
Carbonation solution and oxidation are the processes of ------?
a. Mechanical weathering
b. Biological weathering
c. Chemical weathering
d. None of the above
Answer
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Hint:
The solution refers to the disruption of soluble particles and minerals from rocks with the help of water. Atmospheric oxygen in iron water, while meeting with minerals like iron, is wild and the colour of the rocks turns. The process is called oxidation. When carbon dioxide reacts with the water in the water, new chemical substances such as calcium carbonate and iron carbonate are formed. This process is called carbonation.
Complete solution:
Chemical weathering is through the process of oxidation and carbonation.
The main work on the float of the execution is sensation. Under this, the insert action of weathering and erosion is. There is a static action in weathering, while the dynamic verb is there. Disintegration and chemical weathering add to the disintegration and chemical weathering. The chemical weather is in the tropical humid parts, whereas the physical weather is in trouble and dry desert. They all try to bring the surface to the normal floor, they call the 'processed balance processes'. Notification (degradation) to the erosion of terrestrial by external factors. Filling the lower places of the surface is called aggradation.
Weathering is weakening, breaking, rotting and fragmentation of rocks in their own place is called 'weathering'. This process starts as soon as the rocks are exposed to the ground and are affected by seasonal effects. Weathering is divided into three types based on factors.
- Oxidation,
- Carbonation
- Hydration
Hence, the correct answer is option C.
Note:
Eradication cycle is the combined result of exogenous and endogenous forces. Endogenous forces (plate deforming force, volcanic action, earthquake etc.) create asymmetries on the ground. Mountains, plateaus, hills and surface concavities create lakes, trenches, troughs etc. through surface elevation. As soon as elevation in the ground Asymmetries is created by it, exogenous forces begin to act as levelling forces and they create specific topographies.
The solution refers to the disruption of soluble particles and minerals from rocks with the help of water. Atmospheric oxygen in iron water, while meeting with minerals like iron, is wild and the colour of the rocks turns. The process is called oxidation. When carbon dioxide reacts with the water in the water, new chemical substances such as calcium carbonate and iron carbonate are formed. This process is called carbonation.
Complete solution:
Chemical weathering is through the process of oxidation and carbonation.
The main work on the float of the execution is sensation. Under this, the insert action of weathering and erosion is. There is a static action in weathering, while the dynamic verb is there. Disintegration and chemical weathering add to the disintegration and chemical weathering. The chemical weather is in the tropical humid parts, whereas the physical weather is in trouble and dry desert. They all try to bring the surface to the normal floor, they call the 'processed balance processes'. Notification (degradation) to the erosion of terrestrial by external factors. Filling the lower places of the surface is called aggradation.
Weathering is weakening, breaking, rotting and fragmentation of rocks in their own place is called 'weathering'. This process starts as soon as the rocks are exposed to the ground and are affected by seasonal effects. Weathering is divided into three types based on factors.
- Oxidation,
- Carbonation
- Hydration
Hence, the correct answer is option C.
Note:
Eradication cycle is the combined result of exogenous and endogenous forces. Endogenous forces (plate deforming force, volcanic action, earthquake etc.) create asymmetries on the ground. Mountains, plateaus, hills and surface concavities create lakes, trenches, troughs etc. through surface elevation. As soon as elevation in the ground Asymmetries is created by it, exogenous forces begin to act as levelling forces and they create specific topographies.
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