Understanding the Bouguer Anomaly A Gravimetry Puzzle 1st edition by Roman Pašteka, Ján Mikuška, Bruno Meurers 0128129142 9780128129142

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ISBN-10 :  0128129142 

ISBN-13 : 9780128129142

Author: Roman Pašteka, Ján Mikuška, Bruno Meurers 

Understanding the Bouguer Anomaly: A Gravimetry Puzzle addresses the geophysical and geodetic applications of gravity field interpretation, taking into account the evaluation of the Bouguer anomaly. Containing several contributions that deal with persistent questions in gravity data processing and providing verified workflows, the book covers historical and practical aspects of the Bouguer anomaly.

Geophysicists and exploration geologists will gain advanced knowledge in gravimetry, physical geodesy and an understanding of the evaluation and impact of the Bouguer anomaly in gravity field measurement.

Understanding the Bouguer Anomaly. A Gravimetry Puzzle 1st Table of contents:

1 Introduction
References
2 The Physical Meaning of Bouguer Anomalies—General Aspects Revisited
2.1 Introduction
2.2 Scalar Versus Vector Representation
2.3 The Geophysical Indirect Effect
2.4 Truncation Error of the Mass Correction
2.5 Normal Gravity Calculation in Areas With Negative Ellipsoidal Heights
2.6 Conclusion
References
3 Some Remarks on the Early History of the Bouguer Anomaly
3.1 Introduction
3.2 The Early Days: Geodesic Mission to Ecuador (Then Peru) and the Book of Bouguer (1749)
3.3 Reductions of Gravity or the Pendulum Length to the Sea Level
3.3.1 The So-Called Bouguer Reduction
3.3.2 The So-Called Free-Air or Faye Reduction
3.3.3 When and by Whom the Reductions to the Sea Level Were Introduced Remains at Least Partly Unkno
3.3.4 The First Initiative Against Reductions to the Sea Level
3.4 Additional Discussion
3.4.1 Bouguer (1749)
3.4.1.1 Some Interesting Quotations
3.4.1.2 Prediction or Reduction?
3.4.1.3 Bouguer’s First Term
3.4.1.4 Bouguer’s Second Term: The Free-Air, Faye, or Height Correction/Reduction Is Actually Due
3.4.1.5 Bouguer’s Third Term
3.4.1.6 Some of the Reasons Why Bouguer’s Density Estimation of the Topographic Masses Was Unreali
3.4.2 Faye (1880–95)
3.4.3 Helmert (1884)
3.4.4 Putnam (1895)
3.4.5 Hayford and Bowie (1912)
3.4.6 Bullard (1936)
3.4.7 Abandoning Reductions to the Sea Level
3.4.8 Just Three Terminological Comments
3.5 Conclusions
Acknowledgments
References
4 Normal Earth Gravity Field Versus Gravity Effect of Layered Ellipsoidal Model
4.1 Introduction
4.2 Some Problems With the Normal Field
4.3 The Gravity Potential and Gravity Effect of the Equipotential Model
4.4 The Gravity Potential and Gravity Effect of the Layered Model
4.5 Comparison of the Results for the Equipotential and the Layered Models
4.6 Relation of the Normal Field to the Free-Air Correction
4.7 Conclusion
Acknowledgments
References
5 Numerical Calculation of Terrain Correction Within the Bouguer Anomaly Evaluation (Program Toposk)
5.1 Introduction
5.2 Main Features of the New Software Toposk
5.3 Inner Zone T1
5.4 Intermediate Zone T2
5.5 Outer Zones T31 and T32
5.6 User Interface
5.7 Program Testing on Synthetic Data
5.8 Real Data Calculations
5.9 Conclusions
Acknowledgments
References
6 Efficient Mass Correction Using an Adaptive Method
6.1 Introduction
6.2 Principle of Adaptive Algorithm
6.2.1 Variable resolution representation of topography
6.2.2 Adaptive Algorithm
6.2.3 Forward Calculation of Gravity
6.3 Test of Algorithm
6.3.1 Monte-Carlo-Analysis
6.3.1.1 Results
6.3.1.1.1 Influence of the Range on Success Rate
6.3.2 Real World Data
6.3.2.1 Tibetan Plateau
6.3.2.2 Influence of Resolution
6.3.2.3 Adaptive Algorithm
6.3.2.4 Global Calculation
6.4 Discussion
Acknowledgments
References
7 National Gravimetric Database of the Slovak Republic
7.1 Introduction
7.2 Compilation of Integrated Gravity Database
7.3 New Generation Bouguer Anomalies
7.4 New Linear Features Recognized in the Bouguer Anomaly Map
7.5 New Software for the Reconstruction of the Gravity Field from the Bouguer Anomaly Map
7.6 Conclusions

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Tags: Understanding, the Bouguer Anomaly, Gravimetry Puzzle, Roman Pašteka, Ján Mikuška, Bruno Meurers