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Related Concept Videos

Propagation of Uncertainty from Systematic Error01:10

Propagation of Uncertainty from Systematic Error

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 particular...
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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...
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Flood risk assessment involves careful planning and analysis to ensure the safety of communities near water retention structures. Capacity contours are a vital tool in this process, as they illustrate the potential spread of water at specific levels in a given area. In the context of building a bund across a small valley, these contours play a critical role in evaluating the safety of nearby residential areas.In this example, the bund is intended to store stormwater in the valley. The engineers...
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Variance

The deviations show how spread out the data are about the mean. A positive deviation occurs when the data value exceeds the mean, whereas a negative deviation occurs when the data value is less than the mean. If the deviations are added, the sum is always zero. So one cannot simply add the deviations to get the data spread. By squaring the deviations, the numbers are made positive; thus, their sum will also be positive.The standard deviation measures the spread in the same units as the data.

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Using semivariogram parameter uncertainty in hydrogeological applications.

Eulogio Pardo-Igúzquiza1, Mario Chica-Olmo, Maria Jose Garcia-Soldado

  • 1Department of Geodynamics/CEAMA, University of Granada, Campus Fuentenueva, 18071 Granada, Spain. pardoiguzquiza@yahoo.es

Ground Water
|September 17, 2008
PubMed
Summary
This summary is machine-generated.

Uncertainty in geostatistical models, common in groundwater hydrology, can bias results. This study proposes using a range of plausible models to improve spatial interpolation and risk assessment accuracy.

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Area of Science:

  • Geosciences
  • Hydrogeology
  • Spatial Statistics

Background:

  • Geostatistical methods like kriging and simulation are vital in groundwater hydrology for spatial interpolation and risk assessment.
  • These methods rely on spatial variability models (semivariograms) inferred from limited data, introducing uncertainty.
  • Using a single fitted model with small datasets can lead to biased predictions in groundwater resource management.

Purpose of the Study:

  • To address the uncertainty associated with semivariogram model selection in geostatistics.
  • To develop a methodology that accounts for the range of plausible semivariogram models.
  • To improve the reliability of geostatistical predictions in groundwater hydrology.

Main Methods:

  • Maximum likelihood inference to quantify semivariogram model uncertainty.
  • Propagating uncertainty from plausible semivariogram models into kriging and simulation applications.
  • Applying the methodology to predict groundwater head using log-transmissivity data.

Main Results:

  • Demonstrated a method to evaluate and incorporate semivariogram parameter uncertainty.
  • Showcased the impact of using a range of plausible models versus a single model on final geostatistical results.
  • Successfully applied the approach in a case study of the Vega de Granada aquifer.

Conclusions:

  • Accounting for semivariogram uncertainty is crucial for robust geostatistical analysis in groundwater hydrology.
  • The proposed method enhances the reliability of spatial interpolation and risk assessment by considering model plausibility.
  • This approach provides a more realistic representation of prediction uncertainty in groundwater studies.