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Key Documents

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699624

Sigma-Aldrich

Graphite

nanopowder, graphitized, less than 250 ppm Al, Ti, Fe, Ni, Cu, and Zn combined

Sinónimos:

Carbon, mesoporous, Graphite nanoparticles

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About This Item

Fórmula empírica (notación de Hill):
C
Número de CAS:
1333-86-4
Peso molecular:
12.01
EC Number:
231-955-3
MDL number:
MFCD00133992
UNSPSC Code:
12352302
PubChem Substance ID:
329762148
NACRES:
NA.23

Quality Level

100

form

nanopowder

surface area

50-100 m2/g

pore size

0.25 cm3/g pore volume (typical)
137 Å average pore diameter (typical)

bp

4827 °C

mp

3654-3697 °C

density

1.828 g/cm3 (absolute, typical)

bulk density

0.075 g/cm3

SMILES string

[C]

InChI

1S/C

InChI key

OKTJSMMVPCPJKN-UHFFFAOYSA-N

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General description

Surface area of the graphitized mesoporous carbon was determined to be 77 m2/g. These are highly pure graphitized, porous carbon nanoparticles. Particles have large mesopores and some microporosity. Graphite lattice structure content of approximately 10%. An agglomeration of 30 nm mesoporous nanoparticles (TEM).

Application

The cytotoxic effects of graphitized carbon mesoporous nanopowder and multiwalled carbon nanotubes (MWNTs) was compared on human airway epithelium. Mesoporous carbon was found to have no effect on the epithelium cell morphology.

Storage Class

11 - Combustible Solids

wgk_germany

nwg

flash_point_f

Not applicable

flash_point_c

Not applicable

ppe

dust mask type N95 (US), Eyeshields, Gloves

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Certificados de análisis (COA)

Lot/Batch Number
SHBQ4228
SHBQ4227
SHBQ4226
SHBQ4225
SHBQ4224

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Graphite powder, <20 μm, synthetic

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282863

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NIST2451

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NIST2975

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Sigma-Aldrich

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Graphite powder, <150 μm, 99.99% trace metals basis

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496588

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Multiwalled carbon nanotubes induce altered
morphology and loss of barrier function in human
bronchial epithelium at noncytotoxic doses
Snyder RJ, et al.
Nanomedicine (London, England), 9, 4093-4105 (2014)
Tegan N Lavoie et al.
Environmental science & technology, 49(13), 7904-7913 (2015-07-08)
We report measurements of methane (CH4) emission rates observed at eight different high-emitting point sources in the Barnett Shale, Texas, using aircraft-based methods performed as part of the Barnett Coordinated Campaign. We quantified CH4 emission rates from four gas processing
Catharina Vendl et al.
The Journal of experimental biology, 218(Pt 21), 3425-3434 (2015-11-06)
Fundamental differences in methane (CH4) production between macropods (kangaroos) and ruminants have been suggested and linked to differences in the composition of the forestomach microbiome. Using six western grey kangaroos (Macropus fuliginosus) and four red kangaroos (Macropus rufus), we measured
Garvin A Heath et al.
Proceedings of the National Academy of Sciences of the United States of America, 111(31), E3167-E3176 (2014-07-23)
Recent technological advances in the recovery of unconventional natural gas, particularly shale gas, have served to dramatically increase domestic production and reserve estimates for the United States and internationally. This trend has led to lowered prices and increased scrutiny on
Kirsten Oswald et al.
PloS one, 10(7), e0132574-e0132574 (2015-07-21)
Lakes are a natural source of methane to the atmosphere and contribute significantly to total emissions compared to the oceans. Controls on methane emissions from lake surfaces, particularly biotic processes within anoxic hypolimnia, are only partially understood. Here we investigated
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