C34200
Chlorodifluoroacetic acid
98%
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About This Item
Linear Formula:
F2ClCCOOH
CAS Number:
Molecular Weight:
130.48
UNSPSC Code:
12352106
NACRES:
NA.22
PubChem Substance ID:
EC Number:
200-928-8
Beilstein/REAXYS Number:
956625
MDL number:
Product Name
Chlorodifluoroacetic acid, 98%
InChI
1S/C2HClF2O2/c3-2(4,5)1(6)7/h(H,6,7)
InChI key
OAWAZQITIZDJRB-UHFFFAOYSA-N
SMILES string
OC(=O)C(F)(F)Cl
assay
98%
form
liquid
refractive index
n20/D 1.355 (lit.)
bp
122 °C (lit.)
mp
20-23 °C (lit.)
density
1.54 g/mL at 25 °C (lit.)
Quality Level
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Related Categories
signalword
Danger
hcodes
Hazard Classifications
Skin Corr. 1A
Storage Class
8A - Combustible corrosive hazardous materials
wgk
WGK 3
flash_point_f
Not applicable
flash_point_c
Not applicable
ppe
Faceshields, Gloves, Goggles, type ABEK (EN14387) respirator filter
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J W Harris et al.
Chemical research in toxicology, 4(2), 180-186 (1991-03-01)
1,2-Dichloro-1,1-difluoroethane (HCFC-132b) is a potential substitute for some ozone-depleting chlorofluorocarbons and a model for other 1,1,1,2-tetrahaloethanes under consideration as chlorofluorocarbon substitutes. Male Fischer 344 rats were given 10 mmol/kg HCFC-132b dissolved in corn oil by intraperitoneal injection. An NMR assay
M Zdanowska-Fraczek et al.
Solid state nuclear magnetic resonance, 6(2), 141-146 (1996-04-01)
The reorientation of CClF2 groups in N(CH3)4H(ClF2CCOO)2 has been studied using pulsed NQR and NMR techniques. The temperature dependence of both chlorine (35Cl) NQR and fluorine (19F) NMR spin-lattice relaxation has been measured T1Q of chlorine is attributed to the
M L Hanson et al.
Environmental toxicology and chemistry, 20(12), 2758-2767 (2002-01-05)
Chlorodifluoroacetic acid (CDFA) is a novel haloacetic acid (HAA) and has been recently documented in aquatic systems. It is a suspected degradation product of the refrigerants 1,1,2-trichloro-1,1-difluoroethane (CFC-113) and 1-chloro-1,1-difluoroethane (HCFC-142b). Haloacetic acids can be phytotoxic, putatively acting through inhibition
Keith R Solomon et al.
Photochemical & photobiological sciences : Official journal of the European Photochemistry Association and the European Society for Photobiology, 2(1), 62-67 (2003-03-28)
Increased UV-B through stratospheric ozone depletion leads to an increased chemical activity in the lower atmosphere (the troposphere). The effect of stratospheric ozone depletion on tropospheric ozone is small (though significant) compared to the ozone generated anthropogenically in areas already
Janina Kopyra et al.
The Journal of chemical physics, 135(12), 124307-124307 (2011-10-07)
Negative ion formation following resonant electron attachment to the three title molecules is studied by means of a beam experiment with mass spectrometric detection of the anions. All three molecules exhibit a pronounced resonance in the energy range around 1
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