ISOTOPIC ABUNDANCE IN ATOM TRAP TRACE ANALYSIS

Abstract

A method and system for detecting ratios and amounts of isotopes of noble gases. The method and system is constructed to be able to measure noble gas isotopes in water and ice, which helps reveal the geological age of the samples and understand their movements. The method and system uses a combination of a cooled discharge source, a beam collimator, a beam slower and magneto-optic trap with a laser to apply resonance frequency energy to the noble gas to be quenched and detected.

Description

BACKGROUND OF THE INVENTION

The invention relates to methods and systems for detecting selected isotopes of all noble gases. More particularly, the invention is directed to methods and systems for performing atomic counting based on the atom trap trace analysis method (“ATTA”) to measure ratios of ⁸¹Kr/Kr and ⁸⁵Kr/Kr in environmental samples.

Krypton permeates through the atmosphere at a concentration of about one part per million. There are six stable Kr isotopes, and two rare, long-lived isotopes: ⁸¹Kr(t_1/2=2.29×10⁵ yr, isotopic abundance ⁸¹Kr/Kr=6×10⁻¹³) and ⁸⁵Kr (t_1/2=10 yr, ⁸⁵Kr/Kr−10⁻¹¹). Upon the discovery of ⁸¹Kr in the atmosphere, it has been proposed that ⁸¹Kr is an ideal tracer isotope for dating water and ice in the age range of 10⁵-10⁶ years, a range beyond the reach of ¹⁴C-dating. ⁸¹Kr is mainly produced in the upper atmosphere by cosmic-ray induced spallation and neutron activation of stable Kr. Due to its long residence time, ⁸¹Kr is expected to be distributed uniformly throughout the atmosphere. Subsurface sources and sinks for ⁸¹Kr other than radioactive decay are most likely negligible. Human activities involving nuclear fission have a negligible effect on the ⁸¹Kr concentration because the stable ⁸¹Br shields ⁸¹Kr from the decay of the neutron-rich fission products. All of these favorable conditions combine to support the case for ⁸¹Kr-dating. The other long-lived krypton isotope, ⁸⁵Kr, has a completely different production source. It is a fission product of ²³⁵U and ²³⁹Pu, and is released into the atmosphere primarily by nuclear fuel reprocessing activities. ⁸⁵Kr can be used as a tracer to study air and ocean currents, determine residence time of young groundwater in shallow aquifers and monitor nuclear fuel processing activities.

For ⁸⁵Kr analysis, low level decay counting (LLC) is performed routinely in a few specialized laboratories around the world. LLC was also the first method used to detect ⁸¹Kr and to determine its abundance in the atmosphere, but it is too inefficient for practical ⁸¹Kr-dating because only a fraction 3×10⁻⁸ of ⁸¹Kr atoms in a sample decays in a 100-hour measurement. In general, counting atoms is preferable to counting decays for analyses of long-lived isotopes because of the enhanced efficiency, and because of the immunity to other decay backgrounds from both the sample and the surroundings. An accelerator mass spectrometry (AMS) method for counting ⁸¹Kr ions has been developed, and has been used to perform ⁸¹Kr-dating of four groundwater samples from the Great Artesian Basin of Australia. However, due to the complexity of this technique, which required the use of a high energy (4 GeV) cyclotron to produce fully stripped ⁸¹Kr ions, and the large sample size required (16 tons of water), the AMS effort on ⁸¹Kr-dating was halted following these proof-of-principle measurements.

Atom Trap Trace Analysis (ATTA) is another type of atom-counting method capable of detecting both ⁸¹Kr and ⁸⁵Kr in environmental samples. In ATTA, an atom of a particular isotope is selectively captured by resonant laser light in a magneto-optical trap (MOT) and detected by observing its fluorescence. Following the first demonstration of ATTA, both the reliability and counting efficiency of the ATTA instrument have been improved. An earlier version, ATTA-2, had a counting efficiency of 1×10⁻⁴ and, for each ⁸¹Kr/Kr analysis, needed a sample of 50 μL STP of Kr gas extracted from approximately 1000 kg of water. The ATTA-2 instrument had a limited dynamic range: it could only be used to count the rare ⁸¹′⁸⁵Kr isotopes, not the abundant stable isotopes, for example, ⁸³Kr whose isotopic abundance is 11.5%. The isotopic abundance ⁸¹Kr/Kr had to be measured in two steps: first, a controlled amount of ⁸⁵Kr was introduced into the sample and its ⁸⁵Kr/Kr ratio was determined with LLC; second, ATTA-2 was used to measure ⁸¹Kr/⁸⁵Kr. The two ratios were then combined to obtain ⁸¹Kr/Kr. Despite its dependence on additional measurements with other techniques and the relatively large sample size required, ATTA-2 was used successfully for ⁸¹Kr-dating of old groundwater of the Nubian aquifer in western Egypt. However, none of these prior art methods and systems, including the existing ATTA-2 systems have enabled efficient or commercially practical methods and systems for detection and analysis of ⁸¹Kr/Kr or ⁸⁵Kr/Kr ratios. Consequently, there is a substantial need for a commercially efficient method for Kr isotope measurements and analysis.

SUMMARY OF THE INVENTION

An efficient and selective atom counter (ATTA-3) system and method based on this Atom Trap Trace Analysis (ATTA) method has been developed to measure both ⁸¹Kr/Kr and ⁸⁵Kr/Kr ratios of environmental samples in the range of 10⁻¹⁴-10⁻¹⁰. Compared to the previously reported ATTA-2 instrument, the counting rates of ATTA-3 are higher by two orders of magnitude and the required sample size lower by one order of magnitude. For ⁸¹Kr dating in the age range of 200-1,500 kyr, the required sample size is 5-10 μL STP of krypton gas, which can be extracted from approximately 100-200 kg of water or 40-80 kg of ice. Moreover, a laser-induced quenching scheme was developed to enable measurements of the trap capture rates of both the rare ^81,85Kr and the abundant ⁸³Kr, whose isotopic abundances differ by 11 orders of magnitude. This scheme allows the ATTA-3 system to directly determine ⁸¹Kr/Kr and ⁸⁵Kr/Kr ratios without other supplemental measurements. ATTA-3 represents a highly effective and commercially efficient method and system for routine analysis of these rare noble gas tracers Now for the first time, ⁸¹Kr-dating is available for commercial use and used by the earth science community at large. It should also be appreciated that the described ATTA-3 can also be used to analyze other noble gas isotopes, for example, ³⁹Ar.

These and other advantages and features of the invention, together with the organization and manner of operation thereof, will become apparent from the following Detailed Description when taken in conjunction with the accompanying drawings described below.

BRIEF DESCRIPTION OF THE DRAWINGS

FIG. 1 shows a schematic of the ATTA-3 apparatus of the invention; the total length of the atomic beamline is approximately 2 m. lasers and optics are located on an adjacent laser table of a similar length;

FIG. 2 shows an atomic level diagram of Kr; the 5s[3/2]₂ state is metastable and the cycling transition 5s[3/2]₂-5p[5/2]₃ is excited for trapping and its fluorescence detected for single atom counting of ^81,85Kr; the transition 5s[3/2]₂-5p[5/2]₂ is excited to quench the metastable ⁸³Kr atoms, and the 5s[3/2]₁-5p[5/2]₂ fluorescence is detected for ⁸³Kr measurements;

FIG. 3 shows the detection of single ⁸¹Kr atoms in the trap. (a) the fluorescence image of a single ⁸¹Kr atom in the trap as recorded by the CCD camera. (b) photon counts integrated over a region-of-interest on the CCD image shows discrete steps as individual atoms are captured by or lost from the trap.

FIGS. 4( a)-(b) show trap capture rate versus laser frequency detuning. (a) The integration time for each data point of the ⁸¹Kr peak is one hour, and 10 minutes for ⁸⁵Kr. The atom is detected by collecting the 811 nm fluorescence on the cycling transition. Zero atom counts on both sides of peaks illustrate the immunity of ATTA to any contamination by other species. (b) For ⁸³Kr, 878 nm fluorescence is recorded in the laser induced quenching procedure (see text for details).

FIG. 5 shows comparison of the atom capture rates between the rare ⁸¹Kr and abundant ⁸³Kr for a single test sample under a variety of trapping conditions; the linearity of the fit demonstrates that the 878 nm signal can be used effectively for normalizing the ⁸¹Kr/Kr (or ⁸⁵Kr/Kr) ratio measurements;

FIG. 6 shows comparison of ⁸⁵Kr/Kr ratios measured by ATTA-3 and LLC. ATTA-3 measures the ⁸⁵Kr/⁸³Kr ratio in arbitrary units. LLC measures the ⁸⁵Kr decay activity in the units of decays per minute per cc-STP of krypton gas (dpm/cc); six samples (blue data points) were measured in a blind arrangement—the ATTA-3 and LLC results were only revealed and compared after the measurements had completed; in addition to the points shown in this figure, a sample with ⁸⁵Kr below the LLC detection limit was also analyzed: LLC, ⁸⁵Kr activity <1 dpm/cc; ATTA-3, ⁸⁵Kr/⁸³Kr <2.0 (90% C.L.). ATTA-3 and LLC results agree at the +7% level (chi-square=1.1); and

FIG. 7. shows sample size vs sample age and desired accuracy for ⁸¹Kr-dating; the two curves are for a relative age error off 10% and ±20%, respectively.

DETAILED DESCRIPTION OF THE PREFERRED EMBODIMENTS

An ATTA system 100 constructed in accordance with a method and system of the invention is shown in FIG. 1. In the method of the invention laser trapping and cooling of Kr atoms are achieved by the resonant excitation of the cycling transition 5s[3/2]₂-5p[5/2]₃ (see FIG. 2). This 5s[3/2]₂ state is metastable, and is populated with an efficiency of 10⁻⁴ by sending the sample gas through a RF-driven discharge source. A newly developed discharge source 110 is cooled by a liquid nitrogen reservoir (not shown), resulting in a slower beam of atoms 115 and a gain by a factor of two in the trapping efficiency. A diverging beam 120 of metastable atoms is collimated in a 20 cm long, two-dimensional transverse cooling zone 130. The forward atomic beam flux is enhanced by a factor of one hundred forty, resulting in a gain by a factor of two over the prior art ATTA-2 method. A mechanical beam chopper 135 is used to periodically turn on the atomic beam in the capture phase and to turn it off in the detection phase. A two-dimensional MOT type of trap 150 is installed in the system 100 to focus the already collimated atomic beam, thus boosting the trap capture efficiency by a factor of three. A new Zeeman slower 140, containing a reverse-biased segment near the MOT 150, improves the transition of atoms from the slower into the MOT trap 150, and improves the trapping efficiency by a factor of three. In addition, a factor of three increase in laser power (a total of 2 W) and complete sideband coverage for hyperfine repumping improve the trapping efficiency by a factor of four.

Analyzing an atmospheric Kr sample, the system 100 can capture ⁸³Kr (11.5%) atoms at the rate of ˜1×10¹¹ s⁻¹, ⁸¹Kr(6×10⁻¹³) at the rate of 1,000 per hour and ⁸⁵Kr (10⁻¹¹) at 20,000 per hour. This represents a combined improvement by two orders of magnitude over the previously reported prior art ATTA-2 results. Further, instead of an avalanche photodiode employed in ATTA-2, a sensitive EMCCD camera 160 is used in the system 100 to image the fluorescence of the trapped atom. The described examples utilized a Luca S EMCCD camera made by Andor Technology A single Kr atom in the trap is repeatedly excited on the 5s[3/2]₂-5p[5/2]₃ transition by the resonant trapping laser beams at 811 nm (see FIG. 2). The atom absorbs and emits photons at the rate of 1×10⁷s⁻¹, of which 1% of the fluorescence photons are collected by an imaging lens onto the camera. By providing the spatial as well as the intensity information, the camera image (see FIG. 3a) makes it easier and more reliable to align the single trap. A circular region of interest is defined on the camera image, within which the photon counts are integrated to form a signal of the atom (see FIG. 3b). Background photon counts are caused by both the laser light scattered off walls and the dark counts of the camera. Under the optimum conditions, the signal-to-noise ratio of a single trapped atom is approximately twenty. The threshold for single atom detection is set at seven standard deviations above background.

The system 100 is immune to interference from any other isotope, element, or molecule. When the laser frequency is tuned to the resonance of the desired isotope, ⁸¹Kr or ⁸⁵Kr, only atoms of this specific isotope are trapped (see FIG. 4a). Other species are either deflected before reaching the MOT 150 or are allowed to pass through it without being captured. Indeed, the number of atom counts drops to zero on both sides of the ⁸¹Kr or ⁸⁵Kr peak. There is no interference from counts due to the nearby peak of ⁸³Kr (see FIG. 4b), an isotope that is more abundant by 11 orders of magnitude. This superb selectivity is due to two characteristics of the MOT 150: resonance and repetition—laser trapping works only when the atom resonantly and repeatedly scatters photons at the rate of 10⁷ per second.

Compared to single-atom counting of ⁸¹Kr or ⁸⁵Kr, an accurate determination of the trap capture rate of the abundant isotope ⁸³Kr is surprisingly difficult, yet it is required in order to measure the isotopic abundances of ⁸¹Kr/Kr and ⁸⁵Kr/Kr. Here, we assume that the ⁸³Kr/Kr ratio (=11.5%) is a constant throughout the near-surface Earth environment. Interaction among the large number (10⁹) of ⁸³Kr atoms in the trap causes loss of atoms due to ionization, quenching, and other forms of inelastic collisions. Consequently, the average time for an atom to stay in the MOT 150, the so-called trap lifetime, depends sharply on the number and the density of atoms in the MOT 150, and is difficult to control and determine to the required accuracy (±5%). Since the fluorescence signal of the cycling transition at 811 nm from the trapped ⁸³Kr atoms is proportional to the trap lifetime—the longer an atom stays in the MOT 150, the more fluorescence photons at 811 nm it emits—the large uncertainty in determining the MOT 150 lifetime causes a similar difficulty in accurately determining the capture rate of ⁸³Kr. This is not a problem for counting the rare ^81,85Kr isotope. For one, the number of trapped ^81,85Kr atoms is small, and their trap lifetime is long (1 s) and stable. In addition, the signal size of the 811 nm fluorescence is discrete when there are only a couple of ⁸¹′⁸⁵Kr atoms in the MOT 150, making atom counting of ⁸¹′⁸⁵Kr possible without knowing the trap lifetime.

In prior art ATTA-2 system, this problem was bypassed by injecting a known amount of ⁸⁵Kr into the sample being analyzed and using ⁸⁵Kr as a control isotope for ⁸¹Kr measurement, and vice versa. This procedure introduced additional complexity and potential sources of errors into the final age determination. The system 100 has succeeded in measuring the capture rate of ⁸³Kr accurately with a laser-induced quenching procedure. A 200 μW laser beam of 810 nm is directed at the trapped atoms to resonantly excite the 5s[3/2]₂-5p[5/2]₂ transition (see FIG. 2). An atom excited to the 5p[5/2]₂ state decays to the ground state through the intermediate 5s[3/2]₁ state, emitting two photons at 878 nm and 124 nm, respectively. Once in the ground state, the atom no longer interacts resonantly with the laser beams and is lost from the trap. This quenching process actively reduces the lifetime and, thus, reduces the number of ⁸³Kr atoms in the MOT 150 by one order of magnitude while the collisional loss rate is reduced by two orders. While the 811 nm fluorescence of the cycling transition is proportional to the trap lifetime, the 878 nm fluorescence is not. Instead, each ⁸³Kr atom in the trap emits a single 878 nm photon before dropping to the ground state. The fluorescence at 878 nm, although much weaker, is linearly proportional to the rate of atoms being captured by the trap, and is insensitive to any drifts of laser power and frequency. Detecting the 878 nm fluorescence of ⁸³Kr induced by the quenching laser beam, we have measured both the ⁸¹Kr/⁸³Kr and ⁸⁵Kr/⁸³Kr ratios of a single test sample under a variety of trapping conditions and overall capture rates (see FIG. 5), and found these ratios to remain constant within the statistical uncertainty of ±9% for ⁸¹Kr/⁸³Kr and ±7% for ⁸⁵Kr/⁸³Kr. This new procedure is adopted in the system 100 for all isotope ratio measurements.

Cross-sample contamination is one limitation on the sample size requirement and sample processing time of the system 100. While the discharge is used to excite the Kr atoms to the metastable 5s[3/2]₂ state, it also ionizes the atoms and implants them into the surrounding walls, thus causing a slow loss of the sample. Later on, under the bombardment of the energetic ions, those embedded atoms of the current and previous samples can be slowly released back into the vacuum system. Over time, atoms from previous samples slowly accumulate in the system 100, causing an instrumental memory effect. This effect is mitigated by flushing the system 100 for 36 hours with a xenon gas discharge between measurements. During flushing, the outgassing rate of Kr is recorded with a residual gas analyzer, and is observed to drop by two orders of magnitude down to an acceptable level of 0.015 μL STP per hour. In addition, both the ⁸¹Kr/Kr and ⁸⁵Kr/Kr ratios of the outgassing Kr can be measured directly with atom counting. Although the contamination is small compared to the sample size of 5-10 μL, it is not entirely negligible, particularly when a sample is old and the ⁸¹Kr/Kr abundance is much lower than that of the contaminant from previous samples. Since both the release rate and the ⁸¹Kr/Kr abundance of the contaminant can be determined, a correction is made and its associated error is added to the result of each sample. In the future, this limitation may be removed by replacing the discharge source of metastable atoms with a photon excitation scheme.

The following non-limiting Example illustrates various aspects of the invention.

Example

The ⁸⁵Kr/Kr ratios measured at Argonne National Laboratory with the system 100 were compared to those measured independently at the University of Bern with LLC. A total of 12 Kr samples were prepared in Bern by mixing varying amounts of modern atmospheric Kr with a Kr sample originally taken from air prior to the dawn of the nuclear age containing basically zero ⁸⁵Kr concentration. The resulting ⁸⁵Kr/Kr ratios among these samples varies from 0 to 1×10⁻¹⁰. These ratios were determined both by the volume mixing ratios and by LLC of ⁸⁵Kr. The ⁸¹Kr/Kr ratios are expected to remain constant among all these samples. Using the system 100, both the ⁸⁵Kr/Kr and ⁸¹Kr/Kr ratios were measured several times for each sample, with each measurement consuming approximately 10 STP of Kr. During a measurement, the laser frequency was switched among ⁸¹Kr, ⁸³Kr, and ⁸⁵Kr every few minutes to average out any drifts in trapping and detection efficiencies. The final isotope ratio results, after correction for the memory effect, are displayed in FIG. 6. The system 100 and LLC measurements agree on the ⁸⁵Kr/Kr ratios at the ±7% level (chi-square=1.1). Moreover, the ⁸¹Kr/Kr ratios measured with ATTA-3 indeed remain constant at the ±9% level (chi-square=1.0). We note that the system 100 does not directly measure absolute isotope ratios. Instead, the measured ratios of unknown samples are normalized to those of a standard reference, for this example a well-studied atmospheric krypton sample. 2×2×. It should be appreciated that other samples can be utilized as a standard reference.

The required sample size for applications in ⁸¹Kr-dating depends on both the sample age and the desired uncertainty in age determination (see FIG. 7). ⁸¹ Kr-dating with the system 100 covers an effective age range from 150 kyr to 1.5 Myr, or 0.6-6 times the half-life of the isotope. On the side younger than 150 kyr, the change of ⁸¹Kr/Kr is too small to provide adequate age resolution. On the side older than 1.5 Myr, the ⁸¹Kr/Kr ratio itself is too small compared to the error introduced by the correction for the memory effect. Within the effective age range, a typical sample size is 5-10 μL STP of Kr gas, which can be extracted from approximately 100-200 kg of water or 40-80 kg of ice. It should be noted that these are not absolute requirements; rather, they should be viewed as a guideline. If needed, extraordinary steps, for example prolonged xenon flushing in order to reduce the memory effect, can be taken to further reduce the required sample size and meet the special demands of a particular application. The chemical purity of the krypton sample is not important since the ATTA method is immune to contamination from any other species.

The foregoing description of embodiments of the present invention have been presented for purposes of illustration and description. It is not intended to be exhaustive or to limit the present invention to the precise form disclosed, and modifications and variations are possible in light of the above teachings or may be acquired from practice of the present invention. The embodiments were chosen and described in order to explain the principles of the present invention and its practical application to enable one skilled in the art to utilize the present invention in various embodiments, and with various modifications, as are suited to the particular use contemplated.

Claims

1. A method of measuring noble gas isotopes in a sample, comprising the steps of: providing a source of noble gas isotopes;providing a discharge source for providing a beam of metastable atoms;collimating the beam of atoms;selectively actuating a beam chopper for chopping the beam of atoms;providing a beam slower for enhancing beam trapping efficiency; detecting the metastable atoms in magneto-optical trap, thereby detecting the noble gas isotope present in the beam of atoms; andflushing out noble gas isotopes embedded in surrounding system walls by discharging Xe gas in the system between measuring steps for noble gas isotopes.

2. The method as defined in claim 1 wherein the discharge source comprises a liquid N2 cooled RF discharge source, thereby providing a slower beam of atoms for analysis.

3. The method as defined in claim 1 wherein the collimating of the beam of atoms includes a two-dimensional transverse cooling step.

4. The method as defined in claim 1 wherein the beam chopper is activated in an atom capture phase and turned off in an atom beam detection phase.

5. The method as defined in claim 1 wherein the step of detecting utilizes the step of detecting utilizes a two-dimensional mageto-optical trap.

6. The method as defined in claim 1 further including the step of providing a laser with increased power for resonant laser trapping of the noble gas isotope.

7. The method as defined in claim 1 wherein the step of detecting is performed by a CCD camera.

8. The method as defined in claim 1 wherein the noble gas isotope consists of at least one of 81Kr/Kr and 85Kr/Kr.

9. The method as defined in claim 1 wherein the step of detecting includes setting and applying a laser beam to resonance frequencies of the noble gas isotope.

10. (canceled)

11. The method as defined in claim 1 wherein the noble gas resides in ice or water, thereby enabling dating of water and ice.

12. The method as described in claim 1 wherein the step of detecting includes a laser-induced quenching procedure to accurately measure the capture rate of an abundant noble gas isotope.

13. A system for measuring noble gas isotopes in a sample, comprising: a discharge source for providing a beam of atoms containing the noble gas isotopes;a beam chopper for selectively activating and deactivating to use with the beam of atoms;a beam slower;including a Xe gas source and discharge component to provide a Xe gas discharge in the system; anda magneto-optic trap including a laser beam for applying resonant energy to the noble gas isotopes for trapping and analyzing the noble gas isotopes.

14. The system as defined in claim 13 further including a liquid N2 cooled RF discharge source.

15. The system as defined in claim 13 further including a two-dimensional cooling source for cooling the beam of atoms.

16. The system as defined in claim 13 further including a CCD detector.

17. (canceled)

18. The system as defined in claim 13 further including a source of noble gas isotopes selected from Kr, Ne, Ar and Xe.

19. The system as described in claim 18 wherein the noble gas isotopes reside in ice or water thereby enabling time dating of samples thereof.

20. The system as defined in claim 13 further including a quenching laser system.