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Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol...

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Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 [email protected] 1 Workshop on Hydrofluorocarbon (HFC) Management Montreal Protocol Paris, 11-12 July 2014
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Page 1: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Janet F. Bornman

Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol

Curtin UniversityPerth, Western Australia [email protected]

1

Workshop on Hydrofluorocarbon (HFC) Management

Montreal Protocol

Paris, 11-12 July 2014

Page 2: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Hydrochlorofluorocarbons (HCFCs)

Ozone Depleting Substances (ODS)Greenhouse Gases (GHGs)

Hydrofluorocarbons (HFC)

Greenhouse Gases (GHGs)

2

The effect of HFC and HCFCs on the biosphere

Do they have an effect on the biosphere?

Page 3: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

UV-generated hydroxyl radicals (OH), determine the atmospheric lifetime of climate-relevant compounds including: HFCs, HCFCs, CO, NOx, and SO2, methane ….

3

The effect of HFC and HCFCs on the biosphere

Levels of complexity

UV radiation, ozone, climate, health, environment

HCFCs enter the body by inhalation of air, or by skin contact: breathing difficulties, skin irritation, may affect other internal organs

Page 4: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Ground-level O3, aerosols

UV

NOx Volatile organic compounds

Premature mortality (annual, global) ~1.5 million from particulate matter (sulfate, nitrate, most organic aerosols)~0.5 million from O3 (OECD, 2013)

Agricultural losses of $12-21 billion (Avnery et al., 2011)Complex sensitivity to UV radiation and climate

Air quality and UV radiation

Page 5: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Documented: Effects of decreased O3 and increased UV radiation

Not yet well documented:How will the environment/biosphere be affected by increased O3 and decreased UV radiation?

And how will climate interactions modify the response?

5

Predicted likely decrease in tropospheric OH

Lower OH implies slower removal of many important gases:

HFCs, HCFCs, other VOCs, methane, NOx, SO2

Ozone and climate implications

Page 6: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Trifluoroacetic acid (TFA), a breakdown product of HCFCs and HFCs in the atmosphere

Readily deposits to the Earth’s surface through dry and wet deposition

Some of the new hydrofluoroolefins (HFO, unsaturated HFCs) as replacements for HFCs can lead to increases

in TFA (HFO TFA)

6

The effect of HFC and HCFCs on the biosphere

Page 7: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Salt lakes with no outflow, loss by evaporation only Microbiological

degradation in soil and water

TFA

HFCs, HFOs, and HCFCsCF3-CXyH

O

CF3-C-OH

O

CF2Cl-C-OH

• Strong acid, forms salts with minerals in soil

• Concentrations in flowing water are small

• Accumulation will occur in salt lakes, playas and in the ocean

TFA - Environments at risk

7

Page 8: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

8

The effect of HFC and HCFCs on the biosphere

Trifluoroacetic acid (TFA)

Phytotoxic - negative effects on plant growth

But concentrations not sufficient for observed effects

 

Page 9: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Time (days)-10 0 10 20 30 40 50 60

Leng

th o

f w

ater

milf

oil (

cm)

0

5

10

15

20

25

30

35Control 100 μg/L 1,000 μg/L 30,00 μg/L 10,000 μg/L

No significant effects on plants, even at

high concentrations

9

TFA and TCA

Control

Page 10: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

10

The effect of HFC and HCFCs on the biosphere

Trifluoroacetic acid (TFA)

Phytotoxic - negative effects on plant growth

But concentrations not sufficient for observed effects

 

Anthropogenic sources

Atmospheric degradation of some HCFC and HFCs

Atmospheric degradation of narcotics

Trifluoromethyl containing pesticides, aluminum production

 

Natural sources

Underwater hydrothermal vents (?)

Page 11: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

11

Approximate concentrations of TFA

•Switzerland, Fresh water lakes, springs, rivers: ca 100 ng/L

•USA, Fresh water lakes, springs, rivers: 20 – 140 ng/L

•Europe, Rain water: 0 - 1.5 µg/L

•Oceans: 10 – 200 ng/L

Depositions of TFA largest during the growing seasons

Page 12: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Summary

• HCFC has potential negative health effects

• TFA is not bioaccumulative

• Risks to mammals, including humans, aquatic and terrestrial organisms: negligible

• TFA sources (natural and anthropogenic) and cycling through the biosphere should be considered for their environmental impacts

• Continuing monitoring of TFA in the environment may be required if HFOs are significantly increased to replace HFCs

12

Page 13: Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845 Janet.Bornman@Curtin.edu.au.

Summary

WMO Assessment of Ozone Depletion (2007):

“TFA from the degradation of HCFCs and HFCs will not

result in environmental concentrations capable of

significant ecosystem damage.”

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