Terrestrial Cosmogenic Nuclide Facility
The Cosmogenic Isotope Lab is one of three facilities in Canada that are currently producing cosmogenic nuclide targets, and one of only four facilities in the world to prepare targets for all four cosmogenic radionuclides (10BE, 14C, 26AL, 36CL) used for Earth Surface Processes research. We do not do radiocarbon dating of organic materials such as bone, plants, artifacts, or art work. In the future we hope to prepare targets for protein-specific 14C analysis.
The Terrestrial Cosmogenic Nuclide Facility is made up of four chemistry labs and a computer lab:
- 10Be and 26Al sample prep wet and dry labs
- 36Cl wet lab
- 14C gas extraction lab
- ICP-OES lab
- Computer Lab
Cosmogenic nuclides are used to determine exposure ages and erosion rates of landforms and sediments, and exhumation rates of catchment basins. Production rates of these radioisotopes in minerals exposed to cosmic rays are very low (i.e. tens of atoms per gram of mineral per year ), so the measurement of the radionuclides require accelerator mass spectrometry (AMS).
We use AMS facilities at
- ETH Zurich (14C)
- Lawrence Livermore National Laboratory (10BE and 26AL)
- Purdue University PRIME Lab (36CL and 10BE)
- A.E.Lalonde AMS Laboratory at uOttawa
Preparation of accelerator mass spectrometry targets takes a minimum of one week of mineral purification and an additional week to 10 days for target chemistry. In the case of 10Be, 26Al, or 36Cl the chemistry involves ion chromotography and controlled precipitations. For the 14C extraction from quartz we use a tube furnace and flux to melt the quartz and our custom built ultrahigh vacuum stainless steel extraction line to purify the 14CO2 gas.
The wait times for accelerator mass spectrometry can be long (months), during which time the required elemental analyses are also completed, either by our in-house ICP-OES or by other instruments off campus. The time for data reduction and initial interpretation ranges from a few hours to a week. Projects that involve computation with available calculators or the development of new models or theory will take longer. We normally have samples in the quene for all isotopes.
For 10Be and 26Al we average about 6 months before starting new samples. For
36Cl we average about 4 months delay. For 14C we are still in development mode, so it is not possible to estimate the quene time.
Contact John Gosse for quene times, costs, and other submission questions. While our policy is first come first serve, we try to accomodate students with thesis deadlines.
Each year we train visiting students and research scientists in the sample preparation and interpretation of cosmogenic nuclide data. The benefits include development of isotope geochemistry laboratory skills, appreciation of experimental uncertainty, and the participation in preparing one's own samples. For safety and QA/QC resons it is not possible to allow untrained visitors to prepare their own targets in the first couple of batches. However, visitors who stay for months or return after being trained through a couple of batches can operate independently with limited supervision, depending on lab availability and scheduling.
The TCN facility group is interested in a range of (in some instances previously intractable) scientific problems in geomorphology and landscape evolution. These problems include stream incision and sediment flux, fault kinematics and seismic slip history, tectonic geomorphology, glacial geochronology, permafrost processes and ice dating, landslide and rock avalanche research, chronology for archeology and paleontology. We collaborate with researchers at universities and insititutions worldwide, and conduct service work for geological surveys (e.g. GSC Atlantic, GSC Ottawa, USGS, Norway).
TCN Facility and Field Areas (mostly collaborative)
In the past 7 years
- Alluvial fan chronostratigraphy in the Mojave Desert, Nevada, and Eastern California Shear Zone, Baja California for seismic, tectonic, and paleoclimate research.
- Age of landslides and faulted surfaces in the Andes, Himalayas, and Norway.
- Fault kinematics, crustal shortening, strain partitioning, or tectonic geomorphology in Chili, Argentina, Nepal, Tibet, Eastern California, Mexico, and Mongolia.
- Pliocene sedimentation, geochronology, and erosion in the Arctic, especially related to the Beaufort Formation.
- Glacial geology and geochronology in Baffin Island, Newfoundland and Labrador, Nova Scotia, Yukon, Andes, Mongolia, Ural Mountains.
- Chronology for Archeology and Paleontology in Mongolia and the Canadian Arctic.
- Fluvial incision history in the Grand Canyon, Southern Central Andes, and Mongolia
- Sediment flux measuements from rivers along the Texas gulf, Klondike region of the Yukon, western Canadian Arctic.