PM2.5 Chemical Composition Analysis Dashboard

The INDFIN Project - A collaboration between BMKG Indonesia and FMI Finland

Executive Summary

Comprehensive analysis of PM2.5 chemical composition using X-ray Fluorescence (XRF) and Ion Chromatography (IC) methods reveals distinct seasonal patterns and source contributions in atmospheric aerosols.

The PM2.5 samples were collected during two field campaigns in the dry season (June-September 2024) and in the wet season (December 2024-March 2025).

Key Findings

  • Secondary sulfate aerosols dominate during dry season
  • Sea salt influence more pronounced in wet season
  • Strong correlation between XRF and IC methods validates cross-method consistency
  • Non-sea-salt sulfate contributes >95% of total sulfate
74.54%
Total XRF Variance Explained (4 PCs)
Prevalent Secondary Sulfate
91.21%
Total IC Variance Explained (4 PCs)
Secondary Inorganic Aerosols
1.15
Ionic Balance Slope
Excess of Cations
30%
NH₄⁺ Neutralization Ratio
Acidic Species

Methodology

XRF Analysis

X-ray Fluorescence spectroscopy for elemental composition determination of PM2.5 samples.

IC Analysis

Ion Chromatography for water-soluble ionic species measurement in atmospheric particles.

PCA Analysis

Principal Component Analysis to identify source contributions and chemical associations.

Seasonal Comparison

Statistical analysis of dry vs wet season variations using Mann-Whitney U test.

XRF Principal Component Analysis

Variance explained by each principal component

Component Loadings

Principal Component Interpretations

IC Principal Component Analysis

Variance explained by each principal component

Component Loadings

Principal Component Interpretations

Seasonal Comparison

Statistical Significance Legend

p < 0.05 (Significant)
p ≥ 0.05 (Not Significant)

Ionic Balance

Cation vs Anion Equivalents

Slope: 1.15
Intercept: -0.01

Slight excess of cations over anions on average

SO₄²⁻/NO₃⁻ Ratio Distribution

Distribution of SO₄²⁻/NO₃⁻ ratios, indicating the prevalence of different atmospheric conditions or sources. Dominance of sulfur-based secondary aerosol from SO₂ emissions.

NH₄⁺ Neutralization Ratio Distribution

Distribution of NH₄⁺ neutralization ratios. Under-neutralization indicates some sulfate exists as acidic species.

Non-Sea-Salt Sulfate (nss-SO₄²⁻)

Example:

Total SO₄²⁻: 3.11 μg/m³

nss-SO₄²⁻: 3.07 μg/m³

Anthropogenic SO₂ origin dominates (Contribution >95%).

Cross-Method Validation

Consistency assessment between XRF and IC analytical methods

XRF-IC Sulfur Method Comparison

Strong and direct correlation

XRF-IC Potassium Method Comparison

Consistent cross-method signal

Validation Summary

Sulfur Consistency

Strong correlation between XRF S and IC SO₄²⁻ validates measurement accuracy across both analytical platforms.

Validated

Potassium Cross-Reference

Consistent signal between XRF K and IC K⁺ confirms reliable detection of crustal and biomass burning sources.

Validated

Crustal Elements

Crustal elements show consistent patterns, especially evident in PC4 of IC PCA analysis.

Validated