Kansallisen ydinjätehuollon tutkimusohjelma (KYT 2010) Kolmenarvoisten aktinidien kiinnittyminen savi- ja (hydr)oksidimineraalien pinnoille Sorption of.

Slides:



Advertisements
Similar presentations
Particle size Ions  molecular clusters  nanocrystals  colloids  bulk minerals Small particles can have a significant % of molecules at their surface.
Advertisements

Complexes Complex – Association of a cation and an anion or neutral molecule All associated species are dissolved None remain electrostatically effective.
The Soil Chemical Environment Reading: General background: Sparks,Chapter 1, pp Additional: Essington, Chapter 1 pp
Dissolution and Precipitation
ACTIVITY. Activity Coefficients No direct way to measure the effect of a single ion in solution (charge balance) Mean Ion Activity Coefficients – determined.
Removal of Cu(II) ions from aqueous solution effluent using Melamine-Formaldehyde-DTPA resin in a fixed-bed up-flow column By Ahmad Baraka Supervisors.
U(VI) interactions with carbonates: Spectroscopic studies
Soil Chemical Properties
The attraction between a hydrogen atom on one water molecule and the oxygen atom on another Hydrogen bond.
Sorption of Anions Important because: Several nutrients and agricultural chemicals are negatively charged. –Nitrate, phosphate, sulfate, selenate,… Tropical,
7-1 Ion Exchange Resins General resin information Functional Groups Synthesis Types Structure Resin Data Kinetics Thermodynamics Distribution Radiation.
Introduction For remediation of soils and purification of polluted waters, wastewaters, biosorbents might be considered as prospective groups of materials.
The NEA Sorption Project a multinational cooperative program to advance the use of Thermodynamic Sorption Models Mark Fuhrmann U.S. NRC Office of Nuclear.
Chapter 4- Products of Weathering Several things can happen to products 1- removal of materials by leaching e.g., CaCO 3 2- reaction of materials, either.
Soil Chemistry Chapter 5.
E NVIRONMENTAL CHEMISTRY E 12. water and soil. W ATER AND SOIL Solve problems relating to the removal of heavy- metal ions, phosphates and nitrates from.
Mineral dissolution/precipitation To determine whether or not a water is saturated with an aluminosilicate such as K-feldspar, we could write a dissolution.
Mineral dissolution/precipitation To determine whether or not a water is saturated with an aluminosilicate such as K-feldspar, we could write a dissolution.
Soil OM is 50-65% C, so we use 57.5% SOM x = OC and SOM = OC/0.575 e.g., how much SOM do you have with 2% OC? SOM = 2% ÷ = 3.5% or 2% ÷ 0.50.
Soil Solutions Continued aqueous liquid phase of the soil and its solutes.
Chapter 2 Inorganic Solids in Soil continued.
IS SOLUBILITY THE ONLY CONTROL ON SOLUTE CONCENTRATIONS? The answer is NO! Solubility often controls the concentrations of major solutes such as Si, Ca,
Dissolution and Solubility Processes Dissolution-precipitation equilibria affect many soil processes, plant growth, etc Dissolution is the disintegration.
Chemical Basis of Life. Chemistry Matter is made up of separate chemical components. –Chemistry = Interactions between atoms/molecules. Biological function.
Immobilisation of radionuclides via in situ incorporation into stable mineral phases Janice Littlewood Supervisors: Dr Ian Burke, Dr Sam Shaw, Dr Caroline.
Mass Action & Mass Balance mCa 2+ =mCa 2+ +MCaCl + + mCaCl CaCL CaHCO CaCO CaF + + CaSO CaHSO CaOH + +… Final equation.
Chemical Basis of Life Chapter 2. Chemistry Matter is made up of separate chemical components –Chemistry = Interactions between atoms/molecules.
Chemical Synthesis Lesson 2. Learning objective: To explain the reactions involving acids. Must: Describe the pH scale. Grade D Must: Describe what happens.
Lecture 11 Clay Minerals Clay and organic matter in the soil provide the negative absorptive sites or Cation Exchange Capacity (CEC) Clay can hold positive.
Adsorption Equilibrium Adsorption vs. Absorption –Adsorption is accumulation of molecules on a surface (a surface layer of molecules) in contact with an.
URANIUM ACCUMULATION IN SANDY SOIL IN AN ARID REGION DUE TO AGRICULTURAL ACTIVITIES Dr. Ashraf E. Khater King Saud University, Saudi Arabia Atomic Energy.
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.
Environmental Molecular Science Institute University of Notre Dame Actinides and Heavy Metals in the Environment The Formation, Stability, and Impact of.
Analysis of Total Aluminum and Dissolved Aluminum Louis McDonald and Jeff Skousen Plant & Soil Sciences West Virginia University.
Environmental Processes Partitioning of pollutants 3.i Sorption involving organic matter (between air/soil and water/soil)
Lecture #26 What’s on the Final?
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.
Surface Chemistry: Complexation at the Solid/Water Interface
Inorganic Materials Lab. SKKU Sorption Reaction of Aquatic TcO 4 - or CrO 4 2- on Calcined Mg/Al Layered Double Hydroxide: Reaction Equilibria and Characterization.
LECTURER (CHEMISTRY) GOVT.POLYTECHNIC INSTITUTE LAYYAH.
Surface charge development at the Barite-Water interface in NaCl media, from 15 to 50˚C Heather Williams and Moira K. Ridley Department of Geosciences,
Weathering -II.
E NVIRONMENTAL G EOCHEMISTRY AT T EXAS A&M U NIVERSITY Mineral & Organic Matter Surface Chemistry Controlling.
A.Filby 1, M. Plaschke 1, H. Geckeis 1, Th. Fanghänel 2,3 1) Forschungszentrum Karlsruhe, Institut für Nukleare Entsorgung, Postfach 3640, D-76021, Germany.
Aquatic Chemistry 367 Civil and Environmental Engineering Meeting time: MWF 11:00-11:50am Meeting room: Abbott Auditorium in Pancoe Pavillion Instructor:
PART -III Analytical Methods for Metal Speciation in Water and Solids
Reactions of Aluminosilcates
Summary of Previous Results Atom probe experimentation -Atomic scale measurement of gas-solid reactions of Al and Oxygen - Compound formation - Study of.
Solubility (cont.); Mineral Surfaces & Reactions Lecture 22.
Bjerrum plot showing the activities of inorganic carbon species as a function of pH for a value of total inorganic carbon of mol L -1. In most natural.
Soil colloids. CHEMICAL PROPERTIES OF SOIL: Soil Colloids cat ion Exchange organic matter / Organic carbon Carbon –Nitroge ratio Soil fertility Soil reaction.
CVEN 5424 Environmental Organic Chemistry Lecture 15 – Sorption to Mineral Surfaces.
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.
CVEN 5424 Environmental Organic Chemistry Lecture 16 – Sorption to Mineral Surfaces.
Long term behaviour of glass and steel in interaction with argillite in deep geological conditions O. Bildstein (1), V. Devallois (1), V. Pointeau (1),
TRACE METAL TRANSFER FROM ROCKS TO THE PEDO- AND HYDRO- SPHERES.
Introduction to Chemistry
Soil Chemistry.
Hansell Gonzalez Raymat DOE Fellow
Solubility (cont.); Mineral Surfaces & Reactions
Application of Iron Oxide Nanoparticles/silica Composites on the Removal of Uranium(VI) for Drinking Water Treatment and the Impact of Water Chemistry.
Mass Action & Mass Balance
Aquatic Chemistry 367 Civil and Environmental Engineering
Solid-Water Interface
Complexes Complex – Association of a cation and an anion or neutral molecule All associated species are dissolved None remain electrostatically effective.
A universal uptake mechanism for cobalt(II) on soil constituents: Ferrihydrite, kaolinite, humic acid, and organo-mineral composites Woodward G.L.1, Peacock.
Chapter 2: Geochemistry Background
Intro to Biochemistry What do you think is the cause behind these bird gatherings?? Salt licks/clay licks provide these birds with the minerals and ions.
Activity diagram showing the stability relationships among some minerals in the system K2O-Al2O3-SiO2-H2O at 25°C. The dashed lines represent saturation.
Water = 2 Hydrogen atoms + 1 Oxygen atom “H2O”
Presentation transcript:

Kansallisen ydinjätehuollon tutkimusohjelma (KYT 2010) Kolmenarvoisten aktinidien kiinnittyminen savi- ja (hydr)oksidimineraalien pinnoille Sorption of trivalent actinides onto clay- and (hydr)oxide minerals Nina Huittinen Radiokemian laboratorio, Helsingin Yliopisto

1 - General background  Deep geological formations are considered for the long-term disposal of radioactive waste  Knowledge of geochemical processes essential for a thorough nuclear waste disposal safety assessment – e.g. solid-water interface reactions and redox- and complexation reactions in solution  For a thorough safety assessment over long time-scales, understanding of atomic- and molecular scale interactions of radionuclides with the solid-water environment is imperative

2 – Project motivations  Trivalent actinides  Am and Cm are together with Pu responsible for the long-term radiotoxcicity of spent fuel.  Trivalent oxidation state soluble – radionuclide dissolution and migration  Minerals  Gibbsite α -Al(OH) 3 – used e.g. as a model mineral for aluminosilicates and iron oxides/hydroxides found in vast quantities in natural systems  Kaolinite Al 2 Si 2 O 5 (OH) 4 – one of the main mineral components of clay-rich host formations  Silica SiO 2 – presence of silica ubiquitous in most natural materials and groundwaters, colloids Pu(III) Am(III) Cm(III)

3 – Aim of project  Characterization of present reactive OH-groups on the mineral surface  Determination of surface sites involved in An(III)/Ln(III) sorption  Characterization of sorption mechanisms and surface complexes Possible interactions of radionuclides with present mineral phases

4 - Methods  Mineral synthesis – clean minerals  FTIR - identification of OH groups and knowledge of specific bonding to the surface  Solid state NMR- identification of OH groups and knowledge of specific bonding and coordination to the surface  TRLFS – knowledge of An(III) hydration sphere and surface complexes  SEM  XRD  N 2 -BET  Micro electrophoresis  ICP-MS Mineral characterization

5 – Objectives for 2008  Mineral synthesis  Mineral characterization  Basic sorption studies and mass balance studies (master’s thesis)  IR experiments  NMR experiments  International collaboration with INE, Karlsruhe, Germany - Inclusion of 5- sulphosalicylic acid (model compound for humic acids) to study ternary surface complex formation

6 – Results 2008  Kaolinite synthesis and characterization - Université de Poitiers, France  Gibbsite synthesis and characterization, Department of Chemistry, University of Helsinki  Silica purchase EVONIK industries

6 – Results 2008  Sorption studies and mass balance studies with all chosen minerals Modeling → mass balance of Eu 3+, H +, Al 3+ /Si 2+, anions in solid and liquid phase respectively  ξ-potential measurements → net charge of mineral surface  Batch experiments Ln(III) sorption as a function of pH → K d values and titration curves  Isotherm experiments – concentration of adsorbed Ln(III) as a function of Ln(III) concentration in solution→ types of OH groups

6 – Results 2008  IR-studies, FTIR- NesteOil Oy Finland, ATR-FTIR - Department of Chemistry, University of Helsinki Gibbsite – 6 structural OH groups 1- Intralayer OH groups oriented parallel to the (001) face (OH1, OH2 and OH4) 2- Interlayer OH groups oriented nearly perpendicular to the (001) face (OH3, OH5 and OH6)

7 – Outlook  October 2008 – Spring 2009: Collaboration with the Instute for nuclear waste management (INE), Forschungszentrum Karlsruhe, Germany  TRLFS investigations using synthetic kaolinite and Cm(III)  Addition of model ligand to mineral/metal ion system  Possibly investigations using well characterized humic acid and natural montmorillonite 5-sulfosalicylic acid

7 - Outlook   NMR-studies, National Institute of Chemical Physics and Biophysics, Tallinn, Estonia  IR studies using alumina and silica, possibly kaolinite  Surface complexation modeling  4-5 publications  Ph.D dissertation