DOI https://doi.org/10.36487/ACG_repo/2645_33
Cite As:
Divasto Vergara, C, Barindelli Pizarro, G & Quiroz Alegría, R 2026, 'Fragmentation assessment in caving mining: operational evidence
from Chuquicamata underground mine', in A van As, D Cumming-Potvin & J Wesseloo (eds),
Caving 2026: Proceedings of the Sixth International Conference on Block and Sublevel Caving, Australian Centre for Geomechanics, Perth, pp. 1-14,
https://doi.org/10.36487/ACG_repo/2645_33
Abstract:
A quantitative fragmentation assessment is presented for the Chuquicamata underground mine based on the integration of operational evidence obtained from drawpoint granulometric mapping, records of secondary breakage of oversized fragments, and production extraction reports. The study focuses on the macroblocks MB N01-S01, MB N02-N03, and MB S02-S03, using a comprehensive multi-source database collected between 2019 and 2025. This database comprises more than 7,500 drawpoint inspections, 5,000 geometric measurements of rock fragments, and a continuous record of secondary breakage events. This robust dataset enables a comprehensive evaluation of fragmentation behaviour at the drawpoint scale under deep caving mining conditions.
The analysis examines the relationship between observed fragmentation, the basic geotechnical units (BGUs) model and the extraction height, with the primary objective of identifying systematic trends in granulometric evolution as caving progresses. Furthermore, operationally derived fragmentation results are compared with the prognosis developed by SRK in 2021 for the first lift of extraction (Lift 1). The findings indicate that the measured fragmentation is consistently finer than projected across the analysed sectors, revealing critical deviations in specific units such as the Potassic East Porphyry unit, where models based on discrete fracture network and block caving fragmentation (DFN-BCF) methodology significantly overestimated the rock mass competency and blockiness. Moreover, the results suggest that the model algorithm underestimates the fines fraction due to the comminution process inherent to secondary fragmentation.
Fundamental contributions of this research include identifying a tendency towards more elongated geometries as fragment size increases, which contradicts the traditional spherical assumption commonly used in theoretical estimations. Additionally, the study demonstrates that recorded secondary breakage events constitute a more robust and statistically representative operational proxy for tracking the oversize fraction than visual drawpoint mapping, which is biased toward the fines fraction. Nevertheless, both the frequency of secondary breakage and P80 values from field mapping reflect a consistent tendency to progressively decrease as extraction height increases.
References:
Barindelli, G 2016, Propiedades de Roca Intacta Macrobloques Centrales (Intact Rock Properties of Central Macroblocks), Informe SGT-INF-001/2016, Superintendencia Geotecnia, Gerencia Recursos Mineros & Desarrollo, Mina Subterránea, División Chuquicamata de Codelco-Chile.
Barindelli, G 2018, Estimación de las Propiedades Geotécnicas Macrobloques N2 al N4 y S2 al S3 y Prognosis de Propiedades Geotécnicas Macrobloques N5 al N7 y S4 al S7, Lift 1 (Estimation of Geotechnical Properties for Macroblocks N2 to N4 and S2 to S3 and Prognosis of Geotechnical Properties for Macroblocks N5 to N7 and S4 to S7, Lift 1), Informe GRMD-SPMS-INF-005/2018, Superintendencia Planificación Mina Subterránea, División Chuquicamata de Codelco-Chile.
Castro, R, Arancibia, L & Gómez, R 2022, ‘Quantifying fines migration in block caving through 3D experiments’, International Journal of Rock Mechanics and Mining Sciences, vol. 151, no. 105033, pp. 1365–1609,
Guajardo, C & Russo, A 2021, Reporte Final de la Estimación de Fragmentación para los Macrobloques del Primer y Segundo Nivel de Minera Chuquicamata Subterránea (Final Report of the Fragmentation Estimation for the First and Second Level Macroblocks of the Chuquicamata Underground Mine), SRK Consulting, Santiago, N° Proyecto: 01-2400-01, 42p.
Gy, PM 1967, Memoires du Bureau de Recherches Geologiques Minieres (Memoirs of the Bureau of Geological and Mining Research), no. 56, (Chapitre 4, Theorie de l'enchantillonnageequiprobable, pp. 42-51), Paris.
Hadjigeorgiou, J & Lessard, J 2007, ‘Numerical investigations of ore pass hang-up phenomena’, International Journal of Rock Mechanics and Mining Sciences, vol. 44, issue 6, pp. 820–834,
Sneed, E & Folk, R 1958, ‘Pebbles in the Lower Colorado River, Texas a study in particle morphogenesis’, Journal of Geology, vol. 66, no. 2, pp. 114–150,
Vega, E, Espiñeira, D & Barindelli, G 2024, Generación de Modelo Implícito de Unidades Geotécnicas Básicas Mina Chuquicamata 2024 (Generation of the Implicit Model of Basic Geotechnical Units Chuquicamata Mine 2024), Informe GRMD-SEG-INF-036/2024, Superintendencia de Estudios Geomecánicos, Gerencia de Recursos Mineros y Desarrollo, Mina Subterránea, División Chuquicamata de Codelco-Chile.
Vesilind, P 1980, ‘The Rosin-Rammler Particle Size Distribution’, Resource Recovery and Conservation, vol. 5, pp. 275–277.