110108
cis-Pinonic acid
98%
Synonym(s):
cis-3-Acetyl-2,2-dimethylcyclobutaneacetic acid
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About This Item
Linear Formula:
CH3COC4H4(CH3)2CH2CO2H
CAS Number:
Molecular Weight:
184.23
NACRES:
NA.22
PubChem Substance ID:
UNSPSC Code:
12352100
MDL number:
Assay:
98%
Form:
solid
InChI
1S/C10H16O3/c1-6(11)8-4-7(5-9(12)13)10(8,2)3/h7-8H,4-5H2,1-3H3,(H,12,13)/t7-,8+/m1/s1
SMILES string
CC(=O)[C@@H]1C[C@H](CC(O)=O)C1(C)C
InChI key
SIZDUQQDBXJXLQ-SFYZADRCSA-N
assay
98%
form
solid
mp
104-107 °C (lit.)
functional group
carboxylic acid, ketone
Related Categories
General description
cis-Pinonic acid undergoes oxidation to produce secondary organic aerosol (SOA).
signalword
Warning
hcodes
Hazard Classifications
Eye Irrit. 2 - Skin Irrit. 2 - STOT SE 3
target_organs
Respiratory system
Storage Class
11 - Combustible Solids
wgk
WGK 3
flash_point_f
Not applicable
flash_point_c
Not applicable
ppe
dust mask type N95 (US), Eyeshields, Gloves
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Yuanlong Huang et al.
The journal of physical chemistry. A, 122(31), 6445-6456 (2018-07-17)
Gas and aqueous phases are essential media for atmospheric chemistry and aerosol formation. Numerous studies have focused on aqueous-phase reactions as well as coupled gas/aqueous-phase mass transport and reaction. Few studies have directly addressed processes occurring at the air-water interface
Andrea Arangio et al.
Applied spectroscopy, 73(6), 638-652 (2019-04-17)
The application of electrospray (ES) for quantitative transfer of analytes from solution to an internal reflection element for analysis by attenuated total reflection Fourier transform infrared (ATR FT-IR) spectroscopy has been developed in this work. The ES ATR FT-IR method
Fragmentation vs. functionalization: chemical aging and organic aerosol formation.
Chacon-Madrid HJ and Donahue NM.
Atmospheric Chemistry and Physics, 11(20), 10553-10563 (2011)
Emma Q Walhout et al.
Environmental science & technology, 53(13), 7604-7612 (2019-06-12)
Characterizing the chemical composition of organic aerosols can elucidate aging mechanisms as well as the chemical and physical properties of the aerosol. However, the high chemical complexity and often low atmospheric abundance present a difficult analytical challenge. Milligrams or more
Markus Müller et al.
Analytical chemistry, 89(20), 10889-10897 (2017-09-16)
We report on a new method for analyzing atmospheric submicrometer particulate organic matter which combines direct particle sampling and volatilization with online chemical ionization mass spectrometric analysis. Technically, the method relies on the combined use of a CHARON ("Chemical Analysis
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