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Merck
CN

W274607

Sigma-Aldrich

二甲基硫醚

≥99%, FCC

别名:

DMS, 甲硫醚

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关于此项目

线性分子式:
(CH3)2S
化学文摘社编号:
分子量:
62.13
FEMA编号:
2746
Beilstein:
1696847
EC 号:
欧洲委员会编号:
483
MDL编号:
UNSPSC代码:
12164502
PubChem化学物质编号:
Flavis编号:
12.006
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生物来源

synthetic

管理合规性

FCC

蒸汽密度

2.1 (vs air)

蒸汽压

26.24 psi ( 55 °C)
7.79 psi ( 20 °C)

方案

≥99%

自燃温度

402 °F

expl. lim.

19.7 %

折射率

n20/D 1.435 (lit.)

沸点

38 °C (lit.)

mp

−98 °C (lit.)

密度

0.846 g/mL at 25 °C (lit.)

应用

flavors and fragrances

SMILES字符串

CSC

InChI

1S/C2H6S/c1-3-2/h1-2H3

InChI key

QMMFVYPAHWMCMS-UHFFFAOYSA-N

基因信息

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Peter Arner et al.
Clinical epigenetics, 7, 93-93 (2015-09-10)
Obesity is associated with changes in fat cell gene expression and metabolism. What drives these changes is not well understood. We aimed to explore fat cell epigenetics, i.e., DNA methylation, as one mediator of gene regulation, in obese women. The
David M Snider et al.
PloS one, 10(3), e0118954-e0118954 (2015-03-27)
Rising concentrations of nitrous oxide (N2O) in the atmosphere are causing widespread concern because this trace gas plays a key role in the destruction of stratospheric ozone and it is a strong greenhouse gas. The successful mitigation of N2O emissions
Sabine Vettorazzi et al.
Nature communications, 6, 7796-7796 (2015-07-18)
Acute lung injury (ALI) is a severe inflammatory disease for which no specific treatment exists. As glucocorticoids have potent immunosuppressive effects, their application in ALI is currently being tested in clinical trials. However, the benefits of this type of regimen
Roberto Sommariva et al.
Environmental science & technology, 46(19), 10429-10437 (2012-06-05)
We used a one-dimensional model to simulate the chemical evolution of air masses in the tropical Atlantic Ocean, with a focus on halogen chemistry. The model results were compared to the observations of inorganic halogen species made in this region.
K S Carslaw et al.
Nature, 503(7474), 67-71 (2013-11-10)
The effect of anthropogenic aerosols on cloud droplet concentrations and radiative properties is the source of one of the largest uncertainties in the radiative forcing of climate over the industrial period. This uncertainty affects our ability to estimate how sensitive

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