particulate matter (pm) overview 4 february 2015 rob griffin ([email protected])

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Particulate Matter (PM) Overview 4 February 2015 Rob Griffin ([email protected])

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Page 1: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Particulate Matter (PM) Overview

4 February 2015

Rob Griffin ([email protected])

Page 2: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Who Am I and What Do I Do?I’m a professor in CEVE (despite doing all my degrees in CHE) at Rice in Houston

Page 3: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Who Am I and What Do I Do?Research focuses on what happens to things once they get to the atmosphere – lab-based experiments, measurements in the ambient atmosphere, and computer modeling to describe air quality (often with Dr. Dabdub)

Page 4: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

What is an Aerosol?Metastable suspension of particles in a background gas

Solid or liquid, generally assumed to be spherical

For our interests, the background gas is air

Metastable? Stable enough to persist within a time frame of interest

Rain? Too short – falls too rapidly (within hours)Infinity? Too longGenerally – atmospheric lifetime of ~1 week

Aerosol = gas + particlesParticulate matter (PM) = just the particles

Page 5: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

So How Big Are We Talking?

* This cutoff sometimes defined as 1 m

N ~ 103 -104 cm-3

More in pollutedLess in remote

Particle surface area distribution

Page 6: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Why Do We Even Care About PM?

Aerosol Layer CloudFormation

Deposition

InhalationVisibilityDegradation

Reflectance

Precipitation

HeterogeneousReaction Site

Ab

sorp

tion

Reflectance

Page 7: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

NAAQSPrimary standard – Designed to protect human health, particularly that of sensitive groups

Secondary standard – Designed to protect public welfare (visibility; damage to animals, crops, vegetation, and buildings)

Criteria pollutants: CO, NO2, O3, Pb, SO2, PM2.5, PM10

PM2.5 primary annual average 12 g m-3; secondary annual average 15 g m-3; primary and secondary daily average 35 g m-3

PM10 primary and secondary: 24-hour 150 g m-3

Page 8: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Transport and Deposition

Trans-Atlantic dust transport followed by deposition to the Caribbean has been implicated in coral death (due to microbes)

Other examples: Deposited particles clogging stomata, nutrient cycling,acidification of soil, destruction of artwork

Page 9: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Visibility

Other examples?

Page 10: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Reaction Sites

Aerosols are a heterogeneous source of X in the stratosphere

Page 11: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Climate Impacts

Note level of scientific understanding (IPCC)

Page 12: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Emitted vs. FormedPrimary Secondary

Gas A Gas B

Page 13: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Most Abundant Aerosol Components

IDEAS?

Page 14: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Most Abundant Aerosol Components

WaterSulfateNitrateAmmoniumOrganicsCarbonatesElemental/black carbonSodiumChlorideCrustal/Minerals (Dust)Metals

Page 15: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Global Aerosol SourcesSource Notes Issues Amount (Tg/yr)

Soil dust Wind driven in drier climates; composition varies regionally

Microbes, “dust storms”

1500

Sea salt Wind/wave driven; dominated by NaCl

Displacement 10000

Volcanic debris Composition varies regionally

Secondary chemistry

30

Biological debris Wind driven; mostly organic

Hard to ID 50

Anthropogenic primary aerosol

Linked to combustion; many constituents

Region/source dependence

200

Secondary sulfate

Sulfur + oxidant Very non-volatile 50 anth. SO2; 10 DMS; 20 volc. SO2

Secondary nitrate

Nitrogen + oxidant Size depends on formation route

20 anth; ? natural

SOA VOC + oxidant Hard to ID 10 anth.; ~15 biogenic

Page 16: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

What parameters matter?

Page 17: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

What parameters matter?

How much is there?What is it made of?How many particles are there?How big are they?What are their physical properties?Others…

Page 18: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

How much is there?

Filter-based (pull air through it, weight it before and after) or similar methods

Composition-based (sum up all the stuff you identify)

Size-based (count how many particles you have of a certain size, use geometry and an assumed density)

Page 19: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

What is it made of?

Off-line chemical analytical techniques:You name it, it has probably been done (requires filter

extracts or collection of PM into water sample using a PILS or other collection technique)

On-line chemical techniques:State-of-science = aerosol mass spectrometry (AMS)

Physical characterization:If it is black (determined by light measurement), it’s

almost exclusively black carbon (aethalometer)

Page 20: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

How many particles are there?

Count them!

Typically done using optics (for bigger particles) in an optical particle counter (OPC) or using lasers (for smaller particles) in a condensation nucleus counter (CNC)

Page 21: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

How big are they?

Typically done by applying an external force and seeing how the particle responds (force balance).

For example, a differential mobility analyzer (DMA) puts a charge on a particle and then exposes them to an electric field (voltage across a gap); based on the geometry and flow of the system only a particle of a given size exits the DMA (to then be detected by a CNC)

Page 22: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

What are their physical properties?

Do they scatter light? A nephelometer determines this (think about visibility and climate forcing)

- Shine light in one direction and measure it at a different angle

Do they take up water? A tandem DMA determines this (think about visibility, climate forcing, chemistry…)

- Pick one size particle with a DMA, expose the particles to increased RH, measure size with a second DMA

Page 23: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Aerosol Field Measurements

This list could go on for a really, really long time

As could the list of places where such measurements have been performed (surface-fixed, surface-mobile, airplane-based…)

Page 24: Particulate Matter (PM) Overview 4 February 2015 Rob Griffin (rob.griffin@rice.edu)

Thanks…

For your attention and participation

Please don’t hesitate to contact me with questions about PM, field campaigns, Rice, Houston, etc.