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Clay Court Features:
The elasticity of the dirt field is higher than that of the hard and grass courts, and it can bring the ball to the height above the player's shoulder, so it also eases the rhythm of the game, so some people call the dirt field "slow field". On the other hand, hard courts are called "fast courts" because they can only bounce the ball to the waist or even the height of the clay court to the knee, and the game is fast-paced. For golfers who are good at spinning the ball, it is more advantageous to play on the dirt field.
In addition, standing a little further back is also the secret to winning on the dirt field. On the contrary, in the "fast court" game, players prefer to play in front of the net, which is more advantageous for players who are quick to react and move quickly.
Clay court belongs to the sand court, it is the most typical representative of the sand court, in addition, the common green soil, mud and so on can be called the sand court. This kind of field is not very hard, the surface is paved with a layer of fine sand or brick powder, the ball has a large friction with the ground when it lands, and the jump speed of the ball will be relatively slow when the humidity is normal. Players will have a lot of leeway during the run, especially when making sudden stops and returns, and can make beautiful sliding steps.
Playing on this kind of court is a great test for the players, mainly to test their kung fu and patience on the bottom line. Players generally have to pay several times the sweat and patience to play around with the opponent on the bottom line, and the winner is often not the frequent netter, but the side that struggles the bottom line. This dictates that players must have better mental qualities and better running, movement and balance than they would on other fields.
In this sense, clay courts are often a paradise for base-line players, while players who use serve-and-net tactics struggle to gain a foothold on clay.
Sand courts are softer than hard courts, and your knees are more comfortable when you play the ball. Although relatively inexpensive compared to grass, sand courts are not as widely used as they were in the past, because although they are relatively low, they are also quite cumbersome to maintain and maintain. Usually, it needs to be sprinkled frequently, leveled, drawn, and swept the line, and it must be concocted almost every day before use.
And after the rain, it needs to be leveled, rolled, etc., and the tools and labor required are not at all easy. However, the process is still very beautiful, and a newly organized sand court always makes people more eager to go up and practice.
Playing on clay courts is easy to encounter "mines": the first is near the ** and line, the boundary line nailed to the court is relatively smooth, and the speed of the ball hitting the line will suddenly become faster, but at the same time, the clay court is the easiest for the referee to adjudicate, and the ball will leave an obvious mark after landing, which is not easy to cause controversy; The second is that the surface of the court is inevitably uneven, and the ball may change direction after landing, and even the low ball becomes high and the high ball becomes low. When playing on the dirt field, players need to be prepared for the second reaction, need to comprehensively judge the trajectory of the ball after landing, and once the ball changes direction and speed after landing, players need to make adjustments quickly.
This is also the reason why players are relatively conservative when playing clay.
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The acidity of laterite is strong, and the clay weight of the soil is an unfavorable factor in the utilization of laterite, so the fertility of laterite can be improved by applying more organic fertilizer, applying lime and supplementing phosphate fertilizer in an appropriate amount to prevent laterite erosion.
In view of the low organic matter content of laterite, green manure can be planted to improve the organic matter content and nitrogen fertility of laterite. Laterite available phosphorus is generally lacking, so increasing the application of phosphorus fertilizer and improving its utilization rate is an important measure to increase agricultural yield. Lime application of laterite can generally receive good results.
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The advantages and disadvantages of red loam soil are mainly the following three characteristics:1. Soil clay weight:
The soil inside the red loam is relatively clayey, because the aluminum and iron contained in the soil will be oxidized into hydroxides and oxides, which will gradually accumulate on the soil surface, so that the color of the soil will turn red, and when it rains, the rain will wash the soil into mud, and many times will lead to the clay weight of the red loam.
2. Strong acidity:
The red loam itself is highly acidic, because the minerals inside the soil will release magnesium, potassium, sodium, calcium and other substances after long-term weathering, and because the area where the red loam is located often rains, the rain will take away all these substances, resulting in the loss of alkaline substances, so that the soil itself becomes acidic.
3. Less organic matter
Red soils are characterized by low organic matter, because the area where the red loam soil is located is a hot and humid climate, which will increase the growth rate of plants, so that the organic matter inside the soil is decomposed in large quantities, thus reducing the amount of organic matter. In addition, if the plants are destroyed, the rate of loss of organic matter from the red soil will be accelerated.
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1. High-grade seeds can only be planted in red soil;
2. Ordinary seeds are planted on the red soil, the yield is increased by 10%, the experience value remains the same, and the effect remains the same;
3. Seeds on red soil have a certain probability of mutating into special crops during the growth period;
4. There are also random events on the red land, which are more lucrative and unique than ordinary land prizes;
5. There is a risk when crops on the red soil are picked, which are divided into: normal, one that is not stolen (cups) and stolen double (washing utensils).
The high-grade seeds in QQ Farm can only be planted on the red soil of the farm, not on ordinary land. Types of Advanced Seeds In the first phase, there are only bottled trees, pitcher plants, Tianshan Snow Lotus, and Phnom Penh Ganoderma lucidum. )
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Laterite soil is suitable for planting acid-loving plants such as tea trees, jasmine, rhododendrons, bayberry, eucalyptus, pomegranates, gardenias, etc., because laterite is rich in a lot of iron and is a slightly acidic soil, so it is very suitable for planting southern flower plants in most areas.
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The red soil is suitable for planting barley, wheat, tea trees, camellia, fir and masson pine.
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Barley, wheat, tea tree, camellia, fir and masson pine, rhododendron, camellia, maple, white orchid, Milan, gardenia, pearl orchid, begonia, dove tree, goldenrod tea, citrus, cherry, five-needle pine, podocarpus and other acid-loving plants.
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Hello, the color of the laterite soil is red, its viscosity is high, the soil quality is good, and it is very easy to use in the past to burn fires and smear stoves.
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Laterite refers to the red soil that is oxidized on the surface due to the fact that there are more metal-containing substances, and this kind of land is often related to some metal deposits.
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The laterite industry is the main raw material for smelting nickel pig iron, and is used to smelt medium-grade ferronickel. The use of laterite is to improve the fertility of laterite by applying lime and supplementing phosphate fertilizer in an appropriate amount to prevent laterite erosion. It can also be used to reduce costs by mixing iron ore.
Laterite refers to iron oxides.
Because of the rich iron oxide, the soil glows brown, the best soil quality is black soil, and the worst is red soil. Due to the long-term rain, humus is not easy to store and only leave heavy iron oxide and form.
Distribution of laterite.
It is mainly found in Africa, Asia and Oceania.
and the low latitudes of South America and North America, which are roughly limited to 30° north and south latitudes, and are commonly found in tropical rainforest areas. Europe, especially on the eastern coast of the Mediterranean Sea and the Balkans.
There are also soils similar to laterite in the area.
East Asia. It stretches from the coast of the Yangtze River in the north, to the Nanyang Islands in the South China Sea in the south, to Taiwan in the east and to the Yunnan-Guizhou Plateau in the west.
and the Hengduan Mountains are important distribution areas of laterite.
Laterite soil can generally be planted with rice, tea, silk sugarcane, and mountainous areas are also suitable for planting fir trees, tung oil, citrus and bamboo.
Palms and other economic forest trees. The acidity of laterite is strong, and the clay weight of the soil is an unfavorable factor in the utilization of laterite, so the fertility of laterite can be improved by applying more organic fertilizer, applying lime in an appropriate amount and supplementing phosphate fertilizer to prevent laterite scouring.
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