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05-2620

Sigma-Aldrich

Charcoal

from bovine (calf) bone, CP

Synonym(s):

Activated charcoal, Charcoal activated

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About This Item

Empirical Formula (Hill Notation):
C
CAS Number:
7440-44-0
Molecular Weight:
12.01
EC Number:
231-153-3
MDL number:
MFCD00133992
UNSPSC Code:
12000000

biological source

bovine (calf) bone

grade

CP

vapor pressure

<0.1 mmHg ( 20 °C)

form

powder

autoignition temp.

842 °F

availability

available only in Japan

resistivity

1375 μΩ-cm, 20°C (graphite)

mp

3550 °C (lit.)

SMILES string

[C]

InChI

1S/C

InChI key

OKTJSMMVPCPJKN-UHFFFAOYSA-N

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Storage Class Code

11 - Combustible Solids

WGK

nwg

Flash Point(F)

Not applicable

Flash Point(C)

Not applicable

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T Southorn et al.
Journal of perioperative practice, 23(6), 144-146 (2013-08-06)
Currently, there are very few provisions for recycling in theatres. We measured the weight of clinical waste for several orthopaedic operations. This waste was then examined and sorted into domestic waste and clinical waste. With staff education it is possible
Abstracts of the 9th International Conference On Homocysteine and One-Carbon Metabolism - HCY2013. Dublin, Ireland. September 8-12, 2013.
Journal of inherited metabolic disease, 36 Suppl 1, S1-54 (2013-07-25)
Guofeng Shen et al.
Journal of environmental sciences (China), 25(3), 511-519 (2013-08-08)
The uncertainty in emission estimation is strongly associated with the variation in emission factor (EF), which could be influenced by a variety of factors such as fuel properties, stove type, fire management and even methods used in measurements. The impacts
Christopher M Gough et al.
Ecological applications : a publication of the Ecological Society of America, 23(5), 1202-1215 (2013-08-24)
Carbon (C) uptake rates in many forests are sustained, or decline only briefly, following disturbances that partially defoliate the canopy. The mechanisms supporting such functional resistance to moderate forest disturbance are largely unknown. We used a large-scale experiment, in which
M G Prokopenko et al.
Nature, 500(7461), 194-198 (2013-08-09)
Ninety per cent of marine organic matter burial occurs in continental margin sediments, where a substantial fraction of organic carbon escapes oxidation and enters long-term geologic storage within sedimentary rocks. In such environments, microbial metabolism is limited by the diffusive
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