What kind of mine spring water is delicious now?

Of course, Cestbon is delicious, don't you say?

Remember.

Is there any good or bad mineral water, I drink everything, I just know that my favorite drink is Farmer's Orchard, haha.

The difference between mountain spring water and mineral water is:The water source is different.

Mountain spring water is generally surface water, which is the surface water of mountain streams, rivers, small pools, lakes and other mountain bodies. Mainly in rainwater, mountain springs, or rivers and streams that pass by locally or in other places.

Mineral water is generally groundwater. Mineral water is unpolluted underground mineral water that springs naturally from deep underground or is artificially exposed; Contains a certain amount of mineral salts, trace elements or carbon dioxide gas; Under normal circumstances, its chemical composition, flow rate, water temperature and other dynamics are relatively stable within the natural fluctuation range.

High-quality mountain spring water has seven characteristics:

1.The water quality is zero pollution, and there is no human living area within the hectare with the water source as the center.

2.The degree of mineralization is moderate, and the human body will not burden metabolism after drinking.

3.The total organic carbon and total phosphorus content in the water source is less than 1 mg l (the main source of pollution from bottled water algae outbreaks).

4.Natural low deuterium water.

5.It is rich in natural trace elements, and the proportion is balanced, and no one is too high.

6.Naturally weakly alkaline. It's stupid.

7.Structured small molecule clusters (clusters) of water, half width of 50-70 Hz.

1. Clear spring water.

2. Sweet spring water.

3. Cool spring water.

4. Sparkling spring water.

5. Clean spring water.

Dam water "Dam water" is similar to a pond, that is, digging a size not.

1. The water pits of different depths are introduced into the canal water and snow water, and the daily drinking water of people and livestock depends on it.

For herders who have been living on the edge of the Gobi desert for a long time, it is not easy to get water, and many people need to come back from far away on donkey carts. Therefore, whenever there is a heavy rain or a flood in the mountains, the locals will introduce water into these big pits and store it, and for many years, people in Xinjiang have survived in this way.

However, due to the fact that the water is a stagnant pool, stored for a long time, and shared by people and livestock, the local people in the past lacked awareness of protection and hygiene, and many of them were infected with intestinal diseases. There are bloated bellies, there are big necks, but poverty and technical conditions limit people's imagination.

Not only the locals have drunk this water, but the oil people who have been fighting here for a long time have also drunk it more than once, there were many exploration team members, when they were separated from the camel team, the Gobi Desert, there was no supply, they pounced on the water when they saw it, and they drank it, and they didn't care about the impurities on it, and even floated the feces of the auspicious cover.

Pond. Groundwater

Many people have drunk groundwater, but the salty and bitter groundwater is rarely drunk. For example, the drilling team in the northern part of Tarim in Xinjiang must drill a water well before drilling an oil well for use in drilling operations and slurry. Someone once drank it, diarrhea and abdominal pain were common.

In addition to the Gobi Desert, there is also Jiashi County in Xinjiang, the melon in Jiashi County is very famous, but in the 70s of the last century, many surveys and wells were drilled, and still no drinking water in line with national regulations was found.

Therefore, the main drinking water of people in that era was the water in the canal, which was not only people's drinking water, but also domestic water such as washing and laundry. In the summer, agricultural irrigation water and drinking water are the same route, crops and people grab water, and people downstream wait for that bowl of water in their lives. And the waterlogged dam has long been empty if there is no water source, and it is a blessing to want to drink the water of the waterlogged dam with insects.

In the 90s of the last century, most of these areas were equipped with water stations and hygienic groundwater.

Water station. Tap water

Nowadays, the people of Xinjiang not only drink sanitary water, but also drink healthy water, and the treated tap water completely solves the problem of high salinity of local water quality, from waterlogging dam water to groundwater, and then to tap water, which is the three qualitative leaps in the life of Xinjiang people.

So, when you ask the local elders what kind of water is the best, they will tell you with a smile that the tap water at home is the best.

So, dear friends, when you come to Xinjiang for tourism, you can drink the tap water brought by the villagers, it is the same as in the city!

1. Atmospheric precipitation.

Bai seepage underground along the slope of the rock strata

flow, blocked by intrusive zhi rock mass, under pressure.

DAO water outcrops the surface to form back-spring water.

2. Why doesn't the spring water infiltrate and form underground undercurrents and surface runoff?

In the long geological time, the soluble limestone has undergone many tectonic movements and long-term dissolution, and the karst landform has developed, forming a large number of karst ditches, karst holes, karst caves and underground dark rivers, etc., which together form a vein-like underground network that can store and transport groundwater.

3. What is the ** of underground spring water?

In the places where limestone outcrops and fissure karst develop, a large amount of atmospheric precipitation and surface runoff are absorbed, and abundant fissure karst water is formed by seeping into the ground. These fractured karst waters, blocked by the Archean metamorphic rocks, move horizontally to the north along the direction of the rock stratum, forming underground undercurrents, and encountering the obstruction and fault interception of intrusive rock masses.

4. Where does the pressure come from?

Under the strong hydrostatic pressure, the groundwater passes through the karst fissures, grabs the ground in the contact zone between the limestone and the intrusive rock mass and the weak part of the Quaternary sedimentary layer, gushing out of the surface and forming a natural spring.

5. Is the spring water inexhaustible?

The amount of precipitation, the amount of extraction and the seasonal distribution also have a direct impact on the changes in the spring water.

There are many different reasons for the formation of mountain spring water

1.Rain, fog, and seep out of the sky through the soil (this mountain spring is intermittent).

2.Artesian springs with groundwater backflow rights are generally found in low-lying areas (such springs last for a long time and flow non-stop).

3.Alpine glacial meltwater generally increases when the temperature rises, and the intermittent flow depends on the height and morphology of the mountain and changes in the surrounding environment. ）

If it's a song, it's Xiangxiang's "Spring Water".

Song: Spring Water.

Singer: Xiang Xiang.

Lyrics Composer: Mao Hui.

The spring water used to be a drop of dew in the jar of yang fat jade shins.

It takes away the temperature of forests, rivers, mountains, and rivers.

It's invisible, indifferent and ruthless, pretending not to care.

One day, it will be with the rivers and lakes.

The head of the spring water does not return to the natural simplicity.

People who have drunk forget their worries and go vegetarian from now on.

It's pure and colorless, light and tasteless, and it's a godsend.

How many people have abandoned it.

Flowing through the end of the world, the pine welcomes guests, and the gods also stop.

Stay under the tree for three years, all day long, but no winner or loser.

It flows to the east of the sea and the south of the Yangtze River, and cultivates the West Lake.

Only then did Yang Liu Yiyi's lover return.

Look into your eyes and talk about don't come to the bitterness.

The spring water used to be a pot of wine left over from Li Bai's drinking.

The acid that makes vinegar can't solve the feelings of love and hate.

If someone remembers the knife and cuts off the water, the water still flows.

Flowing to the end of the world, escaping from the tiger's mouth, the world is free to roam.

Fairy Ling Bo took a slight step, Luo shirt fluttered, and he turned back in ten steps.

Shedding funeral flowers with tears Several degrees of reincarnation Where is the Red Mansion.

Only then can there be a thousand catties of family letters.

It is expected that the lady is waiting at the door every day.

How to understand who bears it silently.

Flowing to the end of the world, escaping from the tiger's mouth, the world is free to roam.

Fairy Ling Bo took a slight step, Luo shirt fluttered, and he turned back in ten steps.

Shedding funeral flowers with tears Several degrees of reincarnation Where is the Red Mansion.

Only then can there be a thousand catties of family letters.

It is expected that the lady is waiting at the door every day.

Definition of spring: groundwater gushing out of a crack in a rock or from the ground.

According to the difference in the flow of spring water from the ground, it can be divided into descending spring and rising spring; According to the temperature of the spring water, it can be divided into hot springs, cold springs, and ordinary springs.

Water that comes from groundwater or has been filtered through the surface layer is generally clean and cool.

Spring water: It is formed by the atmospheric precipitation seepage underground flow along the inclined direction of the rock layer, blocked by the intrusive rock mass, and the confined water outcrops the surface.

泉水 [quán shuǐ].

A spring is a place where groundwater naturally outcrops to the surface, or where an underground aquifer is exposed to the surface. Depending on the water flow conditions, it can be divided into geysers and perennial springs. If there is no significant flow of water after the groundwater is exposed to the surface, it is called seepage.

Depending on the temperature of the water flow, springs can be divided into hot springs and cold springs. Springs can be classified into eight levels according to their flow rates, with Class I springs having flows of more than 100 cubic feet (2,800 liters) per second, Class II springs having flows between 10 and 100 cubic feet per second, and Class 8 springs flowing less than 1 pint per minute (8 milliliters per second).