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Rock Engineering and Rock Mechanics: Structures in and on Rock Masses – Alejano, Perucho, Olalla & Jiménez (Eds) © 2014Taylor & Francis Group, London, 978-1-138-00149-7 Artificial Neural Network (ANN) based model for predicting of overall strength ofVolcanic Bimrock H. Sonmez, A. Coskun, M. Ercanoglu, D. Turer & K.E. Kasapoglu Department of Geological Engineering, Applied Geology Division, Hacettepe University, Beytepe, Ankara, Turkey C. Tunusluoglu Department of Geological Engineering, Applied Geology Division, Canakkale Onsekizmart Universitesi, Çanakkale, Turkey ABSTRACT: The uniaxial compressive strength of rock material (UCS) is one of the fundamental input parameters for engineering applications to be constructed on/in rock masses such as deep slopes, tunnels and dams. However, preparation of the high quality cores for laboratory studies is generally difficult for some types of rock such as laminated and/or fragmented rock material. To overcome this difficulty empirical prediction models were developed by considering some input parameters. Geological mixtures composed of rock blocks surrounded by weak matrix material are known as Block-In-Matrix-Rock (Bimrock) in literature. Agglomerate is a special type of Bimrock, which is composed of andesite fragments surrounded by tuff matrix and it is an example of Volcanic Bimrock. Preparation of core samples for experimental studies from agglomerate is problematic due to the strength contrast between andesite rock fragments and tuff matrix. To overcome these difficulties, some prediction tools have been studied by regression analyses in the literature. In this study,Artificial Neural Network (ANN) as a prediction tool was used to construct a model for prediction of overall UCS ofVolcanic Bimrock. While Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and fractal dimensions (1 and 2 dimensional) were selected as input parameters, normalized overall uniaxal strength of agglomerate to uniaxal compressive strength of tuff matrix is output parameter. Fractal geometry has been used as popular method to define irregular shapes as a quantity in literature. The boundary strength between an-desite fragments and tuff matrix is also sensitive to fragment shape and surface roughness of andesite fragments. Therefore fractal dimensions were selected as input parameters to incorporate this effect on boundary strength. While previously developed computer code FRACRUN was used to determine average fractal dimension of andesite fragments in agglomerate cores, previously developed computer code ANNES was used for ANN based model construction. In addition, similar toVolumetric Joint Count (Jv) which is widely used in rock mass characterization,Volumetric Block Count (VBC) was defined as another input parameter for determination of Bimrock UCS considering some of studies about performed in literature. The highest prediction performance was obtained from the model which considers Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and 1D fractal dimension as inputs. 1 INSTRUCTION Uniaxial compressive strength of rock material is a crucial input parameter for engineering designs to be constructed in/on rock masses. The uniaxial com- pressive strength of rock material is determined by conventional laboratory tests employed on high qual- ity core samples. However, for some rocks such as laminated and fragmented rock materials, prepara- tion of high quality cores is almost impossible. To overcome this difficulty some empirical prediction models for Ankara agglomerate studied in literature (Gokceoglu 2002, Sonmez et al. 2004, Sonmez et al 2006a) Mixtures of rocks composed of geotechnically significant strong blocks, within a bonded weak matrix of finer texture defined as Bimrock by Medley (1994). Preparation of cores from Bimrocks is extraordinarily difficult due the strength contrast between blocks and weak matrix. Bimrocks are divided mainly into two subgroups namely welded and unwelded Bimrocks (Altinsoy 2006, Sonmez & Tunusluoglu 2010). While the strength between matrix and blocks is almost equal to the strength of matrix for welded Bimrocks, the strength between matrix and blocks is less than strength of matrix for unwelded Bimrocks. In this study, Ankara agglomerate which is a kind of welded Volcanic Bimrock was considered as the study rock material (Fig. 1). While Volumetric Block Propor- tion (VBP), Volumetric Block Count (VBC), fractal dimensions (1 and 2 dimensional) were selected as input parameters, normalized overall uniaxal strength of agglomerate to uniaxal compressive strength of tuff 83

Artificial Neural Network (ANN) based model for predicting of overall strength of Volcanic Bimrock

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The uniaxial compressive strength of rock material (UCS) is one of the fundamental input parameters for engineering applications to be constructed on/in rock masses such as deep slopes, tunnels and dams. However, preparation of the high quality cores for laboratory studies is generally difficult for some types ofrock such as laminated and/or fragmented rock material. To overcome this difficulty empirical prediction models were developed by considering some input parameters. Geological mixtures composed of rock blocks surrounded by weak matrix material are known as Block-In-Matrix-Rock (Bimrock) in literature. Agglomerate is a special type of Bimrock, which is composed of andesite fragments surrounded by tuff matrix and it is an example ofVolcanic Bimrock. Preparation of core samples for experimental studies from agglomerate is problematic dueto the strength contrast between andesite rock fragments and tuff matrix. To overcome these difficulties, some prediction tools have been studied by regression analyses in the literature. In this study,Artificial Neural Network (ANN) as a prediction tool was used to construct a model for prediction of overall UCS of Volcanic Bimrock. While Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and fractal dimensions (1 and 2dimensional) were selected as input parameters, normalized overall uniaxal strength of agglomerate to uniaxal compressive strength of tuff matrix is output parameter. Fractal geometry has been used as popular method to define irregular shapes as a quantity in literature. The boundary strength between an-desite fragments andtuff matrix is also sensitive to fragment shape and surface roughness of andesite fragments. Therefore fractaldimensions were selected as input parameters to incorporate this effect on boundary strength. While previously developed computer code FRACRUN was used to determine average fractal dimension of andesite fragments in agglomerate cores, previously developed computer code ANNES was used for ANN based model construction. In addition, similar to Volumetric Joint Count (Jv) which is widely used in rock mass characterization, VolumetricBlock Count (VBC) was defined as another input parameter for determination of Bimrock UCS considering some of studies about performed in literature. The highest prediction performance was obtained from the model which considers Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and 1D fractal dimension as inputs.

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Page 1: Artificial Neural Network (ANN) based model for predicting of overall strength of Volcanic Bimrock

Rock Engineering and Rock Mechanics: Structures in and onRock Masses – Alejano, Perucho, Olalla & Jiménez (Eds)

© 2014 Taylor & Francis Group, London, 978-1-138-00149-7

Artificial Neural Network (ANN) based model for predictingof overall strength of Volcanic Bimrock

H. Sonmez, A. Coskun, M. Ercanoglu, D. Turer & K.E. KasapogluDepartment of Geological Engineering, Applied Geology Division, Hacettepe University, Beytepe, Ankara, Turkey

C. TunusluogluDepartment of Geological Engineering, Applied Geology Division, Canakkale Onsekizmart Universitesi,Çanakkale, Turkey

ABSTRACT: The uniaxial compressive strength of rock material (UCS) is one of the fundamental inputparameters for engineering applications to be constructed on/in rock masses such as deep slopes, tunnels anddams. However, preparation of the high quality cores for laboratory studies is generally difficult for some types ofrock such as laminated and/or fragmented rock material. To overcome this difficulty empirical prediction modelswere developed by considering some input parameters. Geological mixtures composed of rock blocks surroundedby weak matrix material are known as Block-In-Matrix-Rock (Bimrock) in literature. Agglomerate is a specialtype of Bimrock, which is composed of andesite fragments surrounded by tuff matrix and it is an example ofVolcanic Bimrock. Preparation of core samples for experimental studies from agglomerate is problematic dueto the strength contrast between andesite rock fragments and tuff matrix. To overcome these difficulties, someprediction tools have been studied by regression analyses in the literature. In this study,Artificial Neural Network(ANN) as a prediction tool was used to construct a model for prediction of overall UCS of Volcanic Bimrock.While Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and fractal dimensions (1 and 2dimensional) were selected as input parameters, normalized overall uniaxal strength of agglomerate to uniaxalcompressive strength of tuff matrix is output parameter. Fractal geometry has been used as popular methodto define irregular shapes as a quantity in literature. The boundary strength between an-desite fragments andtuff matrix is also sensitive to fragment shape and surface roughness of andesite fragments. Therefore fractaldimensions were selected as input parameters to incorporate this effect on boundary strength. While previouslydeveloped computer code FRACRUN was used to determine average fractal dimension of andesite fragments inagglomerate cores, previously developed computer code ANNES was used for ANN based model construction.In addition, similar to Volumetric Joint Count (Jv) which is widely used in rock mass characterization, VolumetricBlock Count (VBC) was defined as another input parameter for determination of Bimrock UCS consideringsome of studies about performed in literature. The highest prediction performance was obtained from the modelwhich considers Volumetric Block Proportion (VBP), Volumetric Block Count (VBC) and 1D fractal dimensionas inputs.

1 INSTRUCTION

Uniaxial compressive strength of rock material is acrucial input parameter for engineering designs tobe constructed in/on rock masses. The uniaxial com-pressive strength of rock material is determined byconventional laboratory tests employed on high qual-ity core samples. However, for some rocks such aslaminated and fragmented rock materials, prepara-tion of high quality cores is almost impossible. Toovercome this difficulty some empirical predictionmodels for Ankara agglomerate studied in literature(Gokceoglu 2002, Sonmez et al. 2004, Sonmez et al2006a) Mixtures of rocks composed of geotechnicallysignificant strong blocks, within a bonded weak matrixof finer texture defined as Bimrock by Medley (1994).

Preparation of cores from Bimrocks is extraordinarilydifficult due the strength contrast between blocks andweak matrix. Bimrocks are divided mainly into twosubgroups namely welded and unwelded Bimrocks(Altinsoy 2006, Sonmez & Tunusluoglu 2010). Whilethe strength between matrix and blocks is almostequal to the strength of matrix for welded Bimrocks,the strength between matrix and blocks is less thanstrength of matrix for unwelded Bimrocks. In thisstudy, Ankara agglomerate which is a kind of weldedVolcanic Bimrock was considered as the study rockmaterial (Fig. 1). While Volumetric Block Propor-tion (VBP), Volumetric Block Count (VBC), fractaldimensions (1 and 2 dimensional) were selected asinput parameters, normalized overall uniaxal strengthof agglomerate to uniaxal compressive strength of tuff

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Figure 1. View from Ankara Agglomerate (Sonmez &Tunuslugolu 2010).

matrix is obtained as the output parameter. The arti-ficial neural network (ANN) was used as a predictiontool for construction of the models. Prediction per-formances of the generated models were compared interms of fractal dimensions (1 and 2 dimensional).

2 PROPERTIES OF THE DATABASE ANDDETERMINATION OF FRACTALDIMENSIONS

In this study, the database established by Sonmez &Tunusluoglu (2010) was considered. Establishment ofdatabase was performed on total of 70 core specimenhaving 6 cm diameter and height between 2 to 2.5. Thetop and the bottom circular surfaces and rectangularcylindrical side of the samples were scanned for imageanalysis. Then unit weight (γ) and uniaxial compres-sive strength (UCS) of each core were determined bylaboratory tests as suggested by ISRM (2007).

As it can be followed from the literature, fractaldimension (D) is a statistical quantity that gives anindication of how completely a fractal appears to fillspace, as one zooms down to finer and finer scales (Das2011). In literature, fractal geometry has been used aspopular tool to define particularly irregular shapes bythe theory of fractal developed by Mandelbrot (1967)(Hyslip & Vallejo 1997, Kruhl & Nega 1996, Bagdeet al. 2002, Gulbin & Evangulova 2003, Pardini 2003,Kolay & Kayabali 2006, Hamdi 2008, Zorlu 2009,Sezer 2009). In this study, square gridcell (box) countmethod for 2D and segment (line) count method for1D were followed in the algorithm of FRACRUN.FRACRUN has the capability of determining frac-tal dimensions of many closed polygons on a singleimage, with a click on the start button.The calculationsin 1D and 2D procedure for a single shape followedby FRACRUN are summarized in Figure 2.

While, the relation between overall strength ofBimrock and volumetric block proportion (VBP) hasbeen widely investigated in the literature, some studieswere focused on the characterization of Bimrocks suchas determination of volumetric block proportion, blocksize distribution and their quantification (Lindquist

Figure 2. Schematically illustration for determination of 2D(box-count) and 1D (segment-line count) fractal dimensionsof a single block (Sonmez & Tunusoglu 2010).

1994, Lindquist & Goodman 1994, Medley 2002). Inthis study, by considering the studies performed onthe quantification of blocks in Bimrocks, volumetricblock count (VBC) was defined as additional inputparameter together with VBP. Because the amount ofthe weakest component may depends not only on VBPbut also on VBC. In counting of the number of block ina volume, the engineering volume should be defined.For this study, engineering volume was considered asthe volume of cores. Therefore the number of blockcounted for each core was used as VBC in number ofblock/cubic unit. The VBC values may include someerrors due to counting of blocks on 2D scanned images.

3 ARTIFICIAL NEURAL NETWORK (ANN)BASED MODELS

Considering the simple regression relations betweenUCS and input parameters, two multi inputs ANNmodels were investigated. While VBP, VBC and 1Dwere used as multi input parameters for the first model,

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Figure 3. A criteria for termination of training and selectionof optimum network architecture (Basheer & Hajmeer, 2000).

2D were considered as input parameters instead of 1Dfor the second model.

ANN has been one of the attractive predictiontool used in geo-engineering applications due to thehigh performance on the modeling of nonlinear mul-tivariate problems (Sonmez et al. 2006b). The back-propagation artificial neural network among the othermethods has been widely considered for empiricalpredication models in geo-engineering applications(Goh et al. 1995, Shi et al. 1998, Neaupane & Achet2004, Lee et al. 2003, Gomez & Kavzoglu 2005,Ermini et al. 2005, Yesilnacar & Topal 2005, Sonmezet al. 2006b).

Although the complexity of BMNN architectureincreases by addition of hidden layers, the simpleststructure having sufficient and applicable predictioncapacity is preferred to avoid overlearning. Each layerincluding input(s) and output(s) layers consist of neu-rons (nodes), and the neurons are joined by weightedlinks. The final weights and thresholds of activationfor decreasing the error between observed and com-puted outputs under a sufficient level defined by useris set by training phase of ANN algorithm (Sonmezet al. 2006b). The sigmoid transfer function is consid-ered as an activation function in this study, because itis commonly preferred in application of predicationpurposes. The maximum number of training cycles(epoch) for back and forward stages is limited by10000, together with the minimum threshold for rootmean square error (RMSE) as 0.001.

Another important point of the ANN applicationis avoiding of overlearning, otherwise ANN maylose its generalization capacity (Fig. 3). While thelearning rate was used as 0.1, the momentum coef-ficient was set to 0.95, considering recommendationand application used in literature. For solution ofthe most problems by ANN one hidden layer maybe sufficient (Rumelhart et al. 1986, Hect-Neilsen1987, Lippmann 1987, Basheer 2000). By considering

Figure 4. The ANN architecture considered in this study.

Figure 5. The graph of root mean square error (RMSE)versus number of cycles (epochs) for two models.

the recommendation mentioned in the literature, onehidden layer was preferred in this study.

Overlearning problem may be observed when largenumber of neurons preferred in hidden layers. For thispropose some recommendation is available in litera-ture (Hecht-Nielsen, 1987, Hush 1989, Ripley 1993,Wang 1994, Masters 1994, Kaastra & Boyd 1996,Kannellopoulas & Wilkinson 1997). In this study,three neurons were used by considering number ofinputs and output (Fig. 4).

Whole data in the database were normalizedbetween 0 and 1. Then the database composed of 70data set was divided into 55 data set for training (∼80%of data) and 15 data set for testing (∼20% of data set).After ANNES was run for both first and second mod-els, the graph for number of training cycle versus rootmean square error for both training and testing datasets were drawn as in Figure 5.

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Figure 6. Cross correlation between predicted and mea-sured UCS values of Bimrock cores for two models.

RMSE values of testing data tends to increase after∼2100 cycles (epoch) and ∼1900 for the first (inputs:VBC, VBP, 1D) and the second (inputs: VBC, VBP,2D), respectively. Therefore, above these thresholds,generalization of the models decreases. By using theweights and thresholds of activation at 2100th and1900th epochs for the two models predicted values oftraining and testing data were generated by ANNES.Then comparison of the two models was made by crosscorrelation graph (Figure 6).

As it can be followed from Figure 6, the first modelwhich consider 1D (segment-line) fractal dimensionexhibit slightly better prediction capacity than the sec-ond model which considers 2D (box-counting) fractaldimension. Because 1D fractal dimension have bettercapability for defining roughness of the blocks.

4 RESULTS AND CONCLUSIONS

In this study, Ankara agglomerate as a kind of vol-canic bimrock was selected for the study material.

Preparation of cores for laboratory test from Bimrocksis extraordinarily difficult due the strength contrastbetween blocks and weak matrix. The artificial neuralnetwork (ANN) was used for construction of the UCSprediction models. The main important findings of thestudy can be summarized as follows.

The use of Volumetric Block Count (VBC) togetherwithVolumetric Block Proportion (VBP) exhibits highimportance on the prediction of overall strength ofBimrocks.

1D (line) fractal dimension seems to be more sensi-tive than 2D fractal as input parameter on prediction ofoverall strength of Bimrock. Because 1D (line) fractaldimension may define roughness of andesite blocks(grain) better than 2D fractal dimension. Similar tothe study carried by Kolay & Kayabali (2006), higher1D fractal dimension is obtained for rougher grains.The contact strength between matrix and blocks maybe expected to be higher with the increase of surfaceroughness of the blocks as emphasized in literature.

ACKNOWLEDGEMENT

The database used in this study was established duringTUBITAK Project (The Scientific and TechnologicalResearch Council of Turkey, Project No: 108Y002).

REFERENCES

Altinsoy H. 2006. Matriks içinde blok içeren kayalarınmakaslama dayanımın belirlenmesi için fiziksel modelesaslı bir arastırma. MSc thesis, Hacettepe University (inTurkish).

Aycan C., Sonmez H., Kasapoglu K.E., Dinc O. & Tunuslu-oglu C., 2010. Determination of Uniaxial CompressiveStrength of Ankara Agglomerate Considering FractalGeometry of Blocks. Geophysical Research Abstracts,Vol. 12, EGU2010-5899, EGU General Assembly 2010.

Bagde M.N., Raina A.K., Chakraborty A.K. & Jethwa J.L.,2002. Rock mass characterization by fractal dimension.Engineering Geology 63, 141–155.

Baheer I., 2000. Selection of methodology for modeling hys-teresis behavior of soils using neural networks. J Computaided Civil Infrastruct Engg 2000; 5(6): 445–463.

Basheer I.A. & Hajmeer, M., 2000. Artificial neural net-works: fundamentals, computing, design, and application.J of Microbiological Methods 2000; 43: 3–31

Das S. 2011. Functional Fractional Calculus. 2nd edition.Springer-Verlag Berlin Heidelberg.

Ermini L. Catani, F. & Casagli N. 2005. Artificial NeuralNetworks applied to landslide susceptibility assessment.Geomorphology 2005; 66: 327–343.

Goh A.T.C., Wong, K.S. & Broms, B.B. 1995. Estimation oflateral wall movements in braced excavations using neuralnetworks. Can Geotech J 1995; 32: 1059–1064.

Gokceoglu C. 2002. A fuzzy triangular chart to predict theuniaxial compressive strength of the Ankara agglomer-ates from their petrographic composition. EngineeringGeology, 66 (1–2), 39–51.

Gomez H. & Kavzoglu T. 2005. Assessment of shallow land-slide susceptibility using artificial neural networks inJabonosa River Basin, Venezuela. Engineering Geology2005; 78: 11–27.

86

Page 5: Artificial Neural Network (ANN) based model for predicting of overall strength of Volcanic Bimrock

Gulbin Y.L. & Evangulova E.B. 2003. Morphometry ofquartz aggregates in granites: fractal images referring tonucleation and growth processes. Mathematical Geology35 (7), 819–833

Hamdi E. 2008.A fractal description of simulated 3D discon-tinuity networks. Rock Mechanics and Rock Engineering41, 587–599.

Hecht-Nielsen R. 1987. Kolmogorov’s mapping neural net-work existence theorem. Poc of the First IEEE Interna-tional Conference on Neural Networks, San Diego CA,USA 1987; 11–14.

Hush D.R. 1989. Classification with neural networks: a per-formance analysis. Proc. Of the IEEE Int Conf on systemsEngg, Dayton Ohia USA 1989; 277-280.

Hyslip J.P. & Vallejo, L.E., 1997. Fractals analysis of theroughness and size distribution of granular materials.Engineering Geology 48, 231–244.

ISRM 2007. Ulusay, R.; Hudson, J.A., eds. The Blue Book –The Complete ISRM Suggested Methods for Rock Char-acterization,Testing and Monitoring: 1974–2006.Ankara:ISRM & ISRM Turkish National Group. p. 628. ISBN978-975-93675-4-1.

Kaastra I. & Boyd M. 1996. Designing a neural network forforecasting financial and economic time series, Neuro-computing 1996; 10(3): 215–236.

Kanellopoulas I. & Wilkinson G.G. 1997. Strategies and bestpractice for neural network image classification, Interna-tional Journal of Remote Sensing 1997; 18: 711–725.

Kolay E. & Kayabali K. 2006. Investigation of the effectof aggregate shape and surface roughness on the slakedurability index using the fractal dimension approach.Engineering Geology 86, 271–294.

Kruhl J.H. & Nega M. 1996. The fractal shape of suturedquartz grain boundaries: application as a geothermometer.Geologische Rundschau 85, 38–43.

Lee S., Ryu J.H., Lee M.J. & Won J.S. 2003. Use of an arti-ficial neural network for analysis of the susceptibility tolandslides at Boun, Korea. Environmental Geology 2003;44: 820-833.

Lindquist E. S. 1994. The Strength and Deformation Proper-ties of Melange, Ph.D. Dissertation, Department of CivilEngineering, University of California at Berkeley.

Lindquist E.S. & Goodman R.E. 1994. Strength and deforma-tion properties of a physical model mélange, Proceedings,1st NorthAmerican Rock Mechanics Symposium,Austin,TX, May 1994.

Lippmann R.P. 1987. An introduction to computing withneural nets. IEEE ASSP Mag 1987; 4: 4–22.

Mandelbrot B. 1967. “How Long Is the Coast of Britain?Statistical Self-Similarity and Fractional Dimension”,Science, New Series, Vol. 156, No. 3775. (May 5, 1967),pp. 636–638.

Masters T. 1994. Practical Neural Network Recipes in C++.Academic Press, Boston MA 1994.

Medley E.W. (1994) “Engineering characterization ofmélanges and similar block-in-matrix rocks (bim-rocks)” PhD Dissertation, Dept. Civil Engineering, Univ.California at Berkeley.

Medley E. 2002. Estimating block size distributions ofmélanges and similar block-in-matrix rocks (bimrocks),Proceedings, 5th North American Rock MechanicsSymposium, University of Toronto, Toronto, Canada,July 2002, pp. 599–606.

Neaupane K.M. & Achet S.H. 2004. Use of backpropagationneural network for landslide monitoring: a case study inthe higher Himalaya. Engineering Geology 2004; 74: 213–236.

Pardini G. 2003. Fractal scaling of surface roughness in arti-ficially weathered smectite rich soil regoliths. Geoderma117, 157–167.

Ripley B.D. 1993. Statistical aspects of neural networks. In:Barndoff-Neilsen OE, Jensen JL, Kendall WS (Eds.), Net-works and Chaos-Statistical and Probabilistic Aspects,Chapman & Hall, London 1993; 40–123.

Rumelhart D.E. & Hinton G.E. 1986. Williams RJ. Learn-ing internal representation by error propogation. In:Rumelhart DE, McClelland JL (Eds.), Parallel DistributedProcessing 1986; 1: 318–362.

Sezer E. 2009. A computer program for fractal dimen-sion (FRACEK) with application on type of massmovement characterization. Computers and Geosciences(doi:10.1016/j.cageo.2009.04.006).

Shi J., Ortiago J.A.R. & Bai, J. 1998. Modular neural net-works for predicting settlements during tunnelling. JGeotech Geo-Env Engg ASCE 1998; 124(5): 389–394

Sonmez H. & Tunusluoglu C. 2010. Eklemli KayaKütleleri ve BIMROCK’lar için Birlestirilmis JeomekanikSınıflama Siteminin ve Genellestirilmis AmpirikYaklasımın Gelistirilmesi. TUBITAK Proje No. 108Y002.(in Turksih)

Sonmez H., Tuncay E. & Gokceoglu C. 2004. Models to pre-dict the uniaxial compressive strength and the modulusof elasticity for Ankara Agglomerate. Int. J. Rock Mech.Min. Sci., 41 (5), 717–729.

Sonmez H., Gokceoglu C., Medley E.W., Tuncay E. &Nefeslioglu H.A. 2006a. Estimating the uniaxialcompressive strength of a volcanic bimrock. Int. J. RockMech. Min. Sci., 43 (4), 554–561.

Sonmez H., Gokceoglu C., Kayabasi A. & Nefeslioglu, H.A.2006b. Estimation of rock modulus: for intact rocks withan artificial neural network and for rock masses with anew empirical equation, Int. J. Rock Mech. Min. Sci., 200643(2), 224–235.

Wang C. 1994. A theory of generalization in learningmachines with neural application. PhD Thesis, The Univof Pennsylvania, USA 1994.

Yesilnacar E.K. & Topal T. 2005. Landslide Susceptibil-ity Mapping: comparison between logistic regressionand neural networks in a medium scale study, Hendekregion TURKEY), No. 251–2. “Engineering Geology”,79, (2005), pp. 251–266.

Zorlu K. 2008. Description of the weathering states of build-ing stones by fractal geometry and fuzzy inference systemin the Olba ancient city (Southern Turkey). EngineeringGeology 101 (2008), 124–133.

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