How are mountain springs formed? How mountain spring water is generated

Atmospheric precipitation seeps underground flows in the inclined direction of the rock layer, and when blocked by the intrusive rock mass, the confined water is exposed to the surface and forms a spring.

First, 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.

Second, 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.

Third, where does the pressure from the spring water 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.

Fourth, 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.

The soil absorbs most of the water when it rains, and the water seeps into the mud and then collects on the catchment line below the ground, so there will be streams in the valleys in the mountains, and as for some stones, the water will seep out again, and it will disappear when there is a drought.

If you are interested, you will learn it in high school geography.

Generally speaking, there is more water in the mountains in the spring, why, because the snow in winter turns into water and flows down after the spring flowers bloom.

But why are there mountain springs in the summer? Because there are trees on the mountain, trees can maintain water and soil, so that when the temperature is low at night and high during the day, some groundwater will seep out, and there are caves on the mountain, which are dark and damp, and will also become the ** of mountain springs.

Generally speaking, there will be no mountain springs on bare mountains, thank you.

Because Nongfu Spring is a little sweet!

Sun Zhi Fuping830 1 minute ago.

The source system of natural mountain spring water seems to be rainwater, but.

In fact, it is "rootless water" – there is no actual source of water. Because the rain comes from the "chaotic clouds" in the sky. The term "turbulent clouds" refers to clouds that are raised by water vapor from different grounds.

Therefore, when the clouds pre-cool and gather to form rain (snow) falling on the ground of a certain place, this rain has no specific source, so it is broadly called "rootless water". However, there is a difference between the "rootless water" referred to here and the "rootless water" in the narrow sense of "medicine introduction" in ancient times, and only the rain in a specific season and solar term is the "rootless water" that can be used as a "medicine introduction" "Sun Gong".

The formation of natural mountain spring water is actually rainwater falling on the mountain, hoarding low-lying places of various sizes, and then seeping into the rocks or flowing from the top to the bottom through cracks, in the process some of which are purified by the rocks, incorporated into different rock compositions, some through the "open channel" entrainment of debris along the way, or both. As a result, a variety of "mountain springs" have been formed at the springs. "Sun Gong".

Since the spring water is made up of rainwater, which in turn is formed by the clouds formed by the water vapor from the ground rising to the sky, the water quality is pure water quality when air pollution (haze) is removed, and the clouds are actually a "reservoir of pure water in the air".

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

2. Artesian springs with backflow of underground water are generally seen in low-lying places (this kind of spring lasts for a long time and will flow non-stop).

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

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

2. Artesian springs with groundwater backflow can generally be seen in low-lying places (this kind of spring water lasts for a long time and will flow non-stop).

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

Hello dear, I am the respondent who provides you with this service, and I am very happy to meet you. Mountain spring water is the water spring that is obtained by the natural environment purification in the mountain after the atmosphere is trapped and contains precipitation, and some will flow along the inclined direction of the rock layer through the seepage underground, and the confined water will be exposed to the surface of the intrusion rock mass to form a spring.

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

2. Artesian springs with groundwater backflow can generally be seen in low-lying places (this kind of spring water lasts for a long time and will flow non-stop).

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

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. ）

At the foot of the mountain, the cliff wall (most of the condensate), the amount of water is very large, it is really difficult to say whether these are mountain springs, most of them are not authentic.

Authentic mountain springs. Mid-mountain water.

2.The top of the hill is uninhabited (to avoid domestic sewage infiltration).

3.The amount of water is small and stable all year round. Most of them are not as big as your tap.

4.Constant temperature, roughly 13 degrees, plus or minus one or two degrees.

5.Super clear, no moss and slippery stones near the outlet.

This water is mainly dependent on rainfall, including partial condensation (the soil on the top of the mountain absorbs dew and water vapor). The water enters the soil from the top of the mountain, and then enters the rocks under the soil, and gradually filters the water from the middle of the mountain, and the process is mineralized by the stones.

Analyze the elements one by one:

The water from the low place cannot be guaranteed not to contain the ground gushing water, whether it is a mountain spring or a mineral spring is difficult to say, the probability is greater most of the local seepage, the quality is not too high.

Not to mention that there is a residential area on the top of the mountain, domestic sewage infiltration and sanitation may not be guaranteed.

The amount of water is small and stable all year round. Ironclad evidence proves the stability of this water purification system, and it is also the best proof of water. Some of the mountains are very large, but in fact, the water is more of a fissure, and the direct current component is large, and the purification is not enough, so he can appear in the form of a large amount of water, of course, most of them are quite clean, but most of them are a little muddy after entering the pool.

Constant temperature, because he comes out of the inside of the mountain, the north is mostly 13 degrees, because the cold and warm on the earth are all near the surface, and the inside of the mountain is actually always at a constant temperature. If it is not for this temperature, one is suspected that there is no surface runoff upstream from the source, and the second is that it is only local water seepage, so the temperature is not too standard, and the quality of local water seepage is of course much worse, including the condensate of the cliff wall.

As I mentioned earlier, most of the water that comes out of the mid-mountain is slightly turbid, and the water only becomes clear when it flows a few dozen meters away. What does it mean? While most of them are clean, it is clear that the infiltration filtration is not thorough enough.

The mountain spring that meets the most standard conditions is super clear, it does not have the conditions for moss growth, and trace elements are not enough to become the elements of moss growth. It means that the water is clear and there are no fish.

For example, some are a mile or two away from the reservoir, and the water from the reservoir is filtered out after the rocks, and some are also very clear and about 13. It is said that the water quality is clear for a long time is the best proof, and the more advanced is that the water flow is even inferior to the faucet is ultra-clean and perfectly mineralized, high-quality mountain spring.

If the temperature is not standard, most of them are not really high-quality springs, and the water formation process or filtration process is flawed.

It is groundwater that appears on the surface for various reasons.