S.Pellegrino
 |
|
| Country | Italy |
|---|---|
| Source | San Pellegrino Terme |
| Type | Sparkling |
| pH | 5.6 |
| Calcium (Ca) | 164 |
| Chloride (Cl−) | 49.4 |
| Bicarbonate (HCO3) | 243 |
| Fluoride (Fl) | 0.5 |
| Lithium (Li) | 0.2 |
| Magnesium (Mg) | 49.5 |
| Nitrate (NO3) | 2.9 |
| Potassium (K) | 2.2 |
| Silica (SiO2) | 7.1 |
| Sodium (Na) | 31.2 |
| Strontium (Sr2) | 2.7 |
| Sulfates (SO4) | 402 |
| TDS | 854 |
| Website | www.SanPellegrino.com |
| All values in milligrams per liter (mg/l) | |
S.Pellegrino is an Italian brand of mineral water and assorted real-fruit sodas, owned by the company Sanpellegrino S.p.A., whose production plant is located in San Pellegrino Terme in the Province of Bergamo, Lombardy, Italy. Sanpellegrino S.p.A. has been part of Nestlé since 1997 and its products are exported to most countries in Europe, the Americas, Australasia and the Middle East, as well as Japan, Taiwan and Hong Kong.
S.Pellegrino has ten production sites in Italy including at its headquarters. Furthermore, more than 1,850 people work in the company. It also manages other brands like Vera, Levissima and Acqua Panna, and its revenue, according to the balance sheet of the year 2016, amounts to 895 million euros, about 96 million euros less than the previous year. 50,000 bottles of water are produced every hour in the San Pellegrino's plant, for a total amount of one million bottles a day including soft drinks, sparkling water and cocktails. The bottles are then sorted to be imported in major countries around the world.
In 2005, five hundred million bottles were sold globally. In 2017, that number had increased to one billion bottles.
San Pellegrino mineral water is produced in San Pellegrino Terme. The water may originate from a layer of rock 400 metres (1,300 ft) below the surface, where it is mineralized from contact with limestone and volcanic rocks. It emerges from three deep springs at a temperature of about 22 °C (72 °F). The springs are located at the foot of a dolomite mountain wall which favours the formation and replenishment of a mineral water basin. The water then seeps to depths of over 700 m (2,300 ft) and flows underground to a distant aquifer.
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