CN108169800A - Controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method - Google Patents
Controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method Download PDFInfo
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- CN108169800A CN108169800A CN201711443327.6A CN201711443327A CN108169800A CN 108169800 A CN108169800 A CN 108169800A CN 201711443327 A CN201711443327 A CN 201711443327A CN 108169800 A CN108169800 A CN 108169800A
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- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
- G01V3/38—Processing data, e.g. for analysis, for interpretation, for correction
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- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
- G01V3/08—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation operating with magnetic or electric fields produced or modified by objects or geological structures or by detecting devices
- G01V3/083—Controlled source electromagnetic [CSEM] surveying
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- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
- G01V3/08—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation operating with magnetic or electric fields produced or modified by objects or geological structures or by detecting devices
- G01V3/083—Controlled source electromagnetic [CSEM] surveying
- G01V2003/086—Processing
Abstract
The invention discloses a kind of controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating methods, belong to the artificial field source frequency domain electromagnetic method data processing field of geophysical exploration, and the method includes：Step A, the current data of time-domain, electric field data, magnetic field data are transformed to frequency domain data using Fourier transformation；Step B, electric field data and magnetic field data in frequency domain data, are calculated Ka Ni Asian TV Station resistivity and phase；Step C, near-field effect is judged whether according to Ka Ni Asian TV Station resistivity and phase property, such as there are near-field effects；Correction parameter is obtained by normalized theoretical the ratio between electric field data and the normalized electric field data of electric current, so as to correct the form partition of apparent resistivity curve, restore low-frequency data form, the data that can visit source audio magnetotelluric method is enable greatly to be applied in data inversion, so as to obtain more underground electrical structure information.
Description
Technical field
The present invention relates to the artificial field source frequency domain electromagnetic method data processing field of geophysical exploration, more specifically,
The invention mainly relates to a kind of controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating methods.
Background technology
The controlled-source audiomagnetotellurics method used at present, it is impossible to work near field region, limit controllable source audio the earth
The exploration construction and data processing of electromagnetic method.At present, the work of controlled-source audiomagnetotellurics method is carried out, it is ensured that receives and dispatches away from big
In 3 to 5 times of skin depth, to achieve the purpose that far field is observed.But since underground apparent resistivity is our exploration targets, because
This, skin depth is a unknown quantity, can only generally be estimated according to existing data.This has resulted in practical transmitting-receiving away from inclined
It is small, it can not meet far zone condition, the apparent resistivity curve finally obtained has apparent near-field effect, and (apparent resistivity curve is in 45 degree
Rise, 0) phase levels off to.At this moment the apparent resistivity curve obtained, it is impossible to truly corresponsively under electrical structure.Therefore,
It needs to research and develop a kind of near-field calibrating method, restores the true apparent resistivity information in apparent resistivity curve.
Invention content
One of the aims of the present invention is to provide...in response to the above drawbacks a kind of controlled-source audiomagnetotellurics method apparent resistivities
Near-field calibrating method is likely to occur near-field effect generation it is expected to solve controlled-source audiomagnetotellurics method apparent resistivity curve
Form partition causes the technical problems such as 45 degree of risings of low-frequency data.
To solve the technical issues of above-mentioned, the present invention uses following technical scheme：
A kind of controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method provided by the present invention, the method
Include the following steps：
Step A, the current data of time-domain, electric field data, magnetic field data are transformed to frequency domain using Fourier transformation
Data；
Step B, electric field data and magnetic field data in frequency domain data, are calculated Ka Ni Asian TV Station resistivity and phase
Position；
Step C, near-field effect is judged whether according to Ka Ni Asian TV Station resistivity and phase property, such as there are near field effects
Should, then continue next step, on the contrary then step terminates；
Step D, using the current data of frequency domain, electric current normalization is carried out to the electric field data of frequency domain, is obtained
The normalized electric field data of electric current of frequency domain；
Step E, according to the Ka Ni Asian TV Station resistivity for having near-field effect, normalized theoretical electric field data is calculated；
Step F, according to normalized theoretical the ratio between electric field data and the normalized electric field data of electric current, correction ginseng is obtained
Number, is corrected the Ka Ni Asian TV Station resistivity data for having near-field effect using correction parameter.
Preferably, further technical solution is：The current data of time-domain, electric field data, magnetic field in the step A
Data are to survey to obtain by instrument.
Further technical solution is：Ka Ni Asian TV Station resistivity and phase property are judged whether to deposit in the step C
It is to judge according to whether apparent resistivity rises into 45 degree with phase saturation in near-field effect.
Further technical solution is：The method further includes step G, according to the Ka Ni Asian TV Station resistivity after correction
Data corrected after Ka Ni Asian TV Station resistivity curve.
Further technical solution is：The method further includes step H, according to the Ka Ni Asian TV Station resistivity after correction
Curve calculates phase, so as to the phase after being corrected.
Further technical solution is：Normalized theoretical electric field data is calculated by following formula in step E：
In formula,For normalized theoretical electric field data, Idl is unit electric dipole moment, and ρ is Ka Ni Asian TV Station resistivity, and e is
Natural constant, i are imaginary unit, and r is transmitting-receiving away from k is wave number；Eelctric dipole is enabled to be located at coordinate origin, measuring point is located at (x, y), formula
Middle y is the ordinate of measuring point.
Further technical solution is：The step D carries out electric current normalizing by following formula to the electric field data of frequency domain
Change correction：
In formula,For the normalized electric field data of electric current, ExFor the electric field data of frequency domain,It is normalized for electric current
Magnetic field data, current datas of the I for frequency domain, HyMagnetic field data for frequency domain.
Further technical solution is：The step B calculates Ka Ni Asian TV Station resistivity by following formula：
In formula, ρ is Ka Ni Asian TV Station resistivity, and μ is magnetic conductivity, and ω is angular frequency, ExFor the electric field data of frequency domain, HyFor
The magnetic field data of frequency domain.
Compared with prior art, one of beneficial effects of the present invention are：Pass through normalized theoretical electric field data and electric current
The ratio between normalized electric field data obtains correction parameter, so as to correct the form partition of apparent resistivity curve, restores low-frequency data
Form enables the data that can visit source audio magnetotelluric method to be greatly applied in data inversion, so as to obtain more
More underground electrical structure information, while a kind of controlled-source audiomagnetotellurics method apparent resistivity near field school provided by the present invention
Correction method is easily achieved, and the resistivity that can be surveyed in all kinds of places is corrected, and application range is wide.
Description of the drawings
Fig. 1 is for illustrating the electric field of model 1 and apparent resistivity calibration coordinate figure in one embodiment of the invention；
Fig. 2 is the phasing coordinate diagram for illustrating model 1 in one embodiment of the invention；
Fig. 3 is for illustrating the electric field of model 2 and apparent resistivity calibration coordinate figure in one embodiment of the invention；
Fig. 4 is the phasing coordinate diagram for illustrating model 2 in one embodiment of the invention；
Specific embodiment
The present invention is further elaborated below in conjunction with the accompanying drawings.
One embodiment of the present of invention is a kind of controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method, the party
Method includes the following steps：
Step S1, the current data of time-domain, electric field data, magnetic field data are transformed to frequency domain using Fourier transformation
Data；
In this step, aforementioned current data, electric field data, magnetic field data are both needed to survey to obtain by instrument；
Step S2, electric field data and magnetic field data in frequency domain data, be calculated Ka Ni Asian TV Station resistivity and
Phase；
In this step, Ka Ni Asian TV Station resistivity can be calculated by following formula：
In formula, ρ is Ka Ni Asian TV Station resistivity, and μ is magnetic conductivity, and ω is angular frequency, ExFor the electric field data of frequency domain, HyFor
The magnetic field data of frequency domain.
Step S3, near-field effect is judged whether according to Ka Ni Asian TV Station resistivity and phase property, such as there are near field effects
Should, then continue next step, on the contrary then step terminates；
In this step, near-field effect is judged whether to Ka Ni Asian TV Station resistivity and phase property, basis can be used
Whether apparent resistivity rises into 45 degree judges with phase saturation；
Step S4, using the current data of frequency domain, electric current normalization is carried out to the electric field data of frequency domain, is obtained
The normalized electric field data of electric current of frequency domain；
In this step, can electric current normalization be carried out to the electric field data of frequency domain by following formula：
In formula,For the normalized electric field data of electric current, ExFor the electric field data of frequency domain,It is normalized for electric current
Magnetic field data, current datas of the I for frequency domain, HyMagnetic field data for frequency domain.
Step S5, according to the Ka Ni Asian TV Station resistivity for having near-field effect, normalized theoretical electric field data is calculated；
In this step, normalized theoretical electric field data can be calculated by following formula：
In formula,For normalized theoretical electric field data, Idl is unit electric dipole moment, and ρ is Ka Ni Asian TV Station resistivity, and e is
Natural constant, i are imaginary unit, and r is transmitting-receiving away from k is wave number；Eelctric dipole is enabled to be located at coordinate origin, measuring point is located at (x, y), formula
Middle y is the ordinate of measuring point.
Step S6, according to normalized theoretical the ratio between electric field data and the normalized electric field data of electric current, correction ginseng is obtained
Number, is corrected the Ka Ni Asian TV Station resistivity data for having near-field effect using correction parameter.
According to another embodiment of the invention, it can also continue to carry out following steps：
Step S7, the Ka Ni Asian TV Station resistivity curve after being corrected according to the Ka Ni Asian TV Station resistivity data after correction；
Step S8, phase is calculated according to the Ka Ni Asian TV Station resistivity curve after correction, so as to the phase after being corrected.
Due to above-described embodiment it is found that method provided by the present invention substantially step is：
The first step, during controlled-source audiomagnetotellurics method field data collection, the electric current transmitted by record current transmitter
Signal i (t), the geographical position coordinates (x, y) of transmitter, the geographical position coordinates (m, n) of receiver, orthogonal electric field Ex(t)
With magnetic field Hy(t) signal, thus to obtain field initial data.
Second step, by the current signal i (t) of time-domain, electric field Ex(t) and magnetic field Hy(t) signal is turned by Fourier Tranform
It is changed to the current signal I of frequency domain, electric field ExWith magnetic field Hy。
Third walks, to electric field ExWith magnetic field HyCarry out current correction：
4th step calculates Ka Ni Asian TV Station resistivity
5th step, according to Ka Niya computation of apparent resistivity theory electric field datas
6th step, according to theoretical electric field dataWith the electric field data of correctionThe ratio between obtain correction parameter.
7th step, according to correction parameter correction card Buddhist nun Asian TV Station resistivity.
Based on the above-mentioned method of the present invention, carry out proving program using two-layer model：
Verify model 1：Middle layer is resistive formation, and resistivity is respectively：10 Ω m, 100 Ω m, 10 Ω m, thickness point
Other 1000m, 2000m, are received and dispatched away from r=10000m.Wherein ExcFor theoretical electric field, ExFor survey electric field, verification coordinate diagram such as Fig. 1 with
Shown in Fig. 2.
Verify model 2：Middle layer is low resistivity layer.Resistivity is respectively：100 Ω m, 10 Ω m, 100 Ω m, thickness
Respectively：1000m, 2000m are received and dispatched away from r=10000m, and verification coordinate diagram is as shown in Figure 3 and Figure 4..
Than that described above, it is also necessary to which explanation is " one embodiment " spoken of in the present specification, " another implementation
Example ", " embodiment " etc. refer to that the specific features, structure or the feature that combine embodiment description are included in the application summary
Property description at least one embodiment in.It is not centainly to refer to same reality that statement of the same race, which occur, in multiple places in the description
Apply example.Furthermore, it is understood that when describing a specific features, structure or feature with reference to any embodiment, what is advocated is knot
Other embodiment is closed to realize that this feature, structure or feature are also fallen within the scope of the present invention.
Although reference be made herein to invention has been described for multiple explanatory embodiments of the invention, however, it is to be understood that
Those skilled in the art can be designed that a lot of other modifications and embodiment, these modifications and embodiment will be fallen in this Shen
It please be within disclosed spirit and spirit.More specifically, it is disclosed, in the range of drawings and claims in the application, it can
A variety of variations and modifications are carried out with the building block to theme combination layout and/or layout.In addition to building block and/or layout
Outside the variations and modifications of progress, to those skilled in the art, other purposes also will be apparent.
Claims (8)
1. a kind of controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method, it is characterised in that the method is included such as
Lower step：
Step A, the current data of time-domain, electric field data, magnetic field data are transformed to frequency domain data using Fourier transformation；
Step B, electric field data and magnetic field data in frequency domain data, are calculated Ka Ni Asian TV Station resistivity and phase；
Step C, near-field effect is judged whether according to Ka Ni Asian TV Station resistivity and phase property, such as there are near-field effect, then
Continue next step, on the contrary then step terminates；
Step D, using the current data of frequency domain, electric current normalization is carried out to the electric field data of frequency domain, obtains frequency
The normalized electric field data of electric current in domain；
Step E, according to the Ka Ni Asian TV Station resistivity for having near-field effect, normalized theoretical electric field data is calculated；
Step F, according to normalized theoretical the ratio between electric field data and the normalized electric field data of electric current, correction parameter is obtained, profit
The Ka Ni Asian TV Station resistivity data for having near-field effect is corrected with correction parameter.
2. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 1, it is characterised in that：
The current data of time-domain, electric field data, magnetic field data are to survey to obtain by instrument in the step A.
3. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 1, it is characterised in that：
Near-field effect is judged whether to Ka Ni Asian TV Station resistivity and phase property in the step C, be according to apparent resistivity whether
Rise into 45 degree and judge with phase saturation.
4. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 1, it is characterised in that：
The method further includes step G, corrected according to the Ka Ni Asian TV Station resistivity data after correction after Ka Ni Asian TV Station resistance
Rate curve.
5. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 4, it is characterised in that：
The method further includes step H, calculates phase according to the Ka Ni Asian TV Station resistivity curve after correction, after being corrected
Phase.
6. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 1, it is characterised in that
Normalized theoretical electric field data is calculated by following formula in the step E：
In formula,For normalized theoretical electric field data, Idl is unit electric dipole moment, and ρ is Ka Ni Asian TV Station resistivity, and e is nature
Constant, i are imaginary unit, and r is transmitting-receiving away from k is wave number；Eelctric dipole is enabled to be located at coordinate origin, measuring point is located at (x, y), and y is in formula
The ordinate of measuring point.
7. the controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 1 or 6, feature exist
Electric current normalization is carried out to the electric field data of frequency domain by following formula in the step D：
In formula,For the normalized electric field data of electric current, ExFor the electric field data of frequency domain,For the normalized magnetic field number of electric current
According to, current datas of the I for frequency domain, HyMagnetic field data for frequency domain.
8. controlled-source audiomagnetotellurics method apparent resistivity near-field calibrating method according to claim 7, it is characterised in that
The step B calculates Ka Ni Asian TV Station resistivity by following formula：
In formula, ρ is Ka Ni Asian TV Station resistivity, and μ is magnetic conductivity, and ω is angular frequency, ExFor the electric field data of frequency domain, HyFor frequency
The magnetic field data in domain.
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Cited By (10)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN109470135A (en) * | 2018-11-12 | 2019-03-15 | 吉林大学 | CSAMT data inactivity bearing calibration |
| CN109884714A (en) * | 2019-03-05 | 2019-06-14 | 中国地质科学院地球物理地球化学勘查研究所 | A kind of controllable source method for electromagnetically measuring, device and its storage medium |
| CN110348568A (en) * | 2019-07-16 | 2019-10-18 | 山东科技大学 | A kind of deep Mined-Out Areas method suitable for strong electromagnetic area |
| CN110989006A (en) * | 2019-12-25 | 2020-04-10 | 中国地质科学院地球物理地球化学勘查研究所 | Static displacement correction method and device in controllable source electromagnetic method measurement and intelligent terminal |
| CN111273356A (en) * | 2020-03-29 | 2020-06-12 | 中南大学 | Active power conduction method based on monitoring potential correction |
| CN111965712A (en) * | 2020-10-21 | 2020-11-20 | 国网江西省电力有限公司电力科学研究院 | Method for correcting static effect of controllable source audio magnetotelluric method |
| CN112379449A (en) * | 2020-10-30 | 2021-02-19 | 中国石油天然气集团有限公司 | Method and device for processing electromagnetic data of controllable source |
| CN114047551A (en) * | 2021-10-13 | 2022-02-15 | 中国舰船研究院 | Real-time monitoring implementation method based on WEM data |
| CN115437024A (en) * | 2022-11-07 | 2022-12-06 | 四川省冶勘设计集团有限公司 | Double-parameter processing method for non-planar wave data of electromagnetic field signal of artificial source frequency domain |
| GB2610366A (en) * | 2020-05-28 | 2023-03-01 | Univ Jiangsu | "Standardized temperature" -based online estimation method for state of health of battery within wide temperature range |
Citations (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| US20090096457A1 (en) * | 2005-06-09 | 2009-04-16 | Srnka Leonard J | Method for determining earth vertical electrical anisotropy in marine electromagnetic surveys |
| CN104656156A (en) * | 2013-11-22 | 2015-05-27 | 中国石油天然气集团公司 | Magnetic reference processing method for acquiring data in three dimensions audio-frequency magnetotelluric sounding |
| CN105911595A (en) * | 2016-02-02 | 2016-08-31 | 中国科学院地质与地球物理研究所 | Method and apparatus for obtaining controllable source audio-frequency magnetotelluric (CSAMT) apparent phase information |
| WO2016137500A1 (en) * | 2015-02-27 | 2016-09-01 | Halliburton Energy Services, Inc. | Formation resistivity measurement apparatus, systems, and methods |
-
2017
- 2017-12-27 CN CN201711443327.6A patent/CN108169800B/en active Active
Patent Citations (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| US20090096457A1 (en) * | 2005-06-09 | 2009-04-16 | Srnka Leonard J | Method for determining earth vertical electrical anisotropy in marine electromagnetic surveys |
| CN104656156A (en) * | 2013-11-22 | 2015-05-27 | 中国石油天然气集团公司 | Magnetic reference processing method for acquiring data in three dimensions audio-frequency magnetotelluric sounding |
| WO2016137500A1 (en) * | 2015-02-27 | 2016-09-01 | Halliburton Energy Services, Inc. | Formation resistivity measurement apparatus, systems, and methods |
| CN105911595A (en) * | 2016-02-02 | 2016-08-31 | 中国科学院地质与地球物理研究所 | Method and apparatus for obtaining controllable source audio-frequency magnetotelluric (CSAMT) apparent phase information |
Non-Patent Citations (1)
| Title |
|---|
| 詹少全 等: "CSAMT全区视电阻率电场正演迭代拟合近场校正方法", 《物探与化探》 * |
Cited By (16)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN109470135A (en) * | 2018-11-12 | 2019-03-15 | 吉林大学 | CSAMT data inactivity bearing calibration |
| CN109884714B (en) * | 2019-03-05 | 2021-11-16 | 中国地质科学院地球物理地球化学勘查研究所 | Controllable source electromagnetic measurement method, device and storage medium thereof |
| CN109884714A (en) * | 2019-03-05 | 2019-06-14 | 中国地质科学院地球物理地球化学勘查研究所 | A kind of controllable source method for electromagnetically measuring, device and its storage medium |
| CN110348568A (en) * | 2019-07-16 | 2019-10-18 | 山东科技大学 | A kind of deep Mined-Out Areas method suitable for strong electromagnetic area |
| CN110348568B (en) * | 2019-07-16 | 2021-02-23 | 山东科技大学 | Deep goaf detection method suitable for strong electromagnetic interference area |
| CN110989006A (en) * | 2019-12-25 | 2020-04-10 | 中国地质科学院地球物理地球化学勘查研究所 | Static displacement correction method and device in controllable source electromagnetic method measurement and intelligent terminal |
| CN111273356A (en) * | 2020-03-29 | 2020-06-12 | 中南大学 | Active power conduction method based on monitoring potential correction |
| CN111273356B (en) * | 2020-03-29 | 2021-04-16 | 中南大学 | Active power conduction method based on monitoring potential correction |
| GB2610366B (en) * | 2020-05-28 | 2023-08-23 | Univ Jiangsu | On-line estimation method of battery state of health in wide temperature range based on standardized temperature |
| GB2610366A (en) * | 2020-05-28 | 2023-03-01 | Univ Jiangsu | "Standardized temperature" -based online estimation method for state of health of battery within wide temperature range |
| CN111965712B (en) * | 2020-10-21 | 2021-03-02 | 国网江西省电力有限公司电力科学研究院 | Method for correcting static effect of controllable source audio magnetotelluric method |
| CN111965712A (en) * | 2020-10-21 | 2020-11-20 | 国网江西省电力有限公司电力科学研究院 | Method for correcting static effect of controllable source audio magnetotelluric method |
| CN112379449A (en) * | 2020-10-30 | 2021-02-19 | 中国石油天然气集团有限公司 | Method and device for processing electromagnetic data of controllable source |
| CN114047551A (en) * | 2021-10-13 | 2022-02-15 | 中国舰船研究院 | Real-time monitoring implementation method based on WEM data |
| CN115437024A (en) * | 2022-11-07 | 2022-12-06 | 四川省冶勘设计集团有限公司 | Double-parameter processing method for non-planar wave data of electromagnetic field signal of artificial source frequency domain |
| CN115437024B (en) * | 2022-11-07 | 2022-12-30 | 四川省冶勘设计集团有限公司 | Artificial source frequency domain electromagnetic field signal of double-parameter processing method of plane wave data |
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