The atmosphere surrounds the planet earth with various gases, it also includes a gas called “oxygen” gas, which not only guarantees the life of all animate objects, but also has a great priority in the regeneration of non-animate objects, because during the chemical process of the earth’s crust, through the interconnection and closure of oxygen with other elements, four such non-animate material objects can be regenerated in the cosmic system. It has been declared as the main pillar, which includes normal oxides, basic oxides, acidic oxides and salts.

Collectively referred to as “oxides” which are directly or indirectly associated with non-living things on the earth’s surface, such as rocks, minerals and ores, as confirmed by geological surveys and chemical analysis, it is concluded that the axis and center of the earth’s chemistry is more or less centered around them, which regenerate valuable resources which in one way or another form the backbone of the industrial and economic development of modern society. is

Here, “oxides” refers to oxygen gas being highly reactive chemically (except for “obal gas” and volatiles halogen matecid) and it easily reacts with other elements and forms compounds of its two elements called oxides like other elements metals (metals are objects through which electricity can pass easily i.e. metals are good conductors of electricity) and non-metals (non-metals are objects through which electricity cannot pass). i.e. non-metals are poor conductors of electricity) with binary compounds called oxides.

When a hydrogen atom and an oxygen atom unite, the regeneration of “basic oxides,” also called hydroxide groups, is a proton acceptor and electron pair donor.

For example: sodium hydroxide etc. Substances that absorb positive hydrogen ions in aqueous solution are called “acid oxides”. For example: Sulfuric acid etc. It is a proton donor or electron pair acceptor, while a compound containing a positive ion (cation) from a base and an anion (anion) from an acid is called a salt.

As it is an ionic compound obtained by neutralization of an acid with a base, it becomes a means of reconstitution of salt and water. For example: When hydrochloric acid reacts with a base (sodium hydroxide), then salt and water are obtained as products.

Those oxides of metals which have the characteristics of both basic and acidic oxides are called ampholeric oxides. For example: aluminum oxide and zinc oxides. Those oxides of non-metals which are neither basic nor acidic in nature are called moderate oxides.

For example: water and carbon dioxide The role of the atmosphere is the most important in terms of regeneration of various oxides, because it is a cover up to 12 km above the surface of the earth, which contains various types of gases, other elements and liquids.

Gases at this altitude are chemically very reactive, therefore, individual bonding with oxygen, carbon, and hydrogen to form nonmetallic oxides such as carbon dioxide and hydrogen oxide (water vapor), respectively.

On the other hand, the metal and mineral components in the lithosphere, in which there is apparently stagnation and no growth is visible, but experiments and observations have revealed the fact that their silence and stagnation is not sustainable and they also continue to grow and change. For example, ancient metal and mineral-bearing rocks on Earth’s surface expand with heat and contract with cold.

This repeated expansion and contraction loosens the bond strength of the components, causing cracks, joints and fissures to appear on the body of metal and mineral deposits. Many of the gases in the Earth’s atmosphere gain access to the molecules inside through these weak zones, but oxygen, carbon dioxide, and water vapor are the most common, because they are volatile agents that easily embed the previously ancient metal and mineral components into the inner body to create a new compound.

For example, there are many types of primitive rocks, but there is one type called iron bearing rocks, represented by olivine and pyroxene. This type of rock contains iron.

The chemical interaction of iron and oxygen will turn the rock reddish brown and its molecular bonds will also weaken. Thus a new compound iron oxide (hematite) is regenerated which is an important iron ore.

During its formation, if the temperature is lower than 42 degrees C, some amount of moisture is trapped between the molecules. In such a situation, the iron objects rust, which is a type of oxide called “Aqueous Iron Oxide” (limonite), which is oxidized due to the effects of weather and the combination of oxygen.

This process is called taksid. For example, the formation of new oxides with iron or sodium or another metal. Here it must be kept in mind that the weathering and metamorphism of metals on Earth are the fields or areas where chemical reactions continue and where regeneration of many metals takes place.

In this process, not only free oxygen entering the earth’s crust from the surface plays a role, but rainwater entering the ground, which contains dissolved oxygen and carbon dioxide, has its effects.

It is estimated that an average liter of air-saturated rainwater contains 25-30 cubic centimeters of gas, consisting of 30% oxygen, 60% nitrogen and 10% carbon dioxide.

As if rain water is completely saturated with oxygen and especially carbon dioxide. The role of rainwater became even less when experts realized that low-grade ore deposits appeared on the surface of the earth.

Can’t live without being affected by weather effects. Rainwater runoff (surface water) dissolves the metal ore from the weathering zone and percolates underground. This redistribution of dissolved metal and mineral components is deposited below the water table.

This process enriches a very low grade primary deposit with a valuable secondary deposit. Consists mostly of primary deposits. Copper, silver, lead, zinc and other metals containing sulphide inclusions. Iron sulfide (pyrite) occurs in almost all primary deposits.

Its weathering results in the regeneration of iron sulfate and sulfuric acid, both soluble in water. Therefore, water mixed with iron sulfate and sulfuric acid dissolves other primary sulfide ores by attacking them. Copper, silver and zinc ore auxiliaries are dissolved by this process.

Ore produced by the effects of chemical dissolution (dissolution) and weathering tends to concentrate in those parts of the base metal deposit that are above the “water table” and where air is present in the pores of the underlying rocks. In addition, easily oxidized oxygen compounds are added to ozone and ores that are low-valent metals. Eg: Manganese and iron etc. During the oxidation process, these metals are replaced by high valence ions but smaller in size, due to which the penile structure becomes weaker and weaker.

Dissolved particles are completely broken down with a tendency to form new mineral compounds, some of which are insoluble in water and some of which are soluble in solution. A solution that occurs in a soluble state as a sulfate metal. As the thin stream begins to trickle down, its ore is precipitated below the surface in the form of sulphides, regenerating a secondary enrichment zone.

Thus, copper can be formed from any of the sulfide alloys commonly used in the electrical industry. Below the “water table,” all the pores of the rock or metal body become completely saturated, causing oxidation and weathering to cease, because air is not present. This chemical environment is perfect for ore ore.

The unaltered part of the ore body that lies below the secondary enrichment zone is called the primary zone. Often low-grade deposits of copper are converted into high-grade deposits after undergoing the same process. Often an iron-bearing porous residue that forms as a surface layer over the sulphide deposit through dissolution and weathering is called “gossan”. The iron oxides and hydroxides that regenerate remain at their place of origin in the form of residues that sometimes indicate valuable underground deposits.

As residual deposits, the metal supports that are usually found in the form of oxides include iron, uranium, gold, bauxite and magnesium, but residual oxides can carry useful metals from the rock body during weathering and oxidation processes to reconstruct the deposit, which can be more resistant to chemical reactions.

The slopes of exposed rocks should be low, so that gravity and rainwater do not carry insoluble material away from their original location during weathering and sedimentation. Here, it is important that there is an adequate amount of rainfall, so that the soluble material affected by weathering and sedimentation can be transported elsewhere to form deposits that contain different oxides. When hydrogen oxide (water) reacts chemically with inanimate objects or metals, a new compound is formed.

The formation of hydro-reduced calcium sulfate (gypsum) is of the same nature, this process is called hydration. Another new compound is formed when oxygen in the form of hydrogen oxide (water) reacts chemically with an inanimate material or metal deposit. For example: Kaolin (China clay) is regenerated by treating mineral orthocliner (potassium aluminum silicate) with hydrogen oxides.

In addition, when water falls on the ground in the form of drops, it absorbs a lot of carbon dioxide from the atmosphere, due to which the water becomes a mild mixture of carbonic acid, called “carbonic acid”, that is, water mixed with carbon dioxide. At the surface, more carbon dioxide is absorbed by trees and converted into strong carbonic acid, which then attacks all rock mineral deposits that contain carbonates.

It gradually dissolves, because carbonic acid converts carbonate, which is insoluble, into bicarbonate, which becomes soluble. When this water accumulates in a sea, lake or any basin, organisms, especially diatoms and radiolarians, use carbon dioxide gas during their growth, which regenerates iron, calcium carbonate, etc.

Calcium carbonate (limestone) and iron carbonate (siderite) which are important building stones. But the oxide that regenerates through oxygen and non-living things such as metal or mineral components and which has a great priority in modern technology is called uranium oxide which is formed by the weathering process in the lower parts of the oxidation zone, which is recognized as the only source of nuclear energy.