Acknowledgements L.J.C., N.K., I.S. and T.R. are funded by BBSRC SARISA BB/L025620/1. K.R.D. is funded by ERC 646809DIMR. L.K.B., P.D.H., T.S.G., M.N. and A.R. are funded by BBSRC BB/J00868/1 and A.G.B. is funded by BB/L025825/1. The James Hutton Institute receives financial support from the Rural & Environment Science & Analytical Services Division of the Scottish Government. I.S. and T.R. are also funded by EPSRC EP/M020355/1. T.R. is also funded by ERC 646809DIMR, BBSRC SARIC BB/P004180/1 and NERC NE/L00237/1. The authors acknowledge the use of the I13 beamline at Diamond Light Source, Oxfordshire, UK (session ID: MT9659). We would like to thank beamline scientist Dr Mirian Garcia Fernandez, who provided considerable help during our beamtime. Additionally, Diamond Light Source funded travel for three people. The authors acknowledge the use of the IRIDIS High Performance Computing Facility, and associated support services at the University of Southampton, in the completion of this work. All data supporting this study are available on request from the University of Southampton repository at https://doi.org/10.5258/soton/d0116.
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