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重要文件

41624

Sigma-Aldrich

二甲基硫醚

puriss., ≥99.0% (GC)

同義詞:

DMS, 甲硫醚

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About This Item

線性公式:
(CH3)2S
CAS號碼:
分子量::
62.13
Beilstein:
1696847
EC號碼:
MDL號碼:
分類程式碼代碼:
12352100
PubChem物質ID:
暫時無法取得訂價和供貨情況

蒸汽密度

2.1 (vs air)

蒸汽壓力

26.24 psi ( 55 °C)
7.79 psi ( 20 °C)

等級

puriss.

化驗

≥99.0% (GC)

形狀

liquid

自燃溫度

402 °F

expl. lim.

19.7 %

折射率

n20/D 1.435 (lit.)
n20/D 1.435

bp

38 °C (lit.)

mp

−98 °C (lit.)

溶解度

H2O: soluble 7.28 g/L at 20 °C

密度

0.846 g/mL at 25 °C (lit.)

儲存溫度

2-8°C

SMILES 字串

CSC

InChI

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

InChI 密鑰

QMMFVYPAHWMCMS-UHFFFAOYSA-N

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產品號碼
描述
訂價

象形圖

Flame

訊號詞

Danger

危險聲明

危險分類

Flam. Liq. 2

儲存類別代碼

3 - Flammable liquids

水污染物質分類(WGK)

WGK 1

閃點(°F)

-32.8 °F - closed cup

閃點(°C)

-36 °C - closed cup

個人防護裝備

Eyeshields, Faceshields, Gloves


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分析證明 (COA)

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Nguyen BC, et al.
Marine Chemistry, 133-141 (1988)
B P Lomans et al.
Applied and environmental microbiology, 65(8), 3641-3650 (1999-07-31)
A newly isolated methanogen, strain DMS1(T), is the first obligately anaerobic archaeon which was directly enriched and isolated from a freshwater sediment in defined minimal medium containing dimethyl sulfide (DMS) as the sole carbon and energy source. The use of
Sheree Yau et al.
The ISME journal, 7(10), 1944-1961 (2013-04-27)
Organic Lake is a shallow, marine-derived hypersaline lake in the Vestfold Hills, Antarctica that has the highest reported concentration of dimethylsulfide (DMS) in a natural body of water. To determine the composition and functional potential of the microbial community and
Hayley E Arnold et al.
Global change biology, 19(4), 1007-1016 (2013-03-19)
The production of the marine trace gas dimethyl sulfide (DMS) provides 90% of the marine biogenic sulfur in the atmosphere where it affects cloud formation and climate. The effects of increasing anthropogenic CO2 and the resulting warming and ocean acidification
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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