Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Propagation of Uncertainty from Random Error00:59

Propagation of Uncertainty from Random Error

1.2K
An experiment often consists of more than a single step. In this case, measurements at each step give rise to uncertainty. Because the measurements occur in successive steps, the uncertainty in one step necessarily contributes to that in the subsequent step. As we perform statistical analysis on these types of experiments, we must learn to account for the propagation of uncertainty from one step to the next. The propagation of uncertainty depends on the type of arithmetic operation performed on...
1.2K
Estimation of the Physical Quantities01:05

Estimation of the Physical Quantities

6.3K
On many occasions, physicists, other scientists, and engineers need to make estimates of a particular quantity. These are sometimes referred to as guesstimates, order-of-magnitude approximations, back-of-the-envelope calculations, or Fermi calculations. The physicist Enrico Fermi was famous for his ability to estimate various kinds of data with surprising precision. Estimating does not mean guessing a number or a formula at random. Instead, estimation means using prior experience and sound...
6.3K
Uncertainty: Confidence Intervals00:54

Uncertainty: Confidence Intervals

5.3K
The confidence interval is the range of values around the mean that contains the true mean. It is expressed as a probability percentage. The interpretation of a 95% confidence interval, for instance, is that the statistician is 95% confident that the true mean falls within the interval. The upper and lower limits of this range are known as confidence limits. The confidence limits for the true mean are estimated from the sample's mean, the standard deviation, and the statistical factor...
5.3K
Uncertainty: Overview00:59

Uncertainty: Overview

1.0K
In analytical chemistry, we often perform repetitive measurements to detect and minimize inaccuracies caused by both determinate and indeterminate errors. Despite the cares we take, the presence of random errors means that repeated measurements almost never have exactly the same magnitude. The collective difference between these measurements - observed values - and the estimated or expected value is called uncertainty. Uncertainty is conventionally written after the estimated or expected value.
1.0K
Quantifying Heat02:46

Quantifying Heat

57.1K
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...
57.1K
Propagation of Uncertainty from Systematic Error01:10

Propagation of Uncertainty from Systematic Error

961
The atomic mass of an element varies due to the relative ratio of its isotopes. A sample's relative proportion of oxygen isotopes influences its average atomic mass. For instance, if we were to measure the atomic mass of oxygen from a sample, the mass would be a weighted average of the isotopic masses of oxygen in that sample. Since a single sample is not likely to perfectly reflect the true atomic mass of oxygen for all the molecules of oxygen on Earth, the mass we obtain from this...
961

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Physics-informed two-tier neural network for non-linear model order reduction.

Advanced modeling and simulation in engineering sciences·2024
Same author

Global sensitivity study for irreversible electroporation: Towards treatment planning under uncertainty.

Medical physics·2023
Same author

3D multi-physics uncertainty quantification using physics-based machine learning.

Scientific reports·2022
Same author

Tuning the Pennes Perfusion Rate to Model Large Vessel Cooling Effects in Hepatic Radiofrequency Ablation.

Journal of biomechanical engineering·2022
Same author

Study of flow effects on temperature-controlled radiofrequency ablation using phantom experiments and forward simulations.

Medical physics·2021
Same author

Simulation study of the cooling effect of blood vessels and blood coagulation in hepatic radio-frequency ablation.

International journal of hyperthermia : the official journal of European Society for Hyperthermic Oncology, North American Hyperthermia Group·2021
Same journal

Application of ephrin-B2 loaded glycol chitosan-silk fibroin hydrogel in the treatment of diabetic refractory wounds.

Scientific reports·2026
Same journal

International expert Delphi consensus on thromboprophylaxis in metabolic and bariatric surgery.

Scientific reports·2026
Same journal

Assessing the cross-region knowledge transfer capability of selected deep learning building vectorization methods in the context of available training datasets.

Scientific reports·2026
Same journal

Feasibility and preliminary effects of outdoor versus indoor cognitive-motor therapy in women with Alzheimer's disease: A randomized single-blind pilot study.

Scientific reports·2026
Same journal

Hallmarks of social action in the vocal turn-taking of wild common marmosets (Callithrix jacchus).

Scientific reports·2026
Same journal

Role and mechanism of AOPPs-induced NOX4-mediated ferroptosis in intervertebral disc degeneration.

Scientific reports·2026
See all related articles

Related Experiment Video

Updated: Sep 30, 2025

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
11:19

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

Published on: October 21, 2016

12.0K

Uncertainty quantification for basin-scale geothermal conduction models.

Denise Degen1, Karen Veroy2,3, Florian Wellmann4

  • 1Computational Geoscience and Reservoir Engineering (CGRE), RWTH Aachen University, Wüllnerstraße 2, 52062, Aachen, Germany. denise.degen@cgre.rwth-aachen.de.

Scientific Reports
|March 11, 2022
PubMed
Summary
This summary is machine-generated.

This study introduces a faster simulation method for geothermal energy, enabling probabilistic predictions. This approach helps quantify subsurface uncertainties for responsible resource management and improved energy transition strategies.

More Related Videos

Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography
08:02

Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography

Published on: February 25, 2015

12.7K
Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

9.5K

Related Experiment Videos

Last Updated: Sep 30, 2025

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
11:19

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

Published on: October 21, 2016

12.0K
Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography
08:02

Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography

Published on: February 25, 2015

12.7K
Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

9.5K

Area of Science:

  • Geophysics
  • Energy Science
  • Computational Science

Background:

  • Geothermal energy is a key renewable resource for the energy transition, offering a low CO2 footprint.
  • Accurate subsurface characterization is crucial for responsible geothermal resource management, but often involves high uncertainties.
  • Traditional deterministic simulations are insufficient for quantifying these uncertainties, and probabilistic approaches are computationally infeasible due to long simulation times.

Purpose of the Study:

  • To develop and implement a computationally efficient method for generating full state predictions in geothermal simulations.
  • To enable probabilistic simulations and inverse approaches by significantly reducing computation time.
  • To provide tools for quantifying and communicating subsurface uncertainties in geothermal energy applications.

Main Methods:

  • Utilized a reduced basis method to significantly decrease geothermal simulation runtimes.
  • Integrated the reduced basis method into an existing simulation framework.
  • Generated 2D and 3D predictive uncertainty maps for geothermal applications.

Main Results:

  • The reduced basis method enables the generation of full state predictions, drastically cutting simulation time.
  • Probabilistic simulations and inverse approaches become feasible, allowing for uncertainty quantification.
  • Predictive uncertainty maps were generated, identifying regions with high temperatures and low uncertainties.

Conclusions:

  • The developed method facilitates responsible geothermal resource management by enabling uncertainty quantification.
  • The approach significantly reduces simulation times, making probabilistic analyses practical.
  • The flexible implementation allows for transferability to other geophysical simulations requiring state and uncertainty information.