Method for direct hydrocarbon reservoir detection and...

Data processing: measuring – calibrating – or testing – Measurement system in a specific environment – Earth science

Reexamination Certificate

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C367S030000

Reexamination Certificate

active

06473695

ABSTRACT:

BACKGROUND OF THE INVENTION
1. Field of the Invention
This invention relates to a method for detecting and for identifying the type and the geometric dimensions of hydrocarbon deposits and other underground fluid deposits.
2. Description of Prior Art
Various, mostly incomplete methods, which partially complement each other, are known for finding deposits of raw materials and deposits having other anomalies in the crust of the earth. Historically, the detection of such deposits, in particular oil and gas deposits, occurred by accident. This is also still the case to a large extent today and is extremely unsatisfactory. A system has been developed through the frequency of such discoveries which initially only referred to the geological structure of the earth and its development over time.
BACKGROUND
Methods have been developed which are of a technical nature and make confirmation of hypotheses easier but which are not suitable to make definite statements regarding the existence of deposits and their geographic composition. With the continuation of the development and new technical possibilities, methods are known today which somewhat make locating possible deposits easier. Such methods include infrared photographs taken from satellites, magnetic methods and seismic methods, which can provide information regarding the geologic structure, and partially also regarding the type of the deposits. These methods are of the active type, as well as of the passive type.
The amount of knowledge in regard to searching for hydrocarbon deposits is still very limited, and is basically limited to performing seismic, geologic, geo-physical or geo-chemical explorations, all of which, however, still have a more or less experimental character and do not permit direct statements regarding the type of deposits. Exact statements regarding the type of the deposits can only be made once the deposits are physically detected.
Initially, an exploration by seismic methods is performed for finding hydrocarbon deposits in new regions. During this, a signal is generated by one or several sources, whose reflections at inhomogeneous zones is again received by sensors, including geophones, and whose chronological progress is evaluated for the identification of inhomogeneities, including the use of propagation time measurement. The results of such explorations provide information regarding the presence and the extent of inhomogeneities, but not with respect to their cause. Such explorations can be evaluated using two-dimensional, as well as three-dimensional methods, however, they are not suited for determining the type of the inhomogeneity but only provide information as to its existence, which is important but not sufficient.
Many seismic methods are based on the investigation of longitudinal wavefronts, triggered by one or several sources, such as explosions or mechanical vibrations, and whose simple or multiple reflections at inhomogeneities of the subsurface, including the transport medium of the propagation effect, are evaluated for geometrically identifying them by receiving the returning wavefront by sensors, including geophones, distributed over the terrain. It is possible by displacement of the propagation time and damping between the initial signal and the received signal to draw conclusions regarding the geometric extent also of geologic formations in the measuring zone.
Basically all these methods operate by means of a very broad frequency spectrum, mainly above 30 Hz. Although it is possible by evaluating the reflections to recognize formations as an image of the reflection properties, it is not possible to determine the type of these formations. Therefore such explorations are called indirect.
Only further mechanical explorations, namely the driving of exploration bore holes and the sequential examination of drilling cores, provide information regarding the type of rocks in the formations, wherein the information is not definitive as long as an exploration bore hole has not been sunk exactly into the deposit.
These known methods are very expensive to perform, and their result can be to find that which is not sought. It is known that the rate of success of these methods is far below 40%.
Methods have also been proposed for the identification of raw materials which utilize the resonance of the entire mass of a deposit as an indicator of its existence and also its type.
Here, the effect of the resonance on one or several variable mechanical oscillators, an electrical analogy would be an absorption circuit, is to be utilized. One disadvantage of these known methods is that they are almost impossible to perform technically and the frequency of the resonance to be exited, to the extent that it is based on workable deposits, is strictly a function of the geometric spread of the deposits, and not of their nature. In this case, no characteristic values exist for defined types of deposits.
SUMMARY OF THE INVENTION
It is one object of this invention to provide a method by which it is possible to directly determine the presence and the type of hydrocarbon deposits. In contrast to the known methods, this method provides both a statement regarding the type of the deposit as well as its geographic position and extent.
In general, this method relates to the presence of multiphase fluid systems in porous bodies, and in particular, to the exploration of subterranean hydrocarbon deposits.
The method of this invention provides a direct statement regarding the type and extent of deposits without necessarily first sinking exploration drill holes. It thus saves costs, is ecologically advantageous and is also suitable for monitoring changes in the deposits, which is important for an efficient working of such deposits.
This object is achieved by a method for detecting and for identifying the type and the geometric dimensions of hydrocarbon deposits and other underground fluid deposits, as set forth in this specification and in the claims.
The method proposed by this invention relates to a geometric location and a determination of the type of deposits, or of deposits causing anomalies in the crust of the earth, in particular to the presence of oil, gas, gas condensate, or generally, hydrocarbons. Deposits are understood to be the presence of any kind of significant, in particular economically usable concentrations, but also any arbitrary significantly appearing bodies, which can be demarcated with respect to their surroundings. In contrast to the known methods, the method proposed by this invention provides a statement regarding the type and nature of the deposits, as well as a statement regarding their geographic position and geometric extent. The method of this invention is not an indirect method, wherein conclusions are drawn from secondary events, but a direct method which can provide a statement of a quantitative nature, as well as a qualitative nature.
During examination of deposits having multiphase fluid systems in porous bodies, an effect can be observed, which can be used to determine the type of the deposits and which is the subject of this invention.
A hydrocarbon deposit collected in a collector, a lithological formation suitable for receiving hydrocarbons, is a multiphase system with different interior energy. This system is capable of taking on different energetic states. The transition from one energy state into another is connected with energy absorption or energy release. Energy release always manifests itself by the emission of a frequency characteristic of the fluid system, and therefore of the type and nature of the deposit. This frequency is essentially determined by the composition of the fluid system, by the porosity of the collector, and by the permeability of the collector and does not correspond to the natural frequency of the deposit, which perhaps could be generated by natural vibrations in the mass volume, which for example is not a function of the geometry of the deposit.
Moreover, the effect is not a resonance effect in the sense of a periodically exited resonator, but the energy release with

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