CN104870067A - Method for determining best shot hole depth in homogeneous mediums - Google Patents

Method for determining best shot hole depth in homogeneous mediums Download PDF

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CN104870067A
CN104870067A CN201480002778.4A CN201480002778A CN104870067A CN 104870067 A CN104870067 A CN 104870067A CN 201480002778 A CN201480002778 A CN 201480002778A CN 104870067 A CN104870067 A CN 104870067A
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explosive
soil body
thrust
well
formula
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杨顺伟
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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/40Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/40Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging
    • G01V1/44Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging using generators and receivers in the same well
    • G01V1/48Processing data
    • G01V1/50Analysing data

Abstract

The present invention provides a method for determining best shot hole depth in homogeneous mediums, which is characterized by comprising the following steps: 1) calculating out a thrust force F of an explosive material at underground explosion according to performance parameters of the explosive material; calculating a F upthrust force generated by exploding of a one-gun combination hole by utilizing a formula : the F upthrust force=combination hole amounts *F/8; 2) calculating a best shot hole depth H by utilizing a formula: the F upthrust force=H*T*Pho*9.8N/kg+F3+F4; wherein, the F upthrust force is obtained from the step 1); H is the shot hole depth, T is a projected area of the ground surrounded by the combination hole; Pho is a soil mass density; F3 is a friction force generated by upward moving soil mass with surrounding rocks; F4 is a horizontal stress suffered by the soil mass in the state of balance.

Description

A kind of method determining best excitation well depth in uniform dielectric
Technical field
The present invention relates to petroleum exploration technology, is a kind of method determining best excitation well depth in uniform dielectric.
Background technology
The design of the current excitation well depth of oil seismic exploration mainly contains two kinds of approach: (1) carries out well depth test, analyzes, determine excitation well depth to single big gun frequency, energy and the signal to noise ratio that well depth is tested; (2) investigated by micro logging, determine the speed of near surface, lithology and the phreatic surface degree of depth, under a certain velocity interface or constitute law, 3-5 rice, is defined as shooting depth.
First method is the method that petroleum exploration industry is continued to use for many years always, adopts identical well number with under the prerequisite of identical total dose, is excited by different well depths, contrasts the single big gun data frequency which kind of excitation well depth obtains high, and energy is strong, and signal to noise ratio is high.
Second method, must under certain physical interface of well depth design first it is contemplated that the energy excited will pass effectively down, and wherein ghosting interface is the interface of a very useful design excitation well depth.
Next considers velocity interface, worked by near-surface investigation, the near surface structure figure in work area can be drawn, therefore, it is possible to the high-speed layer buried depth of each shot position is estimated, the excitation well depth of each shot point is instructed to design, the shortcoming done like this is, well depth is very large by the change in depth at high-speed layer interface, causes excitation well depth to occur violent fluctuating.Also the uniformity of excitation wavelet is made to be deteriorated.
Again consider the lithology excited exactly, according to geophysical general knowledge, well depth is darker, and the compaction of rock stratum is more obvious, and the density of country rock increases, and the property of water-bearing increases, and the coupling of the blasting charge and country rock is better; Such exciton wave frequency is higher, and excitation energy is strong.But the saying of this consideration excitation li thology is completely all qualitatively, can accurately not describe lithology is how to affect stimulation effect, especially in the exploratory area (huge thick soil layer/huge thick drift sand formation) that the variation of lithological of near surface is very faint, lithology does not more have the purposes instructing excitation well depth to design.
Be finally the impact that excitation well depth design will consider phreatic surface factor, in the geophysical exploration study course of classics, below phreatic surface, 3-5m excites and can obtain extraordinary wavelet frequency, can obtain extraordinary excitation energy.Therefore adopting below phreatic surface to excite, is also use maximum seismic prospecting excitation well depth designing methods.The deficiency of first method is that the gatherer process of single big gun of test exists manual operation error, test single shot record carry out frequency, energy and Analysis signal-to-noise ratio (SNR) time because the difference of analysis window size and position, there is greatest differences in analysis result.The deficiency of second method, the interface of near surface alters a great deal, and for high-speed layer, from the scope that 10m-100m is even larger, design result substantial deviation theoretical value, causes great difficulty to the excitation well depth design in work area.But, there is no obvious ghosting interface near surface 100m, there is no high-speed interface, when phreatic surface, be dry loose loess or drift sand near surface, in said method, do not propose criterion and the method for determining excitation well depth.
Summary of the invention
The object of the invention is to provide a kind of does not have obvious ghosting interface on earth's surface, does not have high-speed interface, do not have the drying of phreatic surface loosen the soil body determination uniform dielectric in the method for best excitation well depth.The present invention is realized by following steps:
1) according to using the performance parameter of explosive to calculate the thrust F of explosive at underground explosion; The 1/8 calculating one big gun combination well blast thrust F lifting force upwards of explosive thrust to lifting force according to blast:
F lifting force=combination well number × F ÷ 8;
It is utilize following kinetic energy formula that the thrust F of described blast calculates:
1 2 m v 2 = FS
Wherein, m is quality of explosive, and v is the explosion velocity of explosive, and F is the explosive thrust of a well, and S is half well spacing.
The explosion velocity of described explosive is 5000-6000m/s, and average 5500m/s.
2) best excitation well depth H is calculated with following formula:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
In formula: F lifting force-step 1) in the explosive charge thrust upwards that calculates;
H-excitation well depth;
The floor projection area that T-combination well surrounds;
ρ-soil body density;
F3-soil body moves upward the frictional force produced with surrounding country rock;
The horizontal stress that F4-soil body is subject to when poised state.
The calculating of described soil body density p is the container using known weight and volume, gathers the primary soil sample of more than 2, utilizes density formula m 2=ρ v 2calculate the averag density of soil sample, in formula: m 2the weight of soil sample, v 2it is the volume of soil sample.
The described soil body frictional force F3 produced with surrounding country rock that moves upward adopts following formulae discovery:
The all combination wells of F3=surround the intergranular free frictional resistance of area × soil body of the soil body and surrounding country rock;
The intergranular free frictional resistance measurement of the described soil body is: the same volume soil body slowly topples over the cone of formation to horizontal plane, angle used when the side of cone and the angle theta of horizontal plane are the decomposition being object gravity G on inclined-plane, the intergranular free frictional resistance f of the soil body c: f c=G × sin θ.
Described same volume is bottom surface circular diameter 6.5cm, the cylinder of height 7cm.
The horizontal stress F4 that the described soil body is subject to when poised state adopts following formulae discovery:
F 4 = ( H × T × ρ × 9.8 N kg ) × μ 1 - μ
Wherein: μ is the Poisson's ratio of soil medium.
The invention provides near surface 100m and do not have obvious ghosting interface, do not have high-speed interface, when phreatic surface, is the method for best excitation well depth in the soil body determination uniform dielectric such as dry loose loess or drift sand near surface.By one group of excitation well depth test, do energy spectrometer to the single big gun data gathered, the well depth obtained and the result of theory calculate are closely.
Accompanying drawing explanation
In order to be illustrated more clearly in the embodiment of the present invention or technical scheme of the prior art, below the accompanying drawing used required in describing embodiment is briefly described, apparently, accompanying drawing in the following describes is only some embodiments of the present invention, for those of ordinary skill in the art, under the prerequisite not paying creative work, other accompanying drawing can also be obtained according to these accompanying drawings.
Fig. 1 is the volume of the prismatoid that 11 shooting on group wells are formed in underground.
Fig. 2 utilizes loess cone to calculate the intergranular frictional force of loess.
Fig. 3 is 1m 2the computation model of the intergranular free frictional force of loess on inclined-plane.
Fig. 4 prismatoid moves upward the downward frictional force that four sides are subject to.
Fig. 5 is the cylindrical volume that 2 shooting on group wells are formed in underground.
Fig. 6 utilizes drift sand cone to calculate the intergranular frictional force of drift sand.
Fig. 7 is 1m 2the computation model of the free frictional force between the sand grain of upper reaches, inclined-plane.
Fig. 8 cylinder moves upward the downward frictional force that side is subject to.
Detailed description of the invention
Below in conjunction with the accompanying drawing in the embodiment of the present invention, be clearly and completely described the technical scheme in the embodiment of the present invention, obviously, described embodiment is only the present invention's part embodiment, instead of whole embodiments.Based on the embodiment in the present invention, those of ordinary skill in the art, not making the every other embodiment obtained under creative work prerequisite, belong to the scope of protection of the invention.
The present invention is described in detail below in conjunction with accompanying drawing and experiment embodiment.
The present invention illustrates for oess hills 11 shooting on group factor:
1) with oess hills excitation condition 11 × H × 3kg, well spacing 3m, array pitch 3m are that example calculates, and use the performance parameter of explosive to calculate the thrust F (kN) of explosive at underground explosion;
The calculating of a well explosive thrust utilizes kinetic energy formula:
1 2 m v 2 = FS
Wherein, m is quality of explosive, and v is the explosion velocity of explosive, and F is the thrust that a well (3kg explosive) blast produces, and S is half well spacing (explosive is at the burst radius of loess);
The explosion velocity of explosive is 5000-6000m/s, and average 5500m/s.
Calculate the thrust that a well (3kg explosive) blast produces: F=30250kN;
Well (3kg explosive) blast thrust upwards (be 1/8 of whole space thrust, the energy that the sphere that namely centre of sphere angle is 90 degree distributes, remaining energy passes down the energy with side) and be: F/8=3781.25kN;
One big gun 11 combines (33kg explosive) blast thrust upwards: F lifting force=11 × F/8=41593.75kN.
2) best excitation well depth H is calculated with following formula:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
In formula: F lifting force-step 1) in the explosive charge thrust upwards that calculates;
H-excitation well depth;
T-11 well combination surround at floor projection area;
ρ-loess density;
F3-prismatoid side moves upward the frictional force produced with surrounding country rock;
The horizontal stress that F4-prismatoid is subject to when poised state.
It should be noted that:
(1) T described in is that 11 wells combine the floor projection trapezoidal area surrounded, upper base distance 18m, and go to the bottom distance 15m, and above go to the bottom distance 6m, well spacing 3m, array pitch 3m, and a row is 6 wells, and a row is 5 wells.First the surface projection area T of calculation combination well, 5 wells be upper base, be the length of 5 well spacings; 6 wells while for going to the bottom, be the length of 6 well spacings; Trapezoidal height is the length of 2 well spacings; Then surface projection area T is trapezoidal (see Fig. 1), and T can accurately calculate:
T=(1/2)×(15m+18m)×6m=99m 2
(2) ρ described in is the density of loess.Gather the primary soil sample (loess) in combination well area, calculate density of soil sample;
Described calculating density of soil sample is the container using known weight and volume, gathers 6 primary soil samples, utilizes density formula (m 2=ρ v 2) calculate the averag density of soil sample.
In formula: m 2the weight of soil sample, v 2be the volume of soil sample, calculating density p is=1.613668g/cm3;
(3) F3 described in is that the soil body (prismatoid) moves upward the frictional force produced with surrounding country rock;
The intergranular free frictional resistance of lateral area × loess of F3=prismatoid;
Measure the intergranular free frictional resistance of loess;
Measuring method is: measure the soil body (drift sand and loess) when same volume, the cone of formation is slowly toppled over to horizontal plane, drift sand and loess centrum have different basal diameter and vertebral height, the different physical phenomenon of this centrum shape, be drift sand and loess ground particle between the performance of free frictional resistance difference in size.
Same volume of the present invention is bottom surface circular diameter 6.5cm, the cylinder of height 7cm.
Eventually pass that to test the result that obtains as follows:
Drift sand cone: base diameter 15.2 centimetres, height 4.8cm;
Loess cone: base diameter 13.7 centimetres, height 6cm;
The side of its intermediate cam centrum and the angle of horizontal plane are exactly θ; This angle θ is exactly the angle used when doing the decomposition of object gravity G on inclined-plane.The height of loess cone is 6cm, and bottom surface radius is 6.85cm (see Fig. 2).
sin θ = 6 / 6 2 + 6.85 2 = 0.66
Wherein this inclination angle relation is 1.0m with hypotenuse in fig. 3, and the right-angle side that a certain formation sine value is 0.66 is 0.66m.This relation represents: when θ=arcsin (0.66), the intergranular friction power of loess reaches balance, and namely θ angle increases again, and loess particle will glide.
So, 1m 2on inclined-plane, the intergranular free frictional force of loess is (see Fig. 3):
f1m 2=(1/2)×0.66m×0.75m×1m×1614kg/m3×9.8N/kg×0.66=2583.74N
Calculate the soil body (prismatoid) to move upward the frictional force F3 produced with surrounding country rock;
F3=f1+f2+f3+f4
F1, f2, f3, f4---be the end with trapezoidal, H is 4 sides of the prismatoid of thickness, and wherein upper base length is 18m, length of going to the bottom is 15m, on length of going to the bottom be 6m, and on hypotenuse length of going to the bottom be 6.18m, that produce when moving upward with frictional force (see Fig. 4) that is country rock.
f1=H×18×f1m2=46.507H(kN)
f2=H×15×f1m2=38.756H(kN)
f3=H×6.18×f1m2=15.968H(kN)
f4=H×6.18×f1m2=15.968H(kN)
F3=117.2H(kN)
(4) the horizontal stress F4 that the prismatoid described in is subject to when poised state adopts following formulae discovery:
The horizontal stress that F4=prismatoid is subject to;
F 4 = ( H × T × ρ × 9.8 N kg ) × μ 1 - μ
H × T × ρ × 9.8N/kg---be the vertical stress that loess is subject to;
H-excitation well depth;
The floor projection area that T-11 combination well surrounds;
ρ-loess density;
μ---be the Poisson's ratio of Loess Medium.
Value μ is between 0.40 ~ 0.50 for loess Poisson's ratio, and we get intermediate value μ=0.45.
Then: F4=H × 99m3 × 1614kg/m3 × 9.8N/kg × μ/(1-μ)
=(0.45/0.55)×1565.903H
=1281.19H(kN)
(5) the best excitation well depth in loess is calculated:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
41593.75kN=H×99m3×1614kg/m3×9.8N/kg+117.2H+1281.19H
H=14.031592m
Then " H+ burst radius 1.5m=15.531592m " is exactly in 11 combinations, well spacing 3m, array pitch 3m, and individual well dose 3kg excites, and when the average explosion velocity of explosive is 5500m/s, loess density is theoretical well depth best in the medium of ρ=1.613668g/cm3.
Another example of the present invention is that uniform saturation water drift sand illustrates near surface:
Drift sand is also approaches uniformity medium common in a kind of seismic prospecting, for saturation water drift sand:
1) excitation condition 2 × H × 6kg that saturation water drift sand is main at present, well spacing 5.4m are that example calculates, and use the performance parameter of explosive to calculate the thrust F (kN) of explosive at underground explosion;
The calculating of a well explosive thrust utilizes kinetic energy formula:
1 2 mv 2 = FS
Wherein, m is quality of explosive, and v is the explosion velocity of explosive, and F is the thrust that a well (6kg explosive) blast produces, and S is half well spacing (the burst radius 2.7m of explosive in saturation water drift sand);
The explosion velocity of explosive is 5000-6000m/s, and average 5500m/s.
Calculate the thrust that a well (6kg explosive) blast produces: F=33611.111kN;
Well (6kg explosive) blast thrust upwards (be 1/8 of whole space thrust, the energy that the sphere that namely centre of sphere angle is 90 degree distributes, remaining energy passes down the energy with side) and be: F/8=4201.389kN;
One big gun 2 combines (12kg explosive) blast thrust upwards: F lifting force=2 × F/8=8402.778kN.
2) best excitation well depth H is calculated with following formula:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
In formula: F lifting force-step 1) in the explosive charge thrust upwards that calculates;
H-excitation well depth;
T-2 well combines the circle that surrounds at floor projection area;
ρ-saturation water drift sand density;
F3-cylindrical sides moves upward the frictional force produced with surrounding country rock;
The horizontal stress (known technology-rock-soil mechanics) that F4-cylinder is subject to when poised state.
It should be noted that:
(1) T described in is with 2 combination well (well spacing 5.4m, burst radius is 2.7m) be example, one row totally 2 wells, each well is circular (because well spacing is larger in the projected area on earth's surface, well number is few, rectangle is thought so can not be similar to), T is (see the Fig. 5) that can accurately calculate:
T=2×π×2.7m×2.7m=45.78m 2
(2) ρ described in is the density of saturation water drift sand.Gather the primary rock sample (saturation water drift sand) in combination well area, calculate drift sand density;
Described calculating drift sand density is the container using known weight and volume, gathers the primary drift sand sample of more than 6, utilizes density formula (m 2=ρ v 2) calculate the averag density of saturation water drift sand.
In formula: m 2the weight of saturation water drift sand, v 2be the volume of drift sand, calculating saturation water drift sand density p is=1.890056g/cm3;
(3) F3 described in is that cylinder moves upward the frictional force produced with surrounding country rock;
F3=cylindrical sides amasss the × intergranular free frictional resistance of drift sand;
Wherein the intergranular free frictional resistance of drift sand needs to measure:
Measuring method is: measure the soil body (drift sand and loess) when same volume, the cone of formation is slowly toppled over to horizontal plane, drift sand and loess centrum have different basal diameter and vertebral height, the different physical phenomenon of this centrum shape, be drift sand and loess ground particle between the performance of free frictional resistance difference in size.
Same volume of the present invention is bottom surface circular diameter 6.5cm, the cylinder of height 7cm.
Through overtesting, the result obtained is:
Loess cone: base diameter 13.7 centimetres, height 6cm;
Drift sand cone: base diameter 15.2 centimetres, height 4.8cm;
The side of its intermediate cam centrum and the angle of horizontal plane are exactly θ; This angle θ is exactly the angle used when doing the decomposition of object gravity G on inclined-plane.The height of drift sand cone is 4.8cm, and bottom surface radius is 7.6cm (see Fig. 6).
sin θ = 4.8 4.8 2 + 7.6 2 = 0.53
Wherein this inclination angle relation is 1.0m with hypotenuse in fig. 3, and the right-angle side that a certain formation sine value is 0.66 is 0.53m, and another right-angle side is 0.85m.This relation represents: when θ=arcsin (0.53), the intergranular friction power of drift sand reaches balance, and namely θ angle increases again, and drift sand particle will glide.
So, 1m 2free frictional force between the sand grain of upper reaches, inclined-plane is (see Fig. 7):
f1m 2=(1/2)×0.53m×0.85m×1m×1890kg/m 3×9.8N/kg×0.53=2211.2N
Calculate drift sand (cylinder) to move upward the frictional force F3 produced with surrounding country rock;
F3=f side
F side---take circle the end of as, H is the cylindrical side of thickness, and burst radius is 2.7m, produce when moving upward with the frictional force (see Fig. 8) of country rock.
F3=f side=H × 4 × π × 2.7 × f1m2=75.024H (kN)
F3=75.02H(kN)
(4) horizontal stress that is subject to when poised state of cylinder
The horizontal stress that F4=cylinder drift sand is subject to;
F 4 = ( H × T × ρ × 9.8 N kg ) × μ 1 - μ
H × T × ρ × 9.8N/kg---be the vertical stress that saturation water drift sand is subject to;
H-excitation well depth;
The floor projection circular area that T-2 combination well surrounds;
ρ-saturation water drift sand density;
μ---be the Poisson's ratio of drift sand medium.
By inspection information and the article published: drift sand Poisson's ratio value μ is (less than the Poisson's ratio 0.30-0.35 of sand and the Poisson's ratio 0.35-0.40 of silt) between 0.20 ~ 0.30, and we get intermediate value μ=0.25.
Then: F4=H × 45.78m 3× 1890kg/m 3× 9.8N/kg × μ/(1-μ)
=(0.25/0.75)×847.937H
=282.646H(kN)
(5) the best excitation well depth (innovative technology) in saturation water drift sand is calculated:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
8402.778kN=H×45.78m 3×1890kg/m 3×9.8N/kg+75.02H+282.646H
H=6.969777m
Then " H+ burst radius 2.7m=9.669777m " is exactly in 2 combinations, well spacing 5.4m, and individual well dose 6kg excites, and when the average explosion velocity of explosive is 5500m/s, saturation water drift sand density is theoretical well depth best in the medium of ρ=1.8900g/cm3.
In order to the reliability that argumentation theory calculates, in loess, arranged the test of one group of excitation well depth, adopted 11 mouthfuls of well shootings on group, well depth from 8-21m, individual well dose 3kg.Do energy spectrometer to the single big gun data gathered, the conclusion obtained is between well depth 14-16m, and the energy passed down is obviously strengthened, with the result of theory calculate closely.
Above-described specific embodiment; object of the present invention, technical scheme and beneficial effect are further described; be understood that; the foregoing is only specific embodiments of the invention; the protection domain be not intended to limit the present invention; within the spirit and principles in the present invention all, any amendment made, equivalent replacement, improvement etc., all should be included within protection scope of the present invention.

Claims (8)

1. determine a method for best excitation well depth in uniform dielectric, it is characterized in that adopting following steps to realize:
1) according to using the performance parameter of explosive to calculate the thrust F of explosive at underground explosion; The 1/8 calculating one big gun combination well blast thrust F lifting force upwards of explosive thrust to lifting force according to blast:
F lifting force=combination well number × F ÷ 8;
2) best excitation well depth H is calculated with following formula:
Explosive thrust F lifting force=H × T × ρ × 9.8N/kg+F3+F4;
In formula: F lifting force-step 1) in the explosive charge thrust upwards that calculates;
H-excitation well depth;
The floor projection area that T-combination well surrounds;
ρ-soil body density;
F3-soil body moves upward the frictional force produced with surrounding country rock;
The horizontal stress that F4-soil body is subject to when poised state.
2. method according to claim 1, is characterized in that step 1) described in blast thrust F calculate be utilize following kinetic energy formula:
1 2 mv 2 = FS
Wherein, m is quality of explosive, and v is the explosion velocity of explosive, and F is the explosive thrust of a well, and S is half well spacing.
3. method according to claim 2, feature is the explosion velocity of described explosive is 5000-6000m/s, and average 5500m/s.
4. method according to claim 1, is characterized in that step 2) described in the calculating of soil body density p be the container using known weight and volume, gather the primary soil sample of more than 2, utilize density formula m 2=ρ v 2calculate the averag density of soil sample, in formula: m 2the weight of soil sample, v 2it is the volume of soil sample.
5. method according to claim 1, is characterized in that step 2) described in the soil body frictional force F3 produced with surrounding country rock that moves upward adopt following formulae discovery:
The all combination wells of F3=surround the intergranular free frictional resistance of area × soil body of the soil body and surrounding country rock.
6. method according to claim 1, it is characterized in that step 2) described in the intergranular free frictional resistance measurement of the soil body be: the same volume soil body slowly topples over the cone of formation to horizontal plane, angle used when the side of cone and the angle theta of horizontal plane are the decomposition being object gravity G on inclined-plane, the intergranular free frictional resistance f of the soil body c: f c=G × sin θ.
7. method according to claim 6, feature is described same volume is bottom surface circular diameter 6.5cm, the cylinder of height 7cm.
8. method according to claim 1, feature is step 2) described in the horizontal stress F4 that is subject to when poised state of the soil body adopt following formulae discovery:
F 4 = ( H × T × ρ × 9.8 N kg ) × μ 1 - μ
Wherein: μ is the Poisson's ratio of soil medium.
CN201480002778.4A 2014-09-19 2014-09-19 Method for determining best shot hole depth in homogeneous mediums Pending CN104870067A (en)

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CN112305601A (en) * 2019-07-31 2021-02-02 中国石油化工股份有限公司 Seismic exploration acquisition excitation well design method based on chromatographic inversion
CN112526610B (en) * 2019-09-17 2023-03-21 中国石油化工股份有限公司 Three-dimensional seismic acquisition excitation well depth design method for constrained surface layer modeling

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