Hostname: page-component-74656f9884-8r8nv Total loading time: 0 Render date: 2026-11-09T23:53:02.470Z Has data issue: false hasContentIssue false
  • English
  • Français

An in Situ Gas-Extraction System to Radiocarbon Date Glacier Ice

Published online by Cambridge University Press:  30 January 2017

H. Oeschger ,
B. Alder  and
C. C. Langway Jr.
H. Oeschger
Affiliation:
University of Bern, Bern, Switzerland
B. Alder
Affiliation:
University of Bern, Bern, Switzerland
C. C. Langway Jr.
Affiliation:
U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, New Hampshire, U.S.A.
Rights & Permissions [Opens in a new window]

Abstract

A new down bore-hole instrument to extract atmospheric gases entrapped in glacier ice was designed, developed and tested in a Greenland ice tunnel. Using this ice and a 7.5 kW. source, about 30 hr. are required to melt the approximately 1 metric ton sample, extract the gases, and to separate and collect with molecular sieves the minimum of 100 cm.3 of CO2 necessary for the 14C measurements made later using special low-level counters. Age results using the down bore-hole CO2 samples agree with results obtained earlier from CO2 samples collected at the same tunnel location using a vacuum-vessel melting technique. A mean value of 5,120±200 yr. b.p. is obtained for the seven samples measured using both collection systems, making this the oldest natural polar glacier ice measured to date.

Un nouvel instrument a été mis au point dans un trou de forage, il permet l’extraction des gaz atmosphériques occlus dans la glace. Il a été testé dans un tunnel de glace au Groenland. Dans cette glace, avec une source d’énergie de 7,5 kW, il faut en gros 30 heures pour fondre environ une tonne de glace, en extraire les gaz, et séparer et recueillir avec des tamis moléculaires le minimum de 100 cm3 de CO2 nécessaire pour les mesures au 14C faites en laboratoire à l’aide de compteurs spéciaux à bas-niveau. L’âge des échantillons de CO2 extrait dans les trous de forage est en accord avec celui d’échantillons de CO2 collectés auparavant dans le ramie tunnel et aux mémes emplacements à l’aide de fonte dans une enceinte sous vide. Une valeur moyenne de 5120±200 années a été obtenue pour sept échantillons mesurés avec les deux techniques d’extraction, ce qui constitue actuellement la plus vieille glace polaire naturelle datée.

Zusammenfassung

Zusammenfassung

Für die Entnahme atmosphärischer Gase aus Gletschereis wurde ein nues Bohrloch-Gerät entwickelt und in einem grönländischen Eistunnel erprobt. Bei diesem Eis und mit einer Energiequelle von 7,5 kW dauert es etwa 30 Stunden, bis die Eisprobe von ca. 1 ton Gewicht geschmolzen, die Gase entzogen und mit Molekular-Filtern die 100 cm3 von CO2 getrennt und gesammelt sine’. die mindestens für die späteren 14C-Untersuchungen mit besonderen, niederstufigen Zählern gebraucht werden. Die Altersbestimmungen aus den CO2-Proben des Bohrloches stimmen mit den früheren Ergebnissen aus CO2-Proben überein, die an derselben Tunnelstelle unter Anwendung einer Vakuum-Schmelztechnik gewonnen wurden. Es wurde ein mittleres Alter von 5120±200 Jahren für die 7 untersuchten Proben aus bieden Entnahmesysternen gefunden; dies ist die bisher höchste Altersbestimmung für natürliches Gletschereis aus Polargebieten.

Information

Type
Instruments and Methods
Information
Journal of Glaciology , Volume 6 , Issue 48 , 1967 , pp. 939 - 942
Copyright
Copyright © International Glaciological Society 1967

Introduction

Atmospheric gases become entrapped in polar glacier ice during a natural compaction process. In the first reported attempt to separate the CO2 component of this atmospheric gas from iceberg samples for radiocarbon dating analysis (Reference ScholanderScholander and others, 1962), a vacuum-melting system was used, and 10 to 20 metric tons of ice were required. In 1964, CRREL and the University of Bern conducted a joint project in the TUTO ice tunnel, Greenland (Langway and others, 1965; Reference OeschgerOeschger and others, 1966), where refinements in sample collection, vacuum-melt processing and laboratory low-level measuring techniques (Reference OeschgerOeschger, 1963) allowed smaller samples (1 metric ton) of “cold” glacier ice to be used for radiocarbon-dating purposes. Although the techniques used in this later study considerably reduced the amount of ice sample necessary for age-dating purposes, certain glaciological applications of the radiocarbon method were not possible using a vacuum-melt vessel technique. In the first place, the field logistics required with the vacuum-melt vessel technique are prohibitive at most marginal and inland glacier locations. Furthermore, a valuable application of the radiocarbon-dating method would be to analyze the deep ice cores being recovered in Greenland and Antarctica by CRREL’s deep ice-core drilling program, but this is also not feasible using the vessel technique. Even the reduced requirements of a 1 metric ton ice sample represents, for a 10 cm. diameter ice core, a 140 m. vertical profile, or depending on location, 500 to 2,000 years of accumulation. These considerations made it desirable to develop a system that would allow gas extractions to be made from within a shallow or deep bore hole at any glacier location.

Field Program

In March–April 1966 a team from CRREL and the University of Bern returned to the TUTO ice tunnel in Greenland to test the new down bore-hole device and to take samples from a complete profile along the 400 m. length of the tunnel. The tunnel ice is unfractured and its temperature is constant at −10°C. The earlier 200 m. location where in 1964 14C age dates had been obtained was used as a check point for the down bore-hole tests.

Field Experiments

Figure 1 shows a diagram of the apparatus which consists of two main parts: (1) the seal and (2) the heater. A 4 m. deep bore hole is hand angered and the down bore-hole device inserted. Critical to the success of the down bore-hole concept was the necessity of a vacuum-tight seal of the hole above the heater. The seal used consists of a double-walled latex tube which surrounds a cylindrical brass core. The latex tube is joined to the core at both ends and when in place it is inflated with nitrogen to an over pressure of about 2 atmospheres which presses the rubber seal against the wall of the ice bore hole. The gas extraction line and the power line for the heater pass through the brass core. An energy source of 7.5 kW. is used for the heater. The heating element is wound around a stainless steel cylindrical pipe for mechanical stability and heat reflection, and it was designed not to overheat in air. The bore hole is pumped down to about 2 mm. Hg (the vapor pressure of ice at −10°C.) and held for several hours before the heaters are turned on. Constant pumping is made during heating to extract the gases as the bubbles burst. Continuous checks were made on gas-extraction flow rates, no irregularities indicating leaks were observed. About 30 hr. were required to melt slightly over 1 metric ton of ice to collect the necessary minimum of 100 cm.3 of CO2. During this time the gases passed through a molecular-sieve gas-extraction line. From experience gained in 1964, it was found that the NaOH and molecular sieve CO2 collectors provided compatible results, but since molecular sieves are simpler to handle and process they were adopted for the 1966 investigations.

Fig. 1.

Schematic diagram of a portable down bore-hole gas-extraction system

Laboratory Results

The CO2 contained in the molecular sieves was processed in the Radiocarbon Laboratory at the University of Bern and measured for 14C, using special low-level counters.

The results of the 1964 vacuum-vessel samples and the new 1966 vacuum vessel and the down bore-hole samples are given in Table I.

Table I.

14C Measurements of Ice Samples From the 200 m. Station, TUTO Ice Tunnel, Greenland

Discussion and Conclusions

From Table I we see a close agreement in the ages within the limits of statistical error, determined for both the 1964 and 1966 small and large vacuum-melt vessel samples. Most important, the down bore-hole samples (DH1 and DH2) give essentially the same data. This good agreement is an indication of the validity of all methods used. A mean value of 5,120 yr. b.p. is obtained for the age of the ice at the 200 m. location. To date, this is the oldest natural polar glacier ice ever measured.

The simplicity of the down bore-hole gas-extraction system enables one to apply the carbon-dating method to any natural, undisturbed polar or temperate glacier ice mass which can be sampled by boring. By using helicopters, portable laboratories and shallow, hand core-augering equipment, it is possible to age date the termini of many temperate glaciers or the marginal zones of polar ice sheets for chronological and ice-movement studies. The fascinating problem of 14C dating the entire vertical profile of a contemporary polar ice sheet is now possible (a feasibility study is currently in progress) by attaching a down bore-hole system to the hoist-cable mechanism of the CRREL drilling rig now being used to penetrate through polar ice sheets (Reference Hansen and LangwayHansen and Langway, 1966).

Acknowledgements

We should like to extend our appreciation to the entire U.S. Army Research Support Group at Camp TUTO, Greenland, particularly to CWO G. Simpson, for the unfailing field support which materially contributed to the successful completion of the field project. H. Steuri was instrumental in the development of the down bore-hole device and to the success of the field-collection program. D. Donovan assisted in the field program. H Loosli and T. Riesen conducted many of the laboratory tests and the 14C measurements. Discussions with H. Zellhofer were valuable to the perfection of the seal mechanism.

The United States National Science Foundation and the Swiss National Science Foundation provided financial support for parts of this work.

References

Hansen, B. L. Langway, C. C. jr. 1966. Deep core drilling in ice and core analysis at Camp Century, Greenland, 1961–1966. Antarctic Journal of the U.S., Vol. 1, No. 5, p. 207–08.Google Scholar
Langway, C. C. jr., and others. Sampling Polar ice for radiocarbon dating, [by] C. C. Langway, Jr., H. Oeschger, B. Alder, A. Renaud. Nature, Vol. 206, No. 4983, p. 500–01.CrossRefGoogle Scholar
Oeschger, H. 1963. Low-level counting methods. (In Radioactive dating. Proceedings of the symposium on radioactive dating held by the International Atomic Energy Agency in co-operation with the Joint Commission on Applied Radioactivity (ICSU) in Athens, 19–23 November 1962. Vienna, International Atomic Energy Agency, p. 13–33.)Google Scholar
Oeschger, H., and others. 1966. Radiocarbon dating of ice, by H. Oeschger, B. Alder, H. Loosli, C. C. Langway, Jr., A. Renaud. Earth and Planetary Science Letters, Vol. 1, No. 2, p. 49–54.CrossRefGoogle Scholar
Scholander, P. F., and others. 1962. Radio-carbon age and oxygen-18 content of Greenland icebergs, by P. F. Scholander, W. Dansgaard, D. C. Nutt, H. deVries, L. K. Coachman, E. Hemmingsen. Meddelelser om Grenland, Bd. 165, Nr. 1.Google Scholar
Figure 0

Fig. 1. Schematic diagram of a portable down bore-hole gas-extraction system

Figure 1

Table I. 14C Measurements of Ice Samples From the 200 m. Station, TUTO Ice Tunnel, Greenland