scholarly journals Application of Frequency-Resonance Methods of Satellite Images Processing for Hydrogen and Living Water Accumulations Searching Within Local Areas in Europe

2021 ◽  
Vol 906 (1) ◽  
pp. 012080
Author(s):  
Mykola Yakymchuk ◽  
Ignat Korchagin ◽  
Arzu Javadova
Keyword(s):  
Cross Section ◽  
Satellite Images ◽  
Deep Structure ◽  
Low Cost ◽  
Exploration Process ◽  
Frequency Resonance ◽  
Basaltic Volcanoes ◽  
Speed Up ◽  
The Cross ◽  
Images Processing

Abstract The results of the application of mobile direct-prospecting technology of frequency-resonance processing and interpretation of satellite images and photo images at the sites hydrogen degassing in various regions are presented. Experimental reconnaissance studies were carried out to study the features of deep structure of the hydrogen degassing areas. The materials of instrumental measurements indicate that in regions of basalt volcano’s location with roots at different depths, signals at hydrogen frequencies are almost always recorded. When scanning the cross-section, responses from hydrogen are recorded from the upper edges of basaltic volcanoes to their roots. It can be assumed that basaltic volcanoes are a kind of channels through which hydrogen migrates to the upper horizons of the cross-section and further into the atmosphere. Within many basaltic volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is curative and can be used for wellness purposes. All surveyed zones of longevity on Earth are located within basalt volcanoes, in which water synthesized at a depth of 68 km migrates to the surface and is used for water supply. Hydrogen deposits can be formed by basaltic volcanoes in adjacent sealed reservoirs. Within some survey areas, responses at hydrogen frequencies from limestones, dolomites and marls were recorded at shallow depths. Direct-prospecting technology can be used to study reservoirs in crystalline rocks (basalts including). Detailed studies and wells drilling in promising areas can be planned and carried out for hydrogen and living water at the same time. The result of investigation indicates the advisability of using direct-prospecting methods of frequency-resonance processing of satellite images to detect zones of hydrogen accumulation in areas of basalt volcano’s location, as well as in areas of hydrogen degassing. The use of mobile and low-cost technology will significantly speed up the exploration process for hydrogen, as well as reduce the financial costs for its implementation.

scholarly journals The results of direct-prospecting geophysical methods used for the detection and localization of zones of hydrogen accumulation and migration in the Earth and the Moon cross-sections

2021 ◽  
pp. 65-76
Author(s):  
M.A. Yakymchuk ◽  
◽  
I.M. Korchagin ◽  
Keyword(s):  
Hydrogen Production ◽  
Satellite Images ◽  
Geophysical Methods ◽  
Experimental Studies ◽  
The Moon ◽  
Frequency Resonance ◽  
The Earth ◽  
Basaltic Volcanoes ◽  
Production Site ◽  
Hydrogen Accumulation

The results of experimental studies at the hydrogen production site, hydrogen degassing sites in various regions, as well as on the Moon are presented. Experiments using the direct-prospecting technology of frequency- resonance processing and interpretation of satellite images and photographs are carried out in order to study the features of the deep structure in the areas of hydrogen degassing. The results of instrumental measurements indicate that, in the areas of the basalt volcanoes location with roots at different depths, signals at hydrogen frequencies are almost always recorded. When scanning the cross-section, responses from hydrogen are recorded practically from the upper edges of basalt volcanoes to their roots. Therefore, it can be assumed that basaltic volcanoes are a kind of channels through which hydrogen migrates to the upper horizons of the crosssection and further into the atmosphere. Deep (living) water is synthesized within many basalt volcanoes at a depth of 68 km. Hydrogen-rich water is healing and can be used for wellness purposes. All previously surveyed longevity zones on the Earth are located within basalt volcanoes, in which water synthesized at a depth of 68 km migrates to the surface and is used for the water supply. Hydrogen deposits can be formed by basaltic volcanoes in adjacent sealed reservoirs. The Mali hydrogen production site is located outside the contour of the basalt volcano; hydrogen responses were recorded from marl at the well site. At local sites in the Carpathians, signals from hydrogen are obtained from dolomites and marls. Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be discovered and localized during areal exploration using the methods of frequency- resonance processing of satellite images and photographs. Direct-prospecting technology can also be used to study reservoirs in crystalline rocks (including basalts). The materials of the article, as well as the previously published results of experimental work in various regions, indicate the advisability of using direct-prospecting methods of frequency–resonance processing of satellite images and photographs to detect zones of hydrogen accumulation in areas, where basalt volcanoes are located, as well as in areas of hydrogen degassing. The use of the mobile low-cost technology will significantly speed up the exploration process for hydrogen, as well as reduce the financial costs for its implementation.

scholarly journals Features of deep structure of the Uzon volcano caldera in Kamchatka and the explosive funnel in Yamal

2020 ◽  
pp. 38-47
Author(s):  
M.A. Yakymchuk ◽  
◽  
I.M. Korchagin ◽  
Keyword(s):  
Cross Section ◽  
Deep Structure ◽  
Sedimentary Rocks ◽  
Experimental Studies ◽  
Oil Field ◽  
Large Area ◽  
Emergency Situations ◽  
Reconnaissance Survey ◽  
Siliceous Rocks ◽  
The Cross

The results of a reconnaissance survey of local zones within the oil site of the Uzon volcano, Bogachevskoye oil field, and site of the explosive crater in Yamal are presented. Experimental studies using the direct-prospecting technology of a frequency-resonance processing and interpretation of satellite images and photographs are carried out to study the features of the deep structures of the survey areas. The results of instrumental measurements indicate that all survey sites are located above volcanoes of sedimentary rocks, within which the synthesis of oil, condensate and gas is almost always carried out at the 57 km border. In the contours of HC-generating volcanoes, there are deep channels through which oil, condensate, and gas migrate to the upper horizons of the cross-section and can replenish the already formed deposits in HC fields. In the absence of reliable seals over such channels, oil, condensate, and gas can migrate to the surface, and gas further enters the atmosphere. Measurements within a relatively large area around the Uzon volcano confirmed the presence of all previously identified types of volcanoes. These are volcanoes filled with: 1) salt; 2) sedimentary rocks of 1-6 groups; 3) limestones; 4) dolomites; 5) marls; 6) siliceous rocks; 7) granites; 8) basalts; 9) ultramafic rocks; 10) kimberlites. Additional evidence obtained by instrumental measurements in favor of the deep (abiogenic) genesis of oil, condensate, and gas is of fundamental importance. Numerous facts of fixing the signals from oil, condensate, and gas at the boundary of their synthesis 57 km within the survey areas and in other regions of the world allow us to state that abiogenic methane is migrating into Earth’s atmosphere in colossal volumes! Local zones of the gas migration into the atmosphere can serve as indicators of the activity of volcanoes in which hydrocarbons are synthesized. In these cases, drilling wells in the areas of the location of deep channels for the migration of abiogenic hydrocarbons to the upper horizons of the cross-section may be associated with great risks — with emergency situations during the drilling.

scholarly journals Hydrocarbons in the Gulf of Mexico: their genesis and extents of migration to the surface and to the atmosphere

2020 ◽  
pp. 51-60
Author(s):  
M.A. Yakymchuk ◽  
◽  
I.M. Korchagin ◽  
Keyword(s):  
Gulf Of Mexico ◽  
Cross Section ◽  
Deep Structure ◽  
Experimental Studies ◽  
Hydrocarbon Synthesis ◽  
Emergency Situations ◽  
Reconnaissance Survey ◽  
Siliceous Rocks ◽  
Hydrocarbon Fields ◽  
The Cross

The results of a reconnaissance survey of local areas, where a number of oil slicks are located in various regions of the Gulf of Mexico, are presented. Experimental studies using the direct-prospecting technology of frequency- resonance processing and the interpretation of satellite and photo images were carried out in order to study the features of the deep structure in the areas, where slicks are located. The results of instrumental measurements indicate that all nine survey sites in the Gulf are located above volcanoes, within which the synthesis of oil, condensate, and gas is carried out at the conditional border of 57 km. In the contours of such volcanoes, there are deep channels through which oil, condensate, and gas migrate to the upper horizons of the cross-section and can replenish the already formed deposits in hydrocarbon fields. In the absence of reliable seals over such channels, oil, condensate, and gas can migrate into the water column, and gas further into the atmosphere. During this migration, gas seeps are formed on the seabed and oil slicks on the water surface. The measurements confirmed the presence of all previously established types of volcanoes, in which conditions for the hydrocarbon synthesis exist at a depth of 57 km. These are volcanoes filled with 1) salt, 2) sedimentary rocks, 3) limestones, 4) granites, and 5) ultramafic rocks. Studies at the site near the emergency well indicate that there are a significant number of volcanoes in the Gulf, within which there are no conditions for the synthesis of hydrocarbons and amber. These are volcanoes filled with 1) dolomites, 2) marls, 3) siliceous rocks, as well as 4) basalts and 5) kimberlites. The additional evidence is obtained by instrumental measurements in favor of the deep (abiogenic) genesis of oil, condensate, and gas is of fundamental importance. Numerous facts of fixing the signals from oil, condensate, and gas at the conditional boundary of their synthesis of 57 km in the Gulf of Mexico and in other regions of the world allow us to make an assumption about the migration of abiogenic methane into the Earth’s atmosphere in colossal volumes! Methane seeps and oil slicks can serve as indicators of the activity of volcanoes in which hydrocarbons are synthesized. In these cases, drilling wells in the areas of the location of deep channels of the migration of abiogenic hydrocarbons to the upper horizons of the cross-section may be associated with great risks — with emergency situations during drilling.

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