.VMS

SiO2 clean time series.vms (2.99 kB)

.XLSX

TGA QMS of sythetic MnO.xlsx (244.7 kB)

.XLSX

TGA QMS of nod (marine) MnO.xlsx (80.1 kB)

.XLSX

TGA QMS of HH (terrestrial) MnO 3 october 2020.xlsx (313.78 kB)

.VMS

15-088_HHMnO solid pellets_UVO and Na hypochlorite decon_01July2015.vms (187.34 kB)

.VMS

AW_Mn_Mid_300atom_8KeV_GCIB.avg.vms (372.66 kB)

.VMS

AW_Mn_Top_300atom_8KeV_GCIB.avg.vms (370.25 kB)

.VMS

AW_Mn_Bottom_300atom_8KeV_GCIB.avg.vms (370.62 kB)

.VMS

Benthic Mn Nodule_mid section_300atom_8kev_gcib.avg.vms (372.66 kB)

.VMS

HHMnOx_AR_550_1000.vms (685.99 kB)

.VMS

synthetic MnO_500_1000_13dec2016.vms (409.36 kB)

.VMS

synthetic mno_500_1000_13dec2016.vms (421.69 kB)

.VMS

synthetic bernessite_ AR.vms (240.77 kB)

.VMS

synthetic bernessite_16-176_19sept2016.vms (229.03 kB)

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14 files

Stable organic carbon formation accelerated by manganese oxide mineral reduction and the implications for the global carbon cycle

dataset

posted on 2022-09-20, 13:28 authored by Graham PurvisGraham Purvis, Elisa Lopez-CapelElisa Lopez-Capel, Jake Sheriff, Karen Johnston, Caroline PeacockCaroline Peacock, Peter Cumpson, Naoko Sano

All Raw XPS spectra in *.VMS file format for the above manuscript

Samples are synthetic, marine (AKA nodule) and terrestrial (AKA HH)

For samples as received, heated to 500 deg. C +/- 50 deg. C and 950 deg. c +/- 100

Digitised raw TG-DSC QMS data *.xls format

Samples are synthetic marine and terrestrial.

Funding

X-ray photoelectron spectra were obtained at the National EPSRC XPS Users’ Service (NEXUS) at Newcastle University, an EPSRC Mid-Range Facility NS/A000015/1.

This research project has also been funded by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (Grant agreement No. 725613 MinOrg).

C.L.P. gratefully acknowledges Royal Society Wolfson Research Merit Award (WRM/FT/170005).

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TGA DSC QMS XPS Stable Carbon Spectra carbon cycle model Manganese Oxide Bernessite

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Stable organic carbon formation accelerated by manganese oxide mineral reduction and the implications for the global carbon cycle

Funding

X-ray photoelectron spectra were obtained at the National EPSRC XPS Users’ Service (NEXUS) at Newcastle University, an EPSRC Mid-Range Facility NS/A000015/1.

This research project has also been funded by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (Grant agreement No. 725613 MinOrg).

C.L.P. gratefully acknowledges Royal Society Wolfson Research Merit Award (WRM/FT/170005).

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