What is the gravitational force equal to? The gravitational constant is not a constant value

GRAVITATION CONSTANT- proportionality coefficient G in the form describing law of gravity.

The numerical value and dimension of a geometric point depend on the choice of the system of units for measuring mass, length, and time. G. p. G, having the dimension L 3 M -1 T -2, where is the length L, weight M and time T expressed in SI units, it is customary to call the Cavendish GP. It is determined in a laboratory experiment. All experiments can be divided into two groups.

In the first group of experiments, the gravitational force. interaction is compared with the elastic force of the thread of horizontal torsion balances. They are a light rocker, at the ends of which equal test masses are fixed. The rocker arm is suspended in gravity on a thin elastic thread. field of reference masses. Magnitude of gravity the interaction of test and standard masses (and, consequently, the value of the G. p.) is determined either by the angle of twist of the thread (static method) or by the change in the frequency of the torsion balance when moving the standard masses (dynamic method). G. was first identified by H. Cavendish using torsion balances in 1798.

In the second group of experiments, the gravitational force. interactions are compared with, for which lever scales are used. G. p. was first defined in this way by F. Jolly in 1878.

The value of Cavendish G. p., included Int. astr. union into the Aster System. permanent (SAP) 1976, Crimea is used to this day, obtained in 1942 by P. Heyl and P. Chrzanowski at the US National Bureau of Measures and Standards. In the USSR, G. p. was first defined in the State Astronomical Inspectorate. in-te them. P. K. Sternberg (SAI) at Moscow State University.

In all modern To determine the Cavendish G. p. (table), torsion balances were used. In addition to those mentioned above, other operating modes of torsion balances were used. If the reference masses rotate around the axis of the torsional thread with a frequency equal to the frequency of natural oscillations of the scales, then by the resonant change in the amplitude of the torsional oscillations one can judge the value of the torsional oscillation (resonance method). Modification of dynamic method is the rotational method, in which the platform, together with the torsional scales and reference masses installed on it, rotates at a constant speed. ang. speed.

The value of the gravitational constant is 10 -11 m 3 / kg * s 2

Hale, Khrzhanovsky (USA), 1942

dynamic

Rose, Parker, Beams et al. (USA), 1969

rotary

Renner (VNR), 1970

rotary

Fasi, Pontikis, Lucas (France), 1972

resonance-

6.6714b0.0006

Sagitov, Milyukov, Monakhov and others (USSR), 1978

dynamic

6.6745b0.0008

Luther, Towler(USA), 1982

dynamic

6.6726b0.0005

Given in table. RMS errors indicate internal convergence of each result. A certain discrepancy in the values ​​of GP obtained in different experiments is due to the fact that the determination of GP requires absolute measurements and therefore systematic measurements are possible. errors in the department results. Obviously, a reliable value of G.p. can be obtained only by taking into account the decomposition. definitions.

Both in Newton's theory of gravitation and in Einstein's general theory of relativity (GTR), gravity is considered as a universal constant of nature, which does not change in space and time and is independent of physics. and chem. properties of the environment and gravitating masses. There are versions of the theory of gravity that predict the variability of the gravitational field (for example, Dirac’s theory, scalar-tensor theories of gravity). Some models of extended supergravity(quantum generalization of general relativity) also predict the dependence of the magnetic field on the distance between interacting masses. However, the currently available observational data, as well as specially designed laboratory experiments, do not yet make it possible to detect changes in GP.

Lit.: Sagitov M.U., Constant of gravitation and, M., 1969; Sagitov M.U. et al., New definition of the Cavendish gravitational constant, "DAN SSSR", 1979, v. 245, p. 567; Milyukov V.K., Does it change? gravitational constant?, "Nature", 1986, No. 6, p. 96.

Qing Li et al. /Nature

Physicists from China and Russia reduced the error in the gravitational constant by four times - to 11.6 parts per million, by conducting two series of fundamentally different experiments and minimizing systematic errors that distort the results. Article published in Nature.

For the first time the gravitational constant G, part of Newton's law of universal gravitation, was measured in 1798 by the British experimental physicist Henry Cavendish. To do this, the scientist used a torsion balance built by the priest John Michell. The simplest torsion balance, the design of which was invented in 1777 by Charles Coulomb, consists of a vertical thread on which a light beam with two weights at the ends is suspended. If you bring two massive bodies to the loads, under the influence of gravity the rocker will begin to rotate; By measuring the angle of rotation and relating it to the mass of the bodies, the elastic properties of the thread and the dimensions of the installation, it is possible to calculate the value of the gravitational constant. You can understand the mechanics of torsion balances in more detail by solving the corresponding problem.

The value obtained by Cavendish for the constant was G= 6.754×10 −11 newtons per square meter per kilogram, and the relative error of the experiment did not exceed one percent.

Model of the torsion balance with which Henry Cavendish first measured the gravitational attraction between laboratory bodies

Science Museum/Science & Society Picture Library

Since then, scientists have carried out more than two hundred experiments to measure the gravitational constant, but have not been able to significantly improve their accuracy. Currently, the value of the constant, adopted by the Committee on Data for Science and Technology (CODATA) and calculated from the results of the 14 most accurate experiments of the last 40 years, is G= 6.67408(31)×10 −11 newtons per square meter per kilogram (the error in the last digits of the mantissa is indicated in parentheses). In other words, its relative error is approximately 47 parts per million, which is only a hundred times less than the error of the Cavendish experiment and many orders of magnitude greater than the error of other fundamental constants. For example, the error in measuring Planck's constant does not exceed 13 parts per billion, Boltzmann's constant and elementary charge - 6 parts per billion, and the speed of light - 4 parts per billion. At the same time, it is very important for physicists to know the exact value of the constant G, as it plays a key role in cosmology, astrophysics, geophysics and even particle physics. In addition, the high error of the constant makes it difficult to redefine the values ​​of other physical quantities.

Most likely, low accuracy of the constant G is associated with the weakness of the gravitational attraction forces that arise in ground-based experiments - this makes it difficult to accurately measure the forces and leads to large systematic errors due to the design of the installations. In particular, some of the experiments used to calculate the CODATA value had a reported error of less than 14 ppm, but their results differed by up to 550 ppm. There is currently no theory that could explain such a wide range of results. Most likely, the fact is that in some experiments scientists overlooked some factors that distorted the values ​​of the constant. Therefore, all that remains for experimental physicists is to reduce systematic errors, minimizing external influences, and repeat measurements on installations with fundamentally different designs.

This is exactly the kind of work that was carried out by a group of scientists led by Jun Luo from the University of Science and Technology of Central China with the participation of Vadim Milyukov from the SAI MSU.

To reduce the error, the researchers repeated the experiments on several installations with fundamentally different designs and different parameter values. In installations of the first type, the constant was measured using the TOS (time-of-swing) method, in which the value G determined by the vibration frequency of the torsion balance. To improve accuracy, the frequency is measured for two different configurations: in the “near” configuration, the external masses are located close to the equilibrium position of the balance (this configuration is shown in the figure), and in the “far” configuration, they are perpendicular to the equilibrium position. As a result, the oscillation frequency in the “far” configuration turns out to be slightly lower than in the “near” configuration, and this makes it possible to clarify the value G.

On the other hand, the second type of installation relied on the AAF (angular-acceleration-feedback) method - in this method, the torsion beam and external masses rotate independently, and their angular acceleration is measured using a feedback control system that keeps the thread untwisted. This allows you to get rid of systematic errors associated with the heterogeneity of the thread and the uncertainty of its elastic properties.

Scheme of experimental setups for measuring the gravitational constant: TOS (a) and AAF (b) method

Qing Li et al. /Nature

Photos of experimental installations for measuring the gravitational constant: TOS method (a–c) and AAF (d–f)

Qing Li et al. /Nature

In addition, physicists tried to reduce possible systematic errors to a minimum. Firstly, they checked that the gravitating bodies involved in the experiments are indeed homogeneous and close to a spherical shape - they built the spatial distribution of the density of the bodies using a scanning electron microscope, and also measured the distance between the geometric center and the center of mass by two independent methods. As a result, scientists were convinced that density fluctuations did not exceed 0.5 parts per million, and eccentricity did not exceed one part per million. In addition, the researchers rotated the spheres at a random angle before each experiment to compensate for their imperfections.

Secondly, physicists took into account that a magnetic damper, which is used to suppress zero modes of vibration of the filament, can contribute to the measurement of the constant G, and then redesigned it so that this contribution did not exceed a few parts per million.

Thirdly, the scientists covered the surface of the masses with a thin layer of gold foil to get rid of electrostatic effects, and recalculated the moment of inertia of the torsion balance taking into account the foil. By monitoring the electrostatic potentials of parts of the installation during the experiment, physicists confirmed that electrical charges do not affect the measurement results.

Fourth, the researchers took into account that in the AAF method, torsion occurs in the air, and adjusted the movement of the rocker arm to account for air resistance. In the TOS method, all parts of the installation were in a vacuum chamber, so such effects could not be taken into account.

Fifthly, the experimenters maintained the temperature of the installation constant during the experiment (fluctuations did not exceed 0.1 degrees Celsius), and also continuously measured the temperature of the thread and adjusted the data taking into account subtle changes in its elastic properties.

Finally, scientists took into account that the metal coating of the spheres allows them to interact with the Earth's magnetic field, and assessed the magnitude of this effect. During the experiment, scientists read all the data every second, including the angle of rotation of the filament, temperature, fluctuations in air density and seismic disturbances, and then built a complete picture and calculated the value of the constant based on it. G.

The scientists repeated each of the experiments many times and averaged the results, and then changed the installation parameters and started the cycle all over again. In particular, the researchers conducted experiments using the TOS method for four quartz filaments of different diameters, and in three experiments with the AAF circuit, the scientists changed the frequency of the modulating signal. It took physicists about a year to check each of the values, and in total the experiment lasted more than three years.

(a) Time dependence of the oscillation period of the torsion balance in the TOS method; The lilac points correspond to the “near” configuration, the blue ones to the “far” configuration. (b) Averaged gravitational constant values ​​for different TOS installations

m 1 and m 2 located at a distance r, is equal to: F = G m 1 m 2 r 2 . (\displaystyle F=G(\frac (m_(1)m_(2))(r^(2))).) G= 6.67408(31) 10 −11 m 3 s −2 kg −1, or N m² kg −2.

The gravitational constant is the basis for converting other physical and astronomical quantities, such as the masses of the planets in the Universe, including the Earth, as well as other cosmic bodies, into traditional units of measurement, such as kilograms. Moreover, due to the weakness of gravitational interaction and the resulting low accuracy of measurements of the gravitational constant, the mass ratios of cosmic bodies are usually known much more accurately than individual masses in kilograms.

The gravitational constant is one of the basic units of measurement in the Planck system of units.

Measurement history

The gravitational constant appears in the modern notation of the law of universal gravitation, but was absent explicitly from Newton and the work of other scientists until the beginning of the 19th century. The gravitational constant in its current form was first introduced into the law of universal gravitation, apparently, only after the transition to a unified metric system of measures. Perhaps this was first done by the French physicist Poisson in his “Treatise on Mechanics” (1809), at least no earlier works in which the gravitational constant would appear have been identified by historians [ ] .

G= 6.67554(16) × 10 −11 m 3 s −2 kg −1 (standard relative error 25 ppm (or 0.0025%), the original published value differed slightly from the final value due to a calculation error and was later corrected by the authors).

see also

Notes

  1. In general relativity, notations using the letter G, are rarely used, since there this letter is usually used to denote the Einstein tensor.
  2. By definition, the masses included in this equation are gravitational masses, however, discrepancies between the magnitude of the gravitational and inertial mass of any body have not yet been discovered experimentally. Theoretically, within the framework of modern ideas, they are unlikely to differ. This has generally been the standard assumption since Newton's time.
  3. New measurements of the gravitational constant confuse the situation even more // Elements.ru, 09.13.2013
  4. CODATA Internationally recommended values ​​of the Fundamental Physical Constants(English) . Retrieved June 30, 2015.
  5. Different authors indicate different results, from 6.754⋅10 −11 m²/kg² to (6.60 ± 0.04)⋅10 −11 m³/(kg s³) - see Cavendish experiment#Calculated value.
  6. Igor Ivanov. New measurements of the gravitational constant further confuse the situation (undefined) (September 13, 2013). Retrieved September 14, 2013.
  7. Is the gravitational constant really constant? Archived copy dated July 14, 2014 on the Wayback Machine Science news on the cnews.ru portal // publication dated September 26, 2002
  8. Brooks, Michael Can Earth's magnetic field sway gravity? (undefined) . NewScientist (21 September 2002). [Archived copy on Wayback Machine Archived] February 8, 2011.
  9. Eroshenko Yu. N. Physics news on the Internet (based on electronic preprints), UFN, 2000, v. 170, no. 6, p. 680
  10. Phys. Rev. Lett. 105 110801 (2010) at ArXiv.org
  11. Physics news for October 2010
  12. Quinn Terry, Parks Harold, Speake Clive, Davis Richard. Improved Determination of G Using Two Methods (English) // Physical Review Letters. - 2013. - 5 September (vol. 111, no. 10). - ISSN 0031-9007. - DOI:10.1103/PhysRevLett.111.101102.
  13. Quinn Terry, Speake Clive, Parks Harold, Davis Richard. Erratum: Improved Determination of G Using Two Methods (English) // Physical Review Letters. - 2014. - 15 July (vol. 113, no. 3). - ISSN 0031-9007. - DOI:10.1103/PhysRevLett.113.039901.
  14. Rosi G., Sorrentino F., Cacciapuoti L., Prevedelli M., Tino G. M.

In Newton's theory of gravitation and Einstein's theory of relativity, the gravitational constant ( G) is a universal constant of nature, unchanging in space and time, independent of the physical and chemical properties of the environment and gravitating masses.

In its original form in Newton's formula, the coefficient G was absent. As the source indicates: “The gravitational constant was first introduced into the law of universal gravitation, apparently, only after the transition to a unified metric system of measures. Perhaps this was first done by the French physicist S.D. Poisson in his “Treatise on Mechanics” (1809), at least, historians have not identified any earlier works in which the gravitational constant would appear.”

Introduction of coefficient G was caused by two reasons: the need to establish the correct dimension and to reconcile the gravitational forces with real data. But the presence of this coefficient in the law of universal gravitation still did not shed light on the physics of the process of mutual attraction, for which Newton was criticized by his contemporaries.

Newton was accused for one serious reason: if bodies attract each other, then they must spend energy on this, but it is not clear from the theory where the energy comes from, how it is spent and from what sources it is replenished. As some researchers note: the discovery of this law occurred after the principle of conservation of momentum introduced by Descartes, but from Newton’s theory it followed that attraction is a property inherent in interacting masses of bodies that expend energy without replenishment and do not become less! This is some kind of inexhaustible source of gravitational energy!

Leibniz called Newton's principle of gravity "an immaterial and inexplicable force." The suggestion of gravity in a perfect void was described by Bernoulli as "outrageous"; and the principle of “actio in distans” (action at a distance) did not meet with much favor then than now.

It was probably not out of nowhere that physicists met Newton’s formula with hostility; it really does not reflect the energy for gravitational interaction. Why do different planets have different gravity, and G constant for all bodies on Earth and in Space? Maybe G depends on the mass of bodies, but in its pure form mass does not have any gravity.

Considering the fact that in each specific case the interaction (attraction) of bodies occurs with a different force (effort), this force must depend on the energy of the gravitating masses. In connection with the above, Newton’s formula must contain an energy coefficient responsible for the energy of attracting masses. A more correct statement in the gravitational attraction of bodies would be to speak not about the interaction of masses, but about the interaction of energies contained in these masses. That is, energy has a material carrier, without which it cannot exist.

Since the energy saturation of bodies is related to their heat (temperature), the coefficient should reflect this correspondence, because heat generates gravity!

Another argument about the non-constancy of G. I will quote from a retro physics textbook: “In general, the ratio E = mc 2 shows that the mass of any body is proportional to its total energy. Therefore, any change in the energy of a body is accompanied by a simultaneous change in its mass. So, for example, if a body heats up, its mass increases."

If the mass of two heated bodies increases, then in accordance with the law of universal gravitation, the force of their mutual attraction should also increase. But there is a serious problem here. As the temperature increases, tending to infinity, the masses and forces between gravitating bodies will also tend to infinity. If we assert that the temperature is infinite, and now sometimes such liberties are allowed, then the gravity between two bodies will also be infinite, as a result, when heated, the bodies should compress and not expand! But nature, as you see, does not reach the point of absurdity!

How to get around this difficulty? It’s trivial - you need to find the maximum temperature of a substance in nature. Question: how to find it?

Temperature is finite

I believe that a huge number of laboratory measurements of the gravitational constant have been and are being carried out at room temperature equal to: Θ=293 K(20 0 C) or close to this temperature, because the instrument itself, a Cavendish torsion balance, requires very careful handling (Fig. 2). During measurements, all interference must be excluded, especially vibration and temperature changes. Measurements must be carried out in a vacuum with high accuracy; this is required by the very small size of the measured quantity.

In order for the “Law of Universal Gravitation” to be universal and worldwide, it is necessary to connect it with the thermodynamic temperature scale. The calculations and graphs presented below will help us do this.

Let's take the Cartesian coordinate system OX – OU. In these coordinates we construct the initial function G=ƒ( Θ ).

On the abscissa axis we plot the temperature, starting from zero degrees Kelvin. Let us plot the values ​​of the coefficient G on the ordinate axis, taking into account that its values ​​must fall within the range from zero to one.

Let's mark the first reference point (A), this point with coordinates: x=293.15 K (20⁰С); y=6.67408·10 -11 Nm 2 /kg 2 (G). Let's connect this point to the origin of coordinates and get a graph of the dependence G=ƒ( Θ ), (Fig. 3)

Rice. 3

We extrapolate this graph and extend the straight line until it intersects with the ordinate value equal to one, y=1. There were technical difficulties when constructing the graph. In order to plot the initial part of the graph, it was necessary to greatly increase the scale, since the parameter G has a very small value. The graph has a small elevation angle, so to fit it onto one sheet, we will resort to a logarithmic x-axis scale (Fig.4).

Rice. 4

Now, pay attention!

Intersection of a graph function with an ordinate G=1, gives the second reference point (B). From this point we lower the perpendicular to the abscissa axis, on which we obtain the coordinate value x=4.39 10 12 K.

What is this value and what does it mean? According to the construction condition, this is temperature. The projection of point (B) onto the “x” axis reflects - the maximum possible temperature of a substance in nature!

For ease of perception, let us present the same graph in double logarithmic coordinates ( Fig.5).

Coefficient G cannot have a value greater than one by definition. This point closed the absolute thermodynamic temperature scale, which was started by Lord Kelvin in 1848.

The graph shows that the G coefficient is proportional to body temperature. Therefore, the gravitational constant is a variable quantity, and in the law of universal gravitation (1) it should be determined by the relation:

G E – universal coefficient (UC), in order not to be confused with G, we write it with an index E(Eergy – energy). If the temperatures of the interacting bodies are different, then their average value is taken.

Θ 1– temperature of the first body

Θ 2– temperature of the second body.

Θ max– the maximum possible temperature of a substance in nature.

In this writing, the coefficient G E has no dimension, which confirms it as a coefficient of proportionality and universality.

Let's substitute G E into expression (1) and write the law of universal gravitation in general form:

Only thanks to the energy contained in the masses does their mutual attraction occur. Energy is the property of the material world to do work.

Only due to the loss of energy due to attraction, interaction between cosmic bodies occurs. Energy loss can be identified with cooling.

Any body (substance), when cooled, loses energy and due to this, oddly enough, is attracted to other bodies. The physical nature of gravity of bodies is the desire for the most stable state with the least internal energy - this is the natural state of nature.

Newton's formula (4) took on a systematic form. This is very important for calculating space flights of artificial satellites and interplanetary stations, and will also make it possible to more accurately calculate, first of all, the mass of the Sun. Work G on M known for those planets, the motion of satellites around which was measured with high accuracy. From the motion of the planets themselves around the Sun we can calculate G and the mass of the Sun. The errors in the masses of the Earth and the Sun are determined by the error G.

The new coefficient will finally make it possible to understand and explain why the orbital trajectories of the first satellites (pioneers) did not correspond so far to the calculated ones. When launching satellites, the temperature of the escaping gases was not taken into account. Calculations showed lower rocket thrust, and the satellites rose to a higher orbit; for example, the Explorer-1 orbit turned out to be 360 ​​km higher than the calculated one. Von Braun passed away without understanding this phenomenon.

Until now, the gravitational constant had no physical meaning; it was just an auxiliary coefficient in the law of universal gravitation, serving to connect dimensions. The existing numerical value of this constant turned the law not into a universal one, but into a particular one, for one temperature value!

The gravitational constant is a variable quantity. I will say more, the gravitational constant, even within the limits of gravity, is not a constant value, because It is not the masses of bodies that participate in gravitational attraction, but the energies contained in the measured bodies. This is the reason why it is not possible to achieve high accuracy in measuring the gravitational constant.

Law of Gravity

Newton's Law of Universal Gravitation and the universal coefficient (G E =UC).

Since this coefficient is dimensionless, the formula for universal gravitation received the dimension dim kg 2 / m 2 - this is an extra-system unit that arose as a result of the use of body masses. With dimension, we came to the original form of the formula, which was determined by Newton.

Since formula (4) identifies the force of attraction, which is measured in Newtons in the SI system, we can use the dimensional coefficient (K), as in Coulomb’s law.

Where K is a coefficient equal to 1. To convert the dimension to SI, you can use the same dimension as G, i.e. K= m 3 kg -1 s -2.

Experiments testify: gravity is not generated by mass (matter), gravity is carried out with the help of energies contained in these masses! The acceleration of bodies in a gravitational field does not depend on their mass, so all bodies fall to the ground with the same acceleration. On the one hand, the acceleration of bodies is proportional to the force acting on them and, therefore, proportional to their gravitational mass. Then, according to the logic of reasoning, the formula for the law of universal gravitation should look like this:

Where E 1 And E 2– energy contained in the masses of interacting bodies.

Since it is very difficult to determine the energy of bodies in calculations, we leave masses in Newton’s formula (4), replacing the constant G by energy coefficient G E.

The maximum temperature can be more accurately calculated mathematically from the relationship:

Let's write this ratio in numerical form, taking into account that (G max =1):

From here: Θ max=4.392365689353438 10 12 K (8)

Θ max– this is the maximum possible temperature of a substance in nature, above which no value is possible!

I would like to note right away that this is far from an abstract figure; it suggests that in physical nature everything is finite! Physics describes the world based on the fundamental concepts of finite divisibility, finite speed of light, and accordingly, the temperature must be finite!

Θ max 4.4 trillion degrees (4.4 teraKelvin). It is difficult to imagine, by our earthly standards (sensations), such a high temperature, but its finite value puts a ban on speculation with its infinity. This statement leads us to the conclusion that gravity also cannot be infinite, the ratio G E =Θ/Θ max puts everything in its place.

Another thing is if the numerator (3) is equal to zero (absolute zero) of the thermodynamic temperature scale, then the force F in formula (5) will be equal to zero. The attraction between bodies must stop, bodies and objects will begin to crumble into their constituent particles, molecules and atoms.

Continued in the next article...

(Gravitational constant – size not a constant)

Part 1

Fig.1

In physics, there is only one constant associated with gravity - the gravitational constant (G). This constant was obtained experimentally and has no connection with other constants. In physics it is considered fundamental.

Several articles will be devoted to this constant, where I will try to show the inconsistency of its constancy and the lack of a foundation under it. More precisely, there is a foundation under it, but it is somewhat different.

What is the meaning of constant gravity and why is it measured so carefully? To understand, it is necessary to return again to the law of universal gravitation. Why did physicists accept this law, moreover, they began to call it “the greatest generalization achieved by the human mind.” Its formulation is simple: two bodies act on each other with a force that is inversely proportional to the square of the distance between them and directly proportional to the product of their masses.

G– gravitational constant

Many very nontrivial conclusions follow from this simple formula, but there is no answer to the fundamental questions: how and due to what does the force of gravity act?

This law says nothing about the mechanism by which the force of attraction arises; however, it is still used today and will obviously continue to be used for centuries to come.

Some scientists deride him, others idolize him. Both of them cannot do without it, because... Nothing better was invented or discovered. Practitioners in space exploration, knowing the imperfection of this law, use correction tables, which are updated with new data after each spacecraft launch.

Theorists are trying to correct this law by introducing corrections, additional coefficients, looking for evidence of the existence of an error in the dimension of the gravitational constant G, but nothing takes root, and Newton’s formula remains in its original form.

Considering the variety of ambiguities and inaccuracies in calculations using this formula, it still needs to be corrected.

Newton’s expression is widely known: “Gravity is Universal,” i.e., gravity is universal. This law describes the gravitational interaction between two bodies, no matter where they are in the Universe; This is considered to be the essence of his universalism. The gravitational constant G, included in the equation, is considered as a universal constant of nature.

The constant G allows for satisfactory calculations under terrestrial conditions; logically, it should be responsible for the energy interaction, but what can we take from the constant?

The opinion of a scientist (Kostyushko V.E.), who carried out real experiments to understand and reveal the laws of nature, is interesting, the phrase: “Nature has neither physical laws, nor physical constants with dimensions invented by man.” “In the case of the gravitational constant, science has established the opinion that this quantity has been found and numerically estimated. However, its specific physical meaning has not yet been established, and this is, first of all, because in fact, as a result of incorrect actions, or rather gross errors, a meaningless and completely meaningless quantity with an absurd dimension was obtained.”

I would not like to put myself in such a categorical position, but we need to finally understand the meaning of this constant.

Currently, the value of the gravitational constant is approved by the Committee on Fundamental Physical Constants: G=6.67408·10 -11 m³/(kg·s²) [CODATA 2014] . Despite the fact that this constant is carefully measured, it does not satisfy the requirements of science. The thing is that there is no exact matching of results between similar measurements carried out in different laboratories around the world.

As Melnikov and Pronin note: “Historically, gravity became the first subject of scientific research. Although more than 300 years have passed since the advent of the law of gravity, which we owe to Newton, the gravitational interaction constant remains the least accurately measured compared to the others."

In addition, the main question about the very nature of gravity and its essence remains open. As is known, Newton’s law of universal gravitation itself has been tested with much greater accuracy than the accuracy of the constant G. The main limitation on the accurate determination of gravitational forces is imposed by the gravitational constant, hence such close attention to it.

It is one thing to pay attention, and quite another thing is the accuracy of the results when measuring G. In the two most accurate measurements, the error can reach about 1/10000. But when measurements were carried out at different points on the planet, the values ​​could exceed the experimental error by an order of magnitude or more!

What kind of constant is this when there is such a huge scatter of readings when measuring it? Or maybe it’s not a constant at all, but a measurement of some abstract parameters. Or are the measurements affected by interference unknown to the researchers? This is where new ground appears for various hypotheses. Some scientists refer to the Earth’s magnetic field: “The mutual influence of the Earth’s gravitational and magnetic fields leads to the fact that the Earth’s gravity will be stronger in those places where the magnetic field is stronger.” Followers of Dirac claim that the gravitational constant changes with time, etc.

Some questions are removed due to lack of evidence, while others appear and this is a natural process. But such disgrace cannot continue indefinitely; I hope my research will help establish a direction towards the truth.

The first person credited with pioneering the experiment in measuring constant gravity was the English chemist Henry Cavendish, who in 1798 set out to determine the density of the Earth. For such a delicate experiment, he used torsion balances invented by J. Michell (now an exhibit in the National Museum of Great Britain). Cavendish compared the pendulum oscillations of a test body under the influence of gravity of balls of known mass in the gravitational field of the Earth.

Experimental data, as it turned out later, were useful for determining G. The result obtained by Cavendish was phenomenal, differing by only 1% from what is accepted today. It should be noted what a great achievement this was in his era. For more than two centuries, the science of experiment has advanced by only 1%? It's incredible, but true. Moreover, if we take into account fluctuations and the inability to overcome them, the value of G is assigned artificially, it turns out that we have not advanced at all in the accuracy of measurements since the time of Cavendish!

Yes! We have not advanced anywhere, science is in prostration - not understanding gravity!

Why has science made virtually no progress in accurately measuring this constant over more than three centuries? Maybe it's all about the tool Cavendish used. Torsion balances, an invention of the 16th century, remain in service with scientists to this day. Of course, these are no longer the same torsion scales, look at the photo, fig. 1. Despite the bells and whistles of modern mechanics and electronics, plus vacuum and temperature stabilization, the result has hardly budged. Clearly something is wrong here.

Our ancestors and contemporaries made various attempts to measure G in different geographic latitudes and in the most incredible places: deep mines, ice caves, wells, and on television towers. The designs of torsion balances have been improved. New measurements, in order to clarify the gravitational constant, were repeated and verified. The key experiment was carried out at Los Alamos in 1982 by G. Luther and W. Towler. Their setup resembled a Cavendish torsion balance, with tungsten balls. The result of these measurements, 6.6726(50)?10 -11 m 3 kg -1 s -2 (i.e. 6.6726±0.0005), was the basis recommended by the Committee on Data for Science and Technology (CODATA) values ​​in 1986.

Everything was calm until 1995, when a group of physicists at the German PTB laboratory in Braunschweig, using a modified installation (scales floating on the surface of mercury, with balls of large mass), obtained a G value of (0.6 ± 0.008)% more than the generally accepted one. As a result, in 1998 the error in measuring G was increased by almost an order of magnitude.

Experiments to test the law of universal gravitation, based on atomic interferometry, to measure microscopic test masses and further test Newton's law of gravitation in the microcosm, are currently being actively discussed.

Other methods of measuring G have been attempted, but the correlation between measurements remains virtually unchanged. This phenomenon is today called a violation of the inverse square law or the “fifth force.” The fifth force now includes certain Higgs particles (fields) - particles of God.

It seems that the divine particle was recorded, or rather, calculated, this is how the physicists who participated in the experiment at the Large Hadron Collider (LHC) sensationally presented the news to the World.

Rely on the Higgs boson, but don’t make a mistake yourself!

So what is this mysterious constant that walks by itself, and without it you can’t go anywhere?

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