- Volumes 108-119 (2025)
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Volumes 96-107 (2025)
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Volume 107
Pages 1-376 (December 2025)
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Volume 106
Pages 1-336 (November 2025)
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Volume 105
Pages 1-356 (October 2025)
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Volume 104
Pages 1-332 (September 2025)
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Volume 103
Pages 1-314 (August 2025)
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Volume 102
Pages 1-276 (July 2025)
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Volume 101
Pages 1-166 (June 2025)
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Volume 100
Pages 1-256 (May 2025)
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Volume 99
Pages 1-242 (April 2025)
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Volume 98
Pages 1-288 (March 2025)
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Volume 97
Pages 1-256 (February 2025)
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Volume 96
Pages 1-340 (January 2025)
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Volume 107
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Volumes 84-95 (2024)
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Volume 95
Pages 1-392 (December 2024)
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Volume 94
Pages 1-400 (November 2024)
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Volume 93
Pages 1-376 (October 2024)
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Volume 92
Pages 1-316 (September 2024)
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Volume 91
Pages 1-378 (August 2024)
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Volume 90
Pages 1-580 (July 2024)
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Volume 89
Pages 1-278 (June 2024)
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Volume 88
Pages 1-350 (May 2024)
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Volume 87
Pages 1-338 (April 2024)
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Volume 86
Pages 1-312 (March 2024)
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Volume 85
Pages 1-334 (February 2024)
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Volume 84
Pages 1-308 (January 2024)
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Volume 95
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Volumes 72-83 (2023)
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Volume 83
Pages 1-258 (December 2023)
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Volume 82
Pages 1-204 (November 2023)
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Volume 81
Pages 1-188 (October 2023)
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Volume 80
Pages 1-202 (September 2023)
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Volume 79
Pages 1-172 (August 2023)
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Volume 78
Pages 1-146 (July 2023)
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Volume 77
Pages 1-152 (June 2023)
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Volume 76
Pages 1-176 (May 2023)
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Volume 75
Pages 1-228 (April 2023)
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Volume 74
Pages 1-200 (March 2023)
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Volume 73
Pages 1-138 (February 2023)
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Volume 72
Pages 1-144 (January 2023)
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Volume 83
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Volumes 60-71 (2022)
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Volume 71
Pages 1-108 (December 2022)
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Volume 70
Pages 1-106 (November 2022)
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Volume 69
Pages 1-122 (October 2022)
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Volume 68
Pages 1-124 (September 2022)
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Volume 67
Pages 1-102 (August 2022)
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Volume 66
Pages 1-112 (July 2022)
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Volume 65
Pages 1-138 (June 2022)
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Volume 64
Pages 1-186 (May 2022)
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Volume 63
Pages 1-124 (April 2022)
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Volume 62
Pages 1-104 (March 2022)
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Volume 61
Pages 1-120 (February 2022)
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Volume 60
Pages 1-124 (January 2022)
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Volume 71
- Volumes 54-59 (2021)
- Volumes 48-53 (2020)
- Volumes 42-47 (2019)
- Volumes 36-41 (2018)
- Volumes 30-35 (2017)
- Volumes 24-29 (2016)
- Volumes 18-23 (2015)
- Volumes 12-17 (2014)
- Volume 11 (2013)
- Volume 10 (2012)
- Volume 9 (2011)
- Volume 8 (2010)
- Volume 7 (2009)
- Volume 6 (2008)
- Volume 5 (2007)
- Volume 4 (2006)
- Volume 3 (2005)
- Volume 2 (2004)
- Volume 1 (2003)
• We proposed a sediment height criterion applicable to solids concentration profiles.
• The criterion was able to track the upper and lower sedimentation interfaces.
• Axial concentration profiles are usual outputs of continuum models.
• The proposed methodology fit several tested cases.
The sedimentation process is mainly characterized by two interfaces: the upper interface, which defines the separation between the clarified zone and a concentrated zone; the lower interface, which defines the separation between the compacted structure and the suspension. Continuum models for the sedimentation process usually have the local solids concentration as output. The upper interface is easy to track in many experiments, as just before the interface, the solids concentration is near zero. However, at the compression zone, there may be no jump of concentration to clearly define the lower interface. The difficulty appears also in computational analyses. In this work, we proposed a sediment height criterion to track the lower interface based on the numerical concentration profiles and the derivatives of the concentration with respect to depth. We employed a previously developed and validated continuum model for sedimentation of non-Newtonian suspensions and simulated cases of drilling fluids confined in the annulus of an oil well to evaluate the performance and applicability of the criterion. The model was discretized using the finite volume method and implemented, alongside the proposed criterion. A base case was considered, and derived cases were studied, including cases with linear and geothermal temperature profiles. A case with two confined suspensions was analyzed. The evolution of upper and lower interfaces over time, using the proposed criterion, has shown the expected behavior based on the classical sedimentation theory. The temperature profiles played a key role in the evolution of the interfaces, particularly the upper one, where there was no linear regime. This effect was attributed to changes in the free settling zone caused by local variation of temperature, which impacted the rheology and affected the equilibrium of the zone.