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Cosmogenic isotope measurement inter- comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

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The quality of the measurement is determined by the laboratory. Sound, reliable, precise and accurate measurement requires trace-ability to community agreed reference materials and standards

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Page 1: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Cosmogenic isotope measurement inter-comparison

Marian Scott, Tim JullUniversity of Glasgow, University of

Arizona

July 2008

Page 2: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

The CRONUS inter-comparison

• To assess comparability of measurements made by the different laboratories

• To assist in the definition of overall uncertainty when results from different laboratories used.

• Carried out through a programme of comparisons, small number of samples distributed to the laboratories.

Page 3: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

•The quality of the measurement is determined by the laboratory.

• Sound, reliable, precise and accurate measurement requires trace-ability to

community agreed reference materials and standards

Page 4: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Reference materials

• Basic purpose: improvement of comparability of measurement results

• Possible uses– for calibration, to demonstrate trace-ability– for quality control, to verify the performance of

a method

Page 5: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Reference materials

• For calibration, material often artificially produced so its properties are known with low uncertainty

• for quality control, material is often ‘real world’, so that it behaves as similarly as possible to the samples being measured.

Page 6: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Objectives of TCN within CRONUS

• To explore the comparability of results from the different laboratories – generate consensus values for a range of

reference materials• to assist laboratories in independently

assessing quality and • to quantify precision and accuracy

Page 7: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

What information can be quantified from an inter-comparison?

• Accuracy (from known activity samples)

• Laboratory precision (from duplicate samples) leading ultimately to quantification of

• Measurement uncertainty

• Quality Assurance (QA)

Page 8: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

What is QA?

QA is an early warning system - it is retrospective and dynamic, based on judgement of the measurements on backgrounds, standards and reference samples (including internal laboratory materials).

It is the laboratory paper trail, and in-house checks

Page 9: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Quality issues

User concerns How good are my results? what does the quoted

uncertainty represent? Laboratory concerns Is my system stable? Are there any sources of

contamination in the laboratory? How do the results compare to those expected?, ……How good are my measurements?

Page 10: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

QA involves

Internal checking Measurements made on a series of replicate

samples (Polach (1989) noted ‘internal checking needs suitable quality control and reference materials’.)

Monitoring of background, standards, known-age and reference materials

Independent (external) checking Laboratory inter-comparisons

Page 11: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Time line of activities within CRONUS

• Design the inter-comparison– Identify suitable samples (and criteria) done– Agree timescale for results- done- phase one

results due in April 2008– Define format for reporting results done

• Inform laboratories and ask for expression of interest to participate (done)

• Distribute samples- phase 1: done

Page 12: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Timeline

• For phase 1– Distribution July 2007, results returned April

2008– Archive material for future use

• Location of archive- currently in Arizona- sufficient material for at least 10 more intercomparisons of the same size

– 23 laboratories sent samples

Page 13: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

identified inter-calibration standards

• Noble gasesthere are 2 potential “standards” – the pyroxene of Schaefer and an EU sample (from Wieler) .

– pyroxene sample distributed• AMS standards

prepared and available from Nishizumi- not distributed as part of CRONUS

Page 14: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

identified inter-calibration samples-distributed July 2007

• (A)ntarctic sample: high in Al-26 and Be-10. Quartz was separated at U of Vermont, etched 3 times in HF and washed. Recommended 5g be used. Approx 37g provided

• (N)amibia: a low latitude sample, recommend 20g be used. approx 75g provided

• For in-situ C-14, same samples provided in glass vials.

Page 15: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

typical format for reporting results eg Al-26

Mass of sample (quartz) (g) used in the measurement:AMS Standard used in the measurement Half-life used Background material used  measured 26Al/27Al ratio (1 uncertainty) (specify

units)  mass (number of atoms of 27Al) in sample number of atoms 26Al in lab process blank

Page 16: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Participating laboratories

Al, Be, C- USA, UK, France, Switzerland, Germany, The Netherlands, Sweden, Australia, Canada (24 in total)

Noble gases: USA, UK, Switzerland, France, Germany (14 in total)

Page 17: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Results so far in CRONUS

• So far, results from 7 laboratories for samples A and N, from 2 laboratories for sample P: laboratories have often reported replicate results

• There is general consensus on half-life used for Al, but some variability for Be (1.5,1.51, 1.36, 1.37 x 106)

• Standards used • Be:- NIST SRM4325, Nishiizumi SYD Be01-5-4• Al:- Z92-0222(PRIME, Purdue), Nishiizumi STD Al

0143

Page 18: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Results so far in CRONUS

• Sample A, – Be analysis– 13 results, coefficient of variation (CV)

(stdev/mean*100%) is 4.92– Al analysis– 6 results, CV 7.92%

Page 19: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Results so far in CRONUS

• Sample N (lower Be and Al by approx factor of 100 than sample A), – Be analysis– 15 results, coefficient of variation (CV)

(stdev/mean*100%) is 9.34%– Al analysis– 6 results, CV 9.2%%

Page 20: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Potential analysis• Similar to that used commonly for the C-14 inter-

comparisons, defining reproducibility but will use z-scores, defined as standardised deviations from a consensus value

• for each sample, we define an agreed value (usually a robust estimate based on all results)

• the z-score is defined as the difference between an individual result and the robust value standardised to account for the uncertainty (also based on a robust estimate).

• properties of Z-scores well understood- used internationally in proficiency trials.

Page 21: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

The error in a measurement

• A single value, which represents the difference between the measured value and the true value

• However, for these samples, we do not have the true or real Al/Be atoms/g, so we use the inter-comparison to define this value (as a consensus from the participating laboratories)

Page 22: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Key properties of measurement

• Accuracy of the measurement refers to the deviation (difference) from the true value (or sometimes expected or consensus value)

• Precision refers to the variation (expected or observed) in a series of replicate measurements (obtained under identical conditions). High precision, low uncertainty

Page 23: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Accuracy and precision

Accurate and inaccurate and precise

Accurate and inaccurate and imprecise

Page 24: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Evaluation of accuracy

• In FIRI and VIRI, known-age material is used to define the ‘true’ age

• The figure over shows a measure of accuracy for individual laboratories1009080706050403020100

500400300200100

0-100-200-300-400-500-600

laboratory identifier

Offs

et (y

ears

BP

)

Page 25: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Between laboratory variation

• reproducibility –identical samples, different laboratories

Page 26: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Reliability and reproducibility

• Repeatability (r) refers to measurements made under identical conditions in one laboratory,

• Reproducibility (R) refers to measurements made in different laboratories, under different conditions.

• Reproducibility is the closeness of agreement between test results under conditions where the same method is used in different laboratories.

Page 27: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Reliability and reproducibility

• The reproducibility value R is the value below which the absolute difference between two single results obtained under reproducibility conditions may be expected to lie with probability 0.95.

• A difference larger than R cannot be ascribed to random fluctuations and would warrant investigation of possible sources of systematic differences.

Page 28: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Reproducibility (VIRI phase 1)

2500 3000 3500 4000

Age (Years)

020

4060

8010

0

37.328 3861 61.214 1140 41.239 2932 3437.1 3042 7164 3354 63.137.2 5062.3 69.170.2 4413 545 3646.3 6315 3143.1 62.120 6725.1 13.155 70.157 45.158 453 46.462 62.46 4648 310 2356 25.316 16.125.4 2722.1 925.2 6521 4143 46.267.1 2624 846.1 62.27 2547 43.222 3566 1770 3759 5112 6941.1 66.11 492 5219 18

Archaeological Age = 2850-2900

~95% Confidence Intervals for Age, for Sample D

Page 29: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Estimation of r and R

• Model: Y = m + B + ewhere Y is the measurement, m is the average activity, B is

the between-laboratory variation and e is the random error.

• B is assumed random and var (B) = 2L

• e is assumed random and for a single laboratory var(e) = 2

W.

2W assumed constant for all laboratories, with

average value 2r.

Page 30: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

r and R

• The repeatability value r is 2.8 r

• The reproducibility value R is 2.8 R , where R = (2

L + 2W)

• 2L , 2

W and r must all be estimated.

Page 31: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Conclusions

• All measurement is subject to uncertainty, the test of which is to make replicate measurements

• Inter-laboratory trials provide generic measures of reproducibility and assessment of laboratory comparability

• For cosmogenic isotope work, this is still at an early stage

• CRONUS inter-comparison has archived material for future use, but for satisfactory characterisation, we need more results

Page 32: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

Actions- for 2008

• Finalise acquisition and preparation of the 2nd suite of samples.

• Agree a timescale and distribute the samples (ideally distribute shortly after results of phase 1)

• await results- for phase 2, assuming distributed September 2008, deadline for results- Feb 2009.

• analysis of results from phase 1- reported by August 2008.

Page 33: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

other potential inter-calibration samples

• Antarctic sample: 14C, 10Be, 26Al, 21Ne.• Namibia: 14C, 10Be, 26Al, 21Ne.• Maine: 14C, 10Be, 26Al, 21Ne.• NMT basalt: 36Cl.• Carbonate/sandstone: 36Cl, 10Be, 26Al.Some other potential materials are:• Lake Bonneville basalt sample.• Promontory Point quartzite• Blank quartz

Page 34: Cosmogenic isotope measurement inter-comparison Marian Scott, Tim Jull University of Glasgow, University of Arizona July 2008

acknowledgements

• All the participating laboratories, the sample providers (Paul Bierman and Joerg Schaefer), NSF for funding.