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LEA—A NOVEL LOW ENERGY ACCELERATOR FOR 14C DATING

Published online by Cambridge University Press:  29 September 2023

Urs Ramsperger*
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
Daniele De Maria
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
Philip Gautschi
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
Sascha Maxeiner
Affiliation:
Ionplus AG, Dietikon, Switzerland
Arnold Milenko Müller
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
Hans-Arno Synal
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
Lukas Wacker
Affiliation:
ETH Zürich, Laboratory of Ion Beam Physics, Zurich, Switzerland
*
*Corresponding author. Email: ramsperger@phys.ethz.ch
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Abstract

A newly developed compact AMS, LEA (Low Energy Accelerator), is tested and compared with a state-of-the-art AMS system MICADAS (Mini Carbon Dating System), which has a precision performance of better than 1‰ for modern 14C. The main difference between these two systems is the acceleration voltage, which has been reduced from 200 kV with the MICADAS system to 50 kV with the LEA system. In order to execute the final performance tests, exactly same samples (2 sets consisting of 7 standards, 4 blanks, 26 wood samples) are measured on both systems successively. The results show that the LEA system is fully operational, and the performance is entirely comparable with that of the MICADAS system.

Information

Type
Conference Paper
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2023. Published by Cambridge University Press on behalf of University of Arizona
Figure 0

Figure 1 Schematic representation of the LEA AMS system operating at ETH Zurich. This compact AMS instrument has an overall footprint of just 3 m x 2 m. The beam injector (LE-side) reproduces the one of the MICADAS system. The size of the HE-side has been reduced due to the new design of the accelerator unit and the lower energy of the ions after the tandem acceleration stage (terminal voltage around 50 kV).

Figure 1

Figure 2 Schematic view of the high energy end of the LEA AMS system. The stripper housing is differentially pumped and the conductance limiting aperture is separated from the acceleration section. The following magnetic (p/q) and the electrostatic (E/q) filtering elements are combined to enable an achromatic image of the ions emerging form the stripper tube to the final ion detector. Red: ion trajectories of 14C ions, blue trajectories of 12C and 13C ions, as they are sequentially injected into the acceleration stage by the fast beam bouncing system.

Figure 2

Figure 3 Two energy spectra of a PhA blank sample taken with an isobutane gas detector through 30 nm (blue lines) and 50 nm (red lines) Silicon Nitride membrane windows respectively. The horizontal axis refers to the energy level of the detected particles given in arbitrary units (au). Each spectrum is measured with the same blank sample for 30 min at a HE 12C current of >10 μA. The gap between the background peak and the 14C peak is clearly visible in the measurement taken with the 30 nm window, while the two peaks overlap in the spectrum with the 50 nm window.

Figure 3

Figure 4 Low energy magnet (a) and high energy magnet (b) beam scans taken after optimizing the different isotopic beams. Black squares indicate normalized 12C ion currents, green 13C currents and red 14C normalized counts. The 13C/12C ratio is indicated by yellow circles. Please note the flat region of the 13C/12C isotope ratio in both scans ensuring long-term stable performance of the LEA system. Transparent green areas show possible magnetic field values for a stable measurement, while the blue lines indicate the values we chose for the measurements, BLE = 428.0 mT for the low energy magnet and BHE = 847.2 mT for the high energy magnet. Please note that since the isotopic beams are not perfectly Gaussian, the 14C peak in the HE-magnet scan is chosen slightly left to optimize the transmission. The rather narrow 14C scan is caused by another filter (electrostatic, E/q filter) that the 14C isotopes have to pass (see Figure 2).

Figure 4

Figure 5 (a) 14C/12C ratios measured for two phthalic acid blanks. Each run has a testing time of 300 s and 23 runs are taken of each sample. Statistical uncertainties are indicated by error bars, while mean values and their uncertainties are indicated by solid and dashed black lines, respectively. The radiocarbon age of blank 1 is more than 52,900 years (F14C = 0.00138) and blank 2 more than 54,600 years (F14C = 0.00110), which is not only a strong indication of a good measuring system, but also of clean sample preparation. (b) 14C/12C ratios (13C/12C fractionation corrected) measured for five Oxalic Acid II standards. Each run has a testing time of 300 s and 23 runs are taken of each sample. The total number of 14C events detected is 106 counts per sample. Statistical uncertainties are indicated by error bars, while mean values and their uncertainties are indicated by solid and dashed black lines, respectively.

Figure 5

Figure 6 Dark blue (Data MICADAS set 1) and bright blue (Data MICADAS set 2) dots and lines in the diagram indicate data points of MICADAS measurements, while dark red (Data LEA set 1) and bright red (Data LEA set 2) dots and lines show data points of LEA measurements. The horizontal axis presents the (known) calendar age of the samples and the vertical axis illustrates the measured radiocarbon age. There is excellent agreement between the results of these measurements, showing a mean deviation of 1.0 ± 4.7 yr (< 0.13 ± 0.6‰). In order to ensure sufficient counting statistics, a number of at least 106 detected 14C events is aimed for a standard sample (Oxa2).

Figure 6

Table 1 Comparison of the specifications of the two AMS systems, MICADAS and LEA. The transmission (${}_{}^{12}{\rm{C}}_{{\rm{HE}}}^ + /{}_{}^{12}{\rm{C}}_{{\rm{LE}}}^ - $) is significantly higher with the LEA system but requires a lower beam current for stable measurements. Both properties determine the duration of the experiments, which is, overall, still shorter with the MICADAS system, providing the same level of precision. The accelerator is operated in a tandem configuration, resulting in the total energies for the isotopes being approximately 140 keV for LEA and 420 keV for MICADAS.