Traditional Culture Encyclopedia - Traditional festivals - Is Nongfusanquan mineral water in the true sense of the word?

Is Nongfusanquan mineral water in the true sense of the word?

Nongfushanquan is mountain spring water, and there is no difference between mineral water in the traditional sense.

Some people will feel the sweetness after drinking Nongfushanquan, so Nongfushanquan is mineral water, in this case, many people tend to think that Nongfushanquan is mineral water, but in fact, not, because Nongfushanquan water belongs to the natural weak alkaline water, is not a real mineral water, the two concepts are still very different, so Nongfushanquan is mineral water, so Nongfushanquan is mineral water. The first thing you need to do is to get a good understanding of how to use it.

Generally speaking, natural water is the use of natural high-quality water as raw water, and then processed, which maximizes the retention of natural minerals in the water, so the general quality of water is weak alkaline. And mineral water refers to the natural emergence from the depths of the ground or by artificial exposure of uncontaminated underground mineral water.

Benefits of mountain spring water

As the name suggests, it is the water taken out of the mountain spring containing minerals, but this spring water is not ordinary spring water. Mountain spring water, generally from the formation of special geological conditions due to the formation of good deep ecological environment, after decades, centuries, thousands of years or even tens of thousands of years of deep circulation and a series of very complex process.

Filtered through the earth's crust, flowing through a variety of strata, absorbing a large number of trace elements and minerals, in general, its chemical composition, flow rate, water temperature and other dynamic indicators in the natural cycle fluctuations in the range of relatively stable. Mountain spring water in the high temperature, high pressure and water vapor expansion effect, along the crustal fissure transport rise, and finally gushed out of the surface formation.