Related Experiment Video
Updated: Jan 11, 2026

08:25
Measurements of Local Instantaneous Convective Heat Transfer in a Pipe - Single and Two-phase Flow
Published on: April 30, 2018
7.6K
Development of a Transient Wellbore Heat Transfer Model Validated with Distributed Temperature Sensing Data
Rion Nakamoto1, Smith Leggett1
1Bob L. Herd Department of Petroleum Engineering, Texas Tech University, 807 Boston Ave, Lubbock, TX 79409, USA.
Sensors (Basel, Switzerland)
|November 13, 2025
Summary
Distributed temperature sensing (DTS) provides valuable geothermal well data. A new transient wellbore model, validated with DTS, accurately predicts thermal slug velocity for improved geothermal operations.
Area of Science:
- Geothermal Energy Engineering
- Reservoir Characterization
- Wellbore Heat Transfer
Background:
- Distributed temperature sensing (DTS) is crucial for geothermal energy development, offering insights into wellbore temperature and flow.
- Existing wellbore models often use steady-state assumptions, failing to capture transient dynamics, or are computationally intensive.
Purpose of the Study:
- Develop and validate a transient wellbore heat transfer model for geothermal applications.
- Enhance the interpretation of DTS data for improved operational monitoring and management.
Main Methods:
- Formulated a transient wellbore heat transfer model using a thermal-analogy approach.
- Implemented the model using a finite-difference scheme.
- Validated the model by comparing predicted thermal slug velocities with DTS measurements.
Main Results:
- The model demonstrated strong agreement with DTS data, confirming its reliability.
- Modeled thermal slug velocity was found to be lower than fluid velocity, indicating slower thermal front propagation.
- The computationally efficient model enhances DTS data interpretation.
Conclusions:
- The developed transient wellbore heat transfer model is a reliable tool for analyzing geothermal operations.
- This approach improves the understanding of transient thermal dynamics in wellbores.
- The model facilitates better monitoring and management of geothermal energy resources.
Related Concept Videos
Mechanisms of Heat Transfer II
4.2K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
4.2K
Mechanisms of Heat Transfer I
5.9K
Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.
5.9K
Mechanisms of Heat Transfer
1.6K
Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
1.6K
Quantifying Heat
61.5K
Thermal Energy Microscopically, thermal energy is the kinetic energy associated with the random motion of atoms and molecules. Temperature is a quantitative measure of “hot” or “cold”, which depends on the amount of thermal energy. When the atoms and molecules in an object are moving or vibrating quickly, they have a higher average kinetic energy (KE) (or higher thermal energy), and the object is perceived as “hot”, or it is described as being at a higher temperature. When the...
61.5K
Heat Flow and Specific Heat
6.5K
Heat is a type of energy transfer that is caused by a temperature difference, and it can change the temperature of an object. Since heat is a form of energy, its SI unit is the joule (J). Another common unit of energy often used for heat is the calorie (cal), which is defined as the energy needed to change the temperature of 1 g of water by 1 °C, specifically between 14.5 °C and 15.5 °C, since the energy needed shows a slight temperature dependence. Another commonly used unit is...
6.5K
Mechanism of heat transfer
1.8K
Understanding heat transfer mechanisms is essential for understanding how our bodies maintain balance in different environmental conditions. When the environment is thermoneutral, the body is in a state of balance, neither using nor releasing energy to maintain its core temperature. However, when the environment is not thermoneutral, the body employs four heat transfer mechanisms to maintain homeostasis: conduction, convection, evaporation, and radiation. These mechanisms facilitate heat...
1.8K

