WO2006112750A1 - Procede d'enregistrement de l'irregularite temporelle et spatiale des caracteristiques physiques de l'univers et systeme destine a sa realisation - Google Patents

Procede d'enregistrement de l'irregularite temporelle et spatiale des caracteristiques physiques de l'univers et systeme destine a sa realisation Download PDF

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Publication number
WO2006112750A1
WO2006112750A1 PCT/RU2005/000453 RU2005000453W WO2006112750A1 WO 2006112750 A1 WO2006112750 A1 WO 2006112750A1 RU 2005000453 W RU2005000453 W RU 2005000453W WO 2006112750 A1 WO2006112750 A1 WO 2006112750A1
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WIPO (PCT)
Prior art keywords
control signal
sources
difference
sensors
control parameters
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PCT/RU2005/000453
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English (en)
Russian (ru)
Inventor
Yury Alexeevich Baurov
Alexey Yurievich Baurov
Alexander Yurievich Baurov
Vladimir Alexandrovich Solodovnikov
Tristan Shaun Del
Sidney Sharp
Original Assignee
Yury Alexeevich Baurov
Alexey Yurievich Baurov
Alexander Yurievich Baurov
Solodovnikov Vladimir Alexandr
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Application filed by Yury Alexeevich Baurov, Alexey Yurievich Baurov, Alexander Yurievich Baurov, Solodovnikov Vladimir Alexandr filed Critical Yury Alexeevich Baurov
Publication of WO2006112750A1 publication Critical patent/WO2006112750A1/fr

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    • G—PHYSICS
    • G01—MEASURING; TESTING
    • G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V7/00—Measuring gravitational fields or waves; Gravimetric prospecting or detecting

Definitions

  • the invention relates to research tools of the Universe.
  • the Earth can be explained, if we proceed from the assumption of the existence of spatial and temporal unevenness of the physical characteristics of the Universe.
  • no studies have been conducted to identify the structure of the spatial and temporal unevenness of the physical characteristics of the Universe, the physical nature of which is not known to us, but the existence of which can directly correlate with processes on Earth.
  • the objective of the present invention is to develop a method and device for recording the local spatial and temporal unevenness of the physical characteristics of the Universe with the aim of studying the spatial and temporal scales of the unevenness of the physical characteristics of the Universe, using registration of changes in the characteristics of physical processes, the appearance of which is not related to the impact on the physical processes of known physical fields.
  • a method for recording the local spatial and temporal unevenness of the physical characteristics of the Universe which consists, according to the invention, in that the control parameters measured by at least two sources of the control signal are measured at the same time, the current difference of the control parameters of the indicated sources of the control is measured signal, determine the fluctuation of the difference in the control parameters of these sources, record the moments in the belts and current coordinates of at least one control signal source in the selected coordinate system with increased fluctuation of the control parameter difference, when the fluctuation of the control parameter difference exceeds the statistical error associated with the measurement error, while the indicated current coordinates determine the area of spatial non-uniformity of physical space, and the time interval from the beginning to the end of the increased fluctuation of the difference in the control parameters determines the period of time vnomernosti physical space.
  • At least two identical sensors of the control signal are used as control signal sources.
  • identical control sensors are placed in at least two spatially spaced local measurement zones.
  • the zone of local unevenness is determined by the location of the sensor, which record the greatest fluctuation of the difference in the control parameters.
  • the angular orientation of at least one of the sensors in the selected coordinate system is changed.
  • the angular orientation of the sensor is additionally recorded at which the fluctuation of the difference in the control parameters is maximum.
  • an inhomogeneous field of the magnetic field vector potential is additionally formed.
  • the senor in the area of the additional inhomogeneous field of the vector potential of the magnetic field is placed in the area with a minimum value of the magnetic field strength.
  • stabilized generators of high-frequency electric pulses or oscillations, as well as gravitational field sensors are used as sensors.
  • At least one pilot signal sensor and at least one mathematical model of the pilot signal sensor are used as sources of the control signal, and to determine the increased fluctuation of the control parameter, the current difference of the control parameter of the specified control sensor and control signal is measured parameter generated by the mathematical model of the sensor.
  • at least one radiation source and at least one mathematical model of the radiation source are used as a sensor.
  • the claimed system contains at least two sources of the control signal, each of which produces its own value of the control parameter, a unit for comparing the current values of the control parameters, at least at least two sources of the control signal, which determines the current difference in the values of the control parameters, the computing unit determines the analysis and fluctuation of the current difference in the control parameters, providing the allocation of fluctuations in the current difference of the control parameters in excess of the statistical error associated with the measurement error, a unit for tracking the current temporal and spatial coordinates of the sources of the control signal and a unit for recording measurement results, which stores at least all measurement results with increased fluctuation of the current difference of the control parameters, while the sources of the control signal are connected to the input of the comparison of the current values of the control parameters, the comparator output current values of the control parameters and output unit monitoring current time and the spatial coordinates of the pilot signal sources are connected to the input of the computing unit, whose output is, in turn,
  • At least two identical sensors of the control signal are used as sources of the control signal, while identical sensors of the control signal are located, at least in two spatially separated local measurement zones.
  • the recording system prefferably equips the recording system with at least one device for generating an inhomogeneous field of the vector potential of the magnetic field, while at least one of the sensors is located in the specified device in the region with the minimum value of the magnetic field strength.
  • the registration system with a closed metal camera, while inside the camera there is a device for forming an inhomogeneous field of the vector potential of the magnetic field and at least two identical sensors, one of which is placed inside the device for forming the inhomogeneous field of the vector potential of the magnetic field.
  • gravity field sensors can be used as sensors.
  • At least one pilot signal sensor and at least one mathematical model of the pilot signal sensor are used as sources of the control signal, while it is advisable to use at least one source of radioactive radiation and at least at least one mathematical model of a source of radioactive radiation.
  • the basis of the invention is the assumption that the presence of
  • the control parameters recorded by at least two sources of the control signal are simultaneously measured, the current difference of the control parameters of the indicated sources of the control signal is measured, the fluctuation of the difference of the control parameters of the indicated sources is determined, the time instants and the current coordinates are recorded, at least one source of the control signal in the selected coordinate system with increased fluctuation of the difference in the control parameters when the fluctuation
  • the difference in the control parameters exceeds the statistical error associated with the measurement error, while the indicated current coordinates determine the zone of spatial non-uniformity of the physical space, and the time interval from the beginning to the end of the increased fluctuation of the difference in the control parameters determines the period of temporary non-uniformity of the physical space.
  • the coordinates of the sensors determine the area of unevenness, and the time interval is the duration (registration period) of temporary unevenness.
  • the intensity of the non-uniformity can be estimated by the level of fluctuation relative to its average value.
  • the zone of local non-uniformity is determined by the location of the sensor, for which the greatest fluctuation of the difference in the control parameters is recorded, since in the zone of this sensor there will be the greatest level of exposure to external cosmic factors.
  • Changing the angular orientation of at least one of the sensors in the selected coordinate system, which measure the increased fluctuation of the difference in the control parameters makes it possible to study the anisotropy of the physical characteristics of the Universe in the direction and to relate the region of the occurrence of physical non-uniformity with a specific space object, for example, with the Sun, and possibly - and with other stars, in particular, registering the angular orientation of the sensor at which the fluctuation of the difference in the control parameters is maximum.
  • the inhomogeneous field of the vector potential By forming, at least in the area where one of the sensors is located, the inhomogeneous field of the vector potential, additional data can be obtained on the physical foundations of the local spatial and temporal non-uniformity of the physical characteristics of the Universe, in particular, it is possible to study the anisotropy of the gradient field of the revealed non-uniformity.
  • the sensor By placing the sensor in the zone of the additional inhomogeneous field of the vector potential in the region with the minimum magnetic field strength, the error associated with the effect of the magnetic field on the sensor is reduced, while maintaining a high level of the gradient of the vector potential field in the zone of the sensor.
  • the use of stabilized generators of high-frequency electric pulses or oscillations as control signal sensors increases the accuracy of measurements, since the dependence of the characteristics of these generators on the external effects of known physical fields is well known.
  • gravity field sensors as the control signal sensors provides increased measurement accuracy, since these sensors are one of the most high-precision devices for measuring the physical characteristics of the Universe.
  • the method in which at least one pilot signal sensor and at least one mathematical model of the pilot signal sensor are used as sources of the control signal, wherein, to determine the increased fluctuation of the difference of the control parameters, the current difference of the control parameter of the specified control sensor is measured and the control parameter formed by the mathematical model of the sensor, makes it possible to study the temporal nature of the unevenness of physical characteristics in boundary region of the Universe, since the control signal generated by the mathematical model does not depend on any external influences.
  • At least one source of radioactive radiation as a sensor, since until now it was believed in physics that the half-life of a radioactive element does not depend on the known physical fields of the Earth and at least one mathematical model of the source of radiation describing the theoretical level of activity of a radiation source over time.
  • the elements of the claimed system for recording the local spatial and temporal unevenness of the physical characteristics of the Universe ensure the operations of the claimed method with solving specific elements of the system of the same technical problems as the corresponding operations of the method.
  • Figure l shows a general diagram of a system for recording the local spatial and temporal unevenness of the physical characteristics of the Universe
  • figure 2 presents a special case of the implementation of the claimed registration system using two stabilized generators of high-frequency oscillations
  • in Fig.Z - installation diagram with a shielding chamber
  • figure 4 presents the sensitive system of a quartz gravimeter used in another particular case of the implementation of the claimed registration system
  • 5 is a diagram of a registration system using a radiation sensor
  • 6 and 7 are examples experimental registration of increased fluctuations of the control parameter, confirming the presence of local spatial and temporal unevenness of the physical characteristics of the Universe.
  • a system for recording local spatial and temporal non-uniformity of physical characteristics of the Universe includes at least two sources of control signal 1 and 2, while signals from these two sources 1 and 2 are control parameters for recording the local spatial and temporal unevenness of the physical characteristics of the Universe.
  • Sources 1 and 2 are connected to the unit 3 for comparing the current values of the control parameters, in which the current difference in the values of the control parameters is determined.
  • Block 3 is connected to the computational unit 4 for determining and analyzing fluctuations in the current difference of the control parameters, providing the allocation of fluctuations in the current difference of the control parameter in excess of the statistical error associated with the measurement error.
  • An additional unit 5 is connected to the computing unit 4 for tracking the current temporal and spatial coordinates of each of the sources of the control signal, for example, sources 1 and 2.
  • the output of the computing unit is connected to the unit 6 for recording measurement results, which stores at least all measurement results from increased fluctuation of the current difference of the control parameter.
  • the system may also have a display 7 for visually displaying measurement results.
  • the figure shows two control signal sources that are necessary for the system to work, but the system can work with a large number of control signal sources.
  • blocks 3, 4, 5, 6 and 7 in the system described above can exist as independent blocks, but can also be components of a computer, for example, a personal computer of any type. The system operates as follows.
  • All control signal sources or at least two control signal sources operate simultaneously.
  • Each of the sources of the control signal gives its own value of the control parameter. In this case, these are the values of two control parameters.
  • the measured values of the control parameters are received in block 3, where the current difference in the values of the control parameters is determined.
  • the measured current difference is transmitted to computing unit 4, in which the current difference in the values of the control parameters is compared with previous measurements, the fluctuations of the current difference in the control parameters are determined and analyzed, and the fluctuations of the current difference in the control parameters are selected that exceed the statistical error associated with the measurement error.
  • the unit 5 for tracking the current temporal and spatial coordinates of the control signal sources is supplied to it, which allows localizing in space and time regions with increased fluctuation values of the difference of the control parameters in order to use this information in the future analysis.
  • the measurement results processed in the computing unit are transmitted to the registration unit 6, which stores at least all measurement results with increased fluctuation of the current difference in the control parameters. Other data may be transferred to the registration unit.
  • the display 7 serves to quickly display the information requested from the computing unit 4 or from the registration unit 6.
  • Figure 2 shows a special case of the implementation of the registration system of local spatial and temporal unevenness of the physical characteristics of the Universe using two identical signal sensors, which are used as two identical crystal oscillators (CVGs) of 8 and 9 high-frequency oscillations, generating in the nominal mode two almost identical in frequency of the output signal, which are the control parameters.
  • the stability characteristics of the crystal oscillators is provided by connecting them to a single stabilized power source 10.
  • Each of the crystal oscillators through its own frequency divider (Tp) 1 1 and 12 is connected to a synchronous phase detector (SFD) 13, which determines the difference in the values of the two control parameters as the angle of the frequency shift of one crystal oscillator relative to the other crystal oscillator with the accumulation of the current difference to the specified control values, for example, until a phase angle of 360 ° is reached.
  • the frequency dividers 11 and 12 and the synchronous phase detector 13 form a block 14 comparing the current values of the control parameters.
  • a shaper ( ⁇ ) of 15 standard output pulses is used, generated at the time when the angle of the phase difference of the oscillations reaches 360 °, and a personal computer (PC) 16.
  • Tracking unit for the current temporal and spatial coordinates of the sources of control the signal and the unit for recording measurement results, which stores at least all measurement results with increased fluctuation of the current difference of the control parameters, are included in leaving the system as fragments of a personal computer 16, but it is possible to incorporate the indicated blocks into the system.
  • FIG. 3 shows a third embodiment of the invention using an additional inhomogeneous vector potential field, in particular an inhomogeneous vector magnetic field, and quartz resonators similar to those discussed in the previous example.
  • the experimental setup includes a closed thick-walled metal chamber 17, inside which two quartz oscillators 18 and 19 and a computing unit 20 for primary data processing are installed.
  • a device for generating an inhomogeneous magnetic field of the vector potential is mounted, which is a magnetic system 21 having permanent magnets 22 creating a magnetic field B with a magnetic induction level of up to 3500 G (0.35 T).
  • the circles with a dot and with a cross indicate the direction of the vector potential of the magnetic field (a circle with a dot - the vector is directed at us, a circle with a cross - from us).
  • a pedestal 23 on which the first quartz oscillator 18 is located.
  • the quartz oscillator is located in the region with the minimum magnetic field (in the device B under consideration it is approximately 1 G), but with a large gradient of the change in the vector potential of the magnetic field.
  • the second crystal oscillator 19 is located outside the magnetic system and is a reference sensor, with the readings of which the readings of the first crystal oscillator 18 are compared. The whole system is set relative to the horizon plane. Chamber 17 protects quartz generators 18 and 19 from exposure to external electromagnetic fields, and also serves as a kind of damper for any convection flows. Outside the camera is a personal computer 24, which records the results of the experiment.
  • Figure 4 shows another example implementation of the invention using an additional inhomogeneous field of the vector potential, in particular the inhomogeneous vector potential of the magnetic field.
  • gravity field sensors were used as sensors, in particular, “Single” quartz gravimeters with a “mg” test platinum load suspended on quartz torsion threads.
  • the sensitive system of the quartz gravimeter “Single” was supplemented with a permanent magnet 25, set so that its vector potential field in the location of the platinum load “mg” was directed along the sensitivity axis of the gravimeter, which is collinear to the line of gravity.
  • the sensitive element of the gravimeter are quartz threads 26 and 27. The entire system for processing the results of the experiment completely coincides with that described in the previous examples.
  • Figure 5 shows another example implementation of the invention using radiation sensors as sensors.
  • the decay frequency is recorded by scintillation detectors 31 with photomultipliers 32.
  • the measurement results are transmitted to a computer 33, which incorporates a mathematical model 34 that describes the decay of Cs 137 , and a mathematical model 35 that describes the decay of Co 60, and a unit for determining and analyzing the current difference in the control parameters, in this case the current the difference between the recorded values of the number of decays with their theoretical values corresponding to their mathematical models
  • the measurement results are displayed on the external registration unit 36.
  • the coordinates of the measurements are linked in the same way as in the first embodiment of the invention.
  • the recorded signal "b" is not electromagnetic in nature and refers to signals of a new nature, which may be associated with previously unknown spatial changes in the physical parameters of matter in the Universe.
  • the conducted experiments confirm the presence of local spatial and temporal unevenness of physical characteristics of the Universe and the possibility of recording this unevenness with the help of hardware used in modern physical research.
  • Regular registration of local non-uniformity confirms that we are dealing not with random phenomena, but with regular processes in the Universe.
  • the experimental results confirm that, using the proposed method and registration system, it is possible to study the local spatial and temporal unevenness of the physical characteristics of the Universe, which will allow collecting enough experimental data to refine the physical characteristics of the Universe and develop appropriate theoretical models.

Abstract

L'invention se rapporte aux moyens d'exploration de l'Univers. Le procédé d'enregistrement de l'irrégularité spatiale et temporelle locale de l'Univers consiste à mesurer simultanément le paramètre de contrôle d'au moins deux sources de signal de contrôle, mesurer la différence courante du paramètre de contrôle desdites sources de signal de contrôle, déterminer la fluctuation de différence du paramètre de contrôle desdites sources, enregistrer les moments temporels et les coordonnées d'au moins une des sources de signal de contrôle dans un système de coordonnées choisi, avec fluctuation élevée de la différence du paramètre de contrôle lors du dépassement par la fluctuation de la différence du paramètre de contrôle de la marge statistique liée aux erreurs de mesure. Les coordonnées courantes déterminent la zone de l'irrégularité spatiale de l'espace physique, et l'intervalle temporel entre le début et la fin de la fluctuation élevée de la différence du paramètre de contrôle déterminent la période de l'irrégularité temporelle de l'espace physique. En tant que sources de signal de contrôle on utilise des générateurs stabilisés d'oscillations ou d'impulsions haute fréquence, des capteurs de champ gravitationnel ou des sources de rayonnement radioactif.
PCT/RU2005/000453 2005-04-21 2005-09-06 Procede d'enregistrement de l'irregularite temporelle et spatiale des caracteristiques physiques de l'univers et systeme destine a sa realisation WO2006112750A1 (fr)

Applications Claiming Priority (2)

Application Number Priority Date Filing Date Title
RU2005111790/28A RU2005111790A (ru) 2005-04-21 2005-04-21 Способ регистрации локальной пространственной и временной неравномерности физических характеристик вселенной и система для его осуществления
RU2005111790 2005-04-21

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Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU195505A1 (ru) * В. И. Колесников , В. Н. Тоисев Измеритель разностей высокостабильных близких по значению частот
US2490102A (en) * 1946-05-10 1949-12-06 James H Stein Magnetic field angular gradientometer
SU149812A1 (ru) * 1960-06-27 1961-11-30 В.А. Бунин Способ стабилизации высокостабильных генераторов частоты
GB1149037A (en) * 1966-08-11 1969-04-16 Vnii Razvedochnoi Geofiziki Gravity gradientometer
SU970428A2 (ru) * 1981-04-03 1982-10-30 Войсковая часть 13991 Устройство дл оценки достоверности результатов измерений
SU1330585A1 (ru) * 1986-03-05 1987-08-15 Морской гидрофизический институт АН УССР Измеритель разности значений физических величин

Patent Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU195505A1 (ru) * В. И. Колесников , В. Н. Тоисев Измеритель разностей высокостабильных близких по значению частот
US2490102A (en) * 1946-05-10 1949-12-06 James H Stein Magnetic field angular gradientometer
SU149812A1 (ru) * 1960-06-27 1961-11-30 В.А. Бунин Способ стабилизации высокостабильных генераторов частоты
GB1149037A (en) * 1966-08-11 1969-04-16 Vnii Razvedochnoi Geofiziki Gravity gradientometer
SU970428A2 (ru) * 1981-04-03 1982-10-30 Войсковая часть 13991 Устройство дл оценки достоверности результатов измерений
SU1330585A1 (ru) * 1986-03-05 1987-08-15 Морской гидрофизический институт АН УССР Измеритель разности значений физических величин

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