The document discusses the application of frequency-resonance methods for processing satellite images to detect hydrogen and living water accumulations across various regions in Europe. It highlights past research on natural hydrogen sources, the technology developed for detection, and experimental results from several locations including Latvia, Lithuania, and Greece. The findings emphasize the potential for discovering and localizing hydrogen deposits using innovative geological methodologies.

1. WMESS- 2021, Prague, Czech Republic,
APPLICATION OF FREQUENCY-RESONANCE METHODS OF
SATELLITE IMAGES PROCESSING FOR HYDROGEN AND
LIVING WATER ACCUMULATIONS SEARCHING WITHIN
LOCAL AREAS IN EUROPE
Yakymchuk N.A.1, Korchagin I.N.2, Javadova A.3
1Institute for Applied Problems of Ecology, Geophysics and Geochemistry, Laboratory Lane, 1, Kyiv, 01133,
Ukraine, e-mail: yakymchuk@gmail.com
2S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Palladin Ave., 32, Kyiv, 03680, Ukraine, e-mail:
korchagin.i.n@gmail.com
3MikroPro GMBH, st. Magdeburg 26, b, Gommern, 39245, Germany, e-mail: javadova@micropro.de
1

2. Current situation with the production of Hydrogen
• Problem with the production of hydrogen not yet resolved. The world, does not allow large-scale research for
prospecting and exploration of reserves natural hydrogen. No active search for natural sources of hydrogen
• A natural hydrogen well Bugu-1 provides electricity to a village in Mali. But it is surprising that no one further
studied the deposit. Therefore, until now, the source of hydrogen has not been established there.
• A similar situation in the world was relatively recently with methane. The target product of geological
exploration was oil, and the natural gas fields discovered during geological exploration were simply preserved.
Without any further research. As a result, even now, many regions of the world have been extremely poorly
studied for the presence of methane in their bowels.
• The concept of "initially hydride Earth", according to which the key role in the evolution of the planet is playing
hydrogen. , in the earth's crust it does not contain a fraction of a percent, as was previously thought, and
about 60% by volume and 5% by weight. That is the Earth supersaturated with hydrogen. It is released from
the core of the planet through the earth's crust into the atmosphere, where its constant concentration is kept
at the level of 2.5 million tons. Moreover, in the process of such "hydrogen degassing" of the order of 250
thousand tons of hydrogen goes into space annually.
2

3. Introduction
• In 2019-2021 in various regions of the world, a
large amount of experimental research has been
carried out with the aim of testing frequency-
resonance methods of satellite images and photo
images processing and decoding,
• In the course of the work, the possibility of
purposeful application of mobile direct-
prospecting technology was additionally studied
for hydrogen accumulations detecting in areas of
hydrogen degassing and determining the depths
(intervals) of their occurrence.
• Some results of the experimental investigation in
order to study the possibility of direct-prospecting
methods using for localizing hydrogen
accumulations in the cross-section are given in
EAGE conference 2019
а) б)
в) г)
д) е)
Figure 1 Satellite images of local areas on the
territory of Azerbaijan. Rectangular contours
indicate fragments of frequency-resonance
processing
3

4. Our biggest mistake is not listening in
order to understand. We listen to
answer.
Omar Khayyam and other great
philosophers
Figure 2. Model (fragment) of the Earth's crust: h1 – h3 - thickness of sedimentary rock strata;
1–3 - their dielectric constant;
1-3 - the boundaries of the layers; I – III - antinode of standing waves
I can never forget the first sensations that I experienced when it dawned on my mind that I was watching
something that might have unpredictable consequences for humanity. I felt myself present at the birth of
a new knowledge or at the discovery of a great truth. Nicola Tesla
The developed methods are
based on the standing electric
waves discovered by Nikola
Tesla in 1899
Earth surface
Method
4

5. Remote Sensing
data processing and
interpretation
Forming a Short-Pulsed
Electromagnetic Field
Vertical Electro-
Resonance Sounding
The technology consists of three innovative methods based on
the frequency-resonate concept:
The development of technology took place at the forefront of two
sciences: GEOPHYSICS AND ATMOSPHERIC PHYSICS
Remote Sensing data processing
and interpretation
Fixing pulsed natural
electromagnetic fields of the Earth’s,
it is possible to study also it effects
satellite images of the Earth's
surface in different spectral
channels.
Current development of computer
technology does not allow for the
spectral analysis of all possible
channels recorded by satellites,
where there is also information on
the structure of the Earth and the
objects in it.
To solve this problem author has
used an analog optical processing
method by which it became
possible to carry out the
classification of satellite images and
allocate them abnormal radiation
from various geological bodies in
their frequencies. 5

6. Figure 3 Measuring equipment: on the long line
generator (LLG) (aluminum box) there are three
modifications of the fluxmeter
Figure 4 Sets of frequency resonance
sounding equipment to a depth of 118
km (left) and 25 km (right).
The shown hardware measuring systems have been tested during research at the Ukrainian marine Antarctic Expedition of 2018
Measuring equipment
6

7. Results of instrumental measurements in Latvia and Lithuania
different region
Figure 5. Latvia.
A satellite image of the site
in the area of well drilling
for hydrogen in Latvia. The
drilling location is indicated
by a red marker
Figure 6. Satellite image of
the survey site in Lithuania.
Signals were recorded at
the frequencies of :
depth
scanning the cross-
section with a
step of 10 cm
hydrogen 28 m
the 6th (basalt) group of
igneous rocks
volcano filled with basalts 470 km
the upper edge of
the basalts was
determined at a
depth of 26 m
hydrogen from surface 140-235 m
phosphorus (white) from surface
deep (living) water from surface 317 m
sedimentary rocks of the
9th group (marls) from surface 254 m
igneous rocks of the 6th
group (basalts from surface
The root of the basalt
volcano was identified at
a depth of: 470 km
the upper edge of the
basalts was recorded at
an elevation of: 254 m
Figure 1
Figure 2
Latvia
Lithuania
7

8. Results of instrumental measurements in Ukraina
Figure 7 Satellite image of survey sites in the area of Lake
Chervone (lower right rectangle).
Signals were
recorded at the
frequencies of :
depth
scanning the cross-section
with a step of 10 cm
The lower edge
of basalts was
determined at:
98 k m
the upper edge
was established
by scanning at a
depth of :
100 m
10th group of
sedimentary
(siliceous) rocks
were recorded
on the surface
of:
99 km
the root of the
volcano of these
rocks was
determined at:
723 km
Hydrogen
0 m. migration
into the
atmosphere
By scanning the cross-
section from 80 m, step 10
cm, signals from hydrogen
began to be recorded from
100 m
deep water 112 m
Signals from
dead water were
received at:
71
basalts
By scanning the cross-
section from the surface,
step 1 m recorded from
1010 m and traced to 99
km
The 10th group
of sedimentary
(siliceous) rocks
were obtained
from the lower
part of cross-
section.
On the surface
of 99 km
By fixing the
responses at
different depths
(150, 250, 450,
550, 650, 750,
723 km),
the root of the
volcano with
siliceous rocks
was identified
at a depth of
723 km
1-6 groups of
sedimentary
rocks, oil,
condensate,
amber, carbon
dioxide,
phosphorus
On the surface
of 1010 m
hydrogen were
recorded from
1165 m and
traced to 2 km
By scanning the section
from 1000 m, step 50 cm
carbon dioxide 0
responses from
hydrogen and
phosphorus
absent
deep (living)
water began to
be recorded from
By scanning the cross-
section from 1000 m, step
1 m, 1320 m
hydrogen-rich
water
Additional
examination
of the interval
Figure 3
Figure 7
8

9. Results of instrumental measurements in Poland
Figure 8. Satellite images of survey sites in Poland.
a) b)
Signals were
recorded at the
frequencies of :
depth
scanning the
cross-section
with a step of 10
cm
8th (dolomites), 470 km
9th (marls) ,The
root of the volcano
of marls
98 km
The root of the
volcano of 10th
(siliceous) groups
723 km
The root of the
volcano of 7th
group of
sedimentary rocks
(limestones)
99-217 km
The root of the
volcano of siliceous
rock
217 km
The root of the
ultramafic rocks
470 km
The root of the
volcano of basalts
was determined at
723 km
the 9th (marl) group
of sedimentary
rocks
218-470 km
the upper edge of
the basalts was
fixed at
107 m
hydrogen and
dolomites
107 m
hydrogen and
dolomites
By scanning the
cross-section
from the surface
to a depth of 107
m, step 5 cm 63-
83 m
hydrogen responses
from basalts began
to be recorded
from of living water
scanning the
cross-section
from a depth of
107 m, a step of
10 cm, 139 m
living water 220 m
Figure 4 a)
Figure 4 b)
Figure 8
9

10. Results of instrumental measurements in Ikaria island (Aegean
Sea, Greece
Figure 9. Satellite image of the Ikaria island (Aegean Sea, Greece
Ikaria Island is the island of centenariansю
Water synthesis occurs at a depth of 68. The basalts volcanoes also contain hydrogen. And
hydrogen-rich water has healing properties and promotes longevity
Signals were recorded at
the frequencies of :
depth
scanning the cross-
section with a step
of 10 cm
hydrogen
1) 89-880 m; 2)
2812-3182 m; 3)
3507- (responses
traced up to 15 km)
water
1) 40-93 m; 2) 110-
400 m (traced only
up to 400 m).
When scanning the cross-
section from 70 m, step 10
cm, responses at hydrogen
frequencies from the 8th
group of sedimentary
rocks (dolomites) were
recorded
1) 89-218 m; 2) 244-
356 m; 3) 418-580
m; 4) 650-664 m; 5)
765-812 m; 6) 836-
848 m; 7) 871-880
m; 8) 887-893 m
responses were obtained
from only one sample of
the 8th group of
sedimentary rocks -
oncolytic dolomite, salt
&sedimentary rocks of 1-3
groups
89-893 m,
the root of basalt volcano
was determined at :
By fixing the
responses from
basalts at different
depths (50, 150,
450, 550, 750, 723
km) 723 km
the upper edge of the
basalts
3-4 km
the 14th group of igneous
rocks, in which there are
samples with the
properties of marls
By scanning cross-
section with a step
of 50 cm, signals
from these rocks
were recorded in
the interval of 160-
260 m
By fixing the responses
from basalts at different
depths (50, 150, 450, 550,
750, 723 km), the root of
basalt volcano was
determined at:
723 km
the 8th group of
sedimentary rocks -
oncolytic dolomite;
sedimentary rocks of 1-3
groups ; salt
89-893 m,
Figure 5
Figure 9
10

11. Results of instrumental measurements in Italy
Figure 10. Satellite images of local areas of
hydrogen degassing in Italy.
Signals were recorded at the
frequencies of :
depth
The lower boundary of the
basalts is determined at:
(rectangle 1 ; 2 &3)
99 km
the 9th group of
sedimentary rocks (marls).
(rectangle 1)
99-470 km
the 8th group of
sedimentary rocks
(dolomites),(rectangle 2) ;
the 8th group of
sedimentary rocks (marls)
(rectangle 3)
99-470 km
(rectangle 2)
99-218
(rectangle 3)
the 10th group of
sedimentary rocks (siliceous
rocks)
218-723 km
Figure 7
Figure 10
11

12. Results of instrumental measurements in UK
a) b)
Signals were recorded
at the frequencies of :
depth
scanning the cross-
section with a step of
10 cm
the root of the volcano
of siliceous rocks
470 km
dolomites and basalts
at 723 km
the upper edge of the
basalts
388 m
responses from
dolomites, as well as
hydrogen from
dolomites
At the surface
(depth) of 388 m
hydrogen from
dolomites
from the surface to a
depth of 388 m, step
10 cm 265-378 m
dolomite 265 m
signals at hydrogen
frequencies began to
be recorded from
basalts from: 410 -500 m
living water 425-508 m
Dead water responses
were recorded at: 71 km
Signals from hydrogen
and phosphorus were
recorded at:
0 m, which indicates
their migration into
the atmosphere
Figure 11. Satellite images of survey sites in the
vicinity of London: Heathrow airport area (a); area
of St. Mary Cray, Orpington (b).
Signals were
recorded at the
frequencies of :
depth
scanning the cross-
section with a step
of 10 cm
The upper edge of
the basalts was
determined by
scanning from 0 m,
step 1 cm at
3.5 m
The root of the
basalt volcano was
recorded at
723 km
responses from
hydrogen began to
be recorded from
9 -100 m
living water 25 m
12

13. a)
b) c)
Results of instrumental measurements in
UK & Scotland
Figure 12. Areas of investigation in England: photograph of
Doune Hill and Moorland in Scotland [2] (a); satellite
image of a well at Preston New Road (Lancashire) (b);
photographs of crop circles in England [5] (c).
The results of frequency-resonance processing of satellite
images and photographs of areas of peat bogs in Rivne
and Chernigov regions in Ukraine showed that they are
all located above basalt volcanoes, in the contours of
which hydrogen migrates into the atmosphere
Drilling site in England. During processing a satellite image of a well
for shale gas location in England (figure 8b), responses from
hydrogen and basalts were also recorded. Signals from basalts were
recorded up to 95 km
Signals were
recorded at the
frequencies of :
depth
scanning the
cross-section
with a step of 10
cm
a volcano filled
with sedimentary
rocks of the 9th
group (marls). The
root of the volcano
was identified at:
723 km
Signals from
basalts were
recorded in
4.8-98000 m.
responses from the
9th group of
sedimentary rocks
(marls)
98-723
km
hydrogen from
basalts began to be
recorded from
6 m
living wate 7.5 m
Peatland site in Scotland
Crop circles in England.
On the surface of 0 m
from the upper part of
cross-section, responses
from hydrogen and
phosphorus were
recorded for all circles,
which indicate of these
elements’ migration into
the atmosphere within
areas of circles location
13

14. Results and discussions
A) In the areas and region of the basalt volcano’s location with roots at different depths, signals at hydrogen frequencies
from the surface are almost always recorded.
B) Responses from hydrogen are recorded when scanning section practically from the upper edges of basaltic
volcanoes to their roots
C) In some types of basalt volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is
healing and can be used for wellness purposes. It is advisable to note once again that all surveyed zones and areas of
longevity on Earth are located within (contours) of basalt volcanoes, in which water synthesized at a depth of 68 km
migrates to the surface and is used for water supply and drinking purposes.
D) Hydrogen deposits can be formed by basaltic volcanoes in sealed reservoirs adjacent to basalts. The Mali hydrogen
production site is located outside the contour of the basalt volcano; Hydrogen responses were recorded at the marl well
site. At other survey sites, signals from hydrogen were obtained from dolomites (Carpathians, the island of long-lived
Ikaria), as well as from marls and limestones
E) Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be operatively discovered and
localized during areal exploration using direct-prospecting methods (technology of frequency-resonance processing of
satellite images and photo images, including).
F) The problem of studying reservoirs in crystalline rocks (basalts including) also deserves attention. Direct-prospecting
methods can also be used for this purpose.
G) The facts of hydrogen migration into the atmosphere within the discovered basalt volcanoes in different regions of
the world, recorded by instrumental measurements, should be considered fundamentally important. In general, the above
research results confirm the conclusions of the researchers about the large-scale migration of deep (abiogenic) gas and
hydrogen into the atmosphere of Earth planet!
14

15. Conclusions
• The materials of experimental research of a reconnaissance nature, presented in
the article, clearly demonstrate the working capacity, information content and
promptness of direct-prospecting methods of satellite images and photo images
frequency-resonance processing during an integrated assessment of the prospects
of hydrogen accumulations detecting within survey areas, as well as in the
intervals of cross-section of local site.
• The results of experimental work in various regions indicate the advisability of
using direct-prospecting methods of satellite images and photographs frequency-
resonance processing and decoding to detect and localize zones of hydrogen
accumulation in areas of basalt volcano’s location, as well as within sites of
hydrogen degassing.
• The use of super-operational and low-cost direct-prospecting technology will
significantly accelerate the exploration process for hydrogen, as well as reduce the
financial costs for its implementation
15

16. Additional slides in case of questions
16

17. Technology components
Remote Sensing data processing and interpretation
Furthermore fixing pulsed natural electromagnetic fields of the Earth’s, it is possible to study also it effects satellite images of
the Earth's surface in different spectral channels.
Current development of computer technology does not allow for the spectral analysis of all possible channels recorded by
satellites, where there is also information on the structure of the Earth and the objects in it.
To solve this problem author has used an analog optical processing method by which it became possible to carry out the
classification of satellite images and allocate them abnormal radiation from various geological bodies in their frequencies.
17

18. Fig. 2. A group of carbonate rocks.
Dolomites
Fig. 3. A group of kimberlites and lamproyites Fig. 4. Photographs of samples of
chemical elements and minerals: a)
diamonds; b) hydrogen; c) carbon; d)
amber; e) coal.
Base of magmatic and metamorphic rocks
1. Group of granites and rhyolites. 29 samples.
2. Group of granodiorites and dacites. 7 samples
3. A group of syenites and trachytes. 18 samples.
4. A group of diorites and andesites. 14 samples.
5. Rocks of the lamprophyre group. 14 samples.
6. Group of gabbro and basalt. 32 samples.
7. The group of no-feldspathic no-feldspathoid ultramafic rocks. 20
samples.
8. Group of feldspathoid syenites and phonolites. 23 samples.
9. Group of feldspathoid gabbroids and basaltoids. 6 samples.
10. A group of no-feldspathic ultramafic and mafic rocks. 10
samples.
11. A group of kimberlites and lamproites. 20 samples.
12. Non-silicate rocks. Group of carbonatites. 8 samples.
13. Metamorphic rocks of the granulite group. 10 samples.
14. Metamorphic rocks of the gneiss group. 26 samples.
15. Metamorphic rocks of the group of crystalline schists. 44
samples.
16. Metamorphic rocks of the group of microcrystalline schists
(phyllites). 11 samples.
17. Metamorphosed rocks of the slate group. 2 samples.
18. Iron ore. 5 samples
18

19. Fig. 1. Photos of samples of
oil and gas condensate
Base of sedimentary rocks.
1. Group of detrital rocks. Psefits.
Monomineralic conglomerates. 22 samples.
2. Group of detrital rocks. Psammites 18
samples.
3. Group of detrital rocks. Alevrits,
argillites, clays. 6 samples.
4. Group of detrital and clay rocks. Clay
rocks. Argillite kaolinite. 6 samples.
5. Group of detrital rocks. Clay rocks.
Kaolinite clays. 10 samples.
6. Sedimentary-volcanoclastic rocks. 9
samples.
7. Group of carbonate rocks. Limestone. 24
samples.
8. Group of carbonate rocks. Dolomites. 11
samples.
9. Group of carbonate rocks. Marls. 10
samples.
10. A group of siliceous rocks. 13 samples.
11. Salt. 3 samples.
19