Numerical simulations of comminution slurries over complex topographies: Putting together CFD and pipeline integrity
Author
dc.contributor.author
Trewhela, Tomás
Author
dc.contributor.author
Ihle Bascuñán, Christian
es_CL
Author
dc.contributor.author
Tamburrino Tavantzis, Aldo
es_CL
Admission date
dc.date.accessioned
2014-12-15T14:39:54Z
Available date
dc.date.available
2014-12-15T14:39:54Z
Publication date
dc.date.issued
2014
Cita de ítem
dc.identifier.citation
Minerals Engineering 63 (2014) 139–148
en_US
Identifier
dc.identifier.other
dx.doi.org/10.1016/j.mineng.2014.03.005
Identifier
dc.identifier.uri
https://repositorio.uchile.cl/handle/2250/126572
General note
dc.description
Artículo de publicación ISI
en_US
Abstract
dc.description.abstract
The use of computational fluid dynamics gives new and interesting insights for risk analysis of crosscountry
ore hydraulic transport operations. In particular, they offer the possibility to predict, with reasonable
accuracy, the progression and final condition of spills driven by pipeline leaks at selected locations,
at a relatively modest computational cost. In this work, a depth-averaged, two-dimensional numerical
model is used to simulate an ore concentrate pipeline rupture and subsequent spill, reproduced as a constant
flow condition at the leak point. Although the model is well suited to solve the governing flow equations
on arbitrary topographies by means of digital elevation models, two specific locations featuring
relatively mild and steep slopes, are analysed with regard to their implications on the potential requirements
for emergency team response. Results, obtained using different slurry rheologies, are compared
with those obtained using a simpler, common flow resistance model derived for water flowing over rough
surfaces.
en_US
Patrocinador
dc.description.sponsorship
The authors gratefully acknowledge support from the
Department of Civil Engineering of University of Chile and the
Chilean National Commission for Scientific and Technological
Research, CONICYT, through Fondecyt Project No. 11110201 and
1130910. The first author would also like to thank the scholarship
for Master Program CONICYT-PFCHA/Magíster Nacional/2013 folio
221320183.