cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.5165878.v3
title: Uncatalyzed addition of azides to iodoalkynes

description: Inputs, outputs and orbitals for the species present in the uncatalyzed addition of azides to iodoalkynes, discussed in:<br><br><br><b>Pedro J. Silva</b> and Carlos E. P. Bernardo (2018), Influence of Alkyne and Azide Substituents on the Choice of the Reaction Mechanism of the Cu<sup>+</sup>-Catalyzed Addition of Azides to Iodoalkynes <i>J. Phys. Chem. A,</i> 122, 7497-7507 <br><br>A few catalyzed reactions are also present in this dataset, due to technical difficulties in uploading them to https://doi.org/10.6084/m9.figshare.5035682<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br>A CH3-CC-I and HN3<br>B CH3-CC-I and CH3-N3<br>C CH3-CC-I and PhN3<br>D CH3-CC-I and p-MePhN3<br>E CF3-CC-I and HN3<br>F CH3CH2-CC-I and HN3<br>G Ph-CC-I and HN3<br>H CF3-CC-I and CH3-N3<br>I CH3CH2-CC-I and CH3-N3<br>J Ph-CC-I and CH3-N3<br>K CF3-CC-I and PhN3<br>L CH3CH2-CC-I and PhN3<br>M Ph-CC-I and PhN3<br>N CF3-CC-I and p-MePhN3<br>O CH3CH2-CC-I and p-MePhN3<br>P Ph-CC-I and p-MePhN3<br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.6084/m9.figshare.5165878.v2
title: Uncatalyzed addition of azides to iodoalkynes

description: Inputs, outputs and orbitals for the species present in the uncatalyzed addition of azides to iodoalkynes, discussed in:<br><br>Silva and Bernardo (2017) The reaction mechanism of the Cu+-catalyzed addition of azides to iodoalkynes. (in preparation)<br><br>A few catalyzed reactions are also present in this dataset, due to technical difficulties in uploading them to https://doi.org/10.6084/m9.figshare.5035682<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br>A CH3-CC-I and HN3<br>B CH3-CC-I and CH3-N3<br>C CH3-CC-I and PhN3<br>D CH3-CC-I and p-MePhN3<br>E CF3-CC-I and HN3<br>F CH3CH2-CC-I and HN3<br>G Ph-CC-I and HN3<br>H CF3-CC-I and CH3-N3<br>I CH3CH2-CC-I and CH3-N3<br>J Ph-CC-I and CH3-N3<br>K CF3-CC-I and PhN3<br>L CH3CH2-CC-I and PhN3<br>M Ph-CC-I and PhN3<br>N CF3-CC-I and p-MePhN3<br>O CH3CH2-CC-I and p-MePhN3<br>P Ph-CC-I and p-MePhN3
DOI: 10.6084/m9.figshare.5418688
title: Cu+-catalyzed addition of electron-deficient azides to iodoalkynes

description: Inputs, outputs and orbitals for the species present in the Cu+-catalyzed addition of electron-deficient azides to iodoalkynes, discussed in:<br><br><b>Pedro J. Silva</b> and Carlos E. P. Bernardo (2018), Influence of Alkyne and Azide Substituents on the Choice of the Reaction Mechanism of the Cu<sup>+</sup>-Catalyzed Addition of Azides to Iodoalkynes <i>J. Phys. Chem. A,</i> 122, 7497-7507 <br><br>Other data reported in the same paper have been uploaded to<br>https://doi.org/10.6084/m9.figshare.5035682<br>https://doi.org/10.6084/m9.figshare.5165878<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br><br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.6084/m9.figshare.5418688.v4
title: Cu+-catalyzed addition of electron-deficient azides to iodoalkynes

description: Inputs, outputs and orbitals for the species present in the Cu+-catalyzed addition of electron-deficient azides to iodoalkynes, discussed in:<br><br><b>Pedro J. Silva</b> and Carlos E. P. Bernardo (2018), Influence of Alkyne and Azide Substituents on the Choice of the Reaction Mechanism of the Cu<sup>+</sup>-Catalyzed Addition of Azides to Iodoalkynes <i>J. Phys. Chem. A,</i> 122, 7497-7507 <br><br>Other data reported in the same paper have been uploaded to<br>https://doi.org/10.6084/m9.figshare.5035682<br>https://doi.org/10.6084/m9.figshare.5165878<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br><br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.6084/m9.figshare.5418688.v3
title: Cu+-catalyzed addition of electron-deficient azides to iodoalkynes

description: Inputs, outputs and orbitals for the species present in the Cu+-catalyzed addition of electron-deficient azides to iodoalkynes, discussed in:<br><br>Silva and Bernardo (2017) The reaction mechanism of the Cu+-catalyzed addition of azides to iodoalkynes. (in preparation)<br>Other data reproted in the same paper have been uploaded to<br>https://doi.org/10.6084/m9.figshare.5035682<br>https://doi.org/10.6084/m9.figshare.5165878<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br><br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.6084/m9.figshare.7599125
title: Late Permian-Triassic granitic rocks of Vietnam: the Muong Lat example

description: The Song Ma zone in Northwestern Vietnam is considered as a suture of the South China and Indochina blocks, and plays an important role in understanding the tectonic evolution in Southeast Asia and surrounding areas. Granitic rocks of the Muong Lat complex are distributed in the Song Ma suture, consisting mainly of monzogranite and granodiorite. The rocks are sub-alkaline in affinity with high K contents and characteristics of S-type granite. They have high SiO<sub>2</sub>, total Na<sub>2</sub>O + K<sub>2</sub>O, and Zr contents and high aluminium saturation index values (0.97 to 1.29 with an average of 1.14). All these geochemical signatures, together with high (<sup>87</sup>Sr/<sup>86</sup>Sr)<sub>i</sub> ratios (0.71391 to 0.74568), and low whole rock ε<sub>Nd</sub>(t) and zircon ε<sub>Hf</sub>(t) values (−13.1 to −9.4) suggested an origin from partial melting of crustal source rocks. Primitive mantle normalized trace element contents exhibit positive anomalies of Rb, Th, U and Pb, but negative anomalies of Nb, Ta, and Ti, indicating a collision-related environment. The depleted Nd and Hf zircon model ages from investigated samples, in combination with inherited zircon ages, suggest the existence of Precambrian basement in the study region. S-type granites of the late Permian-early Triassic (the Muong Lat, Phia Bioc and Hai Van complexes) in Vietnam were formed by the subduction-collision of the South China and Indochina blocks.
DOI: 10.6084/m9.figshare.7552940
title: Late Jurassic–Early Cretaceous tectonic evolution of the Great Xing’an Range: geochronological and geochemical evidence from granitoids and volcanic rocks in the Erguna Block, NE China

description: The late Mesozoic magmatic record within the Erguna Block is critical to evaluate the tectonic history and geodynamic evolution of the Great Xing’an Range, NE China. Here, we provide geochronological and geochemical data on Late Jurassic–Early Cretaceous plutonic-volcanic rocks in the northern Erguna Block and discuss their origin within a regional tectonic framework. Late Mesozoic magmatism in the Erguna Block can be divided into two major periods: Late Jurassic (162–150 Ma) and Early Cretaceous (140–125 Ma). Late Jurassic quartz monzonite and dacite show adakite characteristics such as high Al<sub>2</sub>O<sub>3</sub>, high Sr, and steeply fractionated REE patterns. Contemporary granitoids and rhyolites are also characterized by strong enrichment of light rare earth elements (LREE) and significant depletion in heavy rare earth elements (HREE), but with more pronounced negative Eu anomalies. Early Cretaceous trachytes and monzoporphyries exhibit moderate LREE enrichment and relatively flat HREE distributions. Coeval granites and rhyolites have transitional signatures between A-type and fractionated I-type felsic rocks. Both Late Jurassic and Early Cretaceous rocks have distinctive negative Nb, Ta, and Ti anomalies, and positive zircon ε<sub>Hf</sub>(t) values, suggesting that these magmas were derived from partial melting of Meso-Neoproterozoic accreted lower crust, although melting occurred at a variety of crustal levels. The transition from adakite to non-adakite magmatism reflects continued crustal thinning from Late Jurassic to Early Cretaceous. Our data, together with recently reported isotopic data for plutonic and volcanic rocks, as well as geochemical data, in NE China, suggest that Late Jurassic–Early Cretaceous magmatism in the Erguna Block was possibly induced by post-collisional extension after closure of the Mongol-Okhotsk Ocean.
DOI: 10.6084/m9.figshare.5459674.v1
title: Azide binding to Cu+-iodoalkynes

description: Inputs, outputs and orbitals for the species present in the Cu+-catalyzed addition of electron-deficient azides to iodoalkynes, discussed in:<br><b>Pedro J. Silva</b> and Carlos E. P. Bernardo (2018), Influence of Alkyne and Azide Substituents on the Choice of the Reaction Mechanism of the Cu<sup>+</sup>-Catalyzed Addition of Azides to Iodoalkynes <i>J. Phys. Chem. A,</i> 122, 7497-7507 <br><br><br><br>Other data reported in the same paper have been uploaded to<br>https://doi.org/10.6084/m9.figshare.5035682<br>https://doi.org/10.6084/m9.figshare.5165878https://doi.org/10.6084/m9.figshare.5418688<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br><br>A CH3-CC-I and HN3<br>B CH3-CC-I and CH3-N3<br>C CH3-CC-I and PhN3<br>D CH3-CC-I and p-MePhN3<br>E CF3-CC-I and HN3<br>F CH3CH2-CC-I and HN3<br>G Ph-CC-I and HN3<br>H CF3-CC-I and CH3-N3<br>I CH3CH2-CC-I and CH3-N3<br>J Ph-CC-I and CH3-N3<br>K CF3-CC-I and PhN3<br>L CH3CH2-CC-I and PhN3<br>M Ph-CC-I and PhN3<br>N CF3-CC-I and p-MePhN3<br>O CH3CH2-CC-I and p-MePhN3<br>P Ph-CC-I and p-MePhN3<br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.6084/m9.figshare.7599125.v1
title: Late Permian-Triassic granitic rocks of Vietnam: the Muong Lat example

description: The Song Ma zone in Northwestern Vietnam is considered as a suture of the South China and Indochina blocks, and plays an important role in understanding the tectonic evolution in Southeast Asia and surrounding areas. Granitic rocks of the Muong Lat complex are distributed in the Song Ma suture, consisting mainly of monzogranite and granodiorite. The rocks are sub-alkaline in affinity with high K contents and characteristics of S-type granite. They have high SiO<sub>2</sub>, total Na<sub>2</sub>O + K<sub>2</sub>O, and Zr contents and high aluminium saturation index values (0.97 to 1.29 with an average of 1.14). All these geochemical signatures, together with high (<sup>87</sup>Sr/<sup>86</sup>Sr)<sub>i</sub> ratios (0.71391 to 0.74568), and low whole rock ε<sub>Nd</sub>(t) and zircon ε<sub>Hf</sub>(t) values (−13.1 to −9.4) suggested an origin from partial melting of crustal source rocks. Primitive mantle normalized trace element contents exhibit positive anomalies of Rb, Th, U and Pb, but negative anomalies of Nb, Ta, and Ti, indicating a collision-related environment. The depleted Nd and Hf zircon model ages from investigated samples, in combination with inherited zircon ages, suggest the existence of Precambrian basement in the study region. S-type granites of the late Permian-early Triassic (the Muong Lat, Phia Bioc and Hai Van complexes) in Vietnam were formed by the subduction-collision of the South China and Indochina blocks.
DOI: 10.6084/m9.figshare.5459674
title: Azide binding to Cu+-iodoalkynes

description: Inputs, outputs and orbitals for the species present in the Cu+-catalyzed addition of electron-deficient azides to iodoalkynes, discussed in:<br><b>Pedro J. Silva</b> and Carlos E. P. Bernardo (2018), Influence of Alkyne and Azide Substituents on the Choice of the Reaction Mechanism of the Cu<sup>+</sup>-Catalyzed Addition of Azides to Iodoalkynes <i>J. Phys. Chem. A,</i> 122, 7497-7507 <br><br><br><br>Other data reported in the same paper have been uploaded to<br>https://doi.org/10.6084/m9.figshare.5035682<br>https://doi.org/10.6084/m9.figshare.5165878https://doi.org/10.6084/m9.figshare.5418688<br><br>Each file is labelled according to the following table, depending on the specific iodoalkyne/azide combination present<br><br>A CH3-CC-I and HN3<br>B CH3-CC-I and CH3-N3<br>C CH3-CC-I and PhN3<br>D CH3-CC-I and p-MePhN3<br>E CF3-CC-I and HN3<br>F CH3CH2-CC-I and HN3<br>G Ph-CC-I and HN3<br>H CF3-CC-I and CH3-N3<br>I CH3CH2-CC-I and CH3-N3<br>J Ph-CC-I and CH3-N3<br>K CF3-CC-I and PhN3<br>L CH3CH2-CC-I and PhN3<br>M Ph-CC-I and PhN3<br>N CF3-CC-I and p-MePhN3<br>O CH3CH2-CC-I and p-MePhN3<br>P Ph-CC-I and p-MePhN3<br>Q CH3-CC-I and CF3N3<br>R CF3-CC-I and CF3N3<br>S CH3CH2-CC-I and CF3N3<br>T Ph-CC-I and CF3N3<br>U CH3-CC-I and p-NO2-PhN3<br>V CF3-CC-I and p-NO2-PhN3<br>W CH3CH2-CC-I and p-NO2-PhN3<br>X Ph-CC-I and p-NO2-PhN3
DOI: 10.5517/ccdc.csd.cc21pnm1
title: CCDC 1897653: Experimental Crystal Structure Determination

description: Related Article: Meryem Evecen, Hasan Tanak, Ayşen Alaman Ağar, Seher Meral, Namık Özdemir|2021|Optik: international j. light and electron optics|228|166133|doi:10.1016/j.ijleo.2020.166133
description: Related Article: Hasan Tanak|2020|CSD Communication|||
DOI: 10.6084/m9.figshare.9734915
title: Retrieval of Leaf area index and stress conditions for Sundarban mangroves using Sentinel-2 data

description: The potential of Sentinel-2 (S2) data in mapping Leaf area index (LAI) of mangroves having heterogeneous species composition, variable canopy density, and complex backgrounds was studied. Out of the three available near-infrared bands in S2, band-8 of 10 m spatial resolution was found to be the most suitable one for deriving the Normalized Difference Vegetation Index (NDVI) for mangroves. The LAI-NDVI relation did not accord apparently with the earlier reports and the underlying complex background effect was validated with Airborne Visible Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) hyperspectral data. It simulated spectral and spatial conditions of S2 by linear mixing of canopy and background that confirmed the effect of background contributions to the canopy reflectance decorrelating the NDVI from LAI. The compensation for diverse backgrounds was accomplished with optimum-scaled NDVI (scNDVI<sub>m</sub>) obtained from the mean of scaled NDVIs derived with different backgrounds in the mangroves. LAI was well correlated with composite NDVI (NDVI<sub>com</sub>), derived empirically from the most appropriate NDVI (NDVI<sub>S2</sub>) and scNDVI<sub>m</sub> where ground observation controlled the threshold arbitration in extracting the range of scNDVI<sub>m</sub>. It was shown that an improved LAI estimate with a coefficient of determination (<i>R</i><sup>2</sup>) of 0.69 and root-mean-square error (RMSE) of 0.02 could be obtained with NDVI<sub>com</sub>. This method has the advantage of compensating the contaminations due to background reflectance. While the relation between LAI and NDVI<sub>com</sub> was found to be consistent, the application of the same methodology in similar mangroves should be site-specific with ample ground observation. The fusion of NDVI and scNDVI obtained from S2 yields better LAI retrieval for mixed mangroves, such as that of Sundarban.
DOI: 10.6084/m9.figshare.9734915.v1
title: Retrieval of Leaf area index and stress conditions for Sundarban mangroves using Sentinel-2 data

description: The potential of Sentinel-2 (S2) data in mapping Leaf area index (LAI) of mangroves having heterogeneous species composition, variable canopy density, and complex backgrounds was studied. Out of the three available near-infrared bands in S2, band-8 of 10 m spatial resolution was found to be the most suitable one for deriving the Normalized Difference Vegetation Index (NDVI) for mangroves. The LAI-NDVI relation did not accord apparently with the earlier reports and the underlying complex background effect was validated with Airborne Visible Infrared Imaging Spectrometer-Next Generation (AVIRIS-NG) hyperspectral data. It simulated spectral and spatial conditions of S2 by linear mixing of canopy and background that confirmed the effect of background contributions to the canopy reflectance decorrelating the NDVI from LAI. The compensation for diverse backgrounds was accomplished with optimum-scaled NDVI (scNDVI<sub>m</sub>) obtained from the mean of scaled NDVIs derived with different backgrounds in the mangroves. LAI was well correlated with composite NDVI (NDVI<sub>com</sub>), derived empirically from the most appropriate NDVI (NDVI<sub>S2</sub>) and scNDVI<sub>m</sub> where ground observation controlled the threshold arbitration in extracting the range of scNDVI<sub>m</sub>. It was shown that an improved LAI estimate with a coefficient of determination (<i>R</i><sup>2</sup>) of 0.69 and root-mean-square error (RMSE) of 0.02 could be obtained with NDVI<sub>com</sub>. This method has the advantage of compensating the contaminations due to background reflectance. While the relation between LAI and NDVI<sub>com</sub> was found to be consistent, the application of the same methodology in similar mangroves should be site-specific with ample ground observation. The fusion of NDVI and scNDVI obtained from S2 yields better LAI retrieval for mixed mangroves, such as that of Sundarban.
DOI: 10.25345/c5v21b
title: MassIVE MSV000086644 - GNPS - Plant tribe Myoporeae: 291 species and subspecies
title: Paper title: Navigating through chemical space and evolutionary time across the Australian continent in plant genus Eremophila. Author List: Oliver Gericke, Rachael M. Fowler, Allison M. Heskes, Michael J. Bayly, Susan J. Semple, Chi P. Ndi, Dan Stark, Claus J. Loland, Daniel J. Murphy, Bevan J. Buirchell and Birger L. Moller. Citation: bioRxiv, 2020.11.02.364471. doi:10.1101/2020.11.02.364471. Brief description of the data submitted: RAW Files used to generate non-targeted molecular network representing chemical content of the plant tribe Myoporeae. The dataset includes spectral data from 291 species and subspecies, copvering approx. 80% of the tribal species diversity. Network was established with a cosine similarity score cutoff of 0.8 and minimum of 8 matched peaks (FBMN workflow version 18).
DOI: 10.5281/zenodo.4399116
title: Dataset for the publication: Multi-line SiO fluorescence imaging in the flame synthesis of silica nanoparticles from SiCl4

description: Dataset for the publication: Multi-line SiO fluorescence imaging in the flame synthesis of silica nanoparticles from SiCl4 Abbas El Moussawi, Torsten Endres, Sebastian Peukert, Siavash Zabeti, Thomas Dreier, <br> Mustapha Fikri, Christof Schulz in Combustion and Flame This dataset contains the raw LIF imaging data (LIF_Imaging_Rawdata.7z), an overview of the measured flame conditions and their parameters (MeasumentsOverview.xlsx), the determined temperature and SiO-concentration profiles (T&C-SiO-LIF.Exp.Profiles.xlsx), the Origin/Matlab figures from the publication (OriginData&Figures.7z) and the Chemkin project for the kinetic simulations (Chemkin.7z).Remarks.docx contains instructions for performing the Chemkin simulations and information about the software&version used. <br> The Matlab code for analysing the raw data can be found in the separate Zenodo publication:<br> 10.5281/zenodo.4399312<br> However, this is embargoed for 12 months, as a better documented release of the code is planned during this period.
DOI: 10.5281/zenodo.4399115
title: Dataset for the publication: Multi-line SiO fluorescence imaging in the flame synthesis of silica nanoparticles from SiCl4

description: Dataset for the publication: Multi-line SiO fluorescence imaging in the flame synthesis of silica nanoparticles from SiCl4 Abbas El Moussawi, Torsten Endres, Sebastian Peukert, Siavash Zabeti, Thomas Dreier, <br> Mustapha Fikri, Christof Schulz in Combustion and Flame This dataset contains the raw LIF imaging data (LIF_Imaging_Rawdata.7z), an overview of the measured flame conditions and their parameters (MeasumentsOverview.xlsx), the determined temperature and SiO-concentration profiles (T&C-SiO-LIF.Exp.Profiles.xlsx), the Origin/Matlab figures from the publication (OriginData&Figures.7z) and the Chemkin project for the kinetic simulations (Chemkin.7z).Remarks.docx contains instructions for performing the Chemkin simulations and information about the software&version used. <br> The Matlab code for analysing the raw data can be found in the separate Zenodo publication:<br> 10.5281/zenodo.4399312<br> However, this is embargoed for 12 months, as a better documented release of the code is planned during this period.
DOI: 10.25345/c5q78g
title: MassIVE MSV000086645 - GNPS-the mass spectrum of PT of bruker
title: This is the mass spectrum data of a plant extrac .
DOI: 10.6084/m9.figshare.13377077
title: Goniozus legneri.xlsx

description: This data set presents results from four assyas that valuate the capacity of <i>G. legneri</i> to attack, parasite and kill larvae of <i>C. cactorum</i>, to assess its potentiality as a biological control agent
DOI: 10.6084/m9.figshare.13377077.v1
title: Goniozus legneri.xlsx

description: This data set presents results from four assyas that valuate the capacity of <i>G. legneri</i> to attack, parasite and kill larvae of <i>C. cactorum</i>, to assess its potentiality as a biological control agent
DOI: 10.6084/m9.figshare.13498692
title: Raney2study-data.zip

description: These are the original Ivium potentiostat data files relating to the paper "Study of Activity and Super-Capacitance Exhibited by Bifunctional Raney 2.0 Catalyst for Alkaline Water-Splitting Electrolysis" published in the journal MDPI Hydrogen.p, li { white-space: pre-wrap; }
DOI: 10.6084/m9.figshare.13498692.v2
title: Raney2study-data.zip

description: These are the original Ivium potentiostat data files relating to the paper "Study of Activity and Super-Capacitance Exhibited by Bifunctional Raney 2.0 Catalyst for Alkaline Water-Splitting Electrolysis" published in the journal MDPI Hydrogen.p, li { white-space: pre-wrap; }
DOI: 10.6084/m9.figshare.13498692.v1
title: Raney2study-data.zip

description: These are the original Ivium potentiostat data files relating to the paper "Study of Activity and Super-Capacitance Exhibited by Bifunctional Raney 2.0 Catalyst for Alkaline Water-Splitting Electrolysis" published in the journal MDPI Hydrogen.p, li { white-space: pre-wrap; }