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Heterogeneity and non-stationary variance in hard rock hydrogeology

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Heterogeneity and non-stationary variance in hard rock hydrogeology. Extreme variability and its role in hydrogeology. Land and Water Resources Engineering Robert Earon. Introduction. Anistropy. Heterogeneity. Possibilities. Concluding Remarks. - PowerPoint PPT Presentation
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Heterogeneity and non-stationary variance in hard rock hydrogeology Extreme variability and its role in hydrogeology Land and Water Resources Engineering Robert Earon
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Page 1: Heterogeneity and non-stationary variance in hard rock hydrogeology

Heterogeneity and non-stationary variance in hard rock hydrogeology

Extreme variability and its role in hydrogeology

Land and Water Resources EngineeringRobert Earon

Page 2: Heterogeneity and non-stationary variance in hard rock hydrogeology

• Changing Climate• Limited Storage• Increasing residency near coast• Heteroscedasticity

There is no annual shortage of water in Sweden.Problems arise due to temporal distribution of meteoric water and water storage.

Aug/07

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Grou

ndw

ater

Leve

l (m

und

er G

roun

d Su

rfac

e)

Glacial Till

Hard Rock

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 3: Heterogeneity and non-stationary variance in hard rock hydrogeology

Heterogeneity

Range

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Nugget

Sill

Page 4: Heterogeneity and non-stationary variance in hard rock hydrogeology

Spatial AnisotropyIntroduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 5: Heterogeneity and non-stationary variance in hard rock hydrogeology

Spatial AnisotropyIntroduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 6: Heterogeneity and non-stationary variance in hard rock hydrogeology

Spatial AnisotropyIntroduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 7: Heterogeneity and non-stationary variance in hard rock hydrogeology

Heterogeneity in spatial variance

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 8: Heterogeneity and non-stationary variance in hard rock hydrogeology

• ANOVA, t-test both indicate samples significantly (sig.<0.000) different

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 9: Heterogeneity and non-stationary variance in hard rock hydrogeology

Heterogeneity in spatial variance

AreaMedian

Distance (m) n Mean Median Variance Skewness KurtosisNorth 1802 10264 1.04 0.39 3.18 3.92 23.43South 1930 14169 1.45 0.53 5.46 3.33 15.32

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 10: Heterogeneity and non-stationary variance in hard rock hydrogeology

Multivariate Approach to Groundwater Resources

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 11: Heterogeneity and non-stationary variance in hard rock hydrogeology

Multivariate Approach to Groundwater Resources

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 12: Heterogeneity and non-stationary variance in hard rock hydrogeology

Review

• Heterogeneity places a high burden on point estimates for regional or even local characterization

• Heterogenic, anisotropic variability implies caution should be taken when applying statistical tools

• From the standpoint of limited-resource hydrogeological investigation, plausibility of applying and developing other tools

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks

Page 13: Heterogeneity and non-stationary variance in hard rock hydrogeology

Questions?

Introduction PossibilitiesHeterogeneityAnistropy Concluding Remarks


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