remediation measurements

Similar documents
What are Metal Leaching and Acid Rock Drainage and Why are They Important to Mining?

Lecture 15: Adsorption; Soil Acidity

Acid Soil. Soil Acidity and ph

Geochemistry of Mine water and Tailing at Malanjkhand Copper deposit. Abstract

Pyrite in acid sulfate soils: transformation and inhibition of its oxidation by application of natural materials

Understanding Mineralogical Composition, Weathering, and Alteration, to Manage ML/ARD in a Base-Metal Tailings Storage Facility

WEATHERING OF SULFIDE MINE TAILING IMPOUNDMENT O. LINTNEROVÁ

2.2 Acid mine drainage

ABANDONED MINE SLAGS ANALYSIS BY EPMA WDS X-RAY MAPPING

Be sure to show all calculations so that you can receive partial credit for your work!

INTRODUCTION TO MINERALOGY 15

Appendix B6. SEM observations, experiment 2. Coating stage pre Ca(OH) 2 addition

BUFFERING MECHANISM AND SENSITIVITY TO ACID DEPOSITION OF SOILS OF AKWA IBOM STATE, NIGERIA

Sedimentary Rocks and Processes

CLASS EXERCISE 5.1 List processes occurring in soils that cause changes in the levels of ions.

12. Lead, Pb (atomic no. 82)

Response to Wek èezhìi Land and Water Board Undertaking Number One NICO Project Land Use Permit and Type A Water Licence Application

Current issues in establishing geochemical background of trace elements

Tailings and Mineral Carbonation: The Potential for Atmospheric CO 2 Sequestration

Chapter 6. Weathering, Erosion, and Soil

Mine Waste: Pollution Source or Georesource?

Lecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry

Adsorption of ions Ion exchange CEC& AEC Factors influencing ion

Soil Fertility. Fundamentals of Nutrient Management June 1, Patricia Steinhilber

Remediation of heavy metals by microalgae: Productivity impact and end fate of contaminants

ph and Liming Practices Kent Martin Stafford County 1/5/2010

Overview. Rock weathering Functions of soil Soil forming factors Soil properties

EVALUATION OF MIGRATION OF HEAVY METAL CONTAINING SEDIMENT RESULTING FROM WATER EROSION USING A GEO- INFORMATION MODEL

Temperature Effect on the Hypergene Mineral Formation Process (the Case of Tailing Dumps of Komsomolsky Tin-Ore District)

Modelling the Reactivity of Multi-Mineral Systems Application to the Prediction of Copper Heap Leach Drain Down Chemistry

Alleviating Soil Acidity through Organic Matter Management. Malcolm E. Sumner, University of Georgia Marcos A Pavan IAPAR

Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined.

Sedimentary Geology. Strat and Sed, Ch. 1 1

An Investigation into

Redox, ph, pe OUTLINE 9/12/17. Equilibrium? Finish last lecture Mineral stability Aquatic chemistry oxidation and reduction: redox

Monday, October 15 th Grab a textbook! Objective: We will explain the formation of different soils and classify soils according to particle size.

Practice Questions for Lecture 5 Geology 1200

1) What is the volume of a tank that can hold Kg of methanol whose density is 0.788g/cm 3?

SoilGen2 model: data requirements and model output

Chapter 7: Anion and molecular retention

Chemistry of Tiling and Crusting

Only healthy soil can grow a nutrient dense food. You are what you eat!

Soil ph: Review of Concepts

REMEDIATION OF THE MILLTOWN DAM SEDIMENTS IN MONTANA

Acid rain long recognized as a problem; the air pollution problem of the 80s, but it is still with us

Volume Composition of a Desirable Surface Soil

ALPHA OMEGA ZEOLITES FOR THE OILFIELD BRIEF

One major route to NO x deposition: gas phase oxidation

1/31/2013. Weathering Includes Physical, Chemical, Biological processes. Weathering Mechanisms. Wind abrasion forming Ventifacts

Savannah River Site Mixed Waste Management Facility Southwest Plume Tritium Phytoremediation

Chapter 6 9/25/2012. Weathering, Erosion and Soils. Introduction. How Are Earth Materials Altered? Introduction. How Are Earth Materials Altered?

Man, Metals and Mayhem: Earth s Resources

Aquatic Chemistry (10 hrs)

SOLUBILITY AND PRECIPITATION EQUILIBRIA

SOLUBILITY AND PRECIPITATION EQUILIBRIA

ECTON HILL. Field Studies Association. From Minerals. to Chemistry

The gypsum requirement equation for sodic soils: What s the app about? Tom DeSutter 2018 Soil and Soil/Water Workshop

1 st shell holds 2 electrons. 2 nd shell holds 8 electrons

THE MULTI-TECHNIQUE APPROACH

Hydrological Cycle Rain and rivers OUTLINE

Geochemical Investigation of Naturally Occurring Arsenic in Upper Midwest Ground Water

AGRONOMIC POTENTIAL AND LIMITATIONS OF USING PRECIPITATED CALCIUM CARBONATE IN THE HIGH PLAINS

WEATHERING. Turning Rock to Sediment and Solutions 10/22/2012

Chapter 5: Weathering and Soils. Fig. 5.14

LESSONS LEARNED FROM MINING-INFLUENCED WATERS STUDIES AT THE NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES

WEATHERING. Weathering breakdown of rock materials Erosion transport of broken-down materials

Lecture 16: Soil Acidity; Introduction to Soil Ecology

MODULE 5.2 Soil properties

Weathering & Soil. Chpt 6

Identification of geochemically distinct regions at river basin scale using topography, geology and land use in cluster analysis

DISTRIBUTION OF METALS IN PARTICLE SIZE FRACTIONS IN SOILS OF TWO FORESTED CATENAS (SMOLENSK MOSCOW UPLAND)

Synthetic faujasite based on coal by-products for the treatment of acid mine drainage (AMD)

MINERALOGY AND CHEMISTRY OF MINE WASTE ROCK PILES IN MINING DISTRICTS IN SOUTHERN COLORADO AND NEW MEXICO

Lecture 6. Physical Properties. Solid Phase. Particle Composition

The Chemistry of Salinity in Soils. Naomi Waissman Assadian Texas A&M Research and Extension Center at El Paso September 4, 2002

Lecture 16 Guest Lecturer this week. Prof. Greg Ravizza

Environmental Resources Management

Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized?

11. GEOCHEMICAL CHARACTERIZATION

HEAVY METAL AVAILABILITY IN SOIL IN THE PRESENCE OF ANIONIC SURFACTANTS

Lecture 6: Soil Profiles: Diagnostic Horizons

Mineralogical characterisation of gold ores: collaboration is the best technique! Dorrit de Nooy (Senior Mineralogist, Metallurgy Services)

Metal fluxes from a sea deposit site for mine tailings

CHAPTER 7 EFFECT OF CONDITIONING ph ON SULPHUR, GOLD AND URANIUM FLOTATION

Effect of Particle Size on Solubility and Neutralizing Ability of Carbonate Minerals

THE INFLUENCE OF WATER QUALITY ON THE FLOTATION OF THE ROSH PINAH COMPLEX LEAD-ZINC SULFIDES.

The Role of Soil Organic Matter in Potassium Fixation Nathan Smith

Processed Food Production. Consistent product Long shelf life Low cost

Effect of chemical composition to large scale CO 2 Injection in Morrow Sandstone, Farnsworth Hydrocarbon Field, Texas, USA

+ 3 can also be bound to the soil complex,

A few more details on clays, Soil Colloids and their properties. What expandable clays do to surface area. Smectite. Kaolinite.

Assess the Potential for Accumulation of Toxic Trace Elements in Biota near Burton Island Ash Disposal Site Indian River Bay, Delaware

Chem 101 Practice Exam 3 Fall 2012 You will have a Solubility Table and Periodic Table

The Lithosphere. Definition

Geochemical & Physical Weathering of Acid Generating Rock - Implications for Long-Term Stability of Mine Slopes and Waste Dumps

This is how we classify minerals! Silicates and Non-Silicates

FRACTIONATION OF METALS IN SEDIMENTS AFFECTED BY MINING WASTES IN THE TRI-STATE MINING DISTRICT

INCREASING TREND IN DUST CLOUD INTRUSIONS FROM THE SAHARA OVER ISRAEL. Department of Geophysics and Planetary Sciences, Tel Aviv University

Colluvial debris: Rocks that have fallen down hills. Types of Parent Material

Priority Pollutants in Untreated and Treated Discharges from Coal Mines

Transcription:

IUNG Institute of Soil Science and Plant Cultivation PULAWY, POLAND International Workshop Current developments in remediation of contaminated lands Contamination by a pyrite mine spill in Spain: effect on soils and remediation measurements 27 29 October 25 Francisco Martín Peinado Soil Science Department University of Granada. Spain.

Location (mm) Climate 3 25 2 15 1 5 EFMAMJ JASOND 17.7ºC mean annual +1ºC in winter TERMIC and XERIC (USDA, 1999) 3 25 2 15 1 5 (ºC) pp (mm) ETP (mm) Tª(ºC) 6 mm annual pp 9 mm annual ETP Soil use 13 15 Agrio and Guadiamar river basins To the border of Doñana National Park (World Heritage by UNESCO in 1994) 21 51 Crops Grazing Nat. Veg. Riverbed

MAIN MINERALS 2,1 5,4 1,4,9 7,1 83,1 Pyrite Sphalerite Galena Chalcopyrite Arsenopyrite Non productives FeS 2 ZnS PbS CuFeS 2 AsFeS EXTRACTED ELEMENTS: Zn, Pb, Cu, As Others: Cd, Tl, Sb, Ag, Bi, Cr, Hg, Ni

THE ACCIDENT Aznalcóllar s mine (Boliden-Apirsa) 25 th April 1998 2 hm 3 TAILINGS 4 hm 3 ACIDIC WATERS

km 5 m 4 km Tailings Thickness of tailings: > 1 m near the mine < 3 cm at the bottom Ton Ton Zn 16 Cu 4 Pb 16 Tl 1 58 km Acidic waters As 1 Cd 5

MAIN IMPACTS Total affected area: 42.9 km 2 4,2% Doñana Natural Park,2% Doñana National Park Loss of all crops (in and next to the area) Death of fauna (37,4 Ton fishes, 17 kg crayfishes, 96 vertebrate) 4 wells directly contaminated by tailing input Soils and waters contaminated by high concentrations of heavy metals and As

INITIAL CONTAMINATION Contamination in depth depended on the soil structure Dry soil (cracks) Good development High penetration Low development Low penetration

1 5,8 <2% <1% Loam 1% 15-2 MINE 5 8, >1% <1% Silty clay 1-2% >2 ENTREMUROS 2 5,9 <1% >35% Sandy loam <.5% <1 SANLÚCAR LA MAYOR AZNALCÁZAR 3 7,7 1% <1% Silty clay loam 1% 15-2 4 7,8 5-1% <1% Loam 1% 1-15 SOIL PROPERTIES ph CaCO 3 Gravel Texture O.C. C.E.C. Soil types

INITIAL SITUATION Tailings saturated in water, reducing conditions, particle of sulphides remain stable SECONDARY CONTAMINATION Drying, tailing oxidation, releasing of contaminants

PYRITE OXIDATION O 2 H 2 O T. Thioox. FeS 2 Fe 3+ Pyrite (FeS 2 ) Sphalerite (ZnS) Chalcopyrite (CuFeS 2 ) Arsenopyrite (AsFeS 2 ) Galena (PbS) Bournonite (PbCuSbS 3 ) SO 4 2- H + Fe 2+ O 2 T. Ferroox. ph < 4,5 STRONG ACIDIFICATION RELEASING OF CONTAMINANTS Fe(OH) 3 H + ph > 4,5 Fe 3+ H 2 O SULPHATE FORMATION

4 May 2 May

Disolution and mobilization of contaminants (rainfalls)

Increasing of soil contamination

Aeolian contamination

1. Clean-up REMEDIATION MEASUREMENTS 5 trucks and 15 diggers 9 workers 2 days 6 hm 3 removed material 38% tailing 62% soil Material disposed of in the open cut mine

1. Clean-up In some areas more than 1.5 m soil were removed October May May 1998 1998

1. Clean-up Riverbed Before After

Total contamination after the clean-up actions (mean values) 1 mg/kg 9 8 7 6 5 4 3 UCS -5 cm -1 cm mg/kg 3 2 1 Cd Tl 2 1 Cu Zn As Pb Area above intervention levels: 82% As; 4% Zn; 24% Pb. EC (ds m -1 ) 12 1 8 6 4 Acidic soil 14 12 1 8 6 4 Basic soil 1998 1999 21 2 2 5 1 Percentiles 5 1 Percentiles

2.1. Liming Sugar-beet scum REMEDIATION MEASUREMENTS High CaCO 3 content (4%) Very fine particle size (reactive) High OM content (15-2%) Cheap (industrial waste) 4 kg m -2 acidic soils 2 kg m -2 neutral-alk. soils Tilling (25 3 cm) Dilution of the element concentrations in the uppermost 1 cm (after cleaning during 3 years and in the moderately contaminated areas)

EFFECT OF CLEAN-UP AND LIMING EVOLUTION OF SOIL PROPERTIES 1 8 Acidic soils 25 2 Basic soils % CaCO 3 6 4 2 15 1 5 5 1 Percentiles 1998 1999 5 1 Percentiles 1 8 Acidic soils 21 1 8 Basic soils ph 6 4 2 6 4 2 5 1 5 1 Percentiles Percentiles

Red soils and iron-rich material for As retention OM for retention of elements and recovery of the soils

REMEDIATION MEASUREMENTS 3. Phytoremediation Accumulator plants tested (de Haro, 1999) Mustards (Brassica juncea and Brassica Carinata) Pb Zn Cu Autochthonous plants collected in the area Amaranthus blitoides Pb, Cu, As Lavatera cretica Cd

Only exploratory level, strong limitations in the area Hard climatic conditions Heterogeneous and persistent contamination

AREA ABOVE INTERVENTION LEVELS IN 24 (Total concentrations) Intervention levels (agricultural soils) (mg/kg) (13%) Zn (39%) (68%) As (82%) ph<7 ph>7 Cu 3 5 Zn 6 1 Cd 7 1 (7%) Pb As 5 5 (24%) Pb 35 5 Tl 5 5 Cu, Cd and Tl = % Uncontaminated soil

,5,4,3,2,1 3,5 3 2,5 2 1,5 1,5 SOLUBLE (in water) concentrations All soils 2 4 6 8 1 Pbw 98 Pbw 99 Pbw 1 Pbw 4 All soils 2% 2 4 6 8 1 Asw 98 Asw 99 Asw 1 Asw 4,7,6,5,4,3,2,1 % Intervention levels (mg/kg) Cu Zn Cd As Pb Tl All soils,7,5,3,4 2 4 6 8 1 1,1 5% Tlw 98 Tlw 99 Tlw 1 Tlw 4

SOLUBLE (in water) concentrations 1 8 6 4 2 Acidic 6 5 4 3 2 1 Acidic 2 4 6 8 1 2 4 6 8 1 Znw 98 5% 22% Cuw 98 Znw 99 Cuw 99 Znw 1 Cuw 1 5 4 3 2 1 Znw 4 Basic 3 2,5 2 1,5 1,5 Basic Cuw 4 2 4 6 8 1 2 4 6 8 1 1% 1% Cd = Cu

EDTA extracted concentrations 1 8 6 4 2 All soils 2 4 6 8 1 ZnE 98 ZnE 99 ZnE 1 ZnE 4 14 12 1 8 6 4 2 All soils 2 4 6 8 1 CuE 98 CuE 99 CuE 1 CuE 4 25 2 15 1 All soils AsE 98 AsE 99 AsE 1 AsE 4 5 4 3 2 All soils CdE 98 CdE 99 CdE 1 CdE 4 5 1 2 4 6 8 1 2 4 6 8 1,5,4,3,2,1 All soils 2 4 6 8 1 TlE 98 TlE 99 TlE 1 TlE 4 35 3 25 2 15 1 5 All soils 2 4 6 8 1 PbE 98 PbE 99 PbE 1 PbE 4

What would happened if the tailings were not removed? Weathering layer (4 days) 6 years 12 mm Tailing 3 years 4 years 6 years cm Pale greyish layer 8 cm 15 cm 7 cm 4 cm Reddish layer 4 cm Unaffected soil

2 4 6 8 1 Strong degradation of the soil properties g/kg 5 1 15 2 cmol c kg -1 1 2 3 4 1 days 6 years % 1 2 3 Depth (mm) 2 4 2 4 2 4 2 4 6 ph CaCO 3 6 6 C.E.C. Calcium carbonate dissolution produced a gypsum precipitation 6 O.M. Fe 2+ + 4SO 4 2- + 4H + + 4CaCO 3 + 8H 2 O Fe 2+ + 4CaSO 4 2H 2 O + 4CO 2 + 4OH - 1 2 3 4 5 6 % 2 4 6 8 1

Partial dissolution of silicates (phylosilicates, feldspars) Fe 3+ + Al 3+ + 4SO 4 2- + 2H + + 4CaCO 3 + 5H 2 O Fe(OH) 3 + Al(OH) 3 + 4CaSO 4 2H 2 O + 4CO 2 K.6 Mg.25 Al 2.3 Si 3.5 O 1 (OH) 2 + 8H + + 2H 2 O.6K + +.25Mg 2+ + 2.3Al 3+ + 3.5H 4 SiO 4

Plumbojarosite [PbFe 6 (SO 4 ) 2 (OH) 12 ] Neoformation of new minerals Jarosite [KFe 3 SO 4 (OH) 6 ] Ferrihydrite [5Fe 2 O 3 9H 2 O] Schwertmannite [Fe 8 O 8 (OH) 6 SO 4 ]

Heavy metals and As Pb t (mg/kg) As w mg/kg 5 1 5 15 1 215 25 2 3 25 35 34 35 45 Depth (mm) 1 2 3 4 5 6 7 8 Depth (mm) 1 2 3 4 5 6 7 8 3 years 4 years 6 years 5 1 15 2 1 As t mg/kg 3 years 4 years 6 years Depth (mm) 2 3 4 5 6 7 8

3 years Heavy metals and As Zn (mg/kg) 2 4 6 8 1 12 14 16 6 years Zn (mg/kg) 2 4 6 8 1 12 14 16 1 1 2 2 Depth (mm) 3 4 5 Zn w Zn t Depth (mm) 3 4 5 6 6 7 8 7 8 = Cd and Cu

The remediation actions minimized the impact of the spill, but the soils have definitely lost their agricultural use 162,5, 63,, zlotych GUADIAMAR GREEN CORRIDOR Supervision and monitoring of the pollution Ecological restoration Soils, geomorfology, hidrology, botany and zoology Alternative development (natural and human systems)

Thanks for your attention