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Download PDF Article Open access Published: 26 March 2019 Differential Diffusion of Helium Isotopes in Glass, Quantum-tunneling 3He Enrichment, and Portable 3He/4He Monitoring of Mantle

Processes Gary M. McMurtry1, James R. DeLuze  ORCID: orcid.org/0000-0001-9858-63422, David R. Hilton3 na1 & …James E. Blessing4 Show authors Scientific Reports volume 9, Article number: 5213

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While studying the scientific and engineering aspects of a field-portable 3He/4He ratio detector, we found elevated ratios at comparatively lower temperatures that appear to result from

differential diffusion of these isotopes in pure quartz glass. The 3He enrichment relative to 4He in lab air, expressed as the ratio R and normalized to the accepted 3He/4He ratio of 1.40

E-06 (Ra), ranges from peak values of about 200 to 600 in dry static samples. Even at the maximum classical 3He/4He diffusivity ratio of 1.15, the expected R would be only 1.61 E-06. Within

a narrow temperature window, the air value in our experimental set up with pure quartz glass can range from about 2.70 to 8.20 E-04, or nearly 1000 times the expected enrichment based upon

classical fractionation. When plotted versus temperature, the narrow 3He net partial pressure peak reveals at least three sharper embedded peaks that may be quantized vibrational entrance

states in quartz glass which are temperature specific. This discovery has implications for relatively low-energy industrial enrichment of scarce 3He from natural sources on Earth, and for

radiogenic and cosmogenic helium dating assumptions in natural glasses. It also has bearing upon designs for field portable 3He/4He ratio detectors aimed at earthquake and volcanic eruption

studies, and monitoring of nuclear sites.

conductivity of warm dense silica from double-shock experiments Article Open access 05 February 2021 86Kr excess and other noble gases identify a billion-year-old radiogenically-enriched

groundwater system Article Open access 30 June 2022 Introduction

Helium is known to diffuse through glass as a function of temperature, pressure, and purity of the silica glass matrix1,2,3. The fractionation of the 3He isotope of helium in glass relative

to its heavier and far more abundant isotope, 4He, is less well understood. Trull4 studied the fractionation of these isotopes during diffusion in natural glasses and silicate minerals and

found that the enrichment of 3He, expressed as the diffusivity isotope ratio D 3He/D 4He was only 1.08 and not compositionally dependent, whereas classical mechanics predicts as much as 1.15

based upon their mass ratio. Earlier work by Shelby5 found that the diffusivity isotope ratio for this pair in vitreous silica was as high as 1.12 at temperatures approaching 600 °C, and

ascribed the effect to a quantum correction first proposed by LeClaire6. Here we report experimental data that indicates the temperature and time-dependent diffusivity ratio, D 3He/D 4He can

be far greater than 1.15 in pure quartz glass at temperatures below 300 °C. Quantum tunneling (e.g. ref.7) over short distances aided by interstice channels is the most plausible mechanism

to explain these large 3He enrichments at comparatively low temperature.

Experiments were conducted on a compact, elongate vacuum apparatus described in the Methods (Fig. 1). The results presented herein were recorded throughout a typical heating cycle, e.g.,

from ambient lab temperature to a maximum temperature usually reached before one hour of applied power and then cooled to near ambient temperature. The trends of a typical, repeatable static

lab air heat ramp are shown in Fig. 2. Two portions of this ramp are highlighted: one (blue) showing enrichments of 3He, HD and H2 and a second portion (purple) showing continued gains in

HD and H2 partial pressure (PP) as the maximum temperature peaks and begins to slowly decrease at the same or slightly higher power level applied to the heating element, i.e., as the glass

cools. Heating power was turned off at the end of these portions. In contrast to the 3He, HD and H2 trends, 4He rises linearly and peaks shortly after heater power ceases. Expressed as the

3He/4He ratio, upon heating a maximum of 8.20 E-04 is seen at a temperature of 263 °C, the peak ranging from ca. 130° to 370 °C (Fig. 2). Such high ratios exceed those of interplanetary dust

particles or the Moon’s regolith8,9. As we demonstrate below, this enrichment results from differential diffusion of 3He and 4He in heated quartz glass. Some diffusion of these gases may

also occur in the lower-temperature glasses used to fuse the quartz glass to metal, such as Pyrex™ and Kovar™, but these glasses contain metals that block the open Si-O ring structure in

pure silica glass, leading to much lower diffusion rates (c.f. ref.3).

Schematic diagram of an experimental set-up with the “Albert” bench-top prototype of a field-portable 3He/4He instrument. Major components are labeled.

Plots of temperature, measured H2 partial pressure (PP), AIMS-calculated HD PP, AIMS-calculated 3He PP, measured 4He PP, and 3He/4He ratio trends for a static laboratory air heat ramp to

maximum 370 °C from ambient lab temperature. The data were generated by the instrument described in Fig. 1 in communication with a laptop PC that commonly used an MKS RGA program recipe and

the standard MKS VQM software. Temperatures fed into the RGA and the RGA scans were averaged over 57 seconds. The HD and 3He curves are 5-point moving averages. (HD in these plots actually

represents the combined abundance of HD, H3 and any environmental 3H that may be present. See Supplementary Information.) Blue shading represents temperature region where 3He, H2 and HD

rapidly rise; purple shading represents temperature region where H2 and HD continue to rise. In contrast, 4He slowly rises linearly through both these temperature regions and peaks shortly

after power to the heater has stopped. Negative PP values for 3He are likely caused by signal suppression near its limit of detection from the 4He build.

Figure 3 presents temporal trend plots of temperature, 4He partial pressure, and Rc/Ra (rationale for this ratio terminology given in caption) for the case of static flow at six

progressively higher power settings. In all cases, heating power was applied for one hour and data recorded until the sample chamber cooled to about 10 °C above ambient, which ranged from

23° to 25 °C. Net isotope integrals represent the integrated peak response above their respective background levels. Yellow shaded areas represent the integrated, corrected 4He partial

pressure for 200 minutes (arbitrarily set by the V = 110 run). The 3He/4He ratio in blue is the corresponding value for 200-minute integrations. Between applied AC power levels of 28 to 100 

W, 3He net partial pressure builds in the vacuum by diffusion through the glass within the first ca. 20–30 minutes of the heat ramp, as shown by the Rc/Ra trend. High Rc/Ra values are

indicated at 3He peak diffusion temperatures. 4He net partial pressure takes considerably longer to build in the instrument vacuum, increasing with power level and maximum temperature (Fig. 

3). The air ratio is achieved in about 200 minutes at V = 130, but takes over 300 minutes at V = 75. Other power settings show intermediate and longer-period results; at V = 25, very little

3He relative to 4He is diffusing through the glass. At higher power settings, above V = 50, the 4He conductance increases with increased maximum glass temperatures as the run progresses. The

result is that by the end of the run, the 4He partial pressure overcomes the low-temperature 3He conductance advantage due to the much greater abundance of 4He. The increased abundance of

4He then raises the noise floor of the quadrupole to above the 3He signal (see panel V = 130, Fig. 3).

Static air temporal trend plots of thermocouple temperature (TC, °C), corrected 4He partial pressure (PP, units of Torr), and Rc/Ra, where the corrected 3He/4He ratio of the sample (Rc) has

been normalized to the accepted air ratio of 1.40 E-06 (Ra). These corrections account for variable peak response of the mass spectrometer to changes made to the filament ionization level

and the electron multiplier detector setting during the analysis. Sample numbers represent ca. 1-minute averages of the scanning MS response and the TC temperature. Heater power levels are

indicated as voltage settings of the Variac™ autotransformer used. V = 25, 50, 75, 90, 110 and 130 panels correspond to applied AC power levels of 28, 100, 220, 320, 470 and 625 W,

respectively. Yellow areas represent net 4He PP accumulated for 200 minutes; corresponding 3He/4He ratios are denoted in blue ink. In all cases, the 3He/4He values reported were calculated

as ratios of net PP accumulations. Numbers at peak temperatures refer to these calculated ratios.

Except for the two lowest power ramps, heat ramps were run progressively, with ≥1-hour exposure to the ion pump to reduce the prior sample’s vacuum pressure, usually by greater than an order

of magnitude. Subsequent heat ramps with the sample chamber under vacuum and with dry tank N2 as a pressure compensation have shown a reservoir effect for helium isotopes in glass, which

can be cleared after 1–2 hours of heating to >400 °C (e.g. ref.10). This effect may have added 3He and 4He to the progressive heat ramps in Fig. 3, but does not change the overall results

presented.

The 3He enrichment relative to 4He in lab air, expressed as the ratio R and normalized to the accepted 3He/4He ratio of 1.40 E-06 (Ra), ranges from peak values of about 200 to 600 in dry

static samples (Figs. 2 and 3). Even at the maximum classical 3He/4He diffusivity ratio of 1.15, the expected R would be only 1.61 E-06. Within a narrow temperature window, the air value in

our experimental set up with pure quartz glass can range from about 2.70 to 8.20 E-04, or nearly 1000 times the expected enrichment based upon classical fractionation. These enormous

enrichment values, and their unexpected variance with temperature are, however, consistent with a quantum tunneling (QT)-enhanced fractionation of 3He/4He in similar molecular ring-structure

matrices (e.g., refs.11,12,13,14,15). However, as indicated in Fig. 3, integration over the duration of the experimental heat ramp produces 3He/4He ratios that closely approach the accepted

value for air. Additional supporting data to the trends presented in Figs. 2 and 3 are presented in the supplementary information section.

The tunneling diffusion that creates the very high 3He/4He fractionation observed in modified graphene is essentially a surface phenomenon involving a few atomic layers and cooled to very

low temperatures, but occurs up to room temperature11,12,13,14,15. It is similar to the resonant tunneling of electrons over distances of about 100 atomic layers in doped semiconductors that

allow fast switching in tunneling diodes (e.g. ref.16). The exact mechanism of resonant tunneling-assisted diffusion in quartz glass up to 2 mm in thickness, as in this study, is presently

unknown, but the vitreous silica contains migration paths for atoms to pass from interstice to interstice through channels formed by Si-O rings10. Indirect evidence for such structural

interstices housing helium is the need for glass heating to high temperature under pressurized nitrogen gas to effectively clear the glass volume of prior helium loads in our experiments.

The diffusion mechanism may be similar to that proposed for hydrogen atom diffusion through amorphous and polycrystalline ice, where tunneling diffusion may occur for a short distance within

each single crystal or domain, whereas it should be highly suppressed for long-distance diffusion beyond steps and grain boundaries17.

When plotted versus temperature, the narrow 3He net partial pressure peak reveals at least three sharper embedded peaks (Fig. 4), corresponding to mean temperatures of 248 °C, 314 °C, and

348 °C within the six heat ramps shown in Fig. 3. These three sharper peaks are temperature specific and likely responsible for most of the differential diffusion effects observed. Because

glass has high thermal insulation properties, the actual temperatures at which selective 3He transmission phenomena occur are believed to be lower than recorded data. The increased

temperatures observed with higher constant power settings (higher voltages) which result in steeper slopes of temperature rise demonstrate aggravation of this thermal lag effect. These peaks

are interpreted as multiple resonant tunneling temperature states in quartz glass for quantum diffusion of 3He (c.f., refs.16,18). Higher sampling rates should improve the resolution of

these temperature peaks, which we anticipate to be very narrow, and in the range of 140° to 300 °C. 3He shares chemical assignation to 4He but during diffusion through glass it resembles the

better-studied quantum tunneling of hydrogen through solids (e.g. ref.17) rather than the much slower diffusion of 4He.

Plots of corrected 3He PP versus temperature for heat ramp power conditions V = 75, V = 75R-1 (replicate), V = 90, V = 90R-P (replicate, pumped air flow), V = 110 and V = 130. Dates in each

panel refer to the run dates at the constant voltage indicated. At least three 3He peaks are identified within each heat ramp, corresponding to average temperatures of 248 ± 46 °C, 314 ± 59 

°C, and 348 ± 65 °C. Red numbers denote the most intense and consistent peaks. Unfortunately, in these early experiments, the poor sampling rates of both ramp temperature and mass

spectrometer scan averages caused peak resolution uncertainty. What is most relevant to our conclusions is the 3He peaks occur at progressively higher temperatures at higher power settings,

due to shorter dwell times at a given temperature. The resolution can potentially be increased with longer heat ramps and increased sampling rates.

Previous investigations established that the diffusion of helium and its isotopes increases with increasing temperature in both natural and synthetic silicate glasses4,19,20. These

investigations also suggested that there is an increasing fractionation of 3He to 4He with temperature, which is opposite in both sign and magnitude with our experimental findings in pure

quartz glass. Craig and Lupton21 and Rison and Craig22 noted the loss of magmatic helium and large changes in the 3He/4He ratios of natural glasses relative to vesicles in young submarine

basalts (with some alkalic basalts containing thin glass vesicle walls of a mm or less thickness) that they ascribed to low-temperature (ca. 2°–4 °C) exchange with seawater. These changes

may have at least been aided by the extreme fractionation we have found due to QT effects in pure quartz glass. When using the 3He/4He ratios of natural glasses as a dating tool21,23, the

assumption of closed system behavior may have yet another complication to address.

The QT effects we have found in pure quartz glass were an inadvertent discovery made while studying the scientific and engineering aspects of a field-portable 3He/4He ratio detector, on a

pathway toward continuous monitoring of these ratios in both natural gases and fluids that would be useful to the study and prediction of large earthquakes and volcanic eruptions

(e.g.24,25,26,27,28). 3He and 4He-based detectors are also useful for monitoring nuclear storage sites and facilities, both as an intrinsic detector and as a detection medium for neutrons

(e.g. ref.29).

The trapping efficiency for 3He and 4He in these experiments can be estimated from their known concentration in dry air, sample volume, average net 3He and 4He PP (from Fig. 3 heat ramps),

and volume of the instrument’s vacuum. These calculated efficiencies are 0.672 and 0.638%, respectively. The 3He/4He diffusion efficiency ratio in quartz glass is, on average, 6.72 E-03/6.38

E-03 = 1.05 ± 0.40. Both isotopes have essentially the same efficiency despite their disparate relative concentrations in air and temperature dependence. This ratio is similar to the

diffusivity ratio reported for natural glasses by Trull4. It is important to note that the calculations assume that the integration times over the temperature history account for these

differential diffusion effects in quartz glass, and similar integrations may explain why these differential diffusion effects were not previously recognized. Efficiency calculations are

shown below.

Molar 3He concentration in air sample = n = PV/RT = (1 atm) Ra * [4He] * sample volume = (1 atm) 1.40 E-06 (5.22 ppm) (3.28 L) = 1.40 E-06 (5.22 E-06) (3.28 L) = 7.31 E-12 (3.28 L) = 2.40

E-11/[0.08206 (298)] = 9.81 E-13 moles. Molar 3He concentration in inst. vacuum = n = PV/RT = (0.97 ± 0.34 E-12 Torr [Average and standard error of net integrations for four highest power

heat ramps in Fig. 3.]) (1 atm/7.60 E + 02 Torr) (40.5 C.F. [C.F. = conversion factor calculated between the NIST-traceable ART mass spectrometer-390-gauge PP and those recorded by the MKS

Spectra mass spectrometer. Conversion factors were calculated from highly linear regression slopes of PPs for in-common H2 and 4He, and extrapolated for 3He at intermediate mass/charge.])

(3.12 L)/RT = 6.60 E-15 moles. Absolute 3He diffusion efficiency = 6.60 E-15 moles/9.81 E-13 moles = 6.72 E-03 or 0.672%.

For 4He, these calculations are: Molar 4He concentration in air sample = n = PV/RT = (1 atm) [4He] * sample volume = (1 atm) (5.22 ppm) (3.28 L)/[0.08206 (298)] = 5.22 E-06 (3.28 L)/24.45 = 

7.00 E-07 moles. Molar 4He concentration in inst. vacuum = n = PV/RT = (5.91 ± 2.23 E-07 Torr [Average and standard error of net integrations for four highest power heat ramps in Fig. 3.])

(1 atm/7.60 E + 02 Torr)(45 C.F. [C.F. = conversion factor calculated between the NIST-traceable ART mass spectrometer-390-gauge PP and those recorded by the MKS Spectra mass spectrometer.

Conversion factors were calculated from highly linear regression slopes of PPs for in-common H2 and 4He, and extrapolated for 3He at intermediate mass/charge.]) (3.12 L)/RT = (7.78 E-10 atm)

(45 C.F.) (3.12 L)/[0.08206 (298)] = 1.09 E-07/24.45 = 4.46 E-09 moles. Absolute 4He diffusion efficiency = 4.46 E-09 moles/7.00 E-07 moles = 6.38 E-03 or 0.638%.

We conclude that the heat ramps performed with this prototype were not highly efficient at transferring He isotopes from dry air into the instrument’s vacuum. Nevertheless, these experiments

demonstrate an effective measurement of the isotope ratio at air concentrations that is temperature dependent, and suggest that a previously unknown, relatively low-power concentration

method may exist for transferring 3He from the atmosphere, heretofore thought too dilute as a potential resource of this rare isotope. The 3He enrichment window in quartz glass occurs within

ca. 150° to 450 °C, with even narrower peaks within this range that are presently poorly resolved but strongly suggest quantized vibrational entrance temperature states are driving its

diffusion via tunneling. Procedural changes such as greater integration time within the temperature window and higher applied sample pressure, plus design changes such as greater glass

surface area and thinner wall thickness would improve the absolute transfer efficiency (c.f. ref.1). The transparency of the glass transfer medium and the low temperatures required suggest a

passive, solar-heated surface array as a concentration facility, requiring little effort except for occasional sweeps of the vacuum chamber to tantalum getters.

Experiments were made on a compact, elongate vacuum apparatus that featured two vacuums, a high to UHV vacuum chamber and a sample chamber surrounding a glass inlet that could be evacuated

(Fig. 1). We used a cylindrical, “domed” quartz glass adapter assembly sited within a sample chamber where air was introduced via a gas inlet valve and maintained at constant pressure by

pumping or thermally pressurized by valve isolation upon heating. Gases diffuse through the glass and pass into a static UHV Measurement System that contains both mass spectrometers, vacuum

pumps, and total-pressure measurement device. The entire system is constructed with vacuum components consisting of commercial Conflat™-type stainless steel (SS) flanges and housed in

commercial grade 304-stainless steel components with hydrogen partial pressure minimized by Non-Evaporable Getter (NEG) pumping.

We used a high-purity (99.995% SiO2) GE quartz glass cylinder of 2.5-inch (6.35 cm) diameter by 7 inches (17.78 cm) length that was fused with lower-temperature borosilicate glass and Kovar™

to a 4.5 inch (11.43 cm) Conflat™ SS vacuum flange. The glass vacuum fitting was 2 mm in wall thickness. The glass surface area available for the experiment was 532 cm2. Heat was applied

with a Samox®-coated high-temperature heat tape with power controlled by a Variac™ variable autotransformer. Temperature was monitored using an Omega thermocouple (TC) probe placed to within

a few mm of the glass surface via an Agilent data logger with data simultaneously fed into the MKS Microvision-2 quadrupole mass spectrometer (QMS) through a custom TC interface. The

enclosed, vacuum-tight SS sample chamber had a 4-pin electrical feed-through and welded inlet and outlet SS tubing for both pumped and static (no flow) gas options. Lab air relative humidity

ranged from 50 to 60%, and was dried by re-circulated flow through an indicating chemical desiccant trap prior to inlet into the sample chamber.

A SAES Getters NEG pump and a Gamma Vacuum noble diode ion pump maintained high to UHV conditions after bringing the system within range with a turbo-roughing pump station. The vacuum

quality and other gases of interest, specifically H2 and 4He, were monitored with an MKS ART (Auto-Resonant Ion Trap) MS coupled to a NIST-traceable, full-range vacuum gauge (MKS model 390)

running on the same PC computer clock as the QMS. The ART MS computes absolute partial pressures by a ratiometric technique, combining the relative intensity ratios of a chosen peak response

to the total MS response with the total pressure measured simultaneously. The QMS produced factory-calibrated peak response, which we found was offset from the ART by a linearly-calculable

factor used for relating the two MS response values at in-common masses 2 and 4. The MKS Microvision-2 QMS was modified for this application to work at very high frequency in the mass range

1–6 amu, and was thus optimized for sensitivity at relatively high mass resolution.

Scan samples of laboratory air reported herein were continuously collected as near to complete-cycle heat ramps from ambient laboratory temperatures to maximum temperatures determined by the

voltage setting on the Variac. The heating up-ramps were logarithmic curves (R2 ≥ 0.95) that reached 200 °C in 2.8 minutes at V = 130. Reaching this temperature would take over 15.6 hours

at V = 25. After heating for one hour, cooling curves were exponential after line power was cut off (Figs. 2 and 3). Operation of a high-vacuum valve that isolated the ion pump rapidly

cleared He, Ne and Ar which had accumulated in the high vacuum chamber. Hydrogen was continuously pumped by the NEG, along with any reactive species such as H2O and CH4.

The modified MKS quadrupole MS could not resolve contributions to the mass-3 peak from well-known interfering 3He isobars of HD, 3H (tritium) and H3 (triatomic hydrogen). For these

experiments, we assumed the contribution from environmental tritium was negligible and concentrated on resolving the HD plus H3 isobars. HD is 0.01% of environmental hydrogen on Earth but

may suggest a different relative abundance in the vacuum components, as shown in the Supplementary Information section. We used two resolution methods. The first was statistical linear

regression from plots of mass-2 versus mass-3, where the abscissa (x-axis) is the H2 peak response and the ordinate (y-axis) is the combined peak response from 3He and HD. A positive

intercept at zero H2 will be residual 3He, as HD and H2 co-vary with an assumed constant ratio (e.g. ref.30). The second method, called herein Adjusted Ionization Mass Spectrometry (AIMS)

(TIMS of ref.31), works by lowering the ionization potential from the standard 70 eV to less than 30 eV, effectively eliminating any 3He, as helium is not responsive beneath this ionization

threshold. The lower ionization mass-3 response is therefore residual HD and H3 (plus any tritium), to be subtracted from the higher ionization peak with combined 3He, HD, H3, and 3H

response. A co-variance with R2 = 0.79 (n = 44) was found for these two methods as “blind temperature ramps”, where QMS scan measurements were recorded immediately upon cool-down following

1-hour heat ramp completions. Comparison of lab air 3He/4He ratios determined by these two methods were within a factor of 2 of the accepted air ratio of 1.40 E-06 at ramp maximum

temperatures above 300 °C (refs27,28,32; see Supplementary Information).

The datasets generated during and/or analyzed during the current study are available from the corresponding author on reasonable request.

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We thank James Jolly, Mario Williamson, James Babinec and Luis Dasilveira for their helpful assistance with the prototype. We have benefited from advice and encouragement given by Dr.

Gerardo A. Brucker of MKS Instruments, Inc., Granville-Phillips Division. We also thank the two anonymous expert reviewers for comments that improved the manuscript. The MKS Spectra

high-resolution quadrupole mass spectrometer was kindly made available to us by MKS Instruments, Inc. Partial support was provided by a seed grant to G. M. McMurtry and D. R. Hilton from the

DECADE program of the Deep Carbon Observatory, Reservoirs and Fluxes, Carnegie Institute for Research, sponsored by the Alfred P. Sloan Foundation. Additional support was provided by a

grant from the US Geological Survey Innovation Center and from the Volcano Science Center. We thank Shaul Hurwitz, Sara Peek, Debra Bergfeld and Andrew Hunt of the USGS for their field and

lab assistance at Mammoth and Kilauea. This is SOEST Contribution no. 10668.

David R. Hilton is deceased.

Authors and Affiliations Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii, Manoa, Honolulu, HI, 96822, USA

Gary M. McMurtry

Fusion Energy Solutions of Hawaii, 611 University Avenue, Apt. 301, Honolulu, HI, 96826, USA

James R. DeLuze

Scripps Institution of Oceanography, University of California, San Diego, 9500 Gilman Drive, La Jolla, CA, 92093-0244, USA

David R. Hilton

MKS Instruments, Inc., Mass Spectrometry Solutions, 3635 Peterson Way, Santa Clara, CA, 95054, USA

James E. Blessing

AuthorsGary M. McMurtryView author publications You can also search for this author inPubMed Google Scholar

James R. DeLuzeView author publications You can also search for this author inPubMed Google Scholar

David R. HiltonView author publications You can also search for this author inPubMed Google Scholar

James E. BlessingView author publications You can also search for this author inPubMed Google Scholar

G.M. McMurtry designed the study and prepared the original manuscript. J.R. DeLuze assisted in the experiments, instrument design and corrected the text. D.R. Hilton provided technical

oversight and corrected the text. J.E. Blessing provided the M.K.S. quadrupole M.S. and run software. All authors discussed the results and commented on the manuscript.

Corresponding author Correspondence to Gary M. McMurtry.

Two of the co-authors, G. M. McMurtry and J. R. DeLuze, have a US utility patent issued as US 10,005,033 B2, “Isotopic enrichment of helium-3 through glass” on June 26, 2018. Co-author J. E.

Blessing represents the Mass Spectrometry Solutions section of MKS Instruments, Inc., which may have a financial interest in the outcomes of this work.

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About this articleCite this article McMurtry, G.M., DeLuze, J.R., Hilton, D.R. et al. Differential Diffusion of Helium Isotopes in Glass, Quantum-tunneling 3He Enrichment, and Portable

3He/4He Monitoring of Mantle Processes. Sci Rep 9, 5213 (2019). https://doi.org/10.1038/s41598-019-41360-5

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Received: 05 November 2018

Accepted: 04 March 2019

Published: 26 March 2019

DOI: https://doi.org/10.1038/s41598-019-41360-5

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