Vertical seismic profile

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Layout of a Vertical Seismic Profile Station Vertical Seismic Profiling Survey.jpg
Layout of a Vertical Seismic Profile Station

In geophysics, vertical seismic profile (VSP) is a technique of seismic measurements used for correlation with surface seismic data. The defining characteristic of a VSP (of which there are many types) is that either the energy source, or the detectors (or sometimes both) are in a borehole. In the most common type of VSP, hydrophones, or more often geophones or accelerometers, in the borehole record reflected seismic energy originating from a seismic source at the surface.

There are numerous methods for acquiring a vertical seismic profile (VSP). Zero-offset VSPs (A) have sources close to the wellbore directly above receivers. Offset VSPs (B) have sources some distance from the receivers in the wellbore. Walkaway VSPs (C) feature a source that is moved to progressively farther offset and receivers held in a fixed location. Walk-above VSPs (D) accommodate the recording geometry of a deviated well, having each receiver in a different lateral position and the source directly above the receiver. Salt-proximity VSPs (E) are reflection surveys to help define a salt-sediment interface near a wellbore by using a source on top of a salt dome away from the drilling rig. Drill-noise VSPs (F), also known as seismic-while-drilling (SWD) VSPs, use the noise of the drill bit as the source and receivers laid out along the ground. Multi-offset VSPs (G) involve a source some distance from numerous receivers in the wellbore. [1] [2]

A vertical seismic profile is constructed to identify a value known as a source wavelet. This is useful when it comes to a process known as deconvolution. Deconvolution allows for a more readable and more focused VSP. [2] The idea is that the VSP reports any abnormal seismic activity and deconvolution allows for a more focused profile on these abnormal activities. VSPs are used to measure a seismic signal at depth and with that measurement the wavelength at the source of the seismic activity is easily found. With the measurement of the source wavelet, geophysicists can carry out deconvolution on the VSP and decrease the reports of all seismic activity and limit the reports to just abnormal or extreme changes in seismic activity. [2]

In recent years, using a VSP has become more popular in regards to reducing well placement risks as well as improving the monitoring of such wells. [3] The advancement in technology for well monitoring has made VSPs more accurate and more precise with the use of very long baseline interferometry (VLBI). [3] VLBI is an astronomical radio antenna technique that allows for high resolution imaging on a spatial scale. Therefore, using these techniques to create a seismic profile produces incredibly accurate images of wavelets and enhances determination of source wavelets. VSPs are more suitable than other seismic profiles to host the equipment for VLBI. [3] The long vertical length required to create a borehole for a VSP allows for the equipment of a VLBI to analyze data within a larger region. VLBI can produce high resolution results within a region upwards of 50 km. [3]

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A synthetic seismogram is the result of forward modelling the seismic response of an input earth model, which is defined in terms of 1D, 2D or 3D variations in physical properties. In hydrocarbon exploration this is used to provide a 'tie' between changes in rock properties in a borehole and seismic reflection data at the same location. It can also be used either to test possible interpretation models for 2D and 3D seismic data or to model the response of the predicted geology as an aid to planning a seismic reflection survey. In the processing of wide-angle reflection and refraction (WARR) data, synthetic seismograms are used to further constrain the results of seismic tomography. In earthquake seismology, synthetic seismograms are used either to match the predicted effects of a particular earthquake source fault model with observed seismometer records or to help constrain the Earth's velocity structure. Synthetic seismograms are generated using specialized geophysical software.

<span class="mw-page-title-main">Seismic interferometry</span>

Interferometry examines the general interference phenomena between pairs of signals in order to gain useful information about the subsurface. Seismic interferometry (SI) utilizes the crosscorrelation of signal pairs to reconstruct the impulse response of a given media. Papers by Keiiti Aki (1957), Géza Kunetz, and Jon Claerbout (1968) helped develop the technique for seismic applications and provided the framework upon which modern theory is based.

<span class="mw-page-title-main">Surface wave inversion</span>

Seismic inversion involves the set of methods which seismologists use to infer properties through physical measurements. Surface-wave inversion is the method by which elastic properties, density, and thickness of layers in the subsurface are obtained through analysis of surface-wave dispersion. The entire inversion process requires the gathering of seismic data, the creation of dispersion curves, and finally the inference of subsurface properties.

Oil well control is the management of the dangerous effects caused by the unexpected release of formation fluid, such as natural gas and/or crude oil, upon surface equipment of oil or gas drilling rigs and escaping into the atmosphere. Technically, oil well control involves preventing the formation gas or fluid (hydrocarbons), usually referred to as kick, from entering into the wellbore during drilling or well interventions.

<span class="mw-page-title-main">Near-surface geophysics</span> Geophysics of first tens of meters below surface

Near-surface geophysics is the use of geophysical methods to investigate small-scale features in the shallow subsurface. It is closely related to applied geophysics or exploration geophysics. Methods used include seismic refraction and reflection, gravity, magnetic, electric, and electromagnetic methods. Many of these methods were developed for oil and mineral exploration but are now used for a great variety of applications, including archaeology, environmental science, forensic science, military intelligence, geotechnical investigation, treasure hunting, and hydrogeology. In addition to the practical applications, near-surface geophysics includes the study of biogeochemical cycles.

Multidimensional seismic data processing forms a major component of seismic profiling, a technique used in geophysical exploration. The technique itself has various applications, including mapping ocean floors, determining the structure of sediments, mapping subsurface currents and hydrocarbon exploration. Since geophysical data obtained in such techniques is a function of both space and time, multidimensional signal processing techniques may be better suited for processing such data.

<span class="mw-page-title-main">Seismic data acquisition</span>

Seismic data acquisition is the first of the three distinct stages of seismic exploration, the other two being seismic data processing and seismic interpretation. Seismic acquisition requires the use of a seismic source at specified locations for a seismic survey, and the energy that travels within the subsurface as seismic waves generated by the source gets recorded at specified locations on the surface by what is known as receivers.

References

  1. "Diagram of VSP configurations". Schlumberger. Retrieved 4 August 2014.
  2. 1 2 3 Rector, J.W.; Mangriotis, M.D. (2011). "Vertical Seismic Profile". In Gupta, Harsh K. (ed.). Encyclopedia of Solid Earth Geophysics. Encyclopedia of Earth Sciences Series. Dordrecht: Springer Netherlands. doi : 10.1007/978-90-481-8702-7. ISBN   978-90-481-8701-0.
  3. 1 2 3 4 Onajite, Enwenode (2014), Onajite, Enwenode (ed.), "Chapter 7 - Understanding Deconvolution", Seismic Data Analysis Techniques in Hydrocarbon Exploration, Oxford: Elsevier, pp. 93–103, doi : 10.1016/b978-0-12-420023-4.00007-1, ISBN   978-0-12-420023-4