W.L. Oliveira‐Filho, UFOP D.R. Silva, SAMARCO F.E. Almeida, SAMARCO

Slides:



Advertisements
Similar presentations
ENV-2E1Y: Fluvial Geomorphology:
Advertisements

TVI Resource Development (Phils), Inc. September Canatuan Tailings Management Completion of Stage 1 Tailings Management Facilties Gossan Dam and.
1 Terramin TSF Base Lining Examining the design criteria :– a risk based design process Agenda for Strathalbyn CCC Meeting Review of the relevant components.
Bliss Area Sewage System Groundwater Monitoring Pete Ganzel Washington County Department of Public Health & Environment.
Introduction: Slopes either occur naturally or are engineered by humans. An understanding of geology, hydrology, and soil properties is central to applying.
Laboratory Characterization of Municipal Solid Waste Incineration Ash Sita Marie Syal, Mohammad Kabalan, Matt Hambright, and Dr. Dimitrios Zekkos, P.E.
Investigation of Consolidation Promoting Effect by Field and Model Test for Vacuum Consolidation Method Nagasaki University H.Mihara Y.Tanabasi Y.Jiang.
Evaluation of the Strength and Deformation Characteristics in Cohesive Soils caused by Back Pressure (Wednesday) Seoul National University Geotechnical.
Impacts of Seismic Stress on Pore Water Pressure in Clayey Soil By: Qazi Umar Farooq Lecturer Civil Engineering Dept Univ of Engg & Tech Taxila.
Chapter (1) Geotechnical Properties of Soil
Construction Monitoring For Earth Dams 1 Fars Science and Research Branch, Islamic Azad University.
Estimating Streamflow Channel Losses with the Green-Ampt Model Neil Hutten Ag Eng 558 April 20, 2001.
TECHNICAL REVIEW Initiated a review on the Abandonment and Restoration Plan of the Lupin Mine: –conducted August through October Team Members: –EBA.
Earthquake induced LIQUEFACTION by Jimmy McLauchlan Peat Nicholas Case study: Mexico City, 1985.
By John McDonald Industry Development Manager (NGIQ) IAL Conference June 2014.
1 Challenge the future Cake layer characteristics in long time ceramic MF filtration for surface water treatment Mingyang Li Master defence presentation.
MINE WASTE DUMP The Overburden of waste and uneconomic mineralized rock is required to be removed to mine the useful mineral resource in a surface mining.
Runoff Processes Reading: Applied Hydrology Sections 5.6 to 5.8 and Chapter 6 for Tuesday of next week.
LEQ: How does water move through underground layers of soil and rock?
© 2006 IARC VOC Emissions: Correlation between testing methodologies Dr. M Pharaoh, Dr. G.J.Williams, Ms. P Madden, Mr. N Reynolds W M G, University of.
1 st Young North Sea CCS Researchers meeting, 18 June 2014, Rotterdam 1Abidoye Luqman K. Abidoye
Dry Stacking of Cycloned Tailings
Consolidation Theory Examples.
Soil Water ContentSoil Moisture Content Water that may be evaporated from soil by heating at C to a constant weight Gravimetric moisture content.
School of Civil and Environmental Engineering Life Impact The University of Adelaide Water Balance and the Influence of Soil Structural Changes on Final.
Soils Investigation Soil Investigation
SOIL, GEOTECHNICAL ENGINEERING AND FOUNDATION ENGINEERING
Chapter 10: Fluids Three (common) phases of matter: 1. Solid: Maintains shape & size (approx.), even under large forces. 2. Liquid: No fixed shape. Takes.
Lecture 11 Evapotranspiration (4)
Soil Water Reading: Applied Hydrology Sections 4.1 and 4.2 Topics
Reference Manual Chapter 9
Presented by: 1. A measure of how easily a fluid (e.g., water) can pass through a porous medium (e.g., soils) 2 Loose soil - easy to flow - high permeability.
Soil water storage and mobility: Theoretical and Experimental Aspects Dr. Greg Butters Soil Physics Department of Soil and Crop Sciences A lecture for.
Linda C. Schaffner AIWA Conference November 18, 2010.
Damitha Abeynayaka (st109642)
TERRAMIN AUSTRALIA Limited
Soil Water Tension Department of Agricultural and Biological Engineering University of Illinois at Urbana-Champaign.
Dynamic Behaviour of Unsaturated CH soil under Cyclic Loading in Unconsolidated Undrained Conditions 5th Tongji-UBC Symposium on Earthquake Engineering,
 Draw a meander and label these locations: erosion, deposition, faster water, and slower water. Warm – Up 2/6.
P. Simms, S. Sivathayalan, F. Daliri Carleton University Desiccation in dewatering and strength development of high density hard rock tailings.
1 Effect of Tailings Properties on Paste backfill performance M. fall, M. Benzaazoua, S. Quellet ( University of Qucbec in Abitibi- Temiscamingus, Canada)
Geotechnical Engineering
Ground Improvement Dr. Talat Bader
Homework I will be ed It is also posted on the website.
Conclusions The states of the surface and root zoon soil moisture are considered as key variables controlling surface water and energy balances. Force-restore.
Results Time Study Site Measured data Alfalfa Numerical Analysis of Water and Heat Transport in Vegetated Soils Using HYDRUS-1D Masaru Sakai 1), Jirka.
Modern GROUND IMPROVEMENT TECHNIQUES FOR HIGHWAYS
Toolik 2015 Met Station Update Lily Cohen Jessica Cherry Brie Van Dam Photo: Justin Johnson.
 Installation. Schematic of a weighable gravitation lysimeter.
Soil Stress and Pore Water Pressure
Soil Physics David Zumr room: b608 Lecture (and seminar) notes will be available: -
Track Drainage CE2303 Railway Engineering. Drainage-General Drainage is the natural or artificial removal of surface and sub-surface water from an area.
SOIL MECHANICS AND FOUNDATION ENGINEERING-II (CE 311)
Field characterization of problematic earthfills, by DMT. A case history Nuno Cruz - MOTA-ENGIL; Universidade de Aveiro, Portugal Isabel Caspurro - Estradas.
CALCASEIU RIVER AND PASS DREDGED MATERIAL SEDIMENTATION STUDY.
GROUND IMPROVEMENT PRINCIPLES OF COMPACTION. A good foundation has a safe and economic design with the following properties: 1.Have adequate shearing.
Mechanical Operation ( ) Prepared By, Hardev Jadav ( ) Sanjay k Prajapati ( ) Ravina Solanki ( )
Soil wetting patterns under porous clay pipe subsurface irrigation A. A. Siyal 1 and T. H. Skaggs 2 1 Sindh Agriculture University, Tandojam, Sindh, Pakistan.
Soil-Water-Plant Relationships A. Background 1. Holdridge Life Zones 1.
Templars Primary School The development of whole school science planning.
GROUND IMPROVEMENT TECHNIQUES
The Institute of Hydrology of the Slovak Academy of Sciences,
Lecture 11 Evapotranspiration (4)
Methods Used to Determine Hydraulic Conductivity
Study Evaluation of Random Set Method on Results from Reliability analysis of Finite Element in Deep Excavation Article Code: 443 Presenter Mehdi Poormousavian.
Always Advancing Pervious
The application of an atmospheric boundary layer to evaluate truck aerodynamics in CFD “A solution for a real-world engineering problem” Ir. Niek van.
Earth Systems.
Groundwater Learning objectives
Scott McFarlane & Richard Merifield
Presentation transcript:

W.L. Oliveira‐Filho, UFOP D.R. Silva, SAMARCO F.E. Almeida, SAMARCO Thickening of iron ore tailings slimes using sub-aerial deposition: field experimental observations W.L. Oliveira‐Filho, UFOP D.R. Silva, SAMARCO F.E. Almeida, SAMARCO

Contents Introduction Background Field experimental studies Analyses of experimental data Conclusion

Introduction Desiccation & Sub-aerial Studies Timeline

Background Alternative disposal techniques for slimes Types sub-aerial deposition Thickened Paste filtered Common aspects Intermitent: cycles of waiting and disposal periods Physical processes: sedimentation, consolidation and desiccation

Background Desiccation Importance Triggering mechanisms The most effective phenomena for rehabilitation work, optimizing storage, and reducing risks regarding containment structure failure Triggering mechanisms Surface drying Lowering the GWT Driving force and Phases Suction 1D shrinkage 3D shrinkage (cracking) Comprehensive works Abu-Hejleh & Znidarcic (1995) and Yao et al. (2002) Konrad & Ayad (1997) Fujiyasu (1997)

Background Compressibility Constitutive relations Permeability Main input relationships for analyses with CONDES (Yao et al. 2002) Constitutive relations Compressibility Permeability Cracking function a - function

Field experimental studies Goal & strategies To gain some understanding of the main mechanisms that play a role in the sub-aerial method applied to Samarco’s slimes To investigate consolidation separately from desiccation using a field experiment To focus on slimes desiccation because was lesser known and more challenging

Field experimental studies Site & operations Location: inside the Germano tailings impoundment (Samarco Mineração S.A.) in Mariana, MG. Impoundment figures: 3 m high ring dyke, confining an area of 4,850 m2. Foundation: 2 m of coarse siliceous tailings, grading from fine sand to medium silt, underlain by a deep layer of iron tailings slimes. Ground water table: at the contact of those layers, 2 m below the surface. Drainage system: stop logs installed at the lower part (bottom at 2% slope) Access: a pier to the centre of the testing area for instrumentation maintenance and sampling operations Filling: slimes pumped from an adjacent slimes pond at the Germano impoundment Water cover: 5 to 10 cm deep during the filling process and consolidation period to prevent early desiccation. Surface water removal: for the desiccation part of the test.

Field experimental studies Instrumentation, testing & instalation Devices: Geotechnical: Thermistors, settlement devices (staff gauges), tensiometers, piezometers, time domain reflectometry probes (TDRs) Climate: Weather station and a class A pan test Placement: Thermistors and TDR probes launched at certain pond elevations during the deposit filling (movable position) All other instruments at fixed positions Testing Periodic sampling using a stationary sampler Gravimetric water content determination Specific gravity and bulk density.

Field experimental studies Overview of the testing site

Analyses of experimental data Input data for analyses with CONDES Analyses Data/Parameters   Consolidation Compressibility and Permeability parameters A (kPa-1) 2.5438 B -0.1920 C (m/dia) 9.45 x 10-4 D 4.2370 Z (kPa) 0.0495 Boundary conditions Bottom hp= variable Top Surcharge null Specific gravity - G 3.89 Filling rate (m/day) 0.0603 Filling period (day) 34 Desiccation Cracking function parameters A 0.3859 0.0508 C 1.3665 0.626 x 1018 hp= -0.55 m Evap. rate = 0.002 m/day

Analyses of experimental data Progress of the deposit height (at day 84 starts desiccation)

Analyses of experimental data Progress of volumetric water content (day 84 starts desiccation)

Analyses of experimental data Progress of gravimetric water content (desiccation starts at day 84)

Analyses of experimental data Progress of bulk densities (desiccation starts at day 84)

Analyses of experimental data Progress in solids content (desiccation starts at day 84)

Analyses of experimental data Progress of porepressure at base (desiccation starts at day 84)

Analyses of experimental data Meteorological data during field experiments (desiccation starts at day 84)

Analyses of experimental data Progress of evaporation with data from the weather station and Class A device

Analyses of experimental data Progress of cracking (a) day 89, (b) day 92, (c) day 94

Conclusions Characterization of the desiccation behaviour of a fine tailings from the iron ore milling operations was successfully reached. A test section was built and monitored, using an extensive sort of instruments and tests. Material behaviour and boundary conditions were assessed such as settlement, water content, bulk densities, solids content, porewater pressures, evaporation rates, etc. Cracking morphology has also been described. Sub-aerial deposition conditions was examined as a part a large study of alternative methods for slimes. A brief comparison of field data with a numerical modelling of the problem was presented and the results have shown consistent agreement. Overall, the research seems to suggest that reasonable efficiency with slimes thickening can be achieved by the sub-aerial disposition method.

THANK YOU