Origin of soil.
If you can imagine a long stretch or a period of divided time the collapse of a great rock collapsed, soil is mainly rock or heat, water action, friction along with the collapse of animals and vegetables It was greatly involved in this. Friction here means friction and grinding of rock mass to rock mass. Giant rocks, their perfect confusion, bumping, rubbing, thinking settling against each other. What is the result? Well, I think this is all you have to do: A bit of rock was worn off, a lot of heat was generated, the part of the rock was pushed together to form a new rock mass Why, I myself feel it all the stress and tension almost. Can you do it?
And, too, there was a big change in temperature. At the beginning, everything was heated to high temperature and gradually became cold. Just think about breaking, breaking, upavals that such a change must have caused! You thaw to know some of the sudden freezing winter effects! However, most examples of ruptured pipes and broken pitchers have nothing to do in the world at the time. Water and gas in the atmosphere helped along this collapsing task.
From all the actions of this friction it is easy to understand what action we call a machine and sand was formed. This represents one of the major divisions of soil sandy soil. The coast of the sea is a large mass of pure sand. If the soil was broken only if there was nothing in the stone mass, then it was quite poor and unproductive. However, the initial form of collapse of the lives of animals and vegetables became part of the rock mass, resulting in better soil. So sandy soil is mixed with other substances of sand, sometimes clay, sometimes vegetable matter and humus, and often animal waste.
Clay brings us to another class of clay soil. Water will flow over them, there will be a lot of fever, when it is abundant, certain parts of the rock mass will melt. This dissolution mainly occurred because of the presence of specific gases called carbon dioxide or carbon dioxide in the air. This gas attacks and alters certain substances in the rock. Aoamo International Rock part I can eat it although I can not find the commitment. Carbonate did this. It turned this eaten portion into what we call clay. Such a change is not mechanical but chemical. The difference between the two types of change is just this: in one case of sand where the mechanical change continued, you still have what you started. You started with a big rock and ended with a small particle of sand. But you finally did not have a different kind of rock. Mechanical action may be indicated by bulk sugar. Let sugar represent a large mass of rock. Sugar is broken down, even with the smallest bits of sugar. It is just like a rocky mass; in the case of chemical change, you start with one thing and end with another. You started with a large chunk of rocks that had acid-affected parts acting on it. It ended up in a completely different thing we call clay. Therefore, in the case of chemical change, certain things start, and eventually there are completely different things. Clay soil is often referred to as mud, due to the amount of water used to form it.
The third type of soil we must cultivate people is lime soil. Remember that we are considering the soil from the farm's point of view. Of course, this soil was usually formed from limestone. As soon as we mention what we do not know, another thing comes up. And a series of questions follows. Now you are probably saying in yourself.
Lower animal and plant morphology at the age of 1 hour was chosen from lime water particles. With lime they formed a skeleton and house about themselves as protection from large animals. Coral is representative of this class of skeleton-forming animals.
As the animal died, the skeleton remained. Large chunks of this creature all pushed formed limestone together, all together after age. Some limestone is still shaped to see the formation of Shelley yet. Marble, another limestone is somewhat crystalline. Another famous limestone is chalk. Perhaps, you want to know how to always be able to convey limestone. Drop a bit of this acid on some lime. See how it fizzles with foam. It is this white marble in a presentation such as a dish. The same bubbling is done. Lime lime has these three structures. Even household acids like vinegar cause the same result, so you do not need to purchase special acid for this task.
And these are the three types of soil that farmers must deal with and we would like to understand. Studying a single word through a lesson learned as a single study abroad in the soil of the garden.
If you can imagine a long stretch or a period of divided time the collapse of a great rock collapsed, soil is mainly rock or heat, water action, friction along with the collapse of animals and vegetables It was greatly involved in this. Friction here means friction and grinding of rock mass to rock mass. Giant rocks, their perfect confusion, bumping, rubbing, thinking settling against each other. What is the result? Well, I think this is all you have to do: A bit of rock was worn off, a lot of heat was generated, the part of the rock was pushed together to form a new rock mass Why, I myself feel it all the stress and tension almost. Can you do it?
And, too, there was a big change in temperature. At the beginning, everything was heated to high temperature and gradually became cold. Just think about breaking, breaking, upavals that such a change must have caused! You thaw to know some of the sudden freezing winter effects! However, most examples of ruptured pipes and broken pitchers have nothing to do in the world at the time. Water and gas in the atmosphere helped along this collapsing task.
From all the actions of this friction it is easy to understand what action we call a machine and sand was formed. This represents one of the major divisions of soil sandy soil. The coast of the sea is a large mass of pure sand. If the soil was broken only if there was nothing in the stone mass, then it was quite poor and unproductive. However, the initial form of collapse of the lives of animals and vegetables became part of the rock mass, resulting in better soil. So sandy soil is mixed with other substances of sand, sometimes clay, sometimes vegetable matter and humus, and often animal waste.
Clay brings us to another class of clay soil. Water will flow over them, there will be a lot of fever, when it is abundant, certain parts of the rock mass will melt. This dissolution mainly occurred because of the presence of specific gases called carbon dioxide or carbon dioxide in the air. This gas attacks and alters certain substances in the rock. Aoamo International Rock part I can eat it although I can not find the commitment. Carbonate did this. It turned this eaten portion into what we call clay. Such a change is not mechanical but chemical. The difference between the two types of change is just this: in one case of sand where the mechanical change continued, you still have what you started. You started with a big rock and ended with a small particle of sand. But you finally did not have a different kind of rock. Mechanical action may be indicated by bulk sugar. Let sugar represent a large mass of rock. Sugar is broken down, even with the smallest bits of sugar. It is just like a rocky mass; in the case of chemical change, you start with one thing and end with another. You started with a large chunk of rocks that had acid-affected parts acting on it. It ended up in a completely different thing we call clay. Therefore, in the case of chemical change, certain things start, and eventually there are completely different things. Clay soil is often referred to as mud, due to the amount of water used to form it.
The third type of soil we must cultivate people is lime soil. Remember that we are considering the soil from the farm's point of view. Of course, this soil was usually formed from limestone. As soon as we mention what we do not know, another thing comes up. And a series of questions follows. Now you are probably saying in yourself.
Lower animal and plant morphology at the age of 1 hour was chosen from lime water particles. With lime they formed a skeleton and house about themselves as protection from large animals. Coral is representative of this class of skeleton-forming animals.
As the animal died, the skeleton remained. Large chunks of this creature all pushed formed limestone together, all together after age. Some limestone is still shaped to see the formation of Shelley yet. Marble, another limestone is somewhat crystalline. Another famous limestone is chalk. Perhaps, you want to know how to always be able to convey limestone. Drop a bit of this acid on some lime. See how it fizzles with foam. It is this white marble in a presentation such as a dish. The same bubbling is done. Lime lime has these three structures. Even household acids like vinegar cause the same result, so you do not need to purchase special acid for this task.
And these are the three types of soil that farmers must deal with and we would like to understand. Studying a single word through a lesson learned as a single study abroad in the soil of the garden.
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