CN106291722A - A kind of ground well induced-polarization measurement method and relevant device - Google Patents

A kind of ground well induced-polarization measurement method and relevant device Download PDF

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CN106291722A
CN106291722A CN201610727523.5A CN201610727523A CN106291722A CN 106291722 A CN106291722 A CN 106291722A CN 201610727523 A CN201610727523 A CN 201610727523A CN 106291722 A CN106291722 A CN 106291722A
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electrode
measurement
measured
delta
ground
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CN106291722B (en
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薛国强
郭文波
侯东洋
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Institute of Geology and Geophysics of CAS
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Institute of Geology and Geophysics of CAS
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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V3/00Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
    • G01V3/18Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation specially adapted for well-logging
    • G01V3/20Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation specially adapted for well-logging operating with propagation of electric current
    • G01V3/22Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation specially adapted for well-logging operating with propagation of electric current using dc

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  • Engineering & Computer Science (AREA)
  • Environmental & Geological Engineering (AREA)
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  • General Life Sciences & Earth Sciences (AREA)
  • General Physics & Mathematics (AREA)
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  • Geophysics And Detection Of Objects (AREA)

Abstract

A kind of ground well induced-polarization measurement method provided in the embodiment of the present invention and relevant device, use IP in well, there is the prospecting result of its uniqueness, essentially consist in it aborning, utilize boring or tunnel, its power supply or measurement apparatus, closer to detection goal object, the signal of the deep anomaly source therefore observed is stronger, relatively increase depth of exploration, the electric field depth space distribution characteristics that detected object causes can also be measured from different depth not ipsilateral, the most more rich ground electricity data can be obtained, surface electric survey some geological problem insoluble can be solved.

Description

A kind of ground-well induced-polarization measurement method and relevant device
Technical field
The present invention relates to exploration field, particularly to a kind of ground-well induced-polarization measurement method and relevant device.
Background technology
Induced polarization method (abbreviation induced polarization method) is to swash the difference of electrical effect as geophysical exploration with underground difference rock, Ore Basis, swashs electrical effect, with a kind of method of Underground geological condition by observation and research the earth.Search for mineral deposit exploration and Hydrogeology, engineering geology, resource of water supply exploration each side extensive application.For China to look for ore deposit cause to make huge Contribution, not only have found all kinds of non-ferrous metal deposits such as substantial amounts of copper, lead, zinc, molybdenum, and find noble metal ferrous metal, The mineral deposit aspects such as rare metal, have also played important function.
Electricity is measured to the earth for lower galvanic current, the MN above latent natural conduction ore body by AB current electrode Can observe time dependent charge and discharge curve, the moment of power supply between pole, can observe primary current on MN earth resistance Primary potential difference, other places field effect under, the ore body with electronic conduction and there is ionic conduction country rock interface on produce Give birth to stored charge, and defined additional electric field, produce secondary current.Utilize this characteristic, by ground observation secondary The situation of change of electric current, reaches to infer the purpose of the occurrence status of underground ore bodies.
Fig. 1 is that ground excites and intensifies area measurement figure, and wherein AB is emission electrode, respectively arranges three in emission electrode both sides Bar survey line, Hydrographic General Line direction is parallel with emission electrode, thus carries out swashing electricity area and measure.
Sounding of induced polarization is to study rock, ore body vertically apparent chargeability (η under a certain depth measurement points) side that changes Method.Its electrode is arranged identical with resistivity sounding with moving method, and current electrode (A, B) is in measuring point O both sides in opposite direction Be displaced outwardly, and measure electrode (M, N) motionless or with AB keep certain proportionGround moves simultaneously.It is commonly used to estimate The buried depth of polarization body.Utilize ηsCurve approximation estimates that the method for buried depth has turning point method, bathmometry and saturation value point method etc..
Fig. 2 is ground sounding of induced polarization schematic diagram, and it is symmetrical quadrupole device, electrodes of A, B and measurement electrode M, N It is symmetrically arranged point-blank, AO BO=AB/2, MO NO=MN/2, therefore claim symmetrical quadrupole arrangement.As electrode spacing (AB/ 2) change and during the invariant position of measuring point O, then constitute symmetrical four-pole sounding arrangement.
Electromagnetic wave during the method for electrical method physical prospecting mainly has cross beam floor, IP in well, well in well, borehole radar, Self-potential method in well medium and low frequency electromagnetic method and well, can tie with the geology between detecting shaft, around the borehole wall and in well and between earth's surface Structure.Its main working method has ground-well method, well-ground mode and well-well mode, mainly measures apparent resistivity, secondary field electricity The parameter such as potential difference or apparent chargeability.Be widely used in Solid Mineral exploration, the hydrology and engineering field, Petroleum finance with And coal exploration and exploitation, all achieve preferable geological effect.
IP in well is made by boring or probing engineering and current electrode or measurement electrode is put into underground, carries out induced polarization A kind of underlying geophysical prospecting of method observation, IP in well method powers in well or measures, by ground noise and ground mulching layer Impact diminishes, and increases IP effect, thus the method is in widespread attention and development.In well, induced polarization method is mainly adopted at present Use time domain measurement, mainly have ground-well, well-Jing Hejing-ground working method.
Fig. 3 is well-well working method, and well-well mode is that a well is powered, and in another well measurements, A pole is placed on ore bed or has Near the exception of meaning, B pole is laid in earth's surface " infinity " place;Measuring the electrode " MN " arrangement in well is: M is upper, and N exists Under, measuring point is at MN midpoint.Its feature is used for finding between holes ore body or determines that holes finding ore body is electrical connected problem.
Fig. 4 is well-ground working method, and this working method is that current electrode " A " is placed in the ore deposit in boring or in tunnel On body, B beats pole " infinity " place on earth's surface, measures pole layout Mo, Nx, Ny tri-, and by left hand, (middle finger is downward, and forefinger refers to Y, thumb refers to X) rectangular coordinate system arrangement, Mo is origin of coordinate, is again measuring point.During measuring, observation is along profile direction (X-axis) and the primary field of vertical section direction (Y-axis) and secondary field electric potential gradient (including charge rate).The ground that it is solved is interrogated Topic, demand on the ground and draw a circle to approve ore body areal extent, finding adjacent blind mineralization body, IP in well relative to surface electric survey, Having depth of exploration big, resolution capability is strong, and anomaly intensity is big, Explanation Accuracy advantages of higher.Prior art is for the other gold of detecting shaft Belong to sulfide blind orebody and determine ore body counter bored holes spatial distribution scope and state, relevant programme, technology are not provided Personnel add difficulty when surveying.
Summary of the invention
In view of this, a kind of ground-well induced-polarization measurement method and relevant device are embodiments provided.
The embodiment of the present invention provides a kind of ground-well induced-polarization measurement method, including:
It is perpendicular to earth's surface in region to be measured and is vertically arranged the boring for measuring;
Earth's surface around described boring arranges current electrode, and described current electrode is positioned at described region to be measured;
Hole described in surface distance in the described region to be measured position of infinity arranges reference electrode;
Suspending the first measurement electrode and second in described boring and measure electrode, described first measures electrode and described second Measure electrode, at vertical direction, there is predetermined interval;
Obtain described first and measure electrode and described second measurement electrode primary importance information in described boring;
The second position information at test electrode midpoint, wherein, described test electrode midpoint is determined according to described positional information For the point midway between described first test electrode and described second test electrode;
Utilize ground induced polarization method to obtain described test electrode midpoint and be in the first measurement position at described current electrode Time corresponding the first metrical information including the first apparent resistivity and the first apparent chargeability, and described test electrode midpoint exists The second survey including the second apparent resistivity and the second apparent chargeability that described current electrode is corresponding when being in the second measurement position Amount information, and repeat to measure;
Obtain described first metrical information according to repetitive measurement and described second metrical information determines described region to be measured The areal extent of interior ore body, so that determining, according to described areal extent, the blind mineralization body that described boring is adjacent.
Alternatively, the method for described ground induced polarization method calculating apparent resistivity and apparent chargeability includes:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV 1 M N = V 1 M - V 1 N
Wherein, k is electrode coefficient,It is respectively the first test electrode and the second test electricity Primary field, secondary field and the potential difference of total field extremely gone up.
Alternatively, described described first metrical information according to repetitive measurement and described second metrical information determine described in treat The areal extent of ore body in measured zone, including:
Demand on described region to be measured according to primary field and the secondary field electric potential gradient along X-direction and Y direction With delineation ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
Providing a kind of ground-well induced-polarization measurement device in the embodiment of the present invention, described device includes:
Ground-well measurements device transmitter module, for setting up the secondary field measured in environment;
Ground-well measurements device receiver module, for obtaining the potential difference received in described primary field;
Data acquisition module, for described-well measurements device receiver module is gathered at described-well measurements device Transmitter module is in the potential difference of described diverse location and is converted into apparent resistivity and apparent chargeability, and according to being calculated ore body Areal extent.
Alternatively, describedly-well measurements device receiver module includes that the first measurement electrode and second measures electrode, described First measures electrode and described second measures electrode in the setting of vertical direction interval.
Alternatively, the mode of operation of described measurement device and transmitting is automatic mode or fixed model.
Providing a kind of ground-well induced-polarization measurement device in the embodiment of the present invention, described device includes:
First measuring unit, is vertically arranged the boring for measuring for being perpendicular to earth's surface in region to be measured;
First arranges unit, arranges current electrode for the earth's surface around described boring, and described current electrode is positioned at institute State in region to be measured;
Second arranges unit, arranges ginseng for the position of infinity of holing described in the surface distance in described region to be measured Examine electrode;
3rd arranges unit, suspension the first measurement electrode and the second measurement electrode in described boring, and described first Measure electrode and at vertical direction, there is predetermined interval with described second measurement electrode;
First acquiring unit, is used for obtaining described first and measures electrode and described second measurement electrode in described boring Primary importance information;
First determines unit, for determining the second position information at test electrode midpoint according to described positional information, wherein, Described test electrode midpoint is the point midway between described first test electrode and described second test electrode;
Second measuring unit, is used for utilizing ground induced polarization method to obtain described test electrode midpoint at described current electrode The first metrical information including the first apparent resistivity and the first apparent chargeability corresponding when being in the first measurement position, Yi Jisuo State that test electrode midpoint is corresponding when described current electrode is in the second measurement position includes the second apparent resistivity and second Second metrical information of apparent chargeability, and repeat to measure;
Second determines unit, is used for obtaining described first metrical information according to repetitive measurement and described second metrical information is true The areal extent of ore body in fixed described region to be measured, so that determining, according to described areal extent, the blind ore that described boring is adjacent Change body.
Alternatively, described second measuring unit specifically for:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV 1 M N = V 1 M - V 1 N
Wherein, k is electrode coefficient,It is respectively the first test electrode and the second test electricity Primary field, secondary field and the potential difference of total field extremely gone up.
Alternatively, described second determine unit specifically for:
Demand on described region to be measured according to primary field and the secondary field electric potential gradient along X-direction and Y direction With delineation ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
As can be seen from the above technical solutions, the embodiment of the present invention has the advantage that
A kind of ground-well induced-polarization measurement the method provided in the embodiment of the present invention and relevant device, use IP in well, There is the prospecting result of its uniqueness, essentially consist in it aborning, utilize boring or tunnel, its power supply or measurement apparatus, closer to In detection goal object, the signal of the deep anomaly source therefore observed is relatively strong, relatively increases depth of exploration, it is also possible to from difference The degree of depth not ipsilateral measures the electric field depth space distribution characteristics that detected object causes, and can obtain the most more rich ground electricity money Material, can solve surface electric survey some geological problem insoluble.
Accompanying drawing explanation
Fig. 1 is that in prior art, ground excites the schematic diagram intensifying area measurement;
Fig. 2 is the schematic diagram of ground sounding of induced polarization signal in prior art;
Fig. 3 is the schematic diagram that well in prior art-well working method is measured;
Fig. 4 is the schematic diagram that well in prior art-ground working method is measured;
Fig. 5 is a kind of ground-well induced-polarization measurement method instrumentation plan in the embodiment of the present invention;
Fig. 6 is the signal testing electrode shift position in the embodiment of the present invention in a kind ofly-well induced-polarization measurement method Figure;
Fig. 7 is that in the embodiment of the present invention, a kind of ground-well induced-polarization measurement method Zhong Mujia village ground-well swashs electricity composite measurement Schematic diagram;
Fig. 8 is line generalization section signal in a kind of ground-well induced-polarization measurement method Zhong Mujia village 59 in the embodiment of the present invention Figure.
Detailed description of the invention
In order to make those skilled in the art be more fully understood that the present invention program, below in conjunction with in the embodiment of the present invention Accompanying drawing, is clearly and completely described the technical scheme in the embodiment of the present invention, it is clear that described embodiment is only The embodiment of a present invention part rather than whole embodiments.Based on the embodiment in the present invention, ordinary skill people The every other embodiment that member is obtained under not making creative work premise, all should belong to the model of present invention protection Enclose.
Term " first " in description and claims of this specification and above-mentioned accompanying drawing, " second ", " the 3rd " " Four " etc. (if present) is for distinguishing similar object, without being used for describing specific order or precedence.Should manage Solve the data so used can exchange in the appropriate case, in order to the embodiments described herein can be with except here illustrating Or the order enforcement beyond the content described.Additionally, term " includes " and " having " and their any deformation, it is intended that Cover non-exclusive comprising, such as, contain series of steps or the process of unit, method, system, product or equipment need not limit In those steps clearly listed or unit, but can include the most clearly listing or for these processes, method, product Product or intrinsic other step of equipment or unit.
Below in conjunction with the accompanying drawing in the embodiment of the present invention, the technical scheme in the embodiment of the present invention is carried out clear, complete Describe, it is clear that described embodiment is only a part of embodiment of the present invention rather than whole embodiments wholely.Based on Embodiment in the present invention, the every other enforcement that those skilled in the art are obtained under not making creative work premise Example, broadly falls into the scope of protection of the invention.
Effect of induced polarization: under artificial electric current play field or exciting field effect, there is the rock of different electrochemical properties Stone or Ore, owing to electrochemical action will produce time dependent secondary electrical field (induced polarization field).This physical chemistry is made With referred to as effect of induced polarization.It includes effect of induced polarization and the effect of induced polarization of ion conductor of electronic conductor.
The factor affecting effect of induced polarization includes:
1, rock and ore material composition: general, the induced polarization intensity of electronic conduction mineral is relatively big, and polarizability (η) is 10% Above;
2, the content and structure of of metalliferous mineral: general, metalliferous mineral content is the most under same structural condition, polarizability (η) The biggest;In the case of metalliferous mineral content is equal, disseminated structure Ore is bigger than the polarizability (η) of compact shape structure Ore,
3, supply current: electric current density in the range of tens microamperes/square centimeter, voltage of secondary field Δ U2;With power supply Electric current I direct ratio changes, and polarization field potential difference Δ U also increases with multiple, and power-on time also has substantial connection.
Induced polarization method: English: induced polarization method, is according to rock, the induced polarization of Ore Effect is found metal and solves one group of electrical prospecting method of the problems such as hydrogeology, engineering geology.It is divided into again direct current to swash Send out polarization method (time domain method) and alternating current induced polarization method (frequency domain method (SIP)).Conventional electrode arrangement has Middle-gradient to arrange Row, composite profile arrangement, the arrangement of fixing point power supply, symmetrical four-pole sounding arrangement etc..Directly or indirectly can also fill with making ore body The way of electricity is drawn a circle to approve the extension of ore body and increases depth of exploration.
Shown in Fig. 5 and Fig. 6, the embodiment of the present invention provides a kind of ground-well induced-polarization measurement method, including:
S101, be perpendicular in region to be measured earth's surface be vertically arranged for measure boring;
S102, described boring around earth's surface current electrode is set, described current electrode is positioned at described region to be measured In;
Hole described in S103, surface distance in the described region to be measured position of infinity arranges reference electrode;
Suspending the first measurement electrode and second in S104, described boring and measure electrode, described first measures electrode and institute State the second measurement electrode, at vertical direction, there is predetermined interval;
S105, obtain described first measure electrode and described second measure electrode in described boring primary importance letter Breath;
S106, according to described positional information determine test electrode midpoint second position information, wherein, described test electrode Midpoint is the point midway between described first test electrode and described second test electrode;
S107, utilize ground induced polarization method to obtain described test electrode midpoint to be in the first measurement at described current electrode The first metrical information including the first apparent resistivity and the first apparent chargeability corresponding during position, and in described test electrode Point is corresponding when described current electrode is in the second measurement position includes the of the second apparent resistivity and the second apparent chargeability Two metrical informations, and repeat to measure;
S108, obtain described first metrical information according to repetitive measurement and described second metrical information determines described to be measured The areal extent of ore body in region, so that determining, according to described areal extent, the blind mineralization body that described boring is adjacent.
In step s 107, in order to be more conducive to find out the trend of mineralization body and spatial situation, in addition it is also necessary to change power supply The position of electrode A, launches in different positions, and in well, same position is received.According to A1, A2, A3, A4 in Fig. 6 Position lay emission electrode respectively.The orientation of target geological body counter bored holes is referred to as best orientation A1, also referred to as main formula position, its phase Reverse claims reverse A3, and other two orientation are auxiliary orientation A2 and A4, are not defined this.
Alternatively, the method for described ground induced polarization method calculating apparent resistivity and apparent chargeability includes:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV 1 M N = V 1 M - V 1 N
Wherein, k is electrode coefficient,It is respectively the first test electrode and the second test electricity Primary field, secondary field and the potential difference of total field extremely gone up.
Alternatively, described described first metrical information according to repetitive measurement and described second metrical information determine described in treat The areal extent of ore body in measured zone, including:
Demand on described region to be measured according to primary field and the secondary field electric potential gradient along X-direction and Y direction With delineation ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
Shown in Fig. 7 and Fig. 8, below in conjunction with concrete scene, a kind of ground-well mentioned in the embodiment of the present invention is excited Polarization measurement method illustrates, with the effectiveness of verification method:
Ground-well method induced-polarization measurement has been carried out in ZK5901 hole, Copper Mine, the Mu Jia village.
28 ° of perforate orientation, ZK5901 hole, Copper Mine, the Mu Jia village, does not gets to copper mine body in drilling process, carry out subsequently- The induced polarization method of well mode is measured.Electric logging observed result shows, have near 165 meters of well sections the last one natural potential, Charge rate is coincide the most abnormal.Ground well swashs the azimuthal measurement of electricity, at the position of upper and lower tens meters of this well section, has significantly Good lead high polarization anomalous reflection, especially A3, A4 two Δ V in orientation1、ΔV2Anomalous reflection amplitude is big, all in positive and negative value combination Off-note, show that A3, A4 electrode spacing anomaly source is nearest, infer that anomaly source (ore body) main body is positioned at A3, A4 orientation and (bores accordingly Side, southwest, hole), this measurement result is to supplement the strong of drilling data.
The Tu8Wei Mujia village 59 line generalization profile, it is seen that A3 orientation secondary field is anti-s type, A1 orientation secondary field is s type, Infer that anomaly source (ore body) is to well inclined accordingly, say, that ZK5901 beats in hole the tail on anomaly source (ore body) nearly well side Portion.Lay the most again ZK5902 hole, 208 ° of perforate orientation.Get to copper mine body it was confirmed the above-mentioned ore body inferred is relative ZK5901 hole spatial distribution state is correct.
Result of detection shows: IP in well, has the prospecting result of its uniqueness, essentially consists in it aborning, utilizes boring Or tunnel, its power supply or measurement apparatus, closer to detection goal object, the signal of the deep anomaly source therefore observed is relatively strong, phase Increase depth of exploration over the ground.And, also from different depth, not ipsilateral, measure the electric field depth space that detected object causes Distribution characteristics, can obtain more accurate, more rich ground electricity data, can solve surface electric survey some ground insoluble and interrogate Topic.
Additionally providing a kind of ground-well induced-polarization measurement device in the embodiment of the present invention, described device includes:
Ground-well measurements device transmitter module, for setting up the secondary field measured in environment;
Ground-well measurements device receiver module, for obtaining the potential difference received in described primary field;
Data acquisition module, for described-well measurements device receiver module is gathered at described-well measurements device Transmitter module is in the potential difference of described diverse location and is converted into apparent resistivity and apparent chargeability, and according to being calculated ore body Areal extent.
Alternatively, describedly-well measurements device receiver module includes that the first measurement electrode and second measures electrode, described First measures electrode and described second measures electrode in the setting of vertical direction interval.
Alternatively, the mode of operation of described measurement device and transmitting is automatic mode or fixed model.
Additionally providing a kind of ground-well induced-polarization measurement device in the embodiment of the present invention, described device includes:
First measuring unit, is vertically arranged the boring for measuring for being perpendicular to earth's surface in region to be measured;
First arranges unit, arranges current electrode for the earth's surface around described boring, and described current electrode is positioned at institute State in region to be measured;
Second arranges unit, arranges ginseng for the position of infinity of holing described in the surface distance in described region to be measured Examine electrode;
3rd arranges unit, suspension the first measurement electrode and the second measurement electrode in described boring, and described first Measure electrode and at vertical direction, there is predetermined interval with described second measurement electrode;
First acquiring unit, is used for obtaining described first and measures electrode and described second measurement electrode in described boring Primary importance information;
First determines unit, for determining the second position information at test electrode midpoint according to described positional information, wherein, Described test electrode midpoint is the point midway between described first test electrode and described second test electrode;
Second measuring unit, is used for utilizing ground induced polarization method to obtain described test electrode midpoint at described current electrode The first metrical information including the first apparent resistivity and the first apparent chargeability corresponding when being in the first measurement position, Yi Jisuo State that test electrode midpoint is corresponding when described current electrode is in the second measurement position includes the second apparent resistivity and second Second metrical information of apparent chargeability, and repeat to measure;
Second determines unit, is used for obtaining described first metrical information according to repetitive measurement and described second metrical information is true The areal extent of ore body in fixed described region to be measured, so that determining, according to described areal extent, the blind ore that described boring is adjacent Change body.
Alternatively, described second measuring unit specifically for:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV 1 M N = V 1 M - V 1 N
Wherein, k is electrode coefficient,It is respectively the first test electrode and the second test electricity Primary field, secondary field and the potential difference of total field extremely gone up.
Alternatively, described second determine unit specifically for:
Demand on described region to be measured according to primary field and the secondary field electric potential gradient along X-direction and Y direction With delineation ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
A kind of ground-well induced-polarization measurement the method provided in the embodiment of the present invention and relevant device, use IP in well, There is the prospecting result of its uniqueness, essentially consist in it aborning, utilize boring or tunnel, its power supply or measurement apparatus, closer to In detection goal object, the signal of the deep anomaly source therefore observed is relatively strong, relatively increases depth of exploration, it is also possible to from difference The degree of depth not ipsilateral measures the electric field depth space distribution characteristics that detected object causes, and can obtain the most more rich ground electricity money Material, can solve surface electric survey some geological problem insoluble.
Those skilled in the art is it can be understood that arrive, for convenience and simplicity of description, and the system of foregoing description, The specific works process of device and unit, is referred to the corresponding process in preceding method embodiment, does not repeats them here.
In several embodiments provided herein, it should be understood that disclosed system, apparatus and method are permissible Realize by another way.Such as, device embodiment described above is only schematically, such as, and described unit Dividing, be only a kind of logic function and divide, actual can have other dividing mode, the most multiple unit or assembly when realizing Can in conjunction with or be desirably integrated into another system, or some features can be ignored, or does not performs.Another point, shown or The coupling each other discussed or direct-coupling or communication connection can be the indirect couplings by some interfaces, device or unit Close or communication connection, can be electrical, machinery or other form.
The described unit illustrated as separating component can be or may not be physically separate, shows as unit The parts shown can be or may not be physical location, i.e. may be located at a place, or can also be distributed to multiple On NE.Some or all of unit therein can be selected according to the actual needs to realize the mesh of the present embodiment scheme 's.
It addition, each functional unit in each embodiment of the present invention can be integrated in a processing unit, it is also possible to It is that unit is individually physically present, it is also possible to two or more unit are integrated in a unit.Above-mentioned integrated list Unit both can realize to use the form of hardware, it would however also be possible to employ the form of SFU software functional unit realizes.
One of ordinary skill in the art will appreciate that all or part of step in the various methods of above-described embodiment is can Completing instructing relevant hardware by program, this program can be stored in a computer-readable recording medium, storage Medium may include that read only memory (ROM, Read Only Memory), random access memory (RAM, Random Access Memory), disk or CD etc..
One of ordinary skill in the art will appreciate that all or part of step realizing in above-described embodiment method is permissible Instructing relevant hardware by program to complete, described program can be stored in a kind of computer-readable recording medium, on Stating the storage medium mentioned can be read only memory, disk or CD etc..
Above a kind of ground-well induced-polarization measurement method provided by the present invention and relevant device are carried out detailed Jie Continue, for one of ordinary skill in the art, according to the thought of the embodiment of the present invention, in specific embodiments and applications All will change, in sum, this specification content should not be construed as limitation of the present invention.

Claims (9)

1. ground-well induced-polarization measurement method, it is characterised in that including:
It is perpendicular to earth's surface in region to be measured and is vertically arranged the boring for measuring;
Earth's surface around described boring arranges current electrode, and described current electrode is positioned at described region to be measured;
Hole described in surface distance in the described region to be measured position of infinity arranges reference electrode;
Suspending the first measurement electrode and second in described boring and measure electrode, described first measures electrode measures with described second Electrode has predetermined interval at vertical direction;
Obtain described first and measure electrode and described second measurement electrode primary importance information in described boring;
Determine the second position information at test electrode midpoint according to described positional information, wherein, described test electrode midpoint is institute State the point midway between the first test electrode and described second test electrode;
Utilize ground induced polarization method to obtain described test electrode midpoint and be in the first measurement position time institute at described current electrode Corresponding the first metrical information including the first apparent resistivity and the first apparent chargeability, and described test electrode midpoint is described The the second measurement letter including the second apparent resistivity and the second apparent chargeability that current electrode is corresponding when being in the second measurement position Breath, and repeat to measure;
Obtain described first metrical information according to repetitive measurement and described second metrical information determines described region Nei Kuang to be measured The areal extent of body, so that determining, according to described areal extent, the blind mineralization body that described boring is adjacent.
Method the most according to claim 1, it is characterised in that described ground induced polarization method calculates apparent resistivity and regards pole The method of rate includes:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV1 MN=V1 M-V1 N
Wherein, k is electrode coefficient, Δ V1 MN, Δ V2 MN, Δ Vz MNIt is respectively on the first test electrode and the second test electrode Primary field, secondary field and potential difference of total field.
Method the most according to claim 1, it is characterised in that described described first metrical information according to repetitive measurement and Described second metrical information determines the areal extent of ore body in described region to be measured, including:
Demand according to primary field and the secondary field electric potential gradient along X-direction and Y direction and enclose on described region to be measured Determining ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
4. ground-well induced-polarization measurement device, it is characterised in that described device includes:
Ground-well measurements device transmitter module, for setting up the secondary field measured in environment;
Ground-well measurements device receiver module, for obtaining the potential difference received in described primary field;
Data acquisition module, launches at described-well measurements device for gathered by described-well measurements device receiver module Module is in the potential difference of described diverse location and is converted into apparent resistivity and apparent chargeability, and according to being calculated the spread of ore body Scope.
Device the most according to claim 4, it is characterised in that describedly-well measurements device receiver module includes the first survey Amount electrode and second measures electrode, and described first measurement electrode and described second is measured electrode and arranged at vertical direction interval.
Device the most according to claim 5, it is characterised in that the mode of operation of described measurement device and transmitting is automatic mold Formula or fixed model.
7. ground-well induced-polarization measurement device, it is characterised in that described device includes:
First measuring unit, is vertically arranged the boring for measuring for being perpendicular to earth's surface in region to be measured;
First arranges unit, for described boring around earth's surface current electrode is set, described current electrode be positioned at described in treat In measured zone;
Second arranges unit, arranges with reference to electricity for the position of infinity of holing described in the surface distance in described region to be measured Pole;
3rd arranges unit, suspends the first measurement electrode and second and measure electrode in described boring, and described first measures Electrode is measured electrode with described second and is had predetermined interval at vertical direction;
First acquiring unit, measures electrode and described second measure electrode the in described boring for obtaining described first One positional information;
First determines unit, for determining the second position information at test electrode midpoint according to described positional information, wherein, described Test electrode midpoint is the point midway between described first test electrode and described second test electrode;
Second measuring unit, is used for utilizing ground induced polarization method to obtain described test electrode midpoint and is at described current electrode First measures the first metrical information including the first apparent resistivity and the first apparent chargeability corresponding during position, and described survey Examination electrode midpoint is corresponding when described current electrode is in the second measurement position includes that the second apparent resistivity and second regards pole Second metrical information of rate, and repeat to measure;
Second determines unit, is used for obtaining described first metrical information according to repetitive measurement and described second metrical information determines institute State the areal extent of ore body in region to be measured, so that determining, according to described areal extent, the blind ore that described boring is adjacent Body.
Device the most according to claim 7, it is characterised in that described second measuring unit specifically for:
ρ s M N = k · ΔV 1 M N / I
η s M N = ΔV 2 M N / ΔV z M N = ( ΔV z M N - ΔV 1 M N ) / ΔV z M N
K=2 π rAM·rAN/(rAN-rAM)
ΔV1 MN=V1 M-V1 N
Wherein, k is electrode coefficient, Δ V1 MN, Δ V2 MN, Δ Vz MNIt is respectively on the first test electrode and the second test electrode Primary field, secondary field and potential difference of total field.
Device the most according to claim 7, it is characterised in that described second determine unit specifically for:
Demand according to primary field and the secondary field electric potential gradient along X-direction and Y direction and enclose on described region to be measured Determining ore body areal extent, wherein said X-direction is profile direction, and described Y-axis is vertical section direction.
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CN116611622A (en) * 2023-07-19 2023-08-18 北京建工环境修复股份有限公司 Phytoremediation technical effect evaluation method and system based on well site induced polarization method
CN116611622B (en) * 2023-07-19 2023-09-19 北京建工环境修复股份有限公司 Phytoremediation technical effect evaluation method and system based on well site induced polarization method

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