THE GENESIS OF SOIL

Soil Types as Main Aspects of Agricultural Productivity

Soil basically starts from rock with the decay of animals and plants, if you can imagine a long period or period of time where a large mass of rock would crumble and crumble. Heat, water movement and friction are largely responsible for this. Friction here means rubbing and rubbing the rock mass against the rock mass. Think big boulders, all messy, banging, chipping and sticking together.

What are the results? Well, I’m sure all of you can fix it. This is what happens: the chunks of rock erode, generating a lot of heat, the chunks of rock are pressed together to form new mass, and some parts dissolve in water. Why, myself, I almost feel stressed and stressed over all of that. Can you?

Then there is a big change in temperature. Initially everything is heated to a high temperature, then gradually cools down. Just imagine the cracks, destruction and chaos caused by this change! You know some of the winter effects of sudden freezing and thawing. But the tiny sample of a burst water pipe and a broken jug was nothing in the world at that time. Water and atmospheric gases help this dilapidated business.

Soil the foundation of agriculture sampling

THE GENESIS OF SOIL 2

With all this friction action, which we call mechanical, it’s easy to understand how sand is formed. This is one of the largest sections of sandy soil. The seafront is a nice lump of pure sand. If the soil is nothing but a fragment of rock mass, then it is actually very poor and unproductive. However, the early forms of decomposition of animal and plant life became part of the rock mass and resulted in better soil. So the soil we are talking about is sandy soil mixed with sand with other materials, sometimes clay, sometimes plant material or humus, and often animal waste.

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Clay takes us directly to another class of clay. It happens that certain parts of the rock mass become melted when water falls on them and the heat is abundant and abundant. This decomposition occurs mostly due to the presence of a certain gas in the air called carbon dioxide or carbonic acid gas. This gas attacks and changes some of the material in the rocks. Sometimes you see large rocks with hanging sections that appear to have been eroded. Carbonic acid does this. I turned this part into something else which we call clay.

Changes like this are not mechanical, but chemical. The difference in the two types of change is only this: in the case of a single sand, where a mechanical change occurs, you still have what you started with, except that the block size is smaller. It starts with a large rock, and ends with tiny particles of sand. But you don’t have a different rock type in the end. The mechanical action can be illustrated with a slice of rock sugar. Let the sugar represent the large rock mass. Breaks down sugar, and even the smallest part is sugar.

That is by mass of rock; But when a chemical change occurs, it begins with one thing and ends with something else. It begins with a large chunk of rock that is partially transformed by the acid acting on it. It ends up being a completely different thing that we call clay. So in the case of a chemical change, it starts with a certain thing and we end up with something completely different. Clay is often called clay because of the large amount of water used to form it.

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The third type of soil that the community has to deal with is limestone soil. Remember that we think of land from an agricultural perspective. This soil is formed naturally from limestone. Once we mention something we don’t know, something else comes up and we ignore it. Thus the following series of questions. Now you may be asking yourself, how did limestone first form?

At one time, inferior animal and plant motifs took water molecules from lime. With chalk they form a frame or a house around themselves as protection from large animals. Corals are representatives of this class of skeleton animals.

When the animal dies, the skeleton remains. These huge clumps of living things came together, over the centuries, to form limestone. Some limestone still shaped like shells are still visible. Marble, another limestone, has a somewhat crystalline character. Another famous limestone is chalk. Maybe you want to know how you can always see limestone. Put a little of this acid on top of a little lime.

See how you swing and swing. Then some fell on this chalk as well as on the marble. The same bubble occurs. So chalk should be in all three of these buildings. One does not need to buy a special acid for this to work, even household acids such as vinegar will cause the same results.

So these are the three types of soil that a farmer should handle and that we want to understand. One may learn to know the soil of one’s garden by studying it, just as one learns a lesson by studying it.

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