The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other place...
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irk-123456789-1285572018-01-12T03:03:02Z The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations Brodsky, Yu.B. Gannoshyn, V.P. Геолого-геофізичні дослідження With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based on the interaction between the moving tectonic plates and the Earth's magnetic field. В связи с участившимися случаями проявления сейсмической активности и их катастрофическими последствиями, с учетом опубликованных материалов о сильных землетрясениях в Антарктиде (1998 год), Калининградской области (2004 год), Китае (2008 год), Киргизии (2008 год), Южном Пакистане (2008 год) и многих других представлен анализ влияния сейсмического процесса на эффекты в околоземной плазме. Предложена новая гипотеза связи в системе литосфера–геомагнитное поле, основанная на взаимодействии движущихся тектонических плит с магнитным полем Земли. 2009 Article The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations / Yu.B. Brodsky, V.P. Gannoshyn // Український антарктичний журнал. — 2009. — № 8. — С. 120-125. — Бібліогр.: 8 назв. — англ. 1727-7485 http://dspace.nbuv.gov.ua/handle/123456789/128557 550.348.0985:551.14á en Український антарктичний журнал Національний антарктичний науковий центр МОН України |
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Геолого-геофізичні дослідження Геолого-геофізичні дослідження Brodsky, Yu.B. Gannoshyn, V.P. The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations Український антарктичний журнал |
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With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based on the interaction between the moving tectonic plates and the Earth's magnetic field. |
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Brodsky, Yu.B. Gannoshyn, V.P. |
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Brodsky, Yu.B. Gannoshyn, V.P. |
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Brodsky, Yu.B. |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations |
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hypothesis of the relationship between the current seismic process and the geomagnetic field pulsations |
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Національний антарктичний науковий центр МОН України |
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2009 |
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Геолого-геофізичні дослідження |
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http://dspace.nbuv.gov.ua/handle/123456789/128557 |
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The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations / Yu.B. Brodsky, V.P. Gannoshyn // Український антарктичний журнал. — 2009. — № 8. — С. 120-125. — Бібліогр.: 8 назв. — англ. |
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Український антарктичний журнал |
work_keys_str_mv |
AT brodskyyub thehypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations AT gannoshynvp thehypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations AT brodskyyub hypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations AT gannoshynvp hypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations |
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2025-07-09T09:19:54Z |
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2025-07-09T09:19:54Z |
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1837160514062385152 |
fulltext |
THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT SEISMIC
PROCESS AND THE GEOMAGNETIC FIELD PULSATIONS
Yu.B. Brodsky, V.P. Gannoshyn
Zhitomir National Agroecological University, 7 Stary bulvar, 10008 Zhitomir, e-mail:
YBrodskiy@academy.zt.ua
The hypothesis of the relationship between the current seismic process and the geomagnetic field
pulsations by Yu.B. Brodsky, V.P. Gannoshyn
Abstract. With respect to the increased frequency of the seismic activity symptoms and their disastrous
aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctica (1998),
Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper
presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The
authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based
on the interaction between the moving tectonic plates and the Earth's magnetic field. Alongside with the seismic
process development the linear velocity of the tectonic plate deformation is increasing which results in the change
in the shape of the geomagnetic field intensity line, which, though elastic, is trying to take its initial shape. The
changes in the shape of the geomagnetic field intensity line bring about the appearance of the oscillation process
of the latter (the so-called stationary wave). In the critical moment of time, when the rock reaches its ultimate
stress limit, one can observe the discontinuity or the Earth's crust fault which is accompanied by a rapid increase
in the oscillation amplitude of the force geomagnetic line. The paper also presents the results of modelling the
pulsations of the geomagnetic field Z-component, the above testifying to a direct relationship and the disturbance
of the Earth's magnetic field. The estimates obtained are nicely coordinated with the results of geomagnetic field
pulsation measurements which were carried out on the Academician Vernadsky station before the severe crust
thearthquake in the Antarctics on the 25 of March 1998 (Bakhmutov, Sedova, Mozgovaya, 2003).
Key words: acoustic and gravitation waves, earthquake, Earth's magnetic field, pulsations of the geomagnetic
force line Z-component.
Ðåôåðàò.  ñâÿçè ñ ó÷àñòèâøèìèñÿ ñëó÷àÿìè ïðîÿâëåíèÿ ñåéñìè÷åñêîé àêòèâíîñòè è èõ
êàòàñòðîôè÷åñêèìè ïîñëåäñòâèÿìè, ñ ó÷åòîì îïóáëèêîâàííûõ ìàòåðèàëîâ î ñèëüíûõ çåìëåòðÿñåíèÿõ â
Àíòàðêòèäå (1998 ãîä), Êàëèíèíãðàäñêîé îáëàñòè (2004 ãîä), Êèòàå (2008 ãîä), Êèðãèçèè (2008 ãîä),
Þæíîì Ïàêèñòàíå (2008 ãîä) è ìíîãèõ äðóãèõ ïðåäñòàâëåí àíàëèç âëèÿíèÿ ñåéñìè÷åñêîãî ïðîöåññà íà
ýôôåêòû â îêîëîçåìíîé ïëàçìå. Ïðåäëîæåíà íîâàÿ ãèïîòåçà ñâÿçè â ñèñòåìå ëèòîñôåðà–ãåîìàãíèòíîå
ïîëå, îñíîâàííàÿ íà âçàèìîäåéñòâèè äâèæóùèõñÿ òåêòîíè÷åñêèõ ïëèò ñ ìàãíèòíûì ïîëåì Çåìëè. Ïî
ìåðå ðàçâèòèÿ ñåéñìè÷åñêîãî ïðîöåññà óâåëè÷èâàåòñÿ ëèíåéíàÿ ñêîðîñòü äåôîðìàöèè òåêòîíè÷åñêîé
ïëèòû, ÷òî ïðèâîäèò ê èçìåíåíèþ ôîðìû ñèëîâîé ëèíèè ãåîìàãíèòíîãî ïîëÿ, êîòîðàÿ, îáëàäàÿ
óïðóãîñòüþ, ñòðåìèòñÿ ïðèíÿòü ñâîþ ïåðâîíà÷àëüíóþ ôîðìó. Èçìåíåíèå ôîðìû ñèëîâîé ëèíèè
ãåîìàãíèòíîãî ïîëÿ ïðèâîäèò ê âîçíèêíîâåíèþ êîëåáàòåëüíîãî ïðîöåññà ïîñëåäíåé (ñòîÿ÷àÿ âîëíà). Â
êðèòè÷åñêèé ìîìåíò âðåìåíè, êîãäà äîñòèãàåòñÿ ïðåäåë íàïðÿæåíèÿ ïðî÷íîñòè ïîðîä, ïðîèñõîäèò
íàðóøåíèå ñïëîøíîñòè, èëè ðàçðûâ, çåìíîé êîðû ñ ðåçêèì óâåëè÷åíèåì àìïëèòóäû êîëåáàíèé ñèëîâîé
ã å î ì à ã í è ò í î é ë è í è è . Ï ð å ä ñ ò à â ë å í û ð å ç óë üò à ò û ì î ä å ë è ð î â à í è ÿ ï óë ü ñ à ö è é
Z-ñîñòàâëÿþùåé ãåîìàãíèòíîãî ïîëÿ, ïîäòâåðæäàþùèå ïðÿìóþ ñâÿçü ìåæäó ïðîòåêàþùèì
ñåéñìè÷åñêèì ïðîöåññîì è âîçìóùåíèåì ìàãíèòíîãî ïîëÿ Çåìëè. Ïîëó÷åííûå îöåíêè õîðîøî
ñîãëàñóþòñÿ ñ ðåçóëüòàòàìè èçìåðåíèé ïóëüñàöèé ãåîìàãíèòíîãî ïîëÿ íà ñòàíöèè Àêàäåìèê Âåðíàäñêèé
ïåðåä ñèëüíûì êîðîâûì çåìëåòðÿñåíèåì â Àíòàðêòèäå 25 ìàðòà 1998 ãîäà (Áàõìóòîâ, Ñåäîâà, Ìîçãîâàÿ,
2003).
Êëþ÷åâûå ñëîâà: àêóñòè÷åñêèå è ãðàâèòàöèîííûå âîëíû, çåìëåòðÿñåíèå, ìàãíèòíîå ïîëå Çåìëè,
ïóëüñàöèè Z-ñîñòàâëÿþùåé ãåîìàãíèòíîãî ïîëÿ
ÓÊÐÀ¯ÍÑÜÊÈÉ ÀÍÒÀÐÊÒÈ×ÍÈÉ
ÆÓÐÍÀË
ÓÀÆ ¹ 8, 120-125 (2009)
ÓÄÊ 550.348.0985:551.14á
120
121
óïîòåçà çâ'ÿçêó ñåéñì³÷íîãî ïðîöåñó ç ïóëüñàö³ÿìè ãåîìàãí³òíîãî ïîëÿ.
Þ.Á. Áðîäñüêèé, Â.Ï. Ãàííîøèí
Ðåôåðàò. Ó çâ'ÿçêó ç âèïàäêàìè ïðîÿâó ñåéñì³÷íî¿ àêòèâíîñò³, ùî ïî÷àñò³øàëè, òà ¿õ êàòàñòðîô³÷íèìè
íàñë³äêàìè, ç óðàõóâàííÿì îïóáë³êîâàíèõ ìàòåð³àë³â ïðî ñèëüí³ çåìëåòðóñè â Àíòàðêòèä³ (1998 ð³ê),
Êàë³í³íãðàäñüê³é îáëàñò³ (2004 ð³ê), Êèòà¿ (2008 ð³ê), Êèðãè糿 (2008 ð³ê), ϳâäåííîìó Ïàêèñòàí³ (2008
ð³ê) é áàãàòüîõ ³íøèõ ïðåäñòàâëåíî àíàë³ç âïëèâó ñåéñì³÷íîãî ïðîöåñó íà åôåêòè â íàâêîëîçåìí³é ïëàçì³.
Çàïðîïîíîâàíî íîâó ã³ïîòåçó çâ'ÿçêó â ñèñòåì³ ë³òîñôåðà–ãåîìàãí³òíå ïîëå, çàñíîâàíó íà âçàºìî䳿
ðóõîìèõ òåêòîí³÷íèõ ïëèò ç ìàãí³òíèì ïîëåì Çåìë³.  ì³ðó ðîçâèòêó ñåéñì³÷íîãî ïðîöåñó çá³ëüøóºòüñÿ
ë³í³éíà øâèäê³ñòü äåôîðìàö³¿ òåêòîí³÷íî¿ ïëèòè, ùî ïðèçâîäèòü äî çì³íè ôîðìè ñèëîâî¿ ë³í³¿
ãåîìàãí³òíîãî ïîëÿ, ÿêà, ìàþ÷è ïðóæí³ñòü, ïðàãíå ïðèéíÿòè ñâîþ ïåðâèííó ôîðìó. Çì³íà ôîðìè ñèëîâî¿
ë³í³¿ ãåîìàãí³òíîãî ïîëÿ âèêëèêຠâèíèêíåííÿ êîëèâàëüíîãî ïðîöåñó îñòàííüî¿ (ñòîÿ÷à õâèëÿ). Ó
êðèòè÷íèé ìîìåíò ÷àñó, êîëè äîñÿãàºòüñÿ ìåæà íàïðóãè ì³öíîñò³ ïîð³ä, â³äáóâàºòüñÿ ïîðóøåííÿ
ñóö³ëüíîñò³, àáî ðîçðèâ, çåìíî¿ êîðè ç ð³çêèì çá³ëüøåííÿì àìïë³òóäè êîëèâàíü ñèëîâî¿ ãåîìàãí³òíî¿ ë³í³¿.
Ïðåäñòàâëåíî ðåçóëüòàòè ìîäåëþâàííÿ ïóëüñàö³é Z-ñêëàäîâî¿ ãåîìàãí³òíîãî ïîëÿ, ÿê³ ï³äòâåðäæóþòü
ïðÿìèé çâ'ÿçîê ì³æ ïðîò³êàþ÷èì ñåéñì³÷íèì ïðîöåñîì ³ çáóðåííÿì ìàãí³òíîãî ïîëÿ Çåìë³. Îòðèìàí³
îö³íêè äîáðå óçãîäæóþòüñÿ ç ðåçóëüòàòàìè âèì³ðþâàíü ïóëüñàö³é ãåîìàãí³òíîãî ïîëÿ íà ñòàíö³¿
Àêàäåì³ê Âåðíàäñüêèé ïåðåä ñèëüíèì êîðîâèì çåìëåòðóñîì â Àíòàðêòèä³ 25 áåðåçíÿ 1998 ðîêó
(Áàõìóòîâ, Ѻäîâà, Ìîçãîâà, 2003).
Êëþ÷îâ³ ñëîâà: àêóñòè÷í³ òà ãðàâ³òàö³éí³ õâèë³, çåìëåòðóñ, ìàãí³òíå ïîëå Çåìë³, ïóëüñàö³¿ Z-ñêëàäîâî¿
ãåîìàãí³òíîãî ïîëÿ
1. Introduction
One of the most important problems of ecological safety connected with the modern prediction
of the coming earthquake still remains unsolved. Catastrophic after-effects of this natural
phenomenon put forward a task of informative earthquake forerunners search. Such task presupposes
exposure of different geophysical effects arising during seismic process, their further interpretation
with the aim of new prediction method development.
Earthquake is a rather lasting process which is accompanied by different geophysical
phenomena, manifesting themselves not only in bowels of the earth, separate parts of lithosphere, but
in hydrosphere, biosphere, atmosphere, including bits upper layers – ionosphere. That is why
earthquake should be considered as an event that leads to the misbalance in the system of connected
Earth forms and near-Earth area.
Up to now two opposite views of the researchers have been formed as for the forerunners of the
coming earthquake. The first one is based on the fact that the earthquake source is in the earth's crust,
the second one is based on the fact that the earthquake source is the geophysical influence of Sun and
interplanetary magnetic field.
In this connection the authors focused their investigations on the explanation of the hypothesis
suggested – the interaction between the moving tectonic plates and pulsation of geomagnetic field
before and during earthquake.
2. Short analysis of known interaction hypothesis in the system lithosphere-
atmosphere- ionosphere
We'll consider and analyze the known hypothesis in the system lithosphere-atmosphere-
ionosphere in the preparation period and earthquake origin (Ëèïåðîâñêèé, 2006). Alongside it is
necessary to take into account that up to now there is no generally accepted physical model of
interconnection between the seismic process and phenomena in the near-earth cosmic space.
“Echo” hypothesis of electromagnetic interconnection in the system lithosphere-ionosphere
presupposes that transmittance of electromagnetic energy from lithosphere into ionosphere, heating
and further effecting E-area takes place while stimulating hypothetic resonator in the system
ïðîò³êàþ÷îãî
Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT...
122
lithosphere- ionosphere. However there is no experimental prove testifying the benefit of “echo”
model. That is why, knowing about the possibility of resonance ionosphere effect manifestation, we
can presuppose that these effects are not crucial in lithosphere-ionosphere interconnection.
“Acoustics-gravitation” hypothesis. According to this hypothesis atmosphere acoustics-
gravitational waves (AGW) are generated in the area of earthquake origin near the earth surface,
which are spread through atmosphere reaching the ionosphere tops lead to ionosphere disturbance due
to the collision of ions and neutral molecules. AGW generation can be connected with reciprocating
movement of earth's crust having block structure with non-stable heat anomalies caused by hothouse
gases going out into the atmosphere of earth's crust breaking zones, as well as with non-stable entrance
of lithosphere gas masses into atmosphere. The process of AGW generation has not been investigated
experimentally yet.
The hypothesis of “lithosphere-ionosphere relationship” is based on the effect of radioactivity
and transmittance increase, that leads to the “modification of quasi-stable electric field” in the near-
earth layer of the atmosphere. However, it is impossible to explain the increase of the maximum layer
F2 height and decrease of the electron concentration maximum value within a day before earthquake
in the framework of the hypothesis suggested.
“Acoustic-electric” hypothesis of the disturbance of Es-generators and mini-current systems
in the night E-area of ionosphere under the influence of acoustic impulses coming from the earth is one
of the last hypotheses not confirmed by observations. The latter explains effects of ionosphere at rather
short distances within several hundreds kilometers from the future epicenter, according to this
hypothesis the existence of acoustic impulses is presupposed, they spread from the area of earthquake
preparation to ionosphere height and generating electric current in sporadical layers.
According to “gravitation-electrostatic” hypothesis impulsive radon isolation takes place in
the area of earthquake preparation. If aerosol provided, Freckle local electro gravitational generators
and mini-current systems appear for several minutes and horizontally for the ten of meters. Non-
stationary charge distribution and creation of mini-current system in separate elements, on the one
hand, lead to the splash of infra-red radiation, and, on the other hand, to the transmittance of
corresponding disturbance upward into ionosphere.
Proceeding from the existing hypothesis, it is possible to suppose, that in the period of seismic
process appearance and development a complex of different physical mechanisms are in action, that
leads to the corresponding geophysical effects, consideration of which can give a wide range of
earthquake forerunners.
3. Hypothesis of lithosphere-geomagnetic field relationship
Any earthquake appears as a result of a sudden release of a considerable number of energy in
some volume inside the Earth. As a rule, in some earth areas destruction and some other irreversible
rock deformation.
Proceeding from theoretical preconditions based on “the theory of elastic output” (Reid, 1911),
rotation model of earthquake origin, in case of the irregular turning blocks chain with friction
(Âèêóëèí, Áûêîâ, Ëóíåâà, 2000), caused by “freezing in” line of force of the geomagnetic field in
earth substance (Áî÷êàðåâ, 1985) and the latter “freezing in” ionosphere (Ôèçèêà êîñìîñà.
Ìàëåíüêàÿ ýíöèêëîïåäèÿ, 1986), the hypothesis of tectonic slabs deformation influence on the
amplitude change of Z-component in the Earth magnetic field lies in the following.
At the initial moment (the moment of seismic process origin) the stretching power begins to
influence the element of geomagnetic line of force, situated in the Earth's crust from the side of
deforming tectonic blocks. The other end of geomagnetic line of force is fixed. The stretching power is
slowly increasing in time from 0 till its critical value – ô the break time of homogenic tectonic blocks. êð
Prolongation of geomagnetic line of force (geomagnetic line of force possesses elasticity),
Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT...
geomagnetic line of force tends to become straight. The attempt to take its original form on the side of
geomagnetic line of force leads to the fact that variations appear in every point of geomagnetic line of
force length.
At the moment of ô time tension of rock strength reaches its strength limit, the rock break will êð
occur. In its turn it will lead to the following, on the break side there will be a hit on the geomagnetic
line of force, as the result of it a firm wave will spread with big amplitude of hesitation, than before ô êð
time.
4.Modelling the relationship of the current seismic process and geomagnetic pulsations
Within the framework of the hypothesis suggested we'll consider the behavior of Z-component
of Earth geomagnetic field as a function of distance õ (m) from earthquake epicenter along the
magnetic line of force, time t (day) from the moment of seismic process origin and height h (km) from
earth surface. In this connection we'll consider the wave equation – equation of string hesitation:
(1)
where
T – tension on all string points;
ñ – linear sting density.
Equation solving (1) using Furrier method, meeting a combination of exceeding and initial
conditions usually looks in such a way (Ïèñêóíîâ, 1985):
(2)
where
A string form f (x) is a form of geomagnetic line of force, the speed function ? (õ) is a linear
speed of tectonic blocks deformation.
The results of modeling the amplitude of pulsations Z(x, t, h), the component of the earth
geomagnetic field, as a result of seismic process for maximum atmosphere model (Èñàåâ, Ïóäîâêèí,
1972) and magnitude Ì = 5,0 points are shown in the picture.
123
,
2
2
2
2
2
1
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Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT...
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Picture. Dynamics of the development of Z-component geomagnetic field pulsation.
Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT...
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Conclusions
Within the framework of the hypothesis suggested and the results given modeling of the
geomagnetic field response to the current seismic process it is possible to make several conclusions:
1. At the initial moment of seismic process origin tectonic block undergoes deformation that
must lead to the form change of geomagnetic force line. However, insufficiency of power effect from
the side of deforming tectonic block on the element of geomagnetic force line, which is in earth's crust,
does not contribute to the development of the geomagnetic field wave process.
2. As the seismic process develops the speed of tectonic block deformation increases. On the
th25 day of seismic process the peak outlet of tectonic block deformation linear speed takes place
alongside with loading decrease without breaking earth integrity with the further increase of tectonic
block deformation linear speed. The increase of the latter leads to the change of geomagnetic force line
form. Possessing strength geomagnetic force line tends to take the initial form, that as a result causes a
standing wave along geomagnetic force line (pulsation of geomagnetic field Z – component).
th th3. On the 30 and 50 day tectonic block deformation linear speed suddenly increases,
earthquake or the outlet of accumulated tensions takes place, which occurs as a result of non-stable
deformation localization. Amplitude of pulsation of geomagnetic field Z-component during
thearthquake (50 day) is from 420 till 500 mkm.
4. The given results of modeling pulsation of geomagnetic field Z-component confirm the
relationship between the seismic process and earth magnetic field. The results obtained accord with
the results of measuring pulsations of geomagnetic field at the station of Academician Vernadsky,
which preceded the strongest earthquake in Antarktida on March 25, 1998 (Áàõìóòîâ, Ñåäîâà,
Ìîçãîâàÿ, 2003).
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