Geostatistics is a branch of statistics focusing on spatial or spatiotemporal datasets. Developed originally to predict probability distributions of ore grades for mining operations, it is currently applied in diverse disciplines including petroleum geology, hydrogeology, hydrology, meteorology, oceanography, geochemistry, geometallurgy, geography, forestry, environmental control, landscape ecology, soil science, and agriculture (esp. in precision farming). Geostatistics is applied in varied branches of geography, particularly those involving the spread of diseases (epidemiology), the practice of commerce and military planning (logistics), and the development of efficient spatial networks. Geostatistical algorithms are incorporated in many places, including geographic information systems (GIS) and the R statistical environment.
Geostatistics is intimately related to interpolation methods, but extends far beyond simple interpolation problems. Geostatistical techniques rely on statistical models that are based on random function (or random variable) theory to model the uncertainty associated with spatial estimation and simulation.
A number of simpler interpolation methods/algorithms, such as inverse distance weighting, bilinear interpolation and nearest-neighbor interpolation, were already well known before geostatistics. Geostatistics goes beyond the interpolation problem by considering the studied phenomenon at unknown locations as a set of correlated random variables.
Let Z(x) be the value of the variable of interest at a certain location x. This value is unknown (e.g. temperature, rainfall, piezometric level, geological facies, etc.). Although there exists a value at location x that could be measured, geostatistics considers this value as random since it was not measured, or has not been measured yet. However, the randomness of Z(x) is not complete, but defined by a cumulative distribution function (CDF) that depends on certain information that is known about the value Z(x):
Typically, if the value of Z is known at locations close to x (or in the neighborhood of x) one can constrain the CDF of Z(x) by this neighborhood: if a high spatial continuity is assumed, Z(x) can only have values similar to the ones found in the neighborhood. Conversely, in the absence of spatial continuity Z(x) can take any value. The spatial continuity of the random variables is described by a model of spatial continuity that can be either a parametric function in the case of variogram-based geostatistics, or have a non-parametric form when using other methods such as multiple-point simulation or pseudo-genetic techniques.
By applying a single spatial model on an entire domain, one makes the assumption that Z is a stationary process. It means that the same statistical properties are applicable on the entire domain. Several geostatistical methods provide ways of relaxing this stationarity assumption.
In this framework, one can distinguish two modeling goals:
- Estimating the value for Z(x), typically by the expectation, the median or the mode of the CDF f(z,x). This is usually denoted as an estimation problem.
- Sampling from the entire probability density function f(z,x) by actually considering each possible outcome of it at each location. This is generally done by creating several alternative maps of Z, called realizations. Consider a domain discretized in N grid nodes (or pixels). Each realization is a sample of the complete N-dimensional joint distribution function
- In this approach, the presence of multiple solutions to the interpolation problem is acknowledged. Each realization is considered as a possible scenario of what the real variable could be. All associated workflows are then considering ensemble of realizations, and consequently ensemble of predictions that allow for probabilistic forecasting. Therefore, geostatistics is often used to generate or update spatial models when solving inverse problems.
Kriging is a group of geostatistical techniques to interpolate the value of a random field (e.g., the elevation, z, of the landscape as a function of the geographic location) at an unobserved location from observations of its value at nearby locations.
Multiple-indicator kriging (MIK) is a recent advance on other techniques for mineral deposit modeling and resource block model estimation, such as ordinary kriging. Initially, MIK showed considerable promise as a new method that could more accurately estimate overall global mineral deposit concentrations or grades.
- Turning bands
- Cholesky Decomposition
- Truncated Gaussian
- Spectral simulation
- Sequential Indicator
- Sequential Gaussian
- Dead Leave
- Transition probabilities
- Markov chain geostatistics
- Markov mesh models
- Support vector machine
- Boolean simulation
- Genetic models
- Pseudo-genetic models
- Cellular automata
- Multiple-Point Geostatistics
Definitions and tools
- Regionalized variable theory
- Covariance function
- Range (geostatistics)
- Sill (geostatistics)
- Nugget effect
- Training image
Main scientific journals related to geostatistics
- Water Resources Research
- Advances in Water Resources
- Ground Water
- Mathematical Geosciences
- Computers & Geosciences
- Computational Geosciences
- J. Soil Science Society of America
- Remote Sensing of the Environment
- Stochastic Environmental Research and Risk Assessment
Scientific organisations related to geostatistics
- European Forum for Geography and Statistics (EFGS; formerly the European Forum for Geostatistics)
- GeoEnvia promotes the use of geostatistical methods in environmental applications
- International Association for Mathematical Geosciences
- GsLib A classical open-source package dedicated to geostatistics, source code in Fortran 77 and 90.
- PyGSLIB A python module built with codified GSLIB source code wrapped into python and Cython functions for drillhole processing, block modeling, computational geometry, VTK support and non-linear geostatistics
- SGeMS An open-source package dedicated to geostatistics with user-friendly interface, source code in C++ with the GsTL a dedicated geostatistics C++ template library.
- Isatis A complete proprietary solution for geostatistics and ressource estimation.
- Geostat A complete proprietary solution for geostatistics, geological modelling and ressource estimation, see SGS Genesis.
- The R programming language has around 20 other packages dedicated to geostatistics, and around 30 dedicated to other areas of spatial statistics.
- D-STEM is a software based on the MATLAB language able to handle spatiotemporal univariate and multivariate datasets. The software allows to produce dynamic maps of the observed variables over geographic regions.
- Multivariate interpolation
- Spline interpolation
- Geodemographic segmentation
- Remote sensing
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- Mariethoz, Gregoire, Caers, Jef (2014). Multiple-point geostatistics: modeling with training images. Wiley-Blackwell, Chichester, UK, 364 p.
- Hansen, T.M., Journel, A.G., Tarantola, A. and Mosegaard, K. (2006). "Linear inverse Gaussian theory and geostatistics", Geophysics 71
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- Remy, N., et al. (2009), Applied Geostatistics with SGeMS: A User's Guide, 284 pp., Cambridge University Press, Cambridge.
- Deutsch, C.V., Journel, A.G, (1997). GSLIB: Geostatistical Software Library and User's Guide (Applied Geostatistics Series), Second Edition, Oxford University Press, 369 pp., http://www.gslib.com/
- Chilès, J.-P., and P. Delfiner (1999), Geostatistics - Modeling Spatial Uncertainty, John Wiley & Sons, Inc., New York, USA.
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- Kitanidis, P.K. (1997) Introduction to Geostatistics: Applications in Hydrogeology, Cambridge University Press.
- Wackernagel, H. (2003). Multivariate geostatistics, Third edition, Springer-Verlag, Berlin, 387 pp.
- Deutsch, C.V., (2002). Geostatistical Reservoir Modeling, Oxford University Press, 384 pp.,
- Tahmasebi, P., Hezarkhani, A., Sahimi, M., 2012, Multiple-point geostatistical modeling based on the cross-correlation functions, Computational Geosciences, 16(3):779-79742,
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- Finazzi, F. and Fassò, A. (2014). "D-STEM: A Software for the Analysis and Mapping of Environmental Space-Time Variables", Journal of Statistical Software 62(6)
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- ISO/DIS 11648-1 Statistical aspects of sampling from bulk materials-Part1: General principles
- Lipschutz, S, 1968, Theory and Problems of Probability, McCraw-Hill Book Company, New York.
- Matheron, G. 1962. Traité de géostatistique appliquée. Tome 1, Editions Technip, Paris, 334 pp.
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- McGrew, J. Chapman, & Monroe, Charles B., 2000. An introduction to statistical problem solving in geography, second edition, McGraw-Hill, New York.
- Merks, J W, 1992, Geostatistics or voodoo science, The Northern Miner, May 18
- Merks, J W, Abuse of statistics, CIM Bulletin, January 1993, Vol 86, No 966
- Myers, Donald E.; "What Is Geostatistics?
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- Sharov, A: Quantitative Population Ecology, 1996, http://www.ento.vt.edu/~sharov/PopEcol/popecol.html
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- Strahler, A. H., and Strahler A., 2006, Introducing Physical Geography, 4th Ed., Wiley.
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- Volk, W, 1980, Applied Statistics for Engineers, Krieger Publishing Company, Huntington, New York.
- GeoENVia promotes the use of geostatistical methods in environmental applications, and organizes bi-annual conferences.
- Kriging link, contains explanations of variance in geostats
- Arizona university geostats page
- AI-Geostats, a resource on the internet about geostatistics and spatial statistics
- On-Line Library that chronicles Matheron's journey from classical statistics to the new science of geostatistics
- http://www.geostatscam.com Is the site of Jan W. Merks, who claims that geostatistics is "voodoo science" and a "scientific fraud"
- It is a group for exchanging of ideas and discussion on multiple point geostatistics (MPS).