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Slide 1 - Continental Bureau

VIEWS: 59 PAGES: 67

									        «Yug-neftegazgeology» LTD
               Kiev, Ukraine

        CONTINENTAL BUREAU INC.
         A Florida USA Corporation



  Passive Magnetic Resonance
Subsurface Exploration Technology


         (PMRSE)
 Passive Magnetic
Resonance Subsurface
Exploration Technology
     (PMRSE)
               History and development of the method

             PMRSE is modern geophysical method based on
                the use of nonlinear geopolariton fields for
             determination of the rocks stress – strained state

In 1983, this method was proposed by Yuriy Bogdanov for the first time.
There have been over 40 publications in the periodicals published by the Academy of
Sciences of Ukraine (geology, geophysics) and in other scientific journals. Results of
the conducted works have been presented at the conferences held in Ukraine,
Russia and other CIS countries, European countries, in Peru, India and others.




Unlike the natural impulse of the electromagnetic radiation method, based on
traditional idea about physics of the subsurface electromagnetic emission, PMRSE
emphasizes record of signals caused by non-linear processes of emission
generation and propagation.
                 History and development of the method
 Manual on Use of Multi-Positioning Analysis of the Earth Radio-Wave Background
 to Prospect and Explore Natural Resources Deposits (a passive geopolariton
  probing method) / Authors: Yu.A. Bogdanov, I.G. Zakharov,
 A.M. Golovashkin, V.N. Pavlovich – 2007
 This Manual has been approved by the State Geological Service of Ukraine

                             Examples of publications:

Bogdanov Ju., Chernjakov A., Uvarov V., Voronin V. Radiation of earth entrails: display and
mechanism // 27 General Assembly of the European Geophysical Society, 22-27 April 2002,
Nice, France. Geophysical Research Abstracts. – 2002. – V. 4. – A-00417.
Yu.A. Bogdanov, V.I. Voronin, V.N. Uvarov, A.M. Chernyakov. Electromagnetic Representation
of the Subsurrface Structure / Geophysical Journal. – 2003. – V. 25, No.4. - p.117-125 (in
Russian).
Yu.A. Bogdanov, I.G. Zakharov, O.F. Tyrnov, M. Hayakawa. Electromagnetic Effects Associated
with Regional Seismic Activity in the Crimea during July-August 2002 // J. Atmospheric
Electricity.- 2003.- Vol. 23, No. 2.- P. 57-67.
Yu.A. Bogdanov, V.P. Kobolev, О.М. Rusakov, I.G. Zakharov. Geopolariton Sensing of Gas-
Bearing Structures in the Blask Sea North-Western Shelf // Geology and Natural Resources of
the World’s Water. – 2007. – No. 1. – p. 77–88 (in Russian).
Laboratory Tests
                  Усредненный график зависимости активности излучений от
                     Average profile of emission activity dependence on
                         нагрузки для призмы размером 10х10х40 см
                              pressure put on prism (10x10x40cm)
  им п./с
                                  Micro-crack formation stage
            450



            400



            350


            300



            250



            200
                                                                                т
                  0       2         4         6         8       10   12    14



                                         Experimental data
                                        экспериментальные данные
          Theory of the Method
There are two types of vibrations – acoustic and optical – in a
solid body with a complicated crystal grating (over one atom in a
low-level cell. Strata (mass) are exactly these solids.
Optical vibrations are characterized by a fact that when k->0
(k – wavevector), atoms in a low-level cell vibrate towards each
other in antiphase, thus their vibrations in ionic crystals cause a
change of a dipole crystal moment, followed by generation of
electromagnetic waves.
Interaction of electromagnetic waves and grating optical
vibrations is especially significant in those areas where
wavevectors and energy of photons and backgrounds is similar.
In such a case it is said that a “mix” of grating
electromagnetic and lateral oscillations is distributed across the
crystal. Grating elementary excitations are called polaritons.
               Features and Efficiency of the Technology
-Use of the wide-band receiving device.
-A geological environment is represented as resonating
layers.
-Length of a recorded emission transmitting wave is
 proportional to the stratum thickness.
-Extinction of the integrated emission is not subordinated to
 the exponential law.
-Width of the anomaly in the first approach does not depend
 on electrical properties of rock masses. It is determined by
geometric parameters of geological objects.



                           Technology Efficiency:

- Allows to explore significantly wider areas in the short period of time
- Provides the information about the physical qualities of layers including oil
 and gas (the presence of hydrocarbons)
- PMRSE technology has no environmental impact
- Allows for laying of tectonic dislocations
- integration with other geophysical methods
                                     PMRSE
                              Instrumentation Base
                     Analyzer of the field activity “Astrogon”

    Specifications:
-   frequency range: 500 Hz – 100 KHz
-   exposition time: 1,0 s; 10, s
-   threshold sensitivity > 5 V
-   automatic registration mode
-   weight – 1,5 kg

    Field conditions:
-   air temperature - 50°C - + 40°C
-   relative air humidity < 90 % (at
    20°C)
-   pressure 450-800 mm Hg
-   continuous work time - 8 hours
    (at ultimate temperature conditions
    ~ 3 hours)
                  Equipment comes in portable, car-mounted
                     and airplane-mounted modifications


                                  Detailed survey

                              Portable equipment allows the
                                study of local anomalies

                              Walking survey possible only small area and
                              special condition


      Medium scale survey

        Example of the car utilization
for the sensing under difficult field conditions
         (diesel or electric vechicles)
                    Aerogeophysical Survey Allows Carrying out
                  Regional-, Small- and Intermediate- Scale Studies
Airborne geophysical system mounted on
   superlight airplane X-32 “Bekas” is
       extensively used in Ukraine




                                         Aerogeophysical prospecting for
                                         fracture water in SAR with the use
                                         of hang-gliders

-   Maximum takeoff weight: ~ 450 kg
-   Working speed range: 80… 140 km/h
-   Altitude limit: > 3 km
-   Work range: ~ 1000 km per day


     Airborne geophysical system
     mounted on light airplane Z-37
    allows works at high altitude for
     accurate localization of large-
            scale structures
                   AEROGEOPHYSICAL SURVEY DEVELOPMENT:
                          small unmanned air vehicle


                                    NII PFM KhAI “ASTROGON-SKY” UNMANNED AERIAL
                                                       COMPLEX




The small unmanned air vehicle (mini-UAV) is the most prospective and
effective aerial platform for accommodation of the Earth sensing equipment.
• The number of UAVs in the complex – 5;
• UAV max launching weight – 10 kg;
• Operational speed range – 60-200 km/h
• Operational height range – 40-4000 m;
• Max flight endurance – 4 h;
• UAV operational radius from the ground control station – up to 200 km;
• System output – up to 6000 running km per 24 h.
                               Survey Technology

h = depth

L = length of survey profile
                                                       Profils

l = length of survey area

r = distance between survey
profile                              Survey area

                                                   r
                           Data processing :
                          a set of properties for
                   geological-geophysical interpretation
   Signs for the
                        Geopolariton       Spatial analysis of
possible presence of
                        intensity map    anomalies amplitudes
 geological objects


                                               Singular
     Geological - geophysical               decomposition
             models
                                            Spatial wavelet
                                              transforms


       Geological - geophysical
                                           Spatial correlation
                output:
                                                analysis
        geological structures
    geological cross-section of the
               deposits                   Indication of depth
                               Data processing technique:
                                                  wavelet analysis
      Intermediate results of signal processing:
an example of the set of signal wavelet decompositions
N


                                                                                               - base function 1
N


                                                                                               - base function 2
N


                                                                                               - base function 3
N


                                                                                               - base function 4
N

                                                                                               - base function 5
N

                                                                                               - base function 6
N

                                                                                               - base function 7
    415500   416500   417500    418500   419500     420500   421500   422500   423500
                                                                                        L, m
                            Data processing technique:
                                      wavelet analysis

                         Example of the fault appearance in
                      the set of signal wavelet decompositions
X - component
N
    base function 1




N
    base function 2




N   base function 3

                                                                             L, m

N
    base function 4
                                               Localization of deep fault extension!

                                        L, m      Accuracy of derived depths:
                                                                ±L
                                                (L – step between measurements)
                                                                                                                                                                                Map of intensity:
                                                                                                                  positive and negative anomalies

                                                                                          Survey area – 274 km2
                                                                                          Distance between tracks – 1 km
                                                                                          Total flight time – 6 hour
                                                                                          Processing time – 10 working shifts



                                                                                                               Caspian sea shelf survey:
                                                                                                                                                        Карта интенсивности ГПИ (горизонтальная составляющая)                                                                                                                                                                                         С

Пр I                                                                                                                                                                                                                                                                                                                                                                                                                Пр I


Пр II                                                                                                                                                                                                                                                                                                                                                                                                               Пр II



Пр III                                                                                                                                                                                                                                                                                                                                                                                                              Пр III



Пр IV                                                                                                                                                                                                                                                                                                                                                                                                               Пр IV



Пр V                                                                                                                                                                                                                                                                                                                                                                                                                Пр V



Пр VI                                                                                                                                                                                                                                                                                                                                                                                                               Пр VI



Пр VII                                                                                                                                                                                                                                                                                                                                                                                                              Пр VII



Пр VIII                                                                                                                                                                                                                                                                                                                                                                                                             Пр VIII
          5117000



                    5118000



                              5119000



                                        5120000



                                                  5121000



                                                            5122000



                                                                      5123000



                                                                                5124000



                                                                                           5125000



                                                                                                     5126000



                                                                                                                5127000



                                                                                                                          5128000



                                                                                                                                    5129000



                                                                                                                                              5130000



                                                                                                                                                            5131000



                                                                                                                                                                      5132000



                                                                                                                                                                                5133000



                                                                                                                                                                                          5134000



                                                                                                                                                                                                    5135000



                                                                                                                                                                                                                  5136000



                                                                                                                                                                                                                            5137000



                                                                                                                                                                                                                                      5138000



                                                                                                                                                                                                                                                5139000



                                                                                                                                                                                                                                                          5140000



                                                                                                                                                                                                                                                                    5141000



                                                                                                                                                                                                                                                                              5142000



                                                                                                                                                                                                                                                                                        5143000



                                                                                                                                                                                                                                                                                                  5144000



                                                                                                                                                                                                                                                                                                            5145000



                                                                                                                                                                                                                                                                                                                      5146000



                                                                                                                                                                                                                                                                                                                                5147000



                                                                                                                                                                                                                                                                                                                                          5148000



                                                                                                                                                                                                                                                                                                                                                    5149000



                                                                                                                                                                                                                                                                                                                                                              5150000



                                                                                                                                                                                                                                                                                                                                                                        5151000



                                                                                                                                                                                                                                                                                                                                                                                  5152000



                                                                                                                                                                                                                                                                                                                                                                                            5153000



                                                                                                                                                                                                                                                                                                                                                                                                          5154000
                    Ш кала нормированных значений интенсивности ГПИ
                    -0.1
                    -0.2
                    -0.3
                    -0.4
                    -0.5
                    -0.6
                    -0.7
                    -0.8
                    -0.9
                    -1.0
                    -1.1
                    -1.2
                    -1.3
                    1.3
                    1.2
                    1.1
                    1.0
                    0.9
                    0.8
                    0.7
                    0.6
                    0.5
                    0.4
                    0.3
                    0.2
                    0.1
                    0.0




                                                                                                                                              No depth details!                                               Рис. 3
Types of Anomalies from Coal
                 Profile Construction Technology




+ other information
Kinds of exploration on coal deposits (Donetsk
Coal Basin, Ukraine):

1) Search (tracking) of dislocations

2) Locating of boundaries and depths of coal layers

3) Search of associative gases (gas methane
   of coal deposits)
Search in coal fields of Matrosskaya Area
           (depth 300-350 m)
                                   A




Mine survey
   data
                               A
                             PMRSE data
Search in coal fields of Matrosskaya Area (depth
  300-350 m) Geophysical profile on line A-A
An Example of Search of Dislocation and
    Methane (Tomashovskaya Area)
Search in Coal Fields of Tomashovskaya Area
             (depth 300-350 m)
                      Profile construction



                          Komsomoletz Donbassa Mine
Geological Profile in Coal Area (Donetsk Region)
      3D model
of Yul’evka coal field
Oil and Gas Geology
Interpretations of PMRSE data obtained in the North
      Edge of Dniepr-Donetsk Basin (Ukraine)
              Map of gas-bearing areas

                                                           Legend: (top - bottom)
                                                             areas predicted by at
                                                           least 3 criterions of GS;
                                                             areas predicted by 1-2
                                                           criterions of GS;
                                                             depth of producing
                                                           horizon in the sediment;
                                                             depth of producing
                                                           horizon in the basement;
                                                              well;
                                                              faults;
                                                              profile line;
                                                              contour of the crystalline
                                                           basement top


                              Valkovsky salt dome   Staroverovsky salt dome
  Geological profile of
the Verbovsky salt dome
                                                                                                 Oil field Oimasha (Kazakhstan)
 Oil traps map
                                                                                                                                                               Geophysical profile on line Г-Г
                  А
4808000                                                                                                                    Legend:
4807000
                                                   Б                                                                        Granite dome boundary                   0.5
                                                                                                                                                                         0
                                                                                       В
4806000
                                                                                                                            Faults:                                -0.5
4805000
                                                                                                                              1st order                                      0


4804000

           Г
                                                                                                                             2nd order
                                                                                                                                                                        -500
4803000
                                                                                                                            Well number
                      16

4802000
                                    25
                                                                                                                            Profile line                            -1000
                                             68
                                                                             20
4801000

                                                                                                                            Oil traps in basement:                  -1500
                                             9
4800000
                                                                    10
                                                                         Г
                                                                                                                             certain
                                                                                                                                                                    -2000
4799000
                                                                                                                             uncertain
                                                   Б
4798000
                                                                                                                            Oil traps in Trias:                     -2500

4797000           А
                                                                                                                               certain
                                                                                       В
                                                                                                                                                                    -3000
          53200
          0
                  533000   534000    53500
                                     0
                                                  536000   537000   53800
                                                                    0
                                                                              539000   540000   541000   542000   543000        uncertain
                                                                                                                                                                    -3500            T

               Granite dome surface                                                                                                                                 -4000



                                                                                                                                                                    -4500
                                                                                                                                                                                     Pz
                                                                                                                                                                    -5000
                                                                                                                                                  Legend:                        0        1000   2000   3000   4000   5000   6000


                                                                                                                                                   Oil-reach deposits
                                                                                                                                                   Bed rocks
                                                                                                                                                   Granites
                                                                                                                                                   Bed rocks disintegration zone
                                                                                                                                                   Crush zone
                                                                                                                                                   Invasion zone
Geology of kimberlite
     (West Ukraine)


    Typical Anomaly of
      kimberlite pipe
Geology of iron-ore deposits
 (CITY DNIEPRORUDNIY) Ukraine

           Typical Anomaly of трубки взрыва
           Survey of the North-West Part of Black Sea Shelf
                           Profile 1: Mud volcano “Vladimir Parshin”
                      (was discovered during 27th voyage Research Vessel
Profiles locations           “Professor Vodyanitskiy” in 2006) (after Yu.
                                            Bogdanov)
                                   wavelet decompositions of signal
   1
                          PMRSE Geography




Surveys of 8 coal and 12 oil fields, iron-ore and other fields by the
    PMRSE Technology with the use of car- and airplane-based
 systems were successfully carried out in the following countries;
Ukraine, Kazakhstan, Turkmenistan, Turkey, Jordan, South Africa,
                   UAE, Argentina, Peru, Russia
                  Profils map
                    (Sample)

                               Distance between profils 250 m.

                               Total area – 50 km2.

                               Length of horizontal profil 18250 m.

                               Length of vertical profil 20000 m.
8000 m




                               Total amount of horizontal profils 27.

                               Total amount of vertical profils 33.

                               Total length of horizontal profils 492750
                               m.

                               Total length of vertical profils 660000.

                               Total length of profils 1152750 m.



         6250 m
                  Estimated complete time of works
Pedestrian works (speed of man – 3 km/h) - Total time 384 hours.
Total days, if to work six hours in a day – 60.

Works on a car (speed of car -15 km/h) – Total time 79 hours.
Total days, if to work six hours in a day – 12.

Works on an airplane (speed of airplane -100 km/h) - Total time 12 hours.
Total days, if to work six hours in a day – 2.

                    Total time of processing of data
Presence of geological information and information of well-boring – 3-4 months.
(Show of a few geological cuts for the perspective districts of the well-boring
without the detailed produce of results). This is results for tests of work.

Presence of geological information and information of well- – 6-7 months.
(The detailed show of results in the perspective areas of the well-boring. Map
of perspective areas for the well-boring, recommendation on the choice of place
of the well-boring, delineation of oil fields.)
         Airplane requirements for implementation
               of works by method of PMRSE.

Light airplane. An airplane must have one or two engines.
Seating accommodation: minimum two (pilot and operator).
Aboard an airplane must be GPS with possibility direct routes
for working profils of flight.
Speed of flight of airplane during implementation of works must
be no more 100 km/h.
Height of flight of airplane -200-300 m. The value of height does
not change during all period of works on an area.
Deviation from basic direction of flight over profil must not
exceed 10 m.
The first standard profil above an area must be a not less
50 km.
When select research area it is necessary to take into
account, profil must come forward outside of area on
distance equal to the research depth.
Requirement on mounting of device “ASTROGON-T”
on an airplane.
                                 1. Mounting of block of
                                    antenna of receiver.
                         HWD of 150x110x70 mm. Weight 1.00
                         kg.
                         Antenna must be fastened from below!
                         Antenna must be mounting more distant
                         than engine.
                         Antenna unites with the block of receiver
                         by a wire (diameter 5 mm, long 20 м).
       2. Mounting of receiver of “ASTROGON-T”
HWD of 1140x140x70 mm. Weight 2.00 kg.
A receiver must be aboard an airplane near the place of
operator (under an armchair). Detector does not require
the special fastening.


                    3. Mounting of antenna of GPS.
            HWD of 130x150x145 mm. Weight 1.50 kg.
            Antenna must be fastened outside, from above!
            Length of wire a 2m. Place of operator must be
            remote from antenna not more length of wire.
            Need two openings.
            For fastening of antenna of GPS. Diameter-
            25mm.
            For the cable of antenna of GPS. Diameter-
            25mm.
           4. Mounting of the power supply block
                     and receiver of GPS
HWD of 300x400x150 mm. Weight 5.00 kg.
The power supply bloc of GPS must be aboard an airplane and
be located not more than a 1-1,5 meter of operator. Power
supply bloc does not require the special fastening.
                            GPS




                                                “ASTROGON-T”



             Possible places of fastening of antenna of GPS and antenna of receiver of
             “ASTROGON-T”.
Instrumentation Base
     Specifications:
frequency range: 500 Hz – 100 KHz
exposition time: 1,0 s; 10, s
threshold sensitivity > 5 V
automatic registration mode
weight – 1,5 kg
     Field conditions:
air temperature - 50°C - + 40°C
relative air humidity < 90 % (at 20°C)
pressure 450-800 mm Hg
continuous work time - 8 hours      (at ultimate temperature conditions
~ 3 hours)

Antenna of "ASTROGON-T" receive only the electromagnetic field of
Earth in the range of frequencies 500 Hz – 100 KHz. The surface of
accepting of antenna is directed towards earth.
        Yug-neftegaz

        Yug-neftegazgeology

        CONTINENTAL BUREAU INC.
         A Florida USA Corporation



INNOVATIVE TECHNOLOGIES

INCREASE OF PRODUCTIVITY
      OF OIL, GAS AND
  GAS-CONDENSATE WELLS

GEOPHYSICAL EXPLORATION
                                    TECHNOLOGY OF THE USE OF THE MULTI
                             POSITION METHOD OF THE ANALYSIS OF RADIOWAVE
                               BACKGROUND OF THE EARTH (METHOD OF THE
                                        GEOPOLARITON SENSING)
                                AT THE DECISION OF NATIONAL ECONOMY TASKS
A company "Yug-Neftegasgeology" is a dynamically developing enterprise, specialized on development
and introduction of untraditional methods of the applied geophysics in area of search and exploring of
minerals.

         The base method of research is the controlled from distance, nondestructive method of the passive
  geo-polaration sensing (GPS), allowing with the high degree of authenticity to expose geometry of oil-
  and-gas bearing structures, ore bodies and violations of breaks. It provides the selection of traps of
  hydrocarbons, deposits of minerals on a depth up to 10(ten) km. Finite data can be given both in two- and
  in three-dimensional interpretation.
         Device basis of method is a complex "Tezey", developed by the group of specialists, headed by the
  Candidate of engineering sciences, corresponding Member of Engineering Academy of Sciences of
  Ukraine Bogdanov Y. A., and it is also patented by an enterprise. It includes modifications of devices,
  intended for the pedestrian, motor-car, aviation and well variants of measuring.
         The method of GPS provides the survey of territories in the real time and considerably reduces
  labor costs by complex approach to conducting of works – the geo-polaration sensing of the explored
  area is conducted with the use of motor transport, aero survey (by the easy and ultralight piloted
  airplanes) and with the use of field expeditionary brigades. It allows to conduct regional, local researches
  and, if necessary, go into detail for the most difficult and problem areas of surface.
         In structure of the Company "Yug-Neftegas" specialists work in areas of geology, hydro-geology,
  engineering geology, geodesy and cartography, physics, chemistry, instrument-making and ecology.
  Among them there are an academician of Academy of Mountain Sciences of Ukraine, academician of Oil
  and Gas Academy of Ukraine, professor of Mountain sciences of Ukraine, 2 doctors and 7 candidates of
  sciences.
GPS, research instruments (antenna and wave signal receiver)
1. INCREASE OF THE PRODUCTIVITY OF WELLS BY
AFFECTING THE BOTTOMHOLE FORMATION ZONE
OF LAYER BY COMPOSITIONS WITH POWDERY
ACIDS


2. TECHNOLOGY OF ISOLATION AND LIMITATION OF
WATER INFLOW IN OIL AND GAS WELLS BY
MAGNETOACTIVE SUBSTANCES


3. TECHNOLOGY OF ACID INFLUENCE ON BOTTOMHOLE
FORMATION ZONE OF LAYERWITH SIMULTANEOUS
DISCONNECTING OF AQUIFEROUS INTERLAYER
4. INCREASE OF THE PRODUCTIVITY OF GASLIFT
WELLS BY FOAMY SYSTEMS



5. TECHNOLOGY OF MULTIPLYING THE PRODUCTIVITY
OF INJECTION WELLS BY USING OF POWDERY
NITRIC ACID


6. TECHNOLOGY OF TREATMENT OF BOTTOMHOLE
FORMATION ZONE OF PRODUCING HORIZONTAL WELLS
7. TECHNOLOGY OF INFLUENCE ON A LAYER IN
BOTTOMHOLE FORMATION ZONE OF WELLS BY
NITRIC-ACID MIXTURE WITHOUT BRIGADE OF
UNDERGROUND REPAIR
                       Chart of connection of equipment at
                       treatment of wells by nitric acid
                       mixture:
                       1. casing pipe;
                       2. pipes of pump-compressors;
                       3. bolt;
                       4,6 reverse valve;
                       5. an ejector;
                       7. setting AGU-8K;
                       8. power-station;
                       9. an aggregate 4AN-700;
                       10. an equipment AU-5;
                       11. an auxiliary aggregate;
                       12. a capacity;
                       13. an aggregate Az-3OA;
                       14. a gathering line
8. TECHNOLOGY OF TREATMENT OF OTTOMHOLE
FORMATION ZONE OF PRODUCING HORIZONTAL
WELLS


9. TECHNOLOGY OF SELECTIVE ISOLATION AND
LIMITATIONS OF WATER INFLOW IN
OIL AND GAS WELLS




10. RENEWAL OF THE PRODUCTIVITY OF GAS AND GAS-
CONDENSATE WELLS IN WATERED LAYER
11. EXPRESS-TECHNOLOGY OF LIMITATION OF
WATER PRODUCTION IN EXTRACTIVE WELLS WITH
THE USE OF FOAMY SYSTEMS


12. LIQUIDATION OF BEHIND-THE-CASING FLOWS IN
EXTRACTIVE WELLS WITH THE USE OF FOAM-CEMENT
SOLUTIONS



13. FINISHING THE WELLS BY DRILLING AND
PUMPING-IN OF INFLOW OF OIL AND GAS BY
DIPHASIC FOAMS
14. TECHNOLOGY OF MULTIPLYING THE
PRODUCTIVITY OF PUMPING WELLS




15. TECHNOLOGY OF INCREASE OF INJECTABILITY OF
INJECTION WELL BY APPLICATION OF SULPHURIC ACID
IN NONACTIVE (POWDERY) FORM



16. INCREASE OF THE PRODUCTIVITY OF PUMPING
WELLS WITH HIGH MAINTENANCE OF GAS
17. TECHNOLOGY OF EFFECTIVE RAISING UP
OF HIGH-VISCOSITY OIL BY DEEP PUMP



18. HYDROPROTECTION OF DEEP BAR PLANTS



19. TECHNOLOGY OF CLEANING OF BOTTOM HOLE OF
GAS AND GAS CONDENSATE WELLS FROM LIQUID
20. PREVENTION OF FORMING OF PARAFFIN
DEPOSITS IN TUBING



21. NITRIC HYDRAULIC JET PERFORATION




22. TEAS-M -UNIVERSAL HIGH-PERFORMANCE
SUPERFICIALLY-ACTIVE MATTER (SAM)
23. TECHNOLOGY OF SELECTIVE ACID FOAM
AFFECTING BOTTOMHOLE FORMATION ZONE
OF LAYERS WITH DIFFERENT GEOLOGICAL
AND MINING CONDITIONS
  RESULTS OF INTRODUCTION
       OF INNOVATIVE
  TECHNOLOGIES, SERVICES
We will consider briefly the results of application of
the offered technologies of multiplying the
productivity of oil and gas wells on the deposits of
Ukraine, Russia, Poland, Syria, China, Bulgaria,
Kazakhstan, Turkmenistan, Turkey, Jordan, South
Africa, UAE, Argentina, Peru, Cuba.

Enclosed are some of the result services and
technology in the following countries:
                                    Azerbaijan
Work on limitation of inflow of water were conducted on three oilfields on wells with
the different mining-geological conditions of bedding of productive layers.
Amount of wells for application of technology - 3 wells.
A depth of wells -1700-3680 m.
Type of collector – terrigenous, sandstone.
Permeability – 100---220 mDarcy.
Results of works on limitation of inflow of water with the use of magnetoactive
substances on the deposits of State Oil Company of Azerbaijan Republic
                                               Syria

Basic perspective deposits are concentrated in North, Western and East parts of
Syria.
• A number of treated wells - 20 wells.
• Depths of wells -700 – 2900 m.
• Type of collector – granular, including clay materials.
• Injectability - 0,08 darcy – 0,5 darcy.
Efficiency of acid treatments on the forcing wells of deposit of Suediya, (Syrian Arabic Republic).
                                Syria
        Basic perspective deposits are concentrated in
           North, Western and East parts of Syria.
Performance of works on application of technology of stimulation of inflow of
oil with the use of complex of acids in a nonactive form on the deposit of
Suediya, (Syrian Arabic Republic)
                             Turkmenistan
A number of treated wells - 3 wells.
A depth of wells -1500-1600 m.
Type of collector – terrigenous.
Permeability – 70---100 mDarcy.

Results of works on the use of technology of isolation and limitation of inflows of water
       with the use of magnetoactive substances on the deposit of Goturdepe
                          of National Concern Turkmenneft
                                                China
Basic perspective deposits are located in North, East and Western parts.
• Amount of wells for works on application of technologies of stimulation of inflows of oil and gas by the use
of powdery chemical reagents on the oilfields of China - 20 wells
• Depths of well – 1100-3800m
• Type of collector – granular, fracture - porous.
• Injectability – 0,1 darcy - 0.78 darcy.




                                                                           Results of stimulation of
                                                                         inflow of oil and gas by the
                                                                          use of powdery chemical
                                                                         reagents on the oilfields of
                                                                                    China
                                      Russia
Basic perspective deposits are concentrated in Western and East Siberia. The approximate
balance supplies of oil in the indicated regions make 800 millions – 1 mld. tons of oil.
• A number of treated wells - 480 wells.
• Depths of wells are 1600 – 3100 m.
• Type of collector – granular, fracture - porous.
• Permeability – 0,1 darcy – 0,6 darcy.




                                                                     Efficiency of treatment
                                                                     by acid compositions
                                                                       on the deposits of
                                                                         Western Siberia
                  Russia

Results of the use of magneto-active substances on
      Var'egansk deposit of Western Siberia
                                  Poland
Basic deposits are concentrated in Prikarpatskaya area.
• A number of treated wells - 20 wells.
• A depth of well is 800-1700 m.
• Type of collector – granular
• Injectability – 0,2 darcy – 0,4 darcy.

        Performance of works on application of technology of gas recovery on
           the gas deposit of Zelenogursk oil-and-gas enterprise (Poland)
                                       Bulgaria
Basic deposits are confined to the cracks, fracture - porous and coal layers in the north in
onshore part of country, drilled on a coal layer with the supplies of methane gas.
• Type of collector – difficult, combined: coal, including sandstones.
• Depth of mining holes - 1100 – 1500 m.
• Injectability – 0,01 darcy – 0,03 darcy.

                Results of technology of treatment of wells by the use of
                             magnetically-active substances
                          Ukraine
Ukraine has two oil-and-gas bearing regions: on the east -
"Dnepr-Donetsk cavern (DDC)", on the west - "Deposits of
Predkarpat'e (DP)".
Deposits of the Dnepr-Donetsk cavern:
        Depth of wells - 1500-5700 m
        Type of collector – granular, fracture-porous.
        Permeability – 0,08 darcy – 0,95 darcy.
Deposits of Predkarpat'e:
        Depth of wells - 1400-5300 m..
        Type of collector – granular, with large content of clay
particles (so-called "menilite deposits").
        Permeability - 0,01 darcy – 0,3 darcy.

(The following graphs are tables # 1, 2, 3, 4, 5):
                 Table 1 Performance of works on stimulation of inflow of oil by the use of powdery
                 chemical agents on the oilfields of Ukraine




Table 2 Performance of works on application of technology of stimulation of gas inflow, offered on
Yul'evsk gas-condensate deposit of DK “Khar'kovgazdobycha” and on the deposit of “Vizhomlya” DK
“L'vovgazdobycha” by acid composition in a nonactive form
Table 3 Results of application of technology of bearing-out of liquid on the
deposits of OAO "Ukrneft" and in the Republic of Poland
                  Table 4 Results of application of diphasic foams in gaslift wells on Glinsko-
                  Rozbyshevsk deposit of NGDU "Poltavaneftegaz" (in a numerator - information on
                  debit before the use of technology, in a denominator – after).




Table 5 Results of application of express technology of limitation of water production on the deposits of
NGDU "Dolinaneftegaz" in difficult mining-geological conditions (menilite deposits)
                Yug-neftegazgeology

                 Yug-neftegaz
Our advanced high tech computerized equipment and technology , can explore the
sub-surface of the Earth to a depth of 60 km. The graph is an actual result of our
technology in Ukraine.
            “Yug-neftegazgeology” LTD
                         Kiev, Ukraine

                “Yug-neftegaz“ LLC
                     Odessa, Ukraine


Representative
          CONTINENTAL BUREAU INC.
Gabriel Mnayarji        A Florida USA Corporation
P.O. Box 780696
Orlando, Florida, USA 32878
www.continentalbureau.com
Email: cbureauusa@aol.com
Tel. (321) 947-6586
Thank you for your interest in our technology.

								
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