すべての画像(2)
About This Item
実験式（ヒル表記法）:
C
CAS番号:
分子量:
12.01
MDL番号:
UNSPSCコード:
12141908
PubChem Substance ID:
NACRES:
NA.23
蒸気圧
<0.1 mmHg ( 20 °C)
アッセイ
100%
形状
rod
自己発火温度
842 °F
メーカー／製品名
Goodfellow 809-013-12
抵抗性
1375 μΩ-cm, 20°C (graphite)
サイズ直径
150 mm × 13.0 mm
mp
3550 °C (lit.)
SMILES記法
[C]
InChI
1S/C
InChI Key
OKTJSMMVPCPJKN-UHFFFAOYSA-N
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詳細
For updated SDS information please visit www.goodfellow.com.
法的情報
Goodfellow製品
保管分類コード
13 - Non Combustible Solids
WGK
nwg
引火点(°F)
Not applicable
引火点(℃)
Not applicable
試験成績書（COA）
製品のロット番号・バッチ番号を入力して、試験成績書（COA） を検索できます。ロット番号・バッチ番号は、製品ラベルに「Lot」または「Batch」に続いて記載されています。
B Franz Lang et al.
Proceedings of the National Academy of Sciences of the United States of America, 111(16), 5926-5931 (2014-04-09)
Programmed translational bypassing is a process whereby ribosomes "ignore" a substantial interval of mRNA sequence. Although discovered 25 y ago, the only experimentally confirmed example of this puzzling phenomenon is expression of the bacteriophage T4 gene 60. Bypassing requires translational
Clarissa Gillmann et al.
International journal of radiation oncology, biology, physics, 88(5), 1136-1141 (2014-03-26)
To compare the relative biological effectiveness (RBE)-weighted tolerance doses for temporal lobe reactions after carbon ion radiation therapy using 2 different versions of the local effect model (LEM I vs LEM IV) for the same patient collective under identical conditions.
Elson C Santos et al.
Journal of nanoscience and nanotechnology, 14(6), 4590-4594 (2014-04-18)
The system proposed consists of a flagellum relaxing around a static carbon nanowire to mimics behavior of a natural flagellum moving with damped harmonic motion along a wire under van der Waals and electrostatic forces. This flagellum is composed of
Marshall W Bowles et al.
Science (New York, N.Y.), 344(6186), 889-891 (2014-05-09)
Sulfate reduction is a globally important redox process in marine sediments, yet global rates are poorly quantified. We developed an artificial neural network trained with 199 sulfate profiles, constrained with geomorphological and geochemical maps to estimate global sulfate-reduction rate distributions.
I Tanya Handa et al.
Nature, 509(7499), 218-221 (2014-05-09)
The decomposition of dead organic matter is a major determinant of carbon and nutrient cycling in ecosystems, and of carbon fluxes between the biosphere and the atmosphere. Decomposition is driven by a vast diversity of organisms that are structured in
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