A method of layer being carried out into formula breakdown diagnosis to rock
Technical field
It is especially a kind of that layer being carried out into formula damage to rock the present invention relates to a kind of method carrying out breakdown diagnosis to rock sample
The method of analysis.
Background technology
With going deep into for scientific research, the method for carrying out breakdown diagnosis to rock sample now is to carry out CT to impaired rock sample mostly
Scanning analyzes the extent of damage of rock interior by the size of the bright-dark degree of the imaging after CT scan and CT values.And existing rank
Section by CT scan analyze rock method it is main there are three:
1, comparison of light and shade with the naked eye is carried out to CT images;
The CT scan figure of a certain level of rock, figure is brighter, indicates that rock compactness is better.A small number of stains at middle part indicate
There are localized voids, although can intuitively observe that the hole of rock interior compares using the method, substantially obtains the damage of rock
Hinder rule, the analysis of a quantization can not be but carried out to it, can not accurately determine damage range.
2, the foundation that limited circle takes the CT average values in face to analyze as a whole is chosen in level
Whether there is or not several circumference from the center of circle to periphery, it was therefore concluded that accuracy can be taken with the circle of selection face quantity difference
And it is different, but all the points can not be covered always, so being unable to get an accurate conclusion.
3, criterion of the CT average values of rounding scanning level as scanning level compactness.But this method can not be anti-
The damage comparison inside rock sample is reflected, using the CT values as basis for estimation, can not reflect the inhomogeneities of scanning level.
Invention content
Layer is carried out into the method for formula breakdown diagnosis to rock technical problem to be solved by the invention is to provide a kind of, it can be with
It solves existing method and is unable to get the CT average values for covering all the points, as a result inaccurate problem is accurate to reflect the impaired of rock
The extent of damage in infinitely small damage range can be obtained in degree, easy to operate, does not have to frequent operation.
In order to solve the above technical problems, the technical solution adopted in the present invention is:It is a kind of that layer being carried out into formula damage to rock
The method of analysis, this approach includes the following steps:
Step 1:The a certain cross section on rock sample is chosen, region division is carried out to the cross section:From the cross section
Central point sets out, and marks off the sample ring of N number of equal semidiameters;
Step 2:Calculate the CT average values CT of various kinds ring under original stateTave(N):Respectively to the circle where each sample ring
Initial CT scan is carried out, the CT values for obtaining the circle where each sample ring are CT1 is initial、CT2 is initial、CT3 is initial…CTN is initial, measure each
The area value of circle where sample ring is S1、S2、S3…SN,
The CT average values CT of various kinds ring under original stateTave (N) is initial=(CTN-CTN-1)/(SN-SN-1);
Step 3:It is real to calculate separately each group Frozen-thawed cycled for the freeze-thaw cycle experiment that the different numbers of n groups are carried out to the rock sample
Test the CT average values CT of rear various kinds ringTave (N) n-th group, calculation formula is
CTThe 1st group of Tave (N)=(CTThe 1st group of N-CT(N-1) the 1st group)/(SN-SN-1),
CTThe 2nd group of Tave (N)=(CTThe 1st group of N-CT(N-1) the 2nd group)/(SN-SN-1),
…
CTTave (N) n-th group=(CTN n-th groups-CT(N-1) n-th group)/(SN-SN-1),
In formula, CTN n-th groupsFor the CT values of the circle where n-th sample ring after n-th group freeze-thaw cycle experiment;
Step 4:The data that step 2 and step 3 obtain are arranged, breakdown diagnosis is carried out to rock, judge Frozen-thawed cycled reality
Test the concentration position damaged caused by rock sample.
In step 1, rock sample is the cylindrical rock sample that radius is 2.5 centimetres, from the central point of the cross section, is divided
Go out the sample ring of 5 equal semidiameters, semidiameter is 0.5 centimetre.
The method further includes step 5:
Step 5:Region is carried out again the concentration position that the freeze-thaw cycle experiment that step 4 obtains is damaged caused by rock sample
It divides, from the central point of the cross section, the concentration position of damage is marked off into the M sample ring for waiting semidiameters;According still further to
Above-mentioned steps 2-4 carries out breakdown diagnosis to rock, judges the accurately concentration that freeze-thaw cycle experiment is damaged caused by rock sample
Position.
It is provided by the invention it is a kind of to rock carry out layer into the method for formula breakdown diagnosis, have the beneficial effect that:
1, accurately reflect the extent of damage of rock.All the points can not be covered when previous method CT scan, only with limited
The CT average values reflection of point is so the CT average values put, can not accurately reflect the extent of damage of rock.And this method passes through division
The mode of sample ring including covering all the points, is no longer limited to take the mean CT-number in face to damage rock stratum with limited circle
Wound analysis, then utilizes mathematical formulae, obtains the mean CT-number of various kinds ring, (is declined by the changing value of CT values in comparative sample ring
Value is bigger, and the extent of damage is bigger) it can accurately determine the extent of damage of rock sample various kinds loop section.
2, ring can be divided again to sample ring, the extent of damage in infinitely small damage range can be obtained.Primarily determine various kinds ring
The extent of damage after, ring can be divided again to arbitrary sample ring, obtain several thin rings, by similarly calculating, obtained in each thin ring
CT average values, then by comparing the CT average values in each thin ring, obtain each thin ring extent of damage, further reduce rock by
Damage range.
3, easy to operate, it is not required to frequent operation.Commonsense method obtains a diameter of 0.5 centimetre of cylinder rock sample damage range
The minimum time needed for CT values is 10 minutes, and is only needed using this method 2 minutes, and the operating time is greatly saved.
Description of the drawings
The invention will be further described with reference to the accompanying drawings and examples:
Fig. 1 is 5 sample ring schematic diagrames for waiting semidiameters that step 1 marks off in the embodiment of the present invention one;
Fig. 2 is to be followed according to every sample ring mean CT-number-freeze thawing that the data that step 4 sorts out are made in the embodiment of the present invention one
Ring experiment number curve graph;
Fig. 3 is to be carried out again the concentration position that freeze-thaw cycle experiment is damaged caused by rock sample in the embodiment of the present invention two
The sample ring schematic diagram of region division;
Fig. 4 is to be followed according to every sample ring mean CT-number-freeze thawing that the data that step 4 sorts out are made in the embodiment of the present invention two
Ring experiment number curve graph;
Fig. 5 is that the sample ring of the n equal semidiameters marked off to the rock sample that cross section is rectangle in the embodiment of the present invention three shows
It is intended to.
Specific implementation mode
Embodiment one
Step 1:Rock sample is the cylindrical rock sample that radius is 2.5 centimetres, a certain cross section on rock sample is chosen, to the cross
Section carries out region division:From the central point of the cross section, the sample ring of 5 equal semidiameters is marked off, is labeled as first
Sample ring, the second sample ring, third sample ring, the 4th sample ring, the 5th sample ring, semidiameter are 0.5 centimetre, as shown in Figure 1;
Step 2:Calculate the CT average values CT of various kinds ring under original stateTave(N):Respectively to the circle where each sample ring
Initial CT scan is carried out, the CT values for obtaining the circle where each sample ring are CT1 is initial、CT2 is initial、CT3 is initial…CTN is initial, measure each
The area value of circle where sample ring is S1、S2、S3…SN,
The CT average values CT of various kinds ring under original stateTave (N) is initial=(CTN-CTN-1)/(SN-SN-1)
N=5;
Step 3:It (is respectively 10 freeze-thaw cycle experiments, 30 Frozen-thawed cycled realities to carry out 3 groups of difference numbers to the rock sample
Test and 50 freeze-thaw cycle experiments) freeze-thaw cycle experiment, the CT for calculating separately various kinds ring after each group freeze-thaw cycle experiment is average
Value CTTave (N) n-th group, calculation formula is
CTThe 1st group of Tave (N)=(CTThe 1st group of N-CT(N-1) the 1st group)/(SN-SN-1),
CTThe 2nd group of Tave (N)=(CTThe 1st group of N-CT(N-1) the 2nd group)/(SN-SN-1),
…
CTTave (N) n-th group=(CTN n-th groups-CT(N-1) n-th group)/(SN-SN-1),
In formula, CTN n-th groupsFor the CT values of the circle where n-th sample ring after n-th group freeze-thaw cycle experiment, N=5, n=3, step
The data of 2 and 3 gained are as shown in table 1:
Table 1
Step 4:The data that step 2 and step 3 obtain are arranged, as shown in table 2
Table 2
According to the data of table 2 to every sample ring mean CT-number-freeze-thaw cycle experiment frequency curve figure for making, as shown in Fig. 2,
From figure 2 it can be seen that with the increase of number of freezing and thawing, the CT values amplitude of variation of the 5th sample ring is most apparent, gap
It is more maximum than variation, so Frozen-thawed cycled is concentrated mainly on the 5th sample ring, i.e. layer of the radius at 2.0-2.5 centimetres to the damage of rock
Face range.
Embodiment two
The method further includes step 5:
Step 5:The 5th sample ring mainly concentrated to the damage of rock to the Frozen-thawed cycled that step 4 obtains carries out region again
It divides, from the central point of the cross section, the concentration position of damage is marked off to the sample ring of semidiameters such as M (M=5),
Respectively 5-1 samples ring, 5-2 samples ring, 5-3 samples ring, 5-4 samples ring and 5-5 sample rings, as shown in figure 3, semidiameter is
0.1 centimetre;According still further to the step 2-4 of above-described embodiment one, the data sorted out are as shown in table 3:
Table 3
According to the data of table 3 to every sample ring mean CT-number-freeze-thaw cycle experiment frequency curve figure for making, as shown in figure 4,
Figure 4, it is seen that the CT values amplitude of variation of 5-5 sample rings is most apparent, void ratio variation is maximum, so Frozen-thawed cycled is to rock
The damage of stone is concentrated mainly on 5-5 sample rings, i.e. level range of the radius at 2.4-2.5 centimetres.
This method carries out region division with reference to certain mathematical principle to rock sample, divides the injuring rule one of rule and rock sample
It causes, the degree of injury of rock stratum each section is determined using the changing value of each region CT values, show that rock sample is damaged most serious region, then
The region is divided again, Query refinement, damage range can be accurate to arbitrary small range.
Embodiment three
It can be also rectangle by sample ring design, the sample ring of semidiameters is waited such as to n that the rock sample that cross section is rectangle marks off
Shown in Fig. 5, analyzed according to the step of above-described embodiment one and two.