Link to: www.balloon.co.uk email: b@lloon.com
Link to: www.balloon.co.uk email: b@lloon.com
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Balloons and gas cylinders come in various sizes. Please call us to discuss your requirement.
'V' Size cylinder inflates 110 balloons - £46.80 +vat
'T' Size cylinder inflates 220 balloons - £66.38 +vat
'L' Size cylinder inflates 650 balloons - £104.68 +vat
Delivery & Collection in mainland UK - £30.63 +vat
Click here for Disposable Helium Balloon gas cylinder .jpg)
Prices include filling kit hire. Please note a refundable deposit of £100 cash will be required for each cylinder hired (not disposable cylinder). Damage to cylinder or filling kit may result in loss of deposit. Other information from BOC:
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Helium was first discovered by means of the spectroscope in the sun's stmosphere. The discovery, made in 1868 by the strronomer Sir Norman Lockyer, was followed in 1885 by Sir William Ramsay's proof that the element existed on earth. He found it in the uranium ore, clevite.
Later it was established that helium is formed by the radioactive decay of many elements which emit a-particles (nuclei of helium atoms) and is contained in all radioactive minerals.
The largest source of helium is natural gas, the richest in helium being the gas from certain wells in Utah, USA. Next to hydrogen, helium is the lightest gas known, has a lifting power equal 92% of hyrogen and the advantage that it is inert and non-inflammable.
Helium is used for the inflation of airships, latex balloons and also for cooling. Ordinary air contains 1 part in 200,000 of helium. It was the last gaseous element to be liquefied, this being achieved by Omnes in 1908 in Leyden. Liquid helium has many remarkable properties only imperfectly understood. As as being scientifically fascinating it is indispensable in cryogenics (q.v) as a medium for cooling other substances to temperatures near absolute zero.
Hydrogen fusion in the "H bomb" produces helium.
HELIUM [helium] , gaseous chemical element; symbol He; at. no. 2; at. wt. 4.0026; m.p. below -272°C at 26 atmospheres pressure; b.p. -268.934°C at 1 atmosphere pressure; density 0.1785 grams per liter at STP ; valence usually 0.
Spectroscopic evidence for the presence of helium in the sun was first obtained during a solar eclipse in 1868. A bright yellow emission line was observed and was later shown to correspond to no known element; the new element was named by J. N. Lockyer and E. Frankland from helios [Gr.,=sun].
Helium was isolated (1895) from a sample of the uranium mineral cleveite by Sir William Ramsay. Properties and Isotopes Helium is less dense than any other known gas except hydrogen and is about one seventh as dense as air. Extremely unreactive, it is an inert gas in Group 18 of the periodic table . Natural helium is a mixture of two stable isotopes, helium-3 and helium-4. In helium obtained from natural gas about one atom in 10 million is helium-3. The unstable isotopes helium-5, helium-6, and helium-8 have been synthesized. The alpha particles that are emitted from certain radioactive substances are identical to helium-4 nuclei (two protons and two neutrons). Helium-4 is unusual in that it forms two different kinds of liquids. When it is cooled below 4.22°K (its boiling point at atmospheric pressure) it condenses to liquid helium-I, which behaves as an ordinary liquid. When liquid helium-I is cooled below about 2.18°K (at atmospheric pressure), liquid helium-II is formed. Liquid helium-II has a number of unusual properties. It is sometimes called a superfluid because it has extremely low viscosity. It also has extremely high heat conductivity and expands on cooling. It cannot be contained in an open beaker since a thin film of it creeps up the side, over the lip, and flows down the outside. The study of these phenomena is a part of low-temperature physics. When helium-3 is liquefied and cooled it does not exhibit the properties of liquid helium-II; this difference in properties between helium-3 and helium-4 can be explained in terms of quantum mechanics. Natural Occurrence and Preparation Helium is rare and costly. Wells in Texas (where the Federal Helium Reserve was established in 1925 near Amarillo), Oklahoma, and Kansas are the principal world source. Crude helium is separated by liquefying the other gases present in the natural gas; it is then either further purified or stored for later purification and use. Some helium is extracted directly from the atmosphere; the gas is also found in certain uranium minerals and in some mineral waters, but not in economic quantities. It has been estimated that helium makes up only about 0.000001% of the combined weight of the earth's atmosphere and crust; it is most concentrated in the exosphere, which is the outermost region of the atmosphere, 600-1500 mi (960-2400 km) above the earth's surface. Helium is abundant in outer space; it makes up about 23% of the mass of the visible universe. It is the end product of energy-releasing fusion processes in stars (see interstellar matter ). Uses Helium's noncombustibility and buoyancy (second only to hydrogen) make it the most suitable gas for balloons and other lighter-than-air craft. A mixture of helium and oxygen is often supplied as a breathing mixture for deep-sea divers and caisson workers and is used in decompression chambers; because helium is less soluble in human blood than nitrogen, its use reduces the risk of caisson disease, or the "bends." Helium can also be used wherever an unreactive atmosphere is needed, e.g., in electric arc welding, in growing crystals of silicon and germanium for semiconductors, and in refining titanium and zirconium metals. It is also used to pressurize the fuel tanks of liquid-fueled rockets. Liquid helium is essential for many low temperature applications
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