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MS Physics thesis · LUMS · Supervisor: Prof. Walther Schwarzacher

IceNucleationbyLahoreSmogParticles

The first ice-nucleation characterisation of South Asian urban aerosol.

Headline result+10.7 °CSmog particles raised the droplet freezing temperature by 10.7 °C versus pure water.

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Custom steel high-volume air sampler on the LUMS rooftop
The custom high-volume sampler on the LUMS rooftop during the November 2024 smog season.
02The sampler

A sampler built from scratch

A custom rooftop high-volume sampler — welded steel frame, sheltered inlet, PTFE membrane filters. Running at 15 L/min for 24 h draws 21.6 m³ of air through each filter. It collected ~1.1 mg of mass — about 51 µg/m³ over 24 h, more than 3× the WHO 24-hour PM2.5 guideline — sampled through the November 2024 smog season.

A clean PTFE filter beside one loaded with Lahore particulate matter
Before and after: a clean membrane vs one holding ~1.1 mg of collected PM.
SEM of a loaded filter with dispersed smog particles
The same particles under the SEM — discrete on the fibres.
03What it collected · SEM

Discrete particles, not a smear

Electron microscopy shows particles sitting individually on the filter fibres — not a continuous smear, which is what makes single-particle analysis possible. Soot primary particles run 15–75 nm; the largest mineral grains reach 3–5 µm. (FEI Nova NanoSEM, 10 kV.)

Full SEM/EDX result, size distribution & soot images →
EDX element map of a mineral dust grain
EDX map — silicon and oxygen light up a mineral-dust grain.
04Composition · EDX

Two signatures, two sources

Nine elements appear on the loaded filter and are absent from the control. Two tell a story: alumino-silicate mineral dust — with potassium pointing to feldspar, the most efficient known mineral ice nucleator — and sulphur from combustion as sulphate. Potassium also traces biomass burning; zinc traces traffic.

SiSiliconSilicate mineral dust
AlAluminiumAlumino-silicate — feldspar
KPotassiumFeldspar + biomass burning
CaCalciumCrustal / road dust
FeIronCrustal dust
SSulphurCombustion sulphate
Experimental setup: microscope, cold-stage controller and recording PC
The rig: microscope over the Linkam cold stage, with the controller and recording PC.
The Linkam cold stage with mounted samples and liquid-nitrogen lines
The Linkam cold stage — samples mounted, liquid-nitrogen lines attached.
05The measurement

An in-house cold-stage freezing assay

Droplets are frozen on a temperature-controlled stage: a Linkam T95 with LNP95 liquid-nitrogen cooling, stable to ±0.1 °C. 1 µL droplets sit in a grid, 6–10 per run; freezing is caught optically as each droplet turns from transparent to opaque. A two-stage ramp — 20 °C/min to −10 °C, then 1 °C/min to −40 °C — and a 0.5% DMOAP silane coating for a stable hydrophobic surface.

Lab air
−23.3°
~7 °C scatter
Cleanroom
−28.4°
< 3 °C spread

Pure-water baseline, before vs after moving to a cleanroom.

06A systematic-error lesson

The tell was the scatter, not the temperature

Early pure-water runs froze at −23.3 °C with ~7 °C of scatter. Moving the setup into a cleanroom dropped the baseline to −28.4 °C and cut the spread below 3 °C. That the reproducibility improved as much as the temperature was the clue: the early signal was ambient ice-nucleating particles from lab air contaminating the samples — not a property of the water. Diagnosing and removing that systematic error is what made the real result trustworthy.

07 · The main result

Smog freezes water 10.7 °C warmer

Pure water froze at a median −28.4 °C (±1.1); Lahore smog at −17.7 °C (±0.9) — a reproducible 10.7 °C shift. Published values from Beijing, Delhi and Mexico City fall between −16 and −20 °C; Lahore sits right with them, and this is the first such measurement for South Asian urban aerosol.

My data: droplet-freezing spectrum

Fraction of 12 droplets frozen as they cool. Lahore-smog droplets freeze about 10.7 °C warmer than pure water — direct evidence of active ice-nucleating particles in the smog.

0%25%50%75%100%-30-27-24-21-18-15Temperature (°C)Droplets frozen-28.4°-17.7°10.7 °C shiftPure waterLahore smog

Source: Ice Nucleation Induced by Lahore Smog ParticlesMS Physics thesis · LUMS · 2025 · Fig. 4.5. Pure water's homogeneous-freezing limit is ≈ -38 °C; a cleanroom move sharpened the pure-water result from -23.3 °C to -28.4 °C.

Full photomask carrying eleven microfluidic geometries on one wafer
One photomask, eleven geometries — deliberately redundant.
42-well crystal-hotel array design
The 42-well “crystal hotel”.
Denser well-array design variant
A denser array variant.
Alpha-Step profilometry trace showing a ~19.8 micron SU-8 step height
Profilometry: uniform ~19.8 µm structures (measured step 19,828 nm).
08Pushing the method further

Microfabricated droplet arrays

To beat the 6–10 droplet statistical ceiling, I designed high-density arrays — eleven geometries on one photomask (deliberately redundant), including a 168-well array and a 42-well “crystal hotel”. The SU-8 process was refined to 19.8 µm against a 20 µm target with under 0.5 µm variation across the wafer (UV exposure cut to 4.6 s, staged soft bakes, controlled development). The recipe was validated; the full device was still in fabrication when the project ended.

09Ongoing · Oxford

Designed ice nucleators

With the Jonathan Bath group at the Clarendon Laboratory, Oxford, I'm exploring DNA origami as ice nucleators — where the geometry is chosen rather than inherited, making a designed nucleator a potentially better calibration standard. My contribution: folding by controlled thermal annealing, gel electrophoresis to confirm assembly, dynamic light scattering for size, and sonication to break up aggregates. Freezing measurements are in progress.