01 / From data to insight

One sample. Multiple analytical perspectives.

Using Ba-GIS as a case study, we combine complementary analyses of in situ FTIR and equilibrium adsorption measurements to examine CO₂ adsorption behaviour.

Ba-GIS refers to the Ba3-GIS dataset in the original collaborative research.

The analytical approach

One system. Complementary evidence.

Ba-GIS Experimental system

One material. Two complementary measurement families.

Branch A

In situ FTIR data

Examine how spectral signals evolve across the experimental series.

  • PCA

    Assess data dimensionality and dominant variance.

  • MCR-ALS

    Resolve overlapping spectral contributions and examine their relative evolution.

  • 2D-IRIS

    Explore adsorption heterogeneity through an energy-resolved spectroscopic perspective, within the assumptions of the inversion model.

PCA can inform the number of components tested with MCR-ALS.

Branch B

CO₂ equilibrium adsorption data

Examine adsorption uptake as a function of equilibrium pressure.

Independent experimental evidence

Equilibrium measurements are fitted separately. Neither MCR-ALS nor 2D-IRIS outputs serve as input to these fits.

Scientific interpretation

Integrate complementary evidence from spectroscopy and equilibrium adsorption to build a more complete picture of CO₂ adsorption behaviour, while preserving the limits of each method.

Complementary evidence does not imply a one-to-one correspondence between spectral contributions and adsorption sites.

02 / FTIR measurements

Start with the experimental signal.

The Ba-GIS spectral series records changes during successive CO₂ additions. These measurements provide the common experimental basis for the spectroscopic analyses.

Ba-GIS · Experimental FTIR spectra
Measured dataNew visualization of the measured Ba3-GIS FTIR export: 24 observations and 78 spectral variables, with no added smoothing or normalization. Colour denotes observation order, not equilibrium pressure.

What the data provide

A measured series in which overlapping bands change across the experiment.

These are exported spectral data. The complete historical preprocessing from the raw acquisitions is not reconstructed here.

03 / PCA

How compactly can the variation be described?

PCA assesses the dominant variation in the FTIR matrix. It can guide the component counts tested during MCR-ALS analysis.

PC1
91.878%
PC2
7.409%
PC1 + PC2
99.287%

Explained variance for Ba3-GIS, rounded to three decimals. The archive values are reproduced by column-centred PCA of the available spectral matrix.

Ba-GIS · PCA explained variance
PCA result / Recalculated visualizationPCA recalculated from the exported Ba3-GIS FTIR matrix using column centering, without autoscaling; all 24 observations retained. PC1 + PC2 explain 99.287% of the variance. This does not identify chemical species.

Two dominant components do not establish two chemical species or two adsorption sites.

04 / MCR-ALS

Separate overlapping spectral contributions.

The archived non-negative MCR-ALS solution contains two spectral contributions. Their profiles and relative evolution offer complementary views of the same spectral dataset.

Ba-GIS · Resolved spectral profiles
MCR-ALS result / Replotted archived factorsNew visualization of the archived Ba3-GIS MCR spectral factors, not a new MCR-ALS calculation. Original amplitudes are unchanged. Component 1/2 correspond to the PC1/PC2 export columns, not PCA loadings or identified species.

What resolution adds

Distinct spectral signatures that overlap in the original measurements become easier to examine.

The relative contributions evolve differently across the series. Their amplitudes are not calibrated concentrations or percentages of site populations.

Relative evolution and reconstruction limits
Ba-GIS · Relative MCR contributions
MCR-ALS result / Replotted archived factorsArchived Ba3-GIS MCR contribution amplitudes plotted unchanged against observation order. No rescaling or MCR-ALS recalculation. These are not calibrated concentrations, site percentages, equilibrium-pressure curves or kinetic profiles.

The figures can be traced from the archived factors without rerunning MCR-ALS. The complete historical initialisation, convergence settings and normalisation are not available. Chemical assignment requires additional evidence.

05 / 2D-IRIS

A complementary view of adsorption heterogeneity.

Explore adsorption heterogeneity through an energy-resolved spectroscopic perspective, within the assumptions of the inversion model.

Ba-GIS: 2D-IRIS distribution of adsorbed CO₂ versus wavenumber and ΔadsG°/RT
2D-IRIS result / Recomputed from the exported dataDistribution recomputed from the 24 exported Ba3-GIS difference spectra (0–77 torr, 25 °C) with a Langmuir kernel, Tikhonov regularisation and λ selected on the L-curve (explained variance 99.2 %). The vertical coordinate is a relative, model-dependent apparent affinity, not an absolute energy; lobes are not a count of sites nor a chemical assignment.

A separate spectroscopic analysis

2D-IRIS examines the FTIR data through an inversion model. It is not presented as an output of MCR-ALS.

The recomputed distribution shows two main regions near 2364 and 2339 cm⁻¹ at a weak apparent affinity, joined by a narrower feature near 2350 cm⁻¹ extending towards stronger apparent affinity. Their positions along the vertical axis are relative to the Langmuir model and to the regularisation.

How was this recomputed?

From the same 24 exported difference spectra (0–77 torr, 25 °C), with SpectroChemPy’s Langmuir kernel, an exact quadratic-programming solver and a regularisation parameter selected on the L-curve. Reconstruction explains 99.2 % of the variance. No historical image was digitised.

Explore the 2D-IRIS methodology →

06 / Independent equilibrium adsorption

Confront the measurements with a model.

Ba-GIS equilibrium isotherms at 0, 25 and 50 °C were fitted independently using Langmuir–Freundlich models in OriginPro, reported in the manuscript (Figure 2b) and its supporting information (Figure S8).

This branch is presented here as a methodological account of the published fit and its documented limits, not as a redrawn figure: the underlying isotherm points and native fitting project are not available to us, and no figure is digitised or approximated from the manuscript.

Reading the fit

A good fit is not enough.

Assess parameter uncertainty and physical interpretability alongside fit quality.

Limits of the archived Ba-GIS fits

The Ba3-GIS fit at 25 °C includes poorly constrained parameters. At 50 °C, the two fitted terms are identical. A close fit therefore does not establish two distinct adsorption-site populations. The underlying points and fitting settings are needed before reproducing or extending these fits.

07 / Scientific interpretation

Bring the analytical perspectives together.

Integrate complementary evidence from spectroscopy and equilibrium adsorption to build a more complete picture of CO₂ adsorption behaviour, while preserving the limits of each method.

What becomes actionable

Identify the dominant spectral variation, examine resolved contributions and discuss adsorption behaviour alongside the assumptions of each analysis.

What remains a hypothesis

Unique chemical assignments, site populations and predictions outside the measured conditions require further evidence.

Complementary evidence does not imply a one-to-one correspondence between spectral contributions and adsorption sites.

Research context

A traceable methodological demonstration.

This is collaborative research, not a DataChem client project. Ba-GIS is the public-facing name for the Ba3-GIS dataset; the scientific source files retain their original names.

Tools, provenance and scope

Python and SpectroChemPy are documented for the chemometric analyses; equilibrium isotherm fitting was performed separately in OriginPro. The complete historical code and an automated end-to-end reporting pipeline are not available in the archive.

Abdelhafid Ait Blal is credited in the research submission for methodology, software and formal analysis. The final credit wording remains to be confirmed. Permission for the four FTIR/PCA/MCR visualizations and the recomputed 2D-IRIS distribution has been confirmed by the DataChem owner; the equilibrium-isotherm figure is not reproduced here, since the underlying isotherm points and native fitting project are not available to us.