Ya Li Pear Yabbies Yacon Yadkin Blueberries Yak Yak -- Chauri Yak Butter Tea Yak Cheese Yak Cheese -- Rajya Metok Yaki-Imo Yaki -- Dondon Yaki -- Ebi Tama Yaki -- Gyu Tama Yaki -- Mikkusu Yaki -- Modan Yaki -- Monja Yaki -- Okonomi Yaki Dofu Yakimono Yakiniku Yakiniku Sauce Yakinori Yakitori Yakitori Sauce Yakko -- Hiya Yakumo Pear Yam -- Devil's Tongue Yam -- Japanese Mountain Yam -- White Guinea Yam -- Yellow Guinea Yam Bean Yam Cake Yam Noodles Yam Thread Noodles Yamagoboo Previous | Next | Perrier Water© Copyright 2009. All rights reserved and enforced![]() Perrier Water Perrier is a bottled mineral water. The water comes from a plain in Vergèze a small village in the south of France, 4 miles (7 kilometres) south-west of Nimes. The plain is surrounded by limestone rock hills. The water from precipitation percolates through the rock, down into a 130 foot (40 metre) deep aquifer under the plain, about 16 feet (5 metres) underground. Below the aquifer is carbonaceous rock which, through the natural heat of the earth, releases carbon dioxide gas that finds its way up into the aquifer pool and carbonates the water. The water continuously feeding into the aquifer forces the water up naturally in a spring. But, as the water reaches the surface, the carbon dioxide present in the water escapes from the water, leaving the water less carbonated again. Consequently, bottlers have drilled and installed pipes directly into the carbon dioxide producing rocks to a depth of approximately 1500 feet (450 meters.) The carbon dioxide is extracted through the pipes, then combined under pressure with the water at time of bottling in the plant. The combination of the carbon dioxide and water happens at strictly controlled levels, giving an artificial consistency of production. The gas has to be filtered first, because it contains trace hydrocarbons (specifically, benzene), as well as hydrogen sulphide, argon, ethane, helium, methane, neon, nitrogen, propane, and toluene. Because the carbon dioxide is now being drawn off artificially, that means that there is less to rise naturally into the water in the aquifer.
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