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.


Clarifying the role of acid and base dopants in the hydrogen-ordering phase transitions of ice

Abstract: Using ISIS facilities, our team has discovered three new phases of ice: ices XIII, XIV and XV. These phases form in the presence of small amounts of hydrochloric acid. Yet, the role the acid dopant plays is still very poorly understood. In particular since the preparation of ice XI from the ‘ordinary’ ice I requires base doping and acid doping is ineffective. Now, we have found using calorimetry and X-ray diffraction that ice XIII can also be prepared with lithium hydroxide doping. Since this is the first case where acid and base doping are effective, we now have the perfect system for finally clarifying the role of the dopants. In addition to complementary DFT calculations, the experimental key question is now if acid and base dopants facilitate the same structural pathways leading towards the same ice XIII end-state. This question can only be answered with neutron diffraction.

Principal Investigator: Professor Christoph Salzmann
Experimenter: Dr Alexander Rosu-Finsen
Local Contact: Dr Ronald Smith

DOI: 10.5286/ISIS.E.RB1800100

ISIS Experiment Number: RB1800100

Part DOI Instrument Public release date Download Link
10.5286/ISIS.E.92921913 POLARIS 11 May 2021 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 Christoph Salzmann et al; (2018): Clarifying the role of acid and base dopants in the hydrogen-ordering phase transitions of ice, STFC ISIS Neutron and Muon Source, https://doi.org/10.5286/ISIS.E.RB1800100

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



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