A presentation in defense of the dissertation entitled “ANALYSIS OF FACTORS THAT AFFECT ION BEAM CURRENTS FOR COSMOGENIC 10Be AND 26Al ANALYSIS BY ACCELERATOR MASS SPECTROMETRY (AMS)” by Adam Lewis Hunt In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Specializing in Chemistry at the University of Vermont Outline of dissertation defense I. Introduction to the analysis of cosmogenic 10Be and 26Al II. Investigation of factors which affect the sensitivity of accelerator mass spectrometry (AMS) for cosmogenic 10Be and 26Al isotope analysis III. Metal matrices to optimize ion beam currents for accelerator mass spectrometry IV. Investigation of metal matrix systems for cosmogenic 26Al analysis by accelerator mass spectrometry V. Closing remarks Strategy for isotope quantification Long-lived radioisotopes Nuclide t1/2 Z (p) N (n) 9Be -----stable----1.51 Ma 4 4 5 6 36Cl 0.70 Ma -----stable----5.73 ka 0.30 Ma 13 13 6 17 13 14 8 19 129I 15.7 Ma 53 76 10Be 26Al 27Al 14C Pleistocene Age • 1.806 Ma to 11 ka before now • Latest period of glaciation Significance 10Be and 26Al production Principle sources • Cosmogenesis – Meteoric or “garden variety” (atmospheric) – In situ terrestrial substrate (< 2 m) • Negative muon capture (> 2 m) • Radiogenesis • Interstellar protons Principle mechanism • 10Be (5.2 atoms g-1 a-1) – 16O(n,4p3n)10Be – 28Si(n,6p3n)210Be • 26Al (30.1 atoms g-1 a-1) – 28Si(n,p2n)26Al Dual analysis of cosmogenic nuclides Nuclide activity is a function of: (a) Constants (relatively) • Nuclide half-life • Nuclide production rate • Substrate density • Attenuation length for neutrons (b) Variables • Exposure history • Erosion history 10Be- and 26Al-specific challenges Challenge Solution (nominal) Be is not native to quartz Al is native (feldspars) Add stable Be carrier Acid leech and monitor [Al] Common extraction scheme Stability of Be anion Accelerate BeOChemical behavior Be isobars (B) Al isobars (Mg) Minimize B exposure Accelerate Al- Data courtesy of Middleton, R. A Negative Ion Cookbook, University of Pennsylvania Al2O3 current product (mA) AlO- 20-40 AlO2- 4-6 Al- 1 Analysis of rare isotope abundances Steps of the analytical method Conventional MS 1. Formation of atomic and/or molecular ions 2. Acceleration through electrostatic potential (~kV) 3. Separation of ions based on m/z 4. Measurement of ions in detector Accelerator MS 1. Formation of negative atomic and/or molecular ions 2. Acceleration through electrostatic potential (~kV) 3. Acceleration to MeV energies 4. Separation of ions based on m/z 5. Measurement of ions in detector AMS block diagram Center for Accelerator Mass Spectrometry (CAMS) at LLNL (3) (2) (1) (5) (4) Photographs courtesy of Lawrence Livermore National Laboratories Principles of AMS operation 1. Formation of negative atomic and/or molecular ions • • • • Cs+ sputter source Negative ions Source geometry “Ion Sourcery” 2. Acceleration through electrostatic potential (~kV) • • • Injector magnet Low resolution filter Fast ion switching 3. Acceleration to MeV energies • • • • Tandem accelerator 10 MV terminal Electron stripper Molecular isobars Principles of AMS operation (continued) 4. Separation of ions based on m/z • Magnetic analyzer (ME/q2) • Electrostatic analyzer (E/q) • Velocity analyzer (E/M) 5. Measurement of ions in detector • • • • • Gas ionization detector Isobar-radionuclide pair with same E Stopping power (Z) Electron-ion pairs E vs. DE Figures of merit 10 Cosmogenic Be abundance Sensitivity 1E-13 1E-14 Old Blanks 1E-15 (26Al) 1E-16 1997 New Blanks 0 50 100 Blank # 150 2007 Figures of merit Significance (continued) Accuracy Systematic errors (uncertainty in…) • Production rate • Latitude/longitude scaling • Geomagnetic/solar modulation (temporal) • Assigned constants Precision • External error (rep>3x) • Internal error (Poisson) Poisson 1 n Poisson 1 3% 1100 Throughput • BeO cathode ~ 10 min • Al2O3 cathode ~ 30 min Investigatory Aims Observations • • 10Be analysis is typically limited by B 26Al analysis is typically limited by ion beam currents Ultimate goals • Improve cosmogenic 10Be and 26Al analysis with better wet & analytical chemistry • Improve precision for challenging samples Strategy to improve 10Be and 26Al AMS analyses • Determine effect of sample composition on AMS ion source behavior • Characterize quartz extraction chemistry: – Trace the fate of Be and Al – Track the movement of impurities – Identify problematic areas in the procedure • Make blanks with better background ratios from beryl • Produce AMS cathodes which generate sufficient ion beam current ion beam current (mA) AMS ion beam currents (BeO-) 25 20 Value (mA) Mean=13.1 Median=13.4 Minimum=1.6 Maximum=25.1 15 10 5 0 0 10 20 30 40 50 sample (n=64) 60 Elemental analysis Al Fe concentration in quartz (ppm) 400 Ti Ca Mg Na K (a) native quartz 300 200 100 75th % 400 25th % (b) BeO cathodes 300 200 100 0 Al Be Fe Ti Mn Ca Mg Theoretical ion beam current (mA) Effect of elemental composition on BeO- ion beam currents 25 20 mg a Al -0.02 Be 0.03 Ca 0.03 Fe -0.05 Mg 0.03 Mn -0.02 Ti -0.02 15 10 5 0 0 b 0.01 0.01 0.05 0.12 0.12 0.06 0.01 c -4.15 2.77 0.70 -0.46 0.24 -0.25 -4.03 5 10 15 20 25 30 Predicted ion beam current (mA) d 0.00 0.01 0.49 0.64 0.81 0.80 0.00 Notation • parameter estimate • standard error • t ratio • Prob>t. Concerning the extraction of BeO and Al2O3 from quartz Overview • Empirical procedure • Time consuming – Pre-treatment – Acid-digestion – Separation • Hazardous • Cleanliness (isotopic) Yield trace analysis • Clean and characterize quartz • Supplement native composition • Aliquot during a standard extraction • Elemental analysis by ICP-AES • Matrix matched standards • Dilute into linear dynamic range Separation methods: Part I Separation methods: Part II Fraction of net mass of element recovered Anion exchange chromatography (a) (b) 0.75 Al 0.50 0.25 Parameters • cv: 20 mL • Resin type: AG X18 • Elution rate: 1 drop/s • (a) 8 M HCl • (b) 1.2 M HCl 0.75 Be 0.50 0.25 0.75 Fe 0.50 0.25 0.75 Ti 0.50 0.25 0.00 0 1 2 Column volumes eluted 3 pH selective precipitation Low pH (3.8-4.1) High pH (~8.5) Cation exchange chromatography Fraction of net mass of element recovered (a) (b) (c) (d) 0.75 Be 0.50 0.25 0.75 Al 0.50 0.25 0.75 Mg 0.50 0.25 0.75 Ca 0.50 0.25 0.75 B 0.50 0.25 0.75 Ti 0.50 0.25 0.00 0 5 10 15 Column volumes eluted Parameters • cv: 10 mL • resin: AG 50W-X8 • Rate: 1 drop/s • (a) 0.5 M H2SO4 • (b) 1.2 M HCl • (c) 3.0 M HCl • (d) 6.0 M HCl Key steps in quartz extraction Dissolution by multi-acid digestion • 2H3O+ + [TiF6]2- <=> TiO2 + 6 HF • Selective distillation of HF relative to HClO4 Anion exchange • Good for Fe but not good for Ti separation Precipitations • Poor reproducibility • Qualitative analysis Cation exchange • Triple acid elution • Boron removal • Decent Ti separation The matrix effect Background • Convention of mixing BeO in a metal matrix (e.g Ag or Nb) prior to AMS analysis to provide high ion beam currents • Ion source design Experimental parameters • Amount of metal mixing matrix • Target packing with respect to depth • Matrix composition Long term goal • Understand mechanism of matrix enhancement and predict possible matrix for 26Al Matrix elemental properties Hypothesis Matrix effectiveness is dependent upon •Ion source presentation •Quantitative composition •Physicochemical characteristics of matrix Experimental design Sample preparation • Measuring: volumetric curette • Mixing: BeO with metal • Ratio: serial dilution with mole fraction (cmatrix = 0.50 to 0.95) • Packing: tamped into targets Instrumental analysis • Stable BeO- beam: (10 min) instantaneous and integrated current measurements • Usual matrices: Ag, Nb • Novel matrices: Mo, Ta, V, W, Os 2.5 mm 1 mm Meyhoefer curette Stability for Nb:BeO cathodes (post Ag) i (μA) rsd t=0-660 s 13990 3.59% t=30-330 s 6380 2.76% BeO- beam currents Effect of analyte: matrix ratio mass BeO (mg) mass BeO (mg) 1.08 0.79 0.48 0.17 0.94 0.71 0.48 0.28 0.09 10 4 10 4 10 3 10 3 10 1.0 2 cAg cNb 10 2 0.5 0.6 ion current (mA) ion current (mA) 1.35 0.7 0.8 0.9 1.0 0.5 0.6 0.7 0.8 0.9 Control of cathode presentation depth Experimental design • Depth is defined as space above target surface • Sample composition is an equimolar mixture of matrix and oxide • Depth is measured with a micrometer • Measure integrated currents for a typical analysis period depth CAMS target Implications of depth effect Implications • BeO in Nb has no depth effect • BeO in Ag has a significant depth effect • currents for samples in Ag matrix can be improved (with limited practical value) • Nb and Ag exhibit a different response • Is the Nb “enhancement” related to the depth effect? More BeO ion beam currents Matrix enhancement, part 2 AMS counting efficiency for BeO Correlation to matrix properties Interpretation of matrix effects Observations • Nb is not a magic powder: all of the tested matrices provide some level of BeO signal enhancements • Low e.a. is important (and low k and f) • The mixing ratio effect is important for optimization • The presentation depth effect may be important Practical recommendations • Effect of matrix mole ratio Optimal cNb between 0.5 and 0.65 (4:1 to 7:1 bm) Achieve high beam currents with less BeO • Effect of presentation depth In a Nb matrix, packing depth is not significant Al2O3 ion beam currents cmatrix More Al2O3 ion beam currents Correlation to matrix properties Elemental Al Correlation to matrix properties R2=0.70 R2=95 Future work for Al • Correlate cathode composition with current for Al • Separation of elemental Al • Better characterization of ionization • Analysis of cathodes post-AMS analysis (physical and/or chemical) Acknowledgments • • • • • Committee members Petrucci group Bierman group LLNL CAMS group DOD-EPSCoR 5 10 4 10 3 1.24 cMo ion current (mA) 0.5 10 5 10 4 10 3 0.15 ion current (mA) 10 mass BeO (mg) 0.97 0.7 0.43 0.6 0.7 0.8 0.9 mass BeO (mg) 1.33 1.05 0.74 1.59 0.6 0.7 0.8 5 10 4 10 3 0.4 cV 0.5 10 0.9 1.0 10 5 10 4 10 3 mass BeO (mg) 0.54 0.36 0.2 0.74 0.07 cTa 0.5 1.0 ion current (mA) ion current (mA) Effect of analyte: matrix ratio 0.6 0.7 0.8 0.9 mass BeO (mg) 1.03 0.75 0.45 1.3 1.0 0.16 cW 0.5 0.6 0.7 0.8 0.9 1.0 Titanium in the ion source ion beam current ( m A) TiO2 impurity 3.00 2.50 2.00 1.50 1.00 0.50 0.00 0 500 1000 time (s) 10% TiO2 impurity pure Al2O3 1500 osmium beam currents & elemental properties 25 10 Os 9 Os 8 Ag Nb Os 7 6 15 1:1 10 2.3:1 5 9:1 value ion current (mA) 20 5 4 3 2 1 0 0 100 200 300 400 500 600 time (s) 0 e.a. (ev) k (W/cmK) f (eV) r (n ) DHvap (J/g) AMS counting efficiency for Al2O3 Matrix enhancement Initial digestion • Sample contains – native elements – Be (and sometimes Al carrier) Anion exchange separation • Separate major interferences – soluble ferric and titanic ions Mass ratio (supernatant/precipitate) Selective precipitation (low pH) 10 2 10 1 10 0 10 -1 10 -2 Be Mg Ca Al Ti Fe 10 -3 3.0 3.5 4.0 pH 4.5 A brief history of “ultra-radiation” Victor Hess (1936) • Observation: Radioactive species (a,b,c) • Hypothesis: They come from Earth • Experiment: Electrometry at different altitudes • Results: They come from Space Austria (1912)