexityVSLoss of information

Solution Approach 1:

The patent employs computational algorithms as intermediaries to extract fracture geometry information from the limited DAS data. These algorithms analyze arrival times, amplitude ratios, and spatial distributions of microseismic events to infer fracture orientation and geometry, effectively using computation as a mediator to compensate for the lack of direct directional polarization measurements.

Inventive Principle:
Principle #24Intermediary (Mediator)

Solution Approach 2:

The patent performs preliminary characterization of the offset well geometry and seismic velocity model before conducting microseismic monitoring. This preliminary work includes determining wellbore trajectory, calculating expected wave propagation paths, and establishing reference models. By preparing these foundations in advance, the system maximizes the interpretive value of the DAS data without requiring complex real-time processing during events.

Inventive Principle:
Principle #10Preliminary action

Applied Scientific Principles

This section explains which scientific principles are used to turn an abstract innovation direction into a practical engineering solution.

Function Achieved in This Case

This approach allows for the derivation of accurate three-dimensional microseismic event clouds and fracture geometry parameters, enhancing the accuracy of fracture geometry estimation despite the limitations of DAS cable sensitivity.

Implementation Method 1

a collection of P-wave and S-wave arrival time values from a microseismic event are received from the acoustic sensing cable

Methodology Applied
Scientific EffectAcoustic emission: Acoustic Emission

Data Source

PatentUS11796696B2Spatially locating a microseismic event utilizing an acoustic sensing cable
Publication Date: 2023.10.24 HALLIBURTON ENERGY SERVICES INC
  • US11796696B2 patent drawing
  • US11796696B2 patent drawing
  • US11796696B2 patent drawing

AI summary

The disclosure is directed to a method of utilizing an acoustic sensing cable, such as a fiber optic distributed acoustic sensing (DAS) cable, in a borehole to detect microseismic events and to generate three dimensional fracture plane parameters utilizing the detected events. Alternatively, the method can use various categorizations of microseismic data subsets to generate one or more potential fracture planes. Also disclosed is an apparatus utilizing a single acoustic sensing cable capable of detecting microseismic events and subsequently calculating fracture geometry parameters. Additionally disclosed is a system utilizing a processor to analyze collected microseismic data to generate one or more sets of fracture geometry parameters.