ISIS Neutron and Muon Source Data Journal

This is a page describing data taken during an experiment at the ISIS Neutron and Muon Source. Information about the ISIS Neutron and Muon Source can be found at https://www.isis.stfc.ac.uk.


The dynamics of water in halloysite

Abstract: Water is ubiquitous on Earth, where its presence has shaped the planet and led to life. Halloysite is a clay mineral that is formed by water, holds water in its structure and can subsequently lose water. Therefore, where we find halloysite in nature, we can also find a story of how water was taken up and expelled by the planet. This knowledge can feed into the global water cycle and be useful in agriculture; halloysite is found in soils where the uptake of water can be vital for the nutrition of plants. This experiment aims to reveal how water molecules moves through halloysite by subjecting it to a beam of neutrons. Halloysite is made up of a one-molecule thick water layer, squeezed in between two layers of clay. This is a novel opportunity to study a two-dimensional water layer and will give atomic-level insight, on a water-mineral relationship that is consequential in nature.

Principal Investigator: Professor Neal Skipper
Experimenter: Dr Andrew Seel
Experimenter: Miss Nia Gray
Experimenter: Professor Stephen Hillier
Local Contact: Dr Sanghamitra Mukhopadhyay
Experimenter: Mr Aasim Shaffi

DOI: 10.5286/ISIS.E.RB2000234

ISIS Experiment Number: RB2000234

Part DOI Instrument Public release date Download Link
10.5286/ISIS.E.RB2000234-1 OSIRIS 10 June 2024 Download

Publisher: STFC ISIS Neutron and Muon Source

Data format: RAW/Nexus
Select the data format above to find out more about it.

Data Citation

The recommended format for citing this dataset in a research publication is as:
[author], [date], [title], [publisher], [doi]

For Example:
Professor Neal Skipper et al; (2021): The dynamics of water in halloysite, STFC ISIS Neutron and Muon Source, https://doi.org/10.5286/ISIS.E.RB2000234

Data is released under the CC-BY-4.0 license.



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