BREUSCH-PAGAN TEST: A COMPREHENSIVE EVALUATION OF ITS PERFORMANCE IN DETECTING HETEROSCEDASTICITY ACROSS LINEAR, EXPONENTIAL, QUADRATIC, AND SQUARE ROOT STRUCTURES USING MONTE CARLO SIMULATIONS
DOI:
https://doi.org/10.33003/fjs-2024-0806-2826Keywords:
Breusch-Pagan test, Heteroscedasticity, Monte Carlo simulations, Statistical inference, Econometrics, Regression analysisAbstract
This study provides a comprehensive evaluation of the Breusch-Pagan test's performance in detecting heteroscedasticity across various structures and levels, addressing a significant gap in existing literature. Through Monte Carlo simulations, we investigate the test's power, Type II errors ( = 0), and Type I errors ( 0) in confirming homoscedasticity assumptions at different sample sizes (100, 250, and 500). Our objectives include assessing the test's ability to detect heteroscedasticity at various levels and structures, examining the impact of sample size on its performance, comparing its performance across different structures, and identifying its limitations and potential biases. Our findings reveal that the Breusch-Pagan test's performance varies across different heteroscedasticity structures and levels, with poor detection of low-level heteroscedasticity but improved performance at higher levels, particularly for exponential heteroscedasticity structures (EHS). While increased sample size enhances the test's performance, it remains inadequate for linear heteroscedasticity structures (LHS) and square root heteroscedasticity structures (SQRTHS). Based on our results, we recommend cautious use of the Breusch-Pagan test, especially when dealing with low-level heteroscedasticity or specific structures like LHS and SQRTHS. We suggest using the test with moderate to high sample sizes for improved performance, particularly for EHS and quadratic heteroscedasticity structures (QHS). For researchers with limited sample sizes or dealing with LHS and SQRTHS, alternative tests for heteroscedasticity may be considered. Finally, we emphasize the importance of assessing the underlying structure of heteroscedasticity in the dataset to choose the most suitable test and interpretation.
References
Ajibade, A. C. (1976). Provisional classification of the Schists Belts of North Western Nigeria In: in Kogbe, C.A Geology of Nigeria, Elizabethan Publishing Company, Lagos, Nigeria:pp85-90.
Ajibade. A. C., Woakes, M., and Rahaman, M. A. (1987). Proterozoic Crustal Development in the Pan-African Regime of Nigeria. In: C. A. Kogbe (ed), Geology of Nigeria 2nd revised edition, Rock View Nigeria limited, Jos: pp. 57-69.
Black, R., Caby, R., Monssine Pouchkin, A., Bayer, R., Bertrand, J. M., Bourllier, A. M., Fabri, J. and Lesquer, A. (1979). Evidence for Late Precambrian plate tectonics in West Africa. Nature. 278: 233–237.
Batchelor, R. A, Bowden, P. (1985). Petrogenetic interpretation of granitoid rock series using multicationic parameters. Journal of Chemical Geology 48: 43–55.
Burke, K. C and Dewey, J. F. (1972). Orogeny in Africa. In: African Geology, T.F.J. Dessauvagie and A.J. Whiteman (eds.), University of Ibadan Press: pp583-608.
Chappell, B. W. and White, A. J. R. (1974). Two contrasting granite types. Pacific journal geology, 8: 173-174.
Chappell, B. W., White. A. J. R. (2001). Two Contrasting Granite Types: 25 years later. Australian Journal of Earth Sciences 48: 489-499.
Cox, K. G., Ball, J. D., Pankhurst, R. J. (1979). The Interpretation of Igneous Rocks. Allen and Unwin, London: p. 450.
Dada, S. S. (1999). Geochemistry and petrogenensis of the reworked gneiss complex of North Central Nigeria: Major and trace elements studies on Kaduna amphibolites and migmatite gneisses. Global Journal of Pure and Applied Sciences. 5 (4): 535-543.
Debon, F. and Le Forte, P. (1983). A chemical-mineralogical Classification of common Plutonic Rocks and Association. Earth Sciences, 73: 135-149.
El-Bouseily, A. M. and El-Sokkary A. A. (1975). The relationship between Rb,Sr and Ba in granite rocks. Journal Of chemical geology 16: 207-219.
Eleftheriadis, G., and Koroneos A. (2003). Geochemistry and petrogenesis of post-collision Pangeon Granitoids in Central Macedonia, northern Greece. Chemie der Erde 63 (2): 364–389.
Emmermann, R., Daieva, L., and Schneider, J. (1975). Petrological significance of rare earth distribution in granites. Contribution to mineralogy and petrology, 52: 267-283.
Fitches, W. R., Ajibade, A. C., Egbuniwe, I. G., Holt, R. W., and Wright J. B. (1985). Late Proterozoic Schist belts and plutonism in NM Nigeria. Journal of Geological Society of London. 142: 319–337.
Harker, A. (1909). The natural history of Igneous Rocks. Methuen, London. Pp. 384.
Harris, N. B. W., Pearce, J. A. and Tindle, A. G. (1986). Geochemical characteristics of Collision Zone Magmatism. In: Coward, M.P., Ries, A.C (eds.), Collision Tectonics, Geological Society, London Special Publication, 19: pp. 67-81.
Hassanen M. A., El-nisr S. A., and Mohamed F. H. (1996). Geochemistry and Petrogenesis of Pan-African I-type granitoids at Gabal Igla Ahmar, Eastern Desert, Egypt. Journal of African Earth Science 22 (1): 29-42.
Hayatu and Ibrahim (2024): Field Geology And Petrography Of Basement Rocks Around Makarfi Area, Northwestern Nigeria Basement Complex, Article In press.
Henderson P. (1984): Rare Earth Element geochemistry. Elsevier, Amsterdam: pp. 234- 510.
Janousek V., Vrana S. and Ervan, V. (2002). Petrology, geochemical character and Petrogenesis of a Variscan post-orogenic granite: case study from the Sevetin Massif, Moldanubian batholith, southern Bohemia. Journal of the Czech Geological Society 47: 1-2.
Ogunyele, A., & Akingboye, A. (2018). Tin Mineralisation in Nigeria: A Review. Environmental and Earth Sciences Research Journal, 5(1), 15–23. https://doi.org/10.18280/eesrj.050103.
McCurry, P. (1976). The geology of the Precambrian to Lower Palaeozoic rocks of Northern Nigeria. A review In: C.A. Kogbe, (Editor), Geology of Nigeria. Elizabethan Publication Company, Lagos Nigeria: pp15-39.
Nakamura, N. (1974): Determination of REE, Ba, Fe, Mg, Na and K in Carbonaceous and ordinary Chondrites. Geochemistry Acta, 38: 757-775.
Published
How to Cite
Issue
Section
FUDMA Journal of Sciences