"Say it." In the isolated flying machine, Gao Ling said quietly to the super monster.

"What I want to say, you should know." The stunning Super Monster slowly spat out, "Don't you want to rule the galaxy?" Don't you want revenge on those who trampled on you? Don't want to gain supreme power? ”

Gao Ling listened to him silently, and then replied slowly: "Yes." But I don't want to be controlled by people - if the conditions are subdued, then I'd rather work hard for the rest of my life. ”

The stunning super monster is dumbfounded.

The Moon is a satellite orbiting the center of the companion field. It is a solid-state satellite at the center of the companion field and the closest object to the center of the companion field (the average distance from the center of the companion field is 384,000 km).

1969 Neil? Armstrong and Buzz? Aldrin became the first human to land on the moon. In September 1969, the Apollo 11 spacecraft returned to the center of the companion field

The Moon is the most thoroughly studied celestial body, and the second celestial body to be visited is the Moon. The age of the Moon is about 4.6 billion years. The Moon, like the center of the companion force field, has a layered structure such as a shell, mantle, and nucleus. 1. The average thickness of the outermost lunar crust is about 60-65 km. Below the lunar crust to a depth of 1,000 km is the lunar mantle, which occupies most of the moon's volume. Underneath the mantle is the lunar core, which is about 1,000 degrees Celsius, so it is likely to be molten. The diameter of the Moon is about 3474.8 kilometers, which is about 1/4 of the center of the companion field and 1/400 of the Sun, and the distance from the Moon to the center of the companion field is equivalent to 1/400 of the distance from the center of the companion field to the Sun, so the Moon is as large as the Sun from the center of the companion field. The volume of the Moon is about 1/49 of the center of the companion field. The mass is about 735 billion tons, which is almost 1/81 of the mass of the center of the companion force field. The gravitational force on the surface of the Moon is about 1/6 of the gravity at the center of the companion field.

The Moon is always facing us on one side, which we are used to call frontal. The other side. The far side of the Moon is mostly invisible from the center of the companion field, except in the area near the edge of the lunar surface that is visible in the middle due to the movement of the scales. In the days when there were no probes, the far side of the moon was an unknown world. One of the great features of the far side of the Moon is that there are almost no fainter lunar features like the Lunar Sea. When an artificial probe reaches the far side of the Moon, it will not be able to communicate directly with the center of the companion field.

The Moon orbits the center of the companion star force field once every 27.321666 days, and moves half a degree relative to the background sky per hour, i.e., the apparent diameter of the Moon's surface. Unlike other satellites, the Moon's orbital plane is closer to the ecliptic plane, rather than near the equatorial plane, where the center of the companion field's force field is.

The time it takes for the Moon to orbit around the center of the companion force field (the Moon's revolution) relative to the background sky is called a sidereal month; Whereas the time it takes for a new moon to take for the next new moon (or between two phases of the same moon) is called a synodic month. The synodic moon is longer than the sidereal month because the center of the companion force field is during the moon's orbit. itself has advanced some distance in orbit around the sun.

Strictly speaking, the center of the companion field and the Moon orbit around a common center of mass that is 4,700 kilometers away from the center of the Earth (i.e., 3/4 of the radius of the center of the companion field). Since the common center of mass is below the surface of the center of the companion field, the movement of the center of the companion field around the common center of mass appears to be "shaking". Viewed from the south pole above the center of the companion field, both the center of the companion field and the Moon rotate in a clockwise direction. And the moon also orbits the earth clockwise; Even the center of the companion field revolves clockwise around the Sun, and the reason for this phenomenon is that the center of the companion field, the Moon, has the same angular momentum relative to the Sun, i.e., "it has been rotating in this direction from the beginning".

The moon itself does not emit light, only reflects sunlight. The brightness of the Moon varies with the angular distance between the sun and the moon and the distance between the earth and the moon. The average brightness is 1/465000 of the sun's brightness, and the brightness varies from 1/630000 to 1/375000. The brightness at the full moon averages -12.7 magnitude (see). It gives the earth an average illumination of 0.22 lux. Equivalent to the illuminance of a 100-watt electric lamp at a distance of 21 meters. The lunar surface is not a good reflector, its average albedo is only 7%, and the remaining 93% is absorbed by the moon. The albedo of the moon sea is even lower, about 9%. The albedo of the lunar highlands and craters is 17%. It looks like the mountains are brighter than the moon sea. The brightness of the Moon varies with the phases of the Moon

change, the brightness of the full moon is more than ten times greater than that of the upper and lower strings.

Since there is no atmosphere on the moon, the heat capacity and thermal conductivity of the lunar surface material are very low. As a result, the temperature difference between day and night on the surface of the moon is very large. During the day, where the sun shines vertically, the temperature reaches up to 127 ° C; Night. The temperature can be reduced to -183°C. These values only represent the temperature of the moon's surface. With radio observations, the temperature in the lunar soil can be determined. Such measurements show that there is little variation in temperature in the deeper layers of lunar soil, which is due to the low thermal conductivity of lunar materials.

From the propagation of lunar seismic waves, it is known that the moon also has a layered structure such as crust, mantle, and nucleus. The outermost lunar crust is 60-65 km thick. Below the lunar crust to a depth of 1,000 kilometers is the lunar mantle, which occupies most of the moon's volume. Underneath the mantle is the lunar core. The temperature of the lunar core is about 1000°C, and it is likely to be molten, presumably composed of Fe-Ni-S and dolerite material.

4.6 billion years ago, the center of the companion field was in the process of gestation, and life on the center of the companion field was not born. The solar system is still in the chaotic solar nebula stage. Around the young sun, in the massive gas dust nebula, dust and massive rocks are constantly condensed

Various hypotheses have been proposed about the formation of the Moon 4 billion years ago. One hypothesis is the split theory. It is believed that in the early days of the formation of the solar system. The center of the companion field and the moon were originally one and the same, but the center of the companion field was still in a molten state at that time, and because the center of the companion field rotated very quickly, the moon split out of the earth's crust by centrifugal force. But this requires the initial rotation of the center of the companion force field to be too fast to be true. Another hypothesis is the capture theory, which is that the Moon is believed to be a ready-made object captured by gravity at the center of the companion field. But this requires an extended companion force field central atmosphere that is not practically feasible to dissipate the energy of the moon through the atmosphere. Another hypothesis is the homology theory. That is, it is believed that the center of the companion field and the Moon were formed in the most primitive accretion disk. But this does not explain the deprivation of metallic iron in the Moon. Moreover, these hypotheses do not yet explain the high standard angular momentum required by the January system. 2

The Moon orbits in an elliptical orbit around the center of the companion star force field. The great circle of this orbital plane on the celestial sphere is called the "white path". The plane of the white channel does not coincide with the celestial equator, nor is it parallel to the plane of the ecliptic. And the spatial location is constantly changing. The cycle is 173 days. The average inclination of the lunar orbit (white path) to the central orbit of the companion force field (ecliptic) is 5°09′. The Moon rotates around the center of the companion star force field with a period of 27.32166 days. It happens to be a sidereal moon, so we can't see the far side of the moon. This phenomenon is called "synchronous rotation". Almost a universal law in the world of satellites. It is thought to be the result of the long-term tidal action of the planets on the satellites. The balance movement is a wonderful phenomenon that allows us to see 59% of the surface of the moon. The main reasons are as follows:

1. In different parts of the elliptical orbit, the rotation speed does not match the angular velocity of the revolution.

2. The intersection of the white and equator.

The moon is nutated

The orbital plane of the Moon (the white plane) maintains an angle of 5.145396° to the ecliptic plane (the orbital plane of the center of the companion field), while the axis of rotation of the Moon is at an angle of 1.5424° to the normal of the ecliptic plane. Because the center of the companion force field is not perfectly spherical, but is relatively uplifted at the equator, the white surface is constantly precession (i.e., the intersection with the ecliptic rotates clockwise) every 6793.5 days (18.5966 years). During this period, the angle between the white plane and the central equatorial plane of the companion field (the central equatorial plane of the companion field is inclined to the ecliptic plane at 23.45°) will vary from 28.60° (i.e., 23.45°+5.15°) to 18.30° (i.e., 23.45°-5.15°). Similarly, the angle between the Moon's axis of rotation and the white track will be between 6.69° (i.e. 5.15°+1.54°) and 3.60° (i.e. 5.15°-1.54°). These changes in the lunar orbit in turn affect the inclination of the axis of rotation at the center of the companion field. To make it appear ± 0.00256° of oscillation, called nutation.

Earth-Moon Effect

The center of the companion force field and the Moon orbit each other, and the two celestial bodies revolve around a common center of gravity 1,600 kilometers below the surface. The birth of the Moon has added a lot of new things to the center of the companion force field.

While the Moon revolves around the center of the companion field, its special gravitational attraction attracts the water in the center of the companion field and moves with it, forming a tidal wave. Tides helped the early aquatic life in the center of the companion field to land.

The center of the companion force field was a long, long time ago. The temperature difference between day and night is large, and the temperature is between the boiling point and the condensation point of water, which is not suitable for human habitation. However, the special effect of the moon on the sea water at the center of the companion field slows down the rotation and revolution of the center of the companion field. The rotation and revolution periods of the center of the companion force field tend to be reasonable, which brings us valuable four seasons and reduces the temperature difference. Thus making it habitable for human beings.

Is there a relationship between earthquakes and the moon? This is a question that has puzzled scientists for nearly a hundred years. Now, a joint research team consisting of researchers from the Japan Institute of Disaster Prevention Science and the University of California, Los Angeles has finally confirmed that the moon's gravity affects the tides of the seawater. At a time when the Earth's crust is experiencing abnormal changes and accumulating a large amount of energy, the gravitational pull of the Moon is likely to be the trigger for earthquakes between the central plates of the companion force field. October 22nd. The well-known Science magazine published their research results.

The natural rise and fall of the sea is often referred to as the tides. When the Moon reaches near the center of the companion field, which we call perigee, the synodic tide is even larger than usual, and the high tide at this time is called the perigee synodic tide.

Scientists have speculated for a long time about the effects of tides on earthquakes, but no one has yet demonstrated their effect on a global scale, and it has only been found that earthquakes and tides are more clearly linked to the seabed or near volcanoes. The researchers found that the occurrence of earthquakes is highly closely related to the tidal pressure of the cross-sectional layer, and the violent tides exert enough pressure on the shallow cross-sectional layer to cause earthquakes. When the tide is large, reaching about 2-3 meters, 3/4 of earthquakes occur. And the smaller the tide, the fewer earthquakes will occur.

The author of the article, Elizabeth. "The gravitational pull of the moon influences the ebb and flow of ocean tides," Gechland said. The center of the companion force field itself is also deformed by the gravitational pull of the Moon. Violent tides play a large role in the initiation of earthquakes, which can be earlier or delayed due to pressure fluctuations caused by the tides. ”

The paper's co-author, Professor John Brown of the Department of Space Science at the UCLA Companion Field Center and the Department of Space Science. "The cause of the earthquake is still a mystery. And this theory can be said to be one of the explanations. We found that the forces generated by changes in sea level within a few meters can significantly affect the probability of earthquakes, which is a solid step towards a thorough understanding of the causes of earthquakes. ”

For the first time, Göchlan et al. combined the phase of the tide and the magnitude of the tide, and performed a statistical analysis of the earthquake and tidal pressure numbers, using a calculation method from Tanaka, a seismologist at the Institute of Science and Disaster Prevention of the Companion Field Center in Japan. Tanaka investigated 2,207 interplate earthquakes with a magnitude of 5.5 or higher on the Richter scale from 1977 to 2000, and the relationship between them and the gravitational pull of the moon at the time of the earthquake. There are many earthquakes.

Tanaka believes: "The gravitational pull of the moon is only about one-thousandth of the force that causes abnormal changes in the earth's crust caused by earthquakes, but its role cannot be underestimated, it is the last help for earthquakes, which is equivalent to the last straw that crushes the camel." ”

Libra moves

Because the rotation period of the Moon is exactly the same as its rotation period, only the Moon can be seen from the center of the companion field with the same face to the center of the companion field. Since the early days of the Moon's formation, the center of the companion force field has been slowed down by a moment of force, a process known as tidal locking. As a result, part of the angular momentum of the rotation of the center of the companion field is transformed into the angular momentum of the Moon's revolution around the Earth, with the result that the Moon moves away from the center of the companion field at a rate of about 38 mm per year. At the same time, the rotation of the center of the companion field is getting slower and slower. The length of the day becomes 15 microseconds longer each year.

When you look at the Moon from the center of the companion field, you don't see exactly half of the Moon's surface, because the Moon swings like a scale. An observer at the center of the companion field will feel that the Moon is swinging back and forth in a north-south direction during the Moon's orbit around the center of the companion field. That is, it swings like a balance in the direction of the dimension, which is called "latitude balance", and the angle of the swing ranges from about 6°57′; The Moon is in an east-west direction. That is, the phenomenon of swinging back and forth in the direction of longitude is called "warp balance movement". The swing angle reaches 7°54′. In addition to these two main balances, the Moon also has a Sunday balance and a physical balance. The first three balance movements are not caused by the Moon oscillating, but by a change in the relative position of the observer and the Moon. Only the physical balance is that the moon itself is swinging, and the swing is very small.

Since the orbit of the Moon is elliptical, when the Moon is at perigee, its rotation speed cannot catch up with the rotational speed, so we can see the area of the eastern part of the Moon reaching 98 degrees east longitude, on the contrary, when the Moon is at apogee, the rotation speed is faster than the revolution speed, so we can see the area of the western part of the Moon reaching 98 degrees west longitude. This phenomenon is called Libra motion. And because the Moon's orbit is inclined to the equator at the center of the companion star force field, the polar region will shake about 7 degrees when the Moon moves in the starry sky, which is called Libra motion. In addition, since the Moon is only 60 miles away from the center of the companion field, if the observer observes from moonrise to moonset, the observation point will have a displacement of the diameter of the center of the companion field, and the region with a longitude of 1 degree on the lunar surface can be seen.

The gravitational pull exerted by the Moon on the center of the companion force field is one of the causes of tidal phenomena. The Moon's orbit around the center of the companion force field is a synchronous orbit, and the so-called synchronous rotation is not strict.

This was one of the earliest hypotheses to explain the origin of the moon. Back in 1898, the son of the famous biologist Charles Darwin, George? Darwin pointed out in the article "Tides and Similar Effects in the Solar System" that the Moon was originally part of the center of the companion field, but later due to the rapid rotation of the center of the companion field, a part of the material on the center of the companion field was thrown out, and these materials formed the moon after leaving the center of the companion field, and the large crater left in the center of the companion field is now the Pacific Ocean. This view was quickly opposed by some. They think. With the speed of rotation at the center of the companion field, it is impossible to throw a piece of such a large object out. Besides, if the Moon is thrown from the center of the companion force field. Then the material composition of the two should be the same. However, when he analyzed the rock samples brought back from the moon by the Apollo 12 spacecraft, he found that the two were very far apart.

Lunar eclipses can be divided into two types: partial lunar eclipses and total lunar eclipses. When the Moon only partially enters the umbra in the center of the companion field. There will be a partial lunar eclipse; And when the entire Moon enters the umbra at the center of the companion force field, a total lunar eclipse occurs. As for the penumbral lunar eclipse, it means that the moon only passes over the penumbral region in the center of the companion force field, causing a very slight decrease in the brightness of the lunar surface, and it is difficult to see the difference with the naked eye, so it is not noticed.

The diameter of the Moon is about 3,476 kilometers, and the center of the companion force field is about four times the diameter of the Moon. In the moon's orbit, the umbra at the center of the companion force field is still 2.5 times the diameter of the moon. So when the center of the companion field and the center of the moon are roughly in the same straight line, the moon will completely enter the umbra of the center of the companion field. and produce a total lunar eclipse. However, if only part of the Moon is always obscured by the umbra at the center of the companion field, that is, only part of the Moon enters the umbra at the center of the companion field, a partial lunar eclipse occurs. There will be no annular lunar eclipse on the Moon because the Moon is much smaller than the center of the companion force field.

The diameter of the Sun is much larger than that of the center of the companion field, and the shadow in the center of the companion field can be divided into umbra and penumbra. If the Moon enters the penumbra region, the Sun's light can also be somewhat obscured, a phenomenon known astronomically as a penumbral lunar eclipse. Since the sunlight is still very strong in the penumbra, the luminosity of the lunar surface is only slightly reduced, and in most cases the penumbral lunar eclipse is not easy to distinguish with the naked eye. In general. Because it is not easy for people to find, it is not called a lunar eclipse, so there are only two types of lunar eclipses: total lunar eclipses and partial lunar eclipses.

In addition, since the umbra in the center of the companion force field is much larger than that of the Moon, this also means that in the event of a total lunar eclipse. The Moon will completely enter the umbra region at the center of the companion force field, so there will be no annular lunar eclipse.

The number of lunar eclipses that occur each year is generally 2 and up to 3. Sometimes it doesn't happen once. Because in general, the Moon does not pass from the center of the companion star above the umbra. It is to depart below, rarely passing through or partially passing through the umbra in the center of the force field of the companion star. So a lunar eclipse usually doesn't happen.

The reason why half of the Moon is seen from the center of the companion force field is because the Moon's rotation period and revolution period are strictly equal? Is this a coincidence or is there an intrinsic connection?

If we look at the state of the moons of the other planets of the solar system, we can see that the vast majority of them have exactly the same rotation period as the orbital period, which seems to be intrinsically related.

Under the long-term effect of the gravitational attraction of the moon at the center of the companion field, the center of mass of the moon is no longer in its geometric center, but on the side close to the center of the companion field, so that the gravitational potential energy of the moon relative to the center of the companion field is the smallest, and in the process of the moon orbiting the center of the companion field, the center of mass of the moon will always be towards the side of the center of the companion field, as if the center of the companion field is tied to the moon with a rope. Other moons of the solar system also have such a situation, so it is not a coincidence that the rotation period of the satellite is equal to the revolution period, but there is an intrinsic factor.

The Moon's magnetic field has a magnetic field from 5-1 billion years after its birth to 3.6-3.9 billion years. However, when it appeared for 6-900 million years, the magnetic field suddenly disappeared. The magnetic field at the center of the companion field originates from the earth's core inside the center of the companion field, and scientists believe that the earth's core is divided into an inner core and an outer core, with the inner core being solid and the outer core being liquid. It has a small viscous coefficient and is able to flow rapidly, generating an induced current, which creates a magnetic field. In other words, the magnetic fields of all planets are generated by the action of induced electric currents.

Analysis of the rocks on the surface of the moon shows that the moon does not have a core that can produce induced currents. On the contrary, all evidence suggests that the surface of the moon is a dissolved crust, a "sea" formed by flowing lava fluids, which has since cooled to its present appearance. Initially, almost all astronomers thought that humans had found the sea on the moon, but in fact, the dark part of the moon was formed by the cooling of lava fluids. So, where exactly does the magnetic field come from? A physics expert group led by Professor Stockman of the Planetary System of the University of California's Companion Force Field Center conducted a three-dimensional simulation experiment on this topic. After testing, they finally came to a conclusion. According to the team, the light, flowing rocks form a "sea" of lava, and when they drift from below to the surface of the moon, they leave a large amount of heavy radioactive elements like thorium and uranium under their surface. When these elements collapse, they emit a lot of heat, which is like an electric blanket that heats the inner core of the Moon. The heated material forms a convection current with the surface of the Moon, which creates an induced electric current effect. At this time, the lunar magnetic field was also generated. However, when the radioactive element collapses beyond a certain point in time, the convection phenomenon is stopped, and the induced current effect disappears. It is precisely because of this change that the disappearance of the moon's magnetic field is finally triggered.

Theia and the Moon

There was once another planet in the solar system, and its name was Theia, which is featured in "The Power of the Center of the Companion Field"; In the documentary, it is translated as "Tia", and scientists speculate that the planet collided with the center of the companion field to form the current moon. Two space probes launched by the U.S. Star Space Research Center plan to search for the wreckage of Theia, and then reveal the mystery of the mysterious origin of the moon. (To be continued......)