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Chlorotrifluoromethane

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(Redirected from Freon-13)
Chlorotrifluoromethane
Names
Preferred IUPAC name Chloro(trifluoro)methane
Other names Chlorotrifluoromethane
Monochlorotrifluoromethane
Trifluorochloromethane
Trifluoromethyl chloride
Trifluoromonochlorocarbon
Arcton 3
Freon 13
Genetron 13
R-13
CFC 13
UN 1022
Identifiers
CAS Number
3D model (JSmol)
ChemSpider
ECHA InfoCard 100.000.814 Edit this at Wikidata
EC Number
  • 200-894-4
PubChem CID
RTECS number
  • PA6410000
UNII
CompTox Dashboard (EPA)
InChI
  • InChI=1S/CClF3/c2-1(3,4)5Key: AFYPFACVUDMOHA-UHFFFAOYSA-N
  • InChI=1/CClF3/c2-1(3,4)5Key: AFYPFACVUDMOHA-UHFFFAOYAV
SMILES
  • ClC(F)(F)F
Properties
Chemical formula CClF3
Molar mass 104.46 g/mol
Appearance Colorless gas with sweet odor
Density 1.526 g/cm
Melting point −181 °C (−293.8 °F; 92.1 K)
Boiling point −81.5 °C (−114.7 °F; 191.7 K)
Solubility in water 0.009% at 25 °C (77 °F)
Vapor pressure 3.263 MPa at 21 °C (70 °F)
Thermal conductivity 0.01217 W m K (300 K)
Hazards
Occupational safety and health (OHS/OSH):
Main hazards Ozone depletor and asphyxiant
Flash point Non-flammable
Safety data sheet (SDS) ICSC 0420
Except where otherwise noted, data are given for materials in their standard state (at 25 °C , 100 kPa). ☒verify (what is  ?) Infobox references
Chemical compound

Chlorotrifluoromethane, R-13, CFC-13, or Freon 13, is a non-flammable, non-corrosive, nontoxic chlorofluorocarbon (CFC) and also a mixed halomethane. It is a man-made substance used primarily as a refrigerant. When released into the environment, CFC-13 has a high ozone depletion potential, and long atmospheric lifetime. Only a few other greenhouse gases surpass CFC-13 in global warming potential (GWP). The IPCC AR5 reported that CFC-13's atmospheric lifetime was 640 years.

Production

CFC-13—like all chlorofluorocarbon compounds—contains atoms of carbon (C), chlorine (Cl), and fluorine (F).

It can be prepared by reacting carbon tetrachloride with hydrogen fluoride in the presence of a catalytic amount of antimony pentachloride:

CCl4 + 3 HF → CClF3 + 3 HCl

This reaction can also produce trichlorofluoromethane (CCl3F), dichlorodifluoromethane (CCl2F2) and tetrafluoromethane (CF4).

Montreal Protocol

Main article: Montreal Protocol

Following the unanimous ratification of the 1987 Montreal Protocol—in response to concerns about the role of concentrations of chlorofluorocarbons (CFCs) in ozone layer-depletion in the stratosphere—a process was put into place to gradually phase out and replace CFC-13 and all the other CFCs. Research in the 1980s said that these man-made CFC compound compounds had opened a hole in ozone layer in the upper atmosphere or stratosphere that protects life on earth from UV radiation.

CFC-13's ozone depletion potential (ODP) is high— 1 (CCl3F = 1)—it is categorized as a Class I in the IPCC's list of ozone-depleting substances. CFC-13's radiative efficiency is high which results in a high global warming potential (GWPs) of 13 900 GWP-100 yr that is "surpassed by very few other greenhouse gases." It is categorized as a Class I in the list of ozone-depleting Substances.

Increase in atmospheric abundance of CFC-13 in 2010s

Starting in the 2010s, despite a global ban on the production of CFCs, five of these ozone-damaging emissions were on the rise.

The atmospheric abundance of CFC-13 rose from 3.0 parts per trillion (ppt) in year 2010 to 3.3 ppt in year 2020 based on analysis of air samples gathered from sites around the world. Contrary to the Montreal Protocol, the atmospheric emissions of CFC-13 and four other chlorofluorocarbons (CFCs), increased between 2010 and 2020.

As of 2023, the drivers behind the increase in CFC-13 and CFC-112a emissions were not certain.

Physical properties

The IPCC AR5 reported that CFC-13's Atmospheric lifetime was 640 years.

Property Value
Density (ρ) at -127.8 °C (liquid) 1.603 g⋅cm
Density (ρ) at boiling point (gas) 6.94 kg⋅m
Density (ρ) at 15 °C (gas) 4.41 g⋅cm
Triple point temperature (Tt)
Critical temperature (Tc) 28.8 °C (302 K)
Critical pressure (pc) 3.86 MPa (38.6 bar)
Critical density (ρc) 5.5 mol⋅L
Latent heat of vaporization at boiling point 149.85 kJ⋅kg
Specific heat capacity at constant pressure (Cp) at -34.4 °C 0.06 kJ⋅mol⋅K
Specific heat capacity at constant volume (CV) at -34.4 °C 0.051 kJ⋅mol⋅K
Heat capacity ratio (к) at -34.4 °C 1.168016
Compressibility Factor (Z) at 15 °C 0.9896
Acentric factor (ω) 0.17166
Viscosity (η) at 0 °C (gas) 13.3 mPa⋅s (0.0133 cP)
Viscosity (η) at 25 °C (gas) 14.1 mPa⋅s (0.01440 cP)
Ozone depletion potential (ODP) 1(CCl3F = 1)
Global warming potential (GWP) 14,000 (CO2 = 1)
Atmospheric lifetime 640 years

See also

References

  1. Touloukian, Y.S., Liley, P.E., and Saxena, S.C. Thermophysical properties of matter - the TPRC data series. Volume 3. Thermal conductivity - nonmetallic liquids and gases. Data book. 1970.
  2. Siegemund, Günter; Schwertfeger, Werner; Feiring, Andrew; Smart, Bruce; Behr, Fred; Vogel, Herward; McKusick, Blaine (2002). "Fluorine Compounds, Organic". Ullmann's Encyclopedia of Industrial Chemistry. Weinheim: Wiley-VCH. doi:10.1002/14356007.a11_349. ISBN 978-3527306732.
  3. ^ Vollmer, Martin; Young, Dickon; Trudinger, Cathy; Mühle, Jens; Henne, Stephan; Rigby, Matt; Park, Sunyoung; Li, Shihong; Guillevic, Myriam; Mitrevski, Blagoj; Harth, Christina; Miller, Benjamin; Reimann, Stefan; Yao, Bo; Steele, L.; Wyss, Simon; Lunder, Chris; Arduini, Jgor; McCulloch, Archie; Simmonds, Peter (October 10, 2017). "Atmospheric histories and emissions of chlorofluorocarbons CFC-13 (CClF3), CFC-114 (C2Cl2F4), and CFC-115 (C2ClF5)". Atmospheric Chemistry and Physics Discussions. 2017 (39). doi:10.5194/acp-2017-935. hdl:1721.1/116270.
  4. ^ "Chapter 8". AR5 Climate Change 2013: The Physical Science Basis. p. 731.
  5. ^ Ashworth, James (April 3, 2023). "Mystery emissions of ozone-damaging gases are fuelling climate change". Natural History Museum. Retrieved April 3, 2023.
  6. Elkins, James.W. (2013). "Halocarbons and other Atmospheric Trace Species". NOAA Global Monitoring Laboratory (Press release). Retrieved April 3, 2023 – via US Department of Commerce and NOAA.
  7. Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. p. 304. ISBN 978-0-08-037941-8.
  8. Allen, Kate (April 3, 2023). "Remember ozone-destroying CFCs? They're on the rise again. And the source is a mystery". The Star. Retrieved April 3, 2023.
  9. ^ "Class I Ozone-depleting Substances". Science - Ozone Layer Protection. US EPA. 2007. Archived from the original on 2010-12-10. Retrieved 2010-12-16.
  10. "AGAGE Data and Figures". Massachusetts Institute of Technology. Retrieved 2021-02-11.
  11. ^ Western, Luke M.; Vollmer, Martin K.; Krummel, Paul B.; Adcock, Karina E.; Fraser, Paul J.; Harth, Christina M.; Langenfelds, Ray L.; Montzka, Stephen A.; Mühle, Jens; O’Doherty, Simon; Oram, David E.; Reimann, Stefan; Rigby, Matt; Vimont, Isaac; Weiss, Ray F.; Young, Dickon; Laube, Johannes C. (April 3, 2023). "Global increase of ozone-depleting chlorofluorocarbons from 2010 to 2020". Nature Geoscience. 16 (4): 309–313. Bibcode:2023NatGe..16..309W. doi:10.1038/s41561-023-01147-w. hdl:1983/9e103fef-e61c-49c7-a1a3-902540ec1d7c. ISSN 1752-0908. S2CID 257941769. Retrieved April 3, 2023.
  12. Forster, Piers; Ramaswamy, Venkatachalam; Artaxo, Paulo; Berntsen, Terje; Betts, Richard; Fahey, David W; Haywood, James; Lean, Judith; Lowe, David C; Raga, Graciela; Schulz, Michael; Dorland, Robert Van; Bodeker, G; Etheridge, D; Foukal, P; Fraser, P; Geller, M; Joos, F; Keeling, C D; Keeling, R; Kinne, S; Lassey, K; Oram, D; O’Shaughnessy, K; Ramankutty, N; Reid, G; Rind, D; Rosenlof, K; Sausen, R; Schwarzkopf, D; Solanki, S K; Stenchikov, G; Stuber, N; Takemura, T; Textor, C; Wang, R; Weiss, R; Whorf, T; Nakajima, Teruyuki; Ramanathan, Veerabhadran; Ramaswamy, V; Artaxo, P; Berntsen, T; Betts, R; Fahey, D W; Haywood, J; Lean, J; Lowe, D C; Myhre, G; Nganga, J; Prinn, R; Raga, G; Schulz, M; Dorland, R Van. "Changes in Atmospheric Constituents and in Radiative Forcing". International Panel of Climate Change (IPCC). AR4 Climate Change 2007: The Physical Science Basis.

External links

Halomethanes
Unsubstituted
Monosubstituted
Disubstituted
Trisubstituted
Tetrasubstituted
* Chiral compound.
Fluorine compounds
Salts and covalent derivatives of the fluoride ion
HF ?HeF2
LiF BeF2 BF
BF3
B2F4
+BO3
CF4
CxFy
+CO3
NF3
FN3
N2F2
NF
N2F4
NF2
?NF5
OF2
O2F2
OF
O3F2
O4F2
?OF4
F2 Ne
NaF MgF2 AlF
AlF3
SiF4 P2F4
PF3
PF5
S2F2
SF2
S2F4
SF3
SF4
S2F10
SF6
+SO4
ClF
ClF3
ClF5
?ArF2
?ArF4
KF CaF
CaF2
ScF3 TiF2
TiF3
TiF4
VF2
VF3
VF4
VF5
CrF2
CrF3
CrF4
CrF5
?CrF6
MnF2
MnF3
MnF4
?MnF5
FeF2
FeF3
FeF4
CoF2
CoF3
CoF4
NiF2
NiF3
NiF4
CuF
CuF2
?CuF3
ZnF2 GaF2
GaF3
GeF2
GeF4
AsF3
AsF5
Se2F2
SeF4
SeF6
+SeO3
BrF
BrF3
BrF5
KrF2
?KrF4
?KrF6
RbF SrF
SrF2
YF3 ZrF2
ZrF3
ZrF4
NbF4
NbF5
MoF4
MoF5
MoF6
TcF4
TcF
5

TcF6
RuF3
RuF
4

RuF5
RuF6
RhF3
RhF4
RhF5
RhF6
PdF2
Pd
PdF4
?PdF6
Ag2F
AgF
AgF2
AgF3
CdF2 InF
InF3
SnF2
SnF4
SbF3
SbF5
TeF4
?Te2F10
TeF6
+TeO3
IF
IF3
IF5
IF7
+IO3
XeF2
XeF4
XeF6
?XeF8
CsF BaF2   LuF3 HfF4 TaF5 WF4
WF5
WF6
ReF4
ReF5
ReF6
ReF7
OsF4
OsF5
OsF6
?OsF
7

?OsF
8
IrF2
IrF3
IrF4
IrF5
IrF6
PtF2
Pt
PtF4
PtF5
PtF6
AuF
AuF3
Au2F10
?AuF6
AuF5•F2
Hg2F2
HgF2
?HgF4
TlF
TlF3
PbF2
PbF4
BiF3
BiF5
?PoF2
PoF4
PoF6
AtF
?AtF3
?AtF5
RnF2
?RnF
4

?RnF
6
FrF RaF2   LrF3 Rf Db Sg Bh Hs Mt Ds Rg Cn Nh Fl Mc Lv Ts Og
LaF3 CeF3
CeF4
PrF3
PrF4
NdF2
NdF3
NdF4
PmF3 SmF2
SmF3
EuF2
EuF3
GdF3 TbF3
TbF4
DyF2
DyF3
DyF4
HoF3 ErF3 TmF2
TmF3
YbF2
YbF3
AcF3 ThF3
ThF4
PaF4
PaF5
UF3
UF4
UF5
UF6
NpF3
NpF4
NpF5
NpF6
PuF3
PuF4
PuF5
PuF6
AmF2
AmF3
AmF4
?AmF6
CmF3
CmF4
 ?CmF6
BkF3
BkF
4
CfF3
CfF4
EsF3
EsF4
?EsF6
Fm Md No
PF−6, AsF−6, SbF−6 compounds
AlF−6 compounds
chlorides, bromides, iodides
and pseudohalogenides
SiF2−6, GeF2−6 compounds
Oxyfluorides
Organofluorides
with transition metal,
lanthanide, actinide, ammonium
nitric acids
bifluorides
thionyl, phosphoryl,
and iodosyl
Chemical formulas
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