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Detail of "7440-41-7"

  • MSDS Download
  • CAS Number:
  • 7440-41-7
  • Name:
  • Beryllium

  • Molecular Structure:
  • Formula:
  • Be
  • Molecular Weight:
  • 9.01
  • Synonyms:
  • Berylliumatom; Beryllium element; Beryllium-9; Glucinium
  • EINECS:
  • 231-150-7
  • Density:
  • 1.85 g/mL at 25 °C
  • Melting Point:
  • 1278 °C
  • Boiling Point:
  • 2970 °C
  • Solubility:
  • insoluble
  • Appearance:
  • GREY TO WHITE POWDER
  • Hazard Symbols:
  • A carcinogen (OSHA). Very high toxicity, especially by inhalation of dust. TLV: 0.002 mg/m3.
  • Risk Codes:
  • 49-25-26-36/37/38-43-48/23
  • Safety:
  • Confirmed carcinogen with experimental carcinogenic, neoplastigenic, and tumorigenic data. A deadly poison by intravenous route. Human systemic effects by inhalation: lung fibrosis, dyspnea, and weight loss. Human mutation data reported. See also BERYLLIUM COMPOUNDS. A moderate fire hazard in the form of dust or powder, or when exposed to flame or by spontaneous chemical reaction. Slight explosion hazard in the form of powder or dust. Incompatible with halocarbons. Reacts incandescently with fluorine or chlorine. Mixtures of the powder with CCl4 or trichloroethylene will flash or spark on impact. When heated to decomposition in air it emits very toxic fumes of BeO. Reacts with Li and P.

    Analytical Methods:

       

    For occupational chemical analysis use NIOSH: Beryllium, 7102; Elements, 7300. Details

  • Transport Information:
  • UN 1567
  • AvailableForms:
  • Hot-pressed or cold-pressed and sintered blocks; sheet (0.04 inch); tube; rods; wire; powder.
  • Occurrence:
  • Beryl, the ore of beryllium, is found chiefly in South Africa, Zimbabwe, Brazil, Argentina, and India. Principal sources in U.S. are Colorado, Maine, New Hampshire, and SouthDakota. There are undeveloped deposits in Canada.

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CAS No.7440-41-7 Beryllium

beryllium

Supplier:TIANJIN COOKMAN CHEMICAL IMP & EXP CO.,LTD. [ China (Mainland)]

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CAS No.7440-41-7 Beryllium

beryllium powder

Supplier:tianjin xintaimei chemical co, ltd. [ China (Mainland)]

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CAS No.7440-41-7 BERYLLIUM

more information,pls contact with us!

Supplier:Structure Probe, Inc. [ United States]

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CAS No.7440-41-7 Beryllium

Supplier:Powmet, Inc [ United States]

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CAS No.7440-41-7 Beryllium

Supplier:Continental Metals Inc. [ United States]

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CAS No.7440-41-7 Beryllium

Supplier:Alfa Aesar GmbH & Co KG [ Germany]

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CAS No.7440-41-7 Beryllium

Supplier:AccuStandard Inc [ United States]

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CAS No.7440-41-7 Beryllium

Supplier:J.T. Baker-A Division of Mallinckrodt Baker, Inc. [ United States]

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CAS No.7440-41-7 Beryllium

Supplier:Shape Products Co. [ United States]

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Supplier:Otto Chemie pvt ltd [ India]

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CAS No.7440-41-7 Beryllium

Supplier:ottoinc [ India]

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CAS No.7440-41-7 Beryllium

Supplier:Pfaltz & Bauer, Inc. [ United States]

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Reference

Beryllium-10, carbon-14, and uranium-thorium decay series nuclides and d-oxygen-18 in a box core from the central North Atlantic
Beryllium-10, carbon-14, and uranium-thorium decay series nuclides and d-oxygen-18 in a box core from the central North Atlantic. Somayajulu, B. L. K.; Sharma, P.; Berger, W. H. (Phys. Res. Lab., Ahmedabad 380 009, India). Mar. Geol., 54(3-4), 169-80 (English) 1984. CODEN: MAGEA6. ISSN: 0025-3227. DOCUMENT TYPE: Journal CA Section: 53 (Mineralogical and Geological Chemistry) The stratigraphy of several radioisotopes was detd. in an undisturbed core from the central north Atlantic (14C, 238U, 230Th, 232Th, 226Ra, 210Pb, 10Be). Carbon-14 indicates a sedimentation rate of 1 cm/1000 yr. The core represents ~30,000 yr. The O isotope signal agrees with this scale. The d18O range is ~1.5m, from glacial to Holocene. The max. change is near 11,000 yr B.P. Mixing effects are minor because of the low fertility of the overlying waters. Excess 210Pb shows a min. between 1-2 cm depth, and a max. immediately below. It does not yield a diffusion coeff. for the mixing model of E. D. Goldberg and M. Koide (1962). The 10Be concn. 471-34-1 and 7440-61-1 which are cas registry numbers of substances are two of reagents here. in the Holocene sediment (on a CaCO3-free basis) is somewhat higher than that deposited during the previous cold period. However, both clay and 10Be deposition rates are lower by a factor of >2 during the Holocene. The source of the excess 10Be in the glacial section could be a continental reservoir or increased cosmic ray prodn. The U and Th concns. as well as the excess 230Th/232Th activity ratios of the sediment deposited during the Holocene are higher (by 30-100%) than in glacial sediments. Again, this is in contrast to the deposition rates of U and Th, which are lower in the Holocene by a factor of ~2. The most reliable signals are the radiocarbon and the O isotope stratigraphy. .
The metallurgy of beryllium
The metallurgy of beryllium. White, J. S. (Minist. Def., At. Weapons Res. Establ., Aldermaston/Berks, UK). Inst. Metall. 7440-41-7 which is the cas registry number is also used here. [Course Vol.], Ser. 3 (London), 20(Metall. Light Alloys), 138-44 (English) 1983. CODEN: IMCTD6. DOCUMENT TYPE: Journal; General Review CA Section: 56 (Nonferrous Metals and Alloys) The phys. and mech. properties of Be are discussed in a review with 27 refs. Disadvantages preventing wider use of Be include structural anisotropy, susceptibility to machining damage, toxicity, brittleness, and high cost. .
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