Related Experiment Video
Updated: Feb 28, 2026

09:37
Visualization of Flow Field Around a Vibrating Pipeline Within an Equilibrium Scour Hole
Published on: August 26, 2019
6.2K
Three-Dimensional Array Interpolation Imaging Algorithm of Water Holdup by the Capacitance Array Tool of Oil-Water
Doujuan Zhang1,2, Haimin Guo1,3, Yongtuo Sun1,3
1College of Geophysics and Petroleum Resources, Yangtze University, Wuhan 430100, China.
Sensors (Basel, Switzerland)
|February 27, 2026
Summary
This study introduces a 3D visualization method for oil-water flow in horizontal wells using Capacitance Array Tool data. Natural neighbor interpolation offers superior accuracy for complex flow fields, outperforming linear and cubic spline methods.
Area of Science:
- Petroleum Engineering
- Fluid Dynamics
- Geophysics
Background:
- Gravitational differentiation causes asymmetric oil-water two-phase flow in horizontal wells.
- Existing logging techniques struggle to accurately characterize these complex wellbore flow fields.
- Precise characterization is crucial for reservoir management and production optimization.
Purpose of the Study:
- To develop a 3D visualization method for water holdup fields in horizontal wells.
- To evaluate the performance of linear, cubic spline, and natural neighbor interpolation algorithms for this visualization.
- To identify the most suitable interpolation method for different flow conditions.
Main Methods:
- Utilized data from a Capacitance Array Tool.
- Employed a multiphase flow experimental platform with oil and water.
- Systematically varied flow rates, water cuts, and imaging angles.
- Applied and compared three interpolation algorithms: linear, cubic spline, and natural neighbor.
Main Results:
- Natural neighbor interpolation demonstrated superior accuracy and robustness in complex flow states due to its topological reconstruction capabilities.
- Linear and cubic spline interpolation performed adequately only in stable, low-to-moderate flow conditions.
- The study systematically analyzed 3D imaging characteristics across various experimental parameters.
Conclusions:
- Natural neighbor interpolation is recommended for complex flow states or when high imaging detail is required, despite higher computational costs.
- Linear or cubic spline interpolation are suitable for simpler flow states due to their computational efficiency.
- The proposed 3D visualization method enhances the characterization of challenging multiphase flow in horizontal wells.
Keywords:
Capacitance Array Toolhorizontal wellsinterpolation algorithmsoil–water two-phase flowthree-dimensional visualizationMore Related Videos
Related Concept Videos
Indefinite Integrals
106
The water inflow rate into a storage tank is not constant but increases over time. Initially, the pump delivers water at a rate of 5 L/min. However, the inflow rate increases by 2 L/min for each additional minute due to rising pressure or system adjustments. This scenario can be described mathematically by a linear function:It is necessary to integrate the inflow rate function to measure the total volume of water added to the tank over time. The total water volume V(t) is obtained by performing...
106
Uniform Depth Channel Flow: Problem Solving
560
To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...
560
Uniform Depth Channel Flow
680
Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
680

