Active Chemistry Climate, Earth & Environment

NC S&F In-situ 14C Facility

In plain English

AI plain-English summary

A new national laboratory will extract carbon-14 from the crystal lattices of surface rocks and minerals to measure how landscapes have changed over human timescales. This technique, called cosmogenic in-situ 14C dating, tracks carbon-14 formed by cosmic rays hitting minerals at the Earth's surface. It allows researchers to measure rates of change before and after human impacts—something existing methods cannot do at this timescale. Understanding these natural processes has immediate applications across hazards and risk, soil production and erosion, agricultural development, archaeology, coastal change, glacial and fluvial processes, and the tectonic evolution of mountain ranges. The facility will deliver sample preparation for separating quartz, a single automated extraction line for high-throughput removal of carbon dioxide from mineral samples, and preparation of accelerator mass spectrometry targets for high-precision, low-concentration analyses. If successful, this capability will let UK researchers address critical questions about the planet's future that previously could not be tackled—for example, how fast coastlines retreat, how quickly soil forms or erodes, and how tectonic activity shapes mountain ranges over the span of human civilisation.

View original technical description
Cosmogenic in-situ 14C refers to the carbon-14 that is formed by cosmic ray interaction within the crystal lattice of surface materials. In-situ 14C allows researchers to measure processes that have occurred in the era of human civilisations, giving us unprecedented ability to measure rates of change prior to, and since, human impacts. Understanding natural processes at these timescales, and the impacts on them of human activity, has immediate and important applications in diverse NERC science fields such as: hazards and risk, soil production and erosion, agricultural development, archaeology, coastal change, glacial and fluvial processes, and tectonic evolution of mountain ranges. In response to UK community demand we propose to develop a new cutting-edge national laboratory to facilitate in situ 14C dating. Specifically, we will deliver the following scientific capability: Sample preparation for separating quartz for 'in-situ 14C' analyses. A single automated, bespoke extraction line for high-throughput extraction of carbon dioxide from mineral samples. Preparation of accelerator mass spectrometry targets for high-precision, low-concentration analyses. This new capability will allow UK researchers to address critical questions about the future of our planet that previously could not be addressed.

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Researchers

Darren Francis Mark (Principal Investigator)Derek Fabel (Co-Investigator)

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Original classification

Research Grant

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