Metal concentrations in groundwater around disturbed and undisturbed massive sulfide deposits H. Pauwels, A. Lassin, J.C. Foucher,Y. Deschamps, M. L. Tercier-Waeber,

Slides:



Advertisements
Similar presentations
Complexes Complex – Association of a cation and an anion or neutral molecule All associated species are dissolved None remain electrostatically effective.
Advertisements

Heavy Metals in groundwater around massive sulphide deposits : exploration and environmental aspects H. Pauwels, M. L. Tercier-Waeber, M. Arenas, R. Castroviejo,
Acid Mine Drainage Excercise H-ESD : Environmental and Sustainable Development Michael Staudt, GTK.
Dale T Littlejohn Senior Geologist. What is fate and transport in the vadose zone? Vadose Zone Hydrocarbon release from buried pipeline Aquifer Surface.
Surface Water Geochemistry of Deckers Creek Basin Geology 399 Qingyun Sun.
Fate and Transport of Contaminants from Acid Mine Drainage US EPA Scientist-to-Scientist Meeting Las Vegas, NV June 14-15, 2000 Richard T. Wilkin, Ph.D.
Defending the Rights of Metals: How to Distinguish Naturally High Groundwater Concentrations from Site-Related Contamination Karen Thorbjornsen and Jonathan.
Metals and alloys in external constructions – changes in speciation and bioavailability of corrosion-induced metal runoff upon environmental entry. Associate.
Mid Ocean Ridge Ore Deposits
SUPERGENE SULPHIDE ENRICHMENT
Volcanogenic Massive Sulphide (VMS) Deposits
Acid Mine Drainage. Mining & the Environment Mine overburden & waste soils (mine tailings) are waste products generated by the mining industry. When these.
Hydrogeochemical Processes Influencing Groundwater Quality in the Lower Pra Basin, Ghana. A PhD Thesis By Collins Tay.
Case Study: Heavy metal bioavailability in a soil affected by mineral sulphides contamination following the mine spillage at Aznalcóllars (Spain) Clemente.
LABORATORY METHODS for LEACHATE ANALYSIS RESULTS Temporal and cumulative metal leaching mass. Cumulative leaching (per ha) in control treatments were:
Understanding and managing acid mine drainage
Partner for progress Does arsenic, in groundwaters of the compound Rhine-Meuse delta, menace drinking water supply in the Netherlands? IAH -Meeting, Utrecht,
Figure 4-1. Diagram of a Zn-Cu electrochemical cell. Zn and Cu metal electrodes are immersed in a CuSO 4 solution. Electrons flow from left to right and.
Lecture 263/30/07. E° F 2 (g) + 2e - ↔ 2F Ag + + e - ↔ Ag (s)+0.80 Cu e - ↔ Cu (s)+0.34 Zn e - ↔ Zn (s)-0.76 Quiz 1. Consider these.
Trace Metals & Phytoplankton Gert Vlaming
An Introduction to Acid Mine Drainage by George Mitchell and Tim Craddock.
Ore deposit environments
Lecture 3 Trace Metals in Seawater What are trace elements? Why are they important? Principal of Oceanographic Consistency. Profiles shapes as clues for.

URANIUM ACCUMULATION IN SANDY SOIL IN AN ARID REGION DUE TO AGRICULTURAL ACTIVITIES Dr. Ashraf E. Khater King Saud University, Saudi Arabia Atomic Energy.
Determination of Dominant Trace Metal Sequestration Processes in Two Vertical Flow Bioreactors Using Modified Tessier Extractions J.A. LaBar and R.W. Nairn.
IRON & MANGANESE ENVE 201 Dr. Aslıhan Kerç
Complexes Complex – Association of a cation and an anion or neutral molecule Complex – Association of a cation and an anion or neutral molecule All associated.
29 th International conference SEGH, 8-12 July Toulouse, FRANCE 2013 Health risk estimate for groundwater and soil contamination in the.
Geology, Mining, and Water Quality by Matthew A. Sares.
Cation Exchange Definition: substitution of ions in solution for those held by a mineral grain. Associated with many different types of materials found.
Measuring Metal Release Rate from an Arsenopyrite Sample Chemistry of Metal Sulfide Minerals.
Evaluation of a multisurface complexation reactive transport model on field data. Bert-Jan Groenenberg 1, Joris Dijkstra 2, Rob Comans 2,3 1 Alterra Wageningen.
Seasonal Changes in Biogeochemistry of a Natural Wetland Receiving Drainage from an Abandoned Mine Diane McKnight and Eric August – University of Colorado.
A unifying model of cation binding by humic substances Class: Advanced Environmental Chemistry (II) Presented by: Chun-Pao Su (Robert) Date: 2/9/1999.
Metal Deposits  The specification states that you should be able to:  a) Explain the low crustal abundances of metallic minerals; show an understanding.
In-situ automated Monitoring of Trace metal speciation in Estuaries and Coastal zones in relation with the biogeochemical processes (IMTEC) Eurocean 2004,
Ch.9: Lesson 5 -Intro to Electrochemistry- Ch.9: Lesson 5 -Intro to Electrochemistry-
Aquatic Chemistry 367 Civil and Environmental Engineering Meeting time: MWF 11:00-11:50am Meeting room: Abbott Auditorium in Pancoe Pavillion Instructor:
1 Titration Curve of a Weak Base with a Strong Acid.
Effects of Acid Mine Drainage (AMD) on Nesting Tree Swallows.
Reactions Reference. Solubility Rules 1.All nitrates, acetates, and chlorates are soluble. 2.All chlorides, bromides, and iodides are soluble except for.
Cation Exchange Definition: substitution of ions in solution for those held by a mineral grain. Associated with many different types of materials found.
Contaminant Transport (GTX 719) Muravha Sedzani Elia ( ) 2012/05/23 University of Pretoria1.
Acid Mine Drainage H-ESD : Environmental and Sustainable Development Michael Staudt, GTK.
Water-rock interactions To concentrate a material, water must: –Transport the ions –A ‘trap’ must cause precipitation in a spatially constrained manner.
GEOTRACES Atlantic Basin Workshop September 2007 Aerosol Sampling and Analysis for GEOTRACES: Bill Landing Department of Oceanography Florida State University.
Proposal for estimation of surface water bodies background levels for selected metals Slovak Republic.
Groundwater related research Dr Shafick Adams 21 July 2010.
Characteristics of VMS Deposits VMS deposits are major sources of Cu and Zn and significant quantities of Au, Ag, Pb, Se, Cd, Bi, Sn as well as minor amounts.
Groundwater bodies, chemical characterisation and monitoring for the Water Framework Directive C.R. Meinardi, RIVM.
Presentation for Office of Surface Mines on Potential Use of the Leaching Environmental Assessment Framework to enhance source terms for use of CCRs in.
INTRODUCTION Cd Usually it combined with other elements such: oxygen, chlorine, or sulfur. Cd 2+ activities in soils is about M. levels of Cd in.
SAUD S. AL-OUD Department of Soil Water Science College of Agric. & Vet. Medicine KING SAUD UNIVERSITY.
Acid drainage is a persistent environmental problem in many mineralized areas, especially where mining has taken place. Not all drainage, however, is.
Acid Mine Drainage : Metals in Water and Sediment Upper Lefthand Creek, Northwestern Boulder County 2003 REU Program – August 7, 2003 Roshan Cholas, University.
Issue: Effects of Mine Reflooding
Bulgarian Academy of Sciences, Sofia, Bulgaria
A Look Back at Groundwater Geochemistry as an Exploration Tool for Lead and Zinc Deposits in Sinking Valley 82 Field Conference of Pennsylvania Geologists.
By Reid Brown and Rio Diniakos
Volcanogenic Massive Sulphide (VMS) Deposits
Aquatic Chemistry 367 Civil and Environmental Engineering
French groundwater monitoring networks
METREAU part II Analysis Division March 10,
Solid-Water Interface
Chemical and mineralogical comparison of two antibacterial clays
Soil processes and trace metals
Complexes Complex – Association of a cation and an anion or neutral molecule All associated species are dissolved None remain electrostatically effective.
CATION EXCHANGE CAPACITY
© The Author(s) Published by Science and Education Publishing.
Presentation transcript:

Metal concentrations in groundwater around disturbed and undisturbed massive sulfide deposits H. Pauwels, A. Lassin, J.C. Foucher,Y. Deschamps, M. L. Tercier-Waeber, F. Graziottin, R. Castroviejo, J. Samper, A. López

Objectives To determine water-rock interactions around VMS deposits with application to two VMS ore deposits from Iberian Pyrite Belt: To determine water-rock interactions around VMS deposits with application to two VMS ore deposits from Iberian Pyrite Belt: –the effect of a deeply buried orebody on the composition of groundwaters –metal speciation and solubility controlling role of complexants Applications in exploration and baseline studies Applications in exploration and baseline studies

La Zarza and Masa Valverde VMS La Zarza Masa Valverde Low to very low permeability of host-rock Located in an area of hydrogeological recharge Low to very low permeability of host-rock Located in a hydrogeological discharge zone Buried at m depth Mined between 1853 and 1991 Remaining reserves: 110 Mt Unworked Reserves : 100 Mt Nearly outcropping to more than 500 m depth

Hydrogeology and Chemistry Cl SO 4  CO Masa Valverde La Zarza R 2 = 0.94 R 2 = Cl (mg/l) Na (mg/l La Zarza Masa Valverde. Surroundings Different chemical characteristics strengthened by occurrence of two mixing trends Infiltrating waters Deep groundwater flow Local groundwater flow Eh: Masa Valverde : -285 to -230 mV La Zarza : -30 to mV La Zarza : -30 to mV

Metal determination: VIP and ICP-MS Analysis by ICP-MS for Cu, Pb, Zn, Cd, Fe, Mn, Co, Ni, Al, AsAnalysis by ICP-MS for Cu, Pb, Zn, Cd, Fe, Mn, Co, Ni, Al, As Voltammetric In-situ Profiling System ( VIP): Submersible voltammetric probe Submersible voltammetric probe + Calibration deck unit + Surface deck unit + PC Specificity: measures only the concentration of the mobile fraction of trace metals ( free metal ions + small labile complexes <few nm) Analysis by VIP for Cu, Pb, Zn, Cd, MnAnalysis by VIP for Cu, Pb, Zn, Cd, Mn IDRONAUT s.r.l

Metal contents  ( Zn+Cu+Pb+Cd+As+Ni+Co) in a concentration range of the same order at both sites, despite : - very reducing conditions at Masa Valverde -very low solubility of sulphide minerals Impossible distinction between La Zarza and Masa Valverde G.W. using any particular metal

Metal Speciation: Comparison VIP / ICP-MS ICP-MS Voltammetry La Zarza G.W. : % of concentration measured by VIP with respect to ICP-MS : Cu : less than 6% Zn : 0.5 to 21 % Cd : less than 27 % Pb: 8 to 100% Cu, Zn and Cd present as macromolecules and/or adsorbed on colloids/small particles Pb presents as free ions + small labile complexes

Metal Speciation: Geochemical Modelling Using EQ3NR: - Estimation of undetectable H 2 S from equilibrium with respect to pyrite - Estimation of Cu, Pb, Zn concentrations expected from equilibrium with respect to chalcopyrite, galena and sphalerite Masa Valverde G.W. Cu and Pb present as macromolecules and/or adsorbed on colloids/small particles Zn presents as free ions + small labile complexes

Conclusions and Perspectives Similar total metal concentrations at both disturbed and deep buried unworked depositsSimilar total metal concentrations at both disturbed and deep buried unworked deposits Enhancement of total metal concentrations in GW by the formation of complexes or by metal adsorption on colloids or small particlesEnhancement of total metal concentrations in GW by the formation of complexes or by metal adsorption on colloids or small particles Two major observations :

Conclusions and Perspectives : Mineral exploration Enlarge the field of potential applications for deep orebody exploration using hydrogeochemical methods at local scaleEnlarge the field of potential applications for deep orebody exploration using hydrogeochemical methods at local scale not only restricted in case of acid mine drainage despite low solubility of sulphide minerals Contribute to support the possible role of G.W.-rock interactions in the formation of surface geochemical anomalies identified by enzyme leach, MMI selective digestions and others...Contribute to support the possible role of G.W.-rock interactions in the formation of surface geochemical anomalies identified by enzyme leach, MMI selective digestions and others... These results:

Conclusions and Perspectives : Environmental Assessment Confirm the importance of a natural baseline study in order to determine realistic achievable targets for remediation.Confirm the importance of a natural baseline study in order to determine realistic achievable targets for remediation. Pose the problem of suitable methods for estimating natural background total metal concentration at abandoned mine sites:Pose the problem of suitable methods for estimating natural background total metal concentration at abandoned mine sites: Predictive modeling constitutes an upper limit in the case of acid mine drainage and a lower limit in the absence of significant oxidation. These results: