CN1645101A - Determining method for mechanics quality stable threshold of rock structural face - Google Patents
Determining method for mechanics quality stable threshold of rock structural face Download PDFInfo
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- CN1645101A CN1645101A CN 200510048954 CN200510048954A CN1645101A CN 1645101 A CN1645101 A CN 1645101A CN 200510048954 CN200510048954 CN 200510048954 CN 200510048954 A CN200510048954 A CN 200510048954A CN 1645101 A CN1645101 A CN 1645101A
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- jrc
- stable threshold
- roughness coefficient
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Abstract
A method for confirming stable threshold includes preparing 10cm and 30cm test section on small size rock structural surface, measuring and calculating out necessary data, using JRC dimension effect fractal model to convert out JRC dimension effect fractal dimension D30, using JRC dimension effect rate formula f=(0.1Ln)-D30-(0.1Ln-1)-D30/2-D30-1 to carry out analysis of sampling length Ln to effect rate f for obtaining Ln-f relation chart, confirming that corresponding length of sampling on chart is the stable threshold when f=5% is taken on the chart.
Description
(1) technical field
The present invention relates to mechanics quality stable threshold of rock structural face and determine method.
(2) background technology
Before the present invention makes, still there is not mechanics quality stable threshold of rock structural face to determine method at present.The rock mass discontinuity mechanical property has size effect character, owing to there is not mechanics quality stable threshold of rock structural face to determine method, the specimen size that can't solve the size effect reduction value of indoor mechanical property test findings, the test of on-the-spot mechanical property is determined and the problem such as choose of mechanical property empirical estimating length.
(3) summary of the invention
The objective of the invention is to solve owing to there is not mechanics quality stable threshold of rock structural face to determine method, and the specimen size that can't solve the test of the size effect reduction value of indoor mechanical property test findings, on-the-spot mechanical property is determined and the shortcoming of the problem such as choose of mechanical property empirical estimating length, provide a kind of principle simple, easy to operate, with low cost, result of use is good, is convenient to determine on the small scale structures face method of mechanics quality stable threshold of rock structural face.
Mechanics quality stable threshold of rock structural face of the present invention is determined method, comprises following sequential steps:
(1) on the small size rock mass discontinuity, corresponding required direction of measurement arranges that evenly statistics requisite number purpose length is respectively the survey section of 10cm and 30cm, adopts profilograph to draw the contour curve of above-mentioned survey section;
(2) measure the relief intensity R that above-mentioned 10cm surveys each contour curve of section
Y0, by formula
Calculate each 10cm respectively and survey section roughness coefficient JRC
0Value is surveyed the different roughness coefficient of section according to each 10cm and is calculated JRC
0Expectation value E (JRC
0);
(3) measure the relief intensity R that above-mentioned 30cm surveys each contour curve of section
Y30, by formula
Calculate each 30cm respectively and survey section roughness coefficient JRC
30Value is surveyed the different roughness coefficient of section according to each 30cm and is calculated JRC
30Expectation value E (JRC
30);
(4) by JRC size effect fractal model
Conversion obtains rock mass discontinuity JRC size effect Fractal dimensions
30
(5) the JRC size effect Fractal dimensions that step (4) is obtained
30The relative JRC size effect of value substitution rate formula
Carry out sample length L
nSensitivity analysis with relative JRC size effect rate f obtains L
n-f graph of a relation, as shown in Figure 1.At L
nOn-f the graph of a relation, when getting f=5%, L
nSample length corresponding on the-f relation curve is rock structural plane roughness coefficient stable threshold L
n *
(6) the rock structural plane roughness coefficient stable threshold L that step (5) is determined
n *As mechanics quality stable threshold of rock structural face.
Employing the present invention have the following advantages: with mechanics quality stable threshold of rock structural face L
n *Foundation as the analysis of rock mass discontinuity mechanics quality stable, the specimen size of promptly carrying out the test of the size effect reduction value of the indoor mechanical property test findings of rock mass discontinuity, on-the-spot mechanical property is determined and during the choosing of mechanical property empirical estimating length, the sampling size of selected structural plane should be greater than L
n *, could guarantee that the estimation of stability that the stability and the reliability of mechanical property of structural plane, its result can directly apply to engineering rock mass calculates.Mechanics quality stable threshold of rock structural face determines that the method principle is simple, realize very easily owing to only need on the small size rock mass discontinuity, to carry out the statistical measurement of roughness coefficient, with low cost, result of use is good, be convenient to determine mechanics quality stable threshold of rock structural face, the specimen size that solves the test of the size effect reduction value of indoor mechanical property test findings, on-the-spot mechanical property determines and the problem such as choose of mechanical property empirical estimating length to have bigger implementary value and economic results in society.
(4) description of drawings
Fig. 1 is L
n-f graph of a relation
Fig. 2 is Xiao Langdi SSE group joint L
n-f relation curve
(5) embodiment
Studies show that the size effect of rock mass discontinuity mechanical property is mainly caused by the size effect of roughness coefficient, so can be with the rock structural plane roughness coefficient stable threshold as mechanics quality stable threshold of rock structural face.Diorite joint, Beishan Mountain sampling size is that the JRC statistical measurements of 10cm to 100cm is found, the JRC size effect fractal dimension (D of the different sampling sizes of same structural plane equidirectional
n) have a relative stability, D
nValue is around a certain eigenwert D
n *Fluctuation (is D up and down
n *-δ≤D
n≤ D
n *+ δ, δ are residual error, D
n *Represent sample length less than L
nThe JRC size effect fractal dimension eigenwert of scope inner structure face).Actual measurement statistics substitution JRC size effect fractal model with different sampling size roughness coefficients
Carry out the least square regression analysis and can ask for D
n *Value, be L with sampling size
30=30cm roughness coefficient JRC
30Actual measurement statistical value substitution JRC size effect fractal model
Can obtain D
30Value, to J
1-1The D of 16 samples of joint four measuring direction
n *And D
30Field data carries out statistical study opening relationships formula:
D
n *=0.897D
30????????????????????????????(1)
This character has determined to use small-scale structure surface roughness coefficient measurement result D
30Analyze the stable threshold of large scale rock structural plane roughness coefficient, and then the stable threshold of definite rock mass discontinuity mechanical property; The result of study at diorite joint, the Beishan Mountain shows, at L
n≤ 10
6In the scope of cm, JRC size effect fractal dimension eigenwert D
n *(can be by D
30Expression) is subjected to sampling size L
nThe influence that changes is very responsive, this phenomenon explanation JRC size effect fractal dimension index (D
30) determine that the roughness coefficient stable threshold has very high sensitivity.Above-mentioned two point discoveries have proved by D
30Mensuration ask for the science and the rationality of roughness coefficient stable threshold, can be used for determining mechanics quality stable threshold of rock structural face.
Choose Xiaolangdi Dam Project wind and rain ditch west side slope rock mass SSE group joint, be respectively 10cm and the 30cm contour curve is tried to achieve JRC according to 387 sample lengths
0, JRC
30Statistical measures, and the D that converts by JRC size effect fractal model
30Value the results are shown in table 1.According to table 1 data, draw calcareous packsand joint, clay-with-race rock joint on the strike direction and across strike direction L respectively
n-f relation curve, as shown in Figure 2.Can be obtained by Fig. 2, the roughness coefficient stable threshold L of direction is moved towards at calcareous packsand joint
n *Be 120cm, shown in Fig. 2 a, the roughness coefficient stable threshold L of calcareous packsand joint tendency direction
n *Be 110cm, shown in Fig. 2 b, the roughness coefficient stable threshold L of direction is moved towards at clay-with-race rock joint
n *Be 150cm, shown in Fig. 2 c, the roughness coefficient stable threshold L of clay-with-race rock joint tendency direction
n *Be 160cm, shown in Fig. 2 d.The roughness coefficient stable threshold at above-mentioned all directions joint is corresponding mechanics quality stable threshold of rock structural face.
Table 1 Xiao Langdi SSE group Joint Roughness Coefficient statistical measurements
Joint wall rock | Direction of measurement | ????L n=10cm | ????L n=30cm | ??D 30 | ||
Sample number | ????JRC 0 | Sample number | ???JRC 30 | |||
Calcareous packsand | Move towards direction | ????35 | ????8.61 | ????34 | ??5.50 | ??0.4079 |
The tendency direction | ????31 | ????12.12 | ????30 | ??7.43 | ??0.4454 | |
The clay-with-race rock | Move towards direction | ????88 | ????15.83 | ????84 | ??11.86 | ??0.2628 |
The tendency direction | ????82 | ????20.48 | ????77 | ??15.46 | ??0.2560 |
Claims (1)
1, a kind of mechanics quality stable threshold of rock structural face is determined method, it is characterized in that comprising following sequential steps:
(1) on the small size rock mass discontinuity, corresponding required direction of measurement arranges that evenly statistics requisite number purpose length is respectively the survey section of 10cm and 30cm, adopts profilograph to draw the contour curve of above-mentioned survey section;
(2) measure the relief intensity R that above-mentioned 10cm surveys each contour curve of section
Y0, by formula
Calculate each 10cm respectively and survey section roughness coefficient JRC
0Value,
Survey the different roughness coefficient of section according to each 10cm and calculate JRC
0Expectation value E (JRC
0);
(3) measure the relief intensity R that above-mentioned 30cm surveys each contour curve of section
Y30, by formula
Calculate each 30cm respectively and survey section roughness coefficient JRC
30Value is surveyed the different roughness coefficient of section according to each 30cm and is calculated JRC
30Expectation value E (JRC
30);
(4) by JRC size effect fractal model
Conversion obtains rock mass discontinuity JRC size effect Fractal dimensions
30
(5) the JRC size effect Fractal dimensions that step (4) is obtained
30The relative JRC size effect of value substitution rate formula
Carry out sample length L
nSensitivity analysis with relative JRC size effect rate f obtains L
n-f graph of a relation is at L
nOn-f the graph of a relation, when getting f=5%, L
nSample length corresponding on the-f relation curve is rock structural plane roughness coefficient stable threshold L
n *(6) the rock structural plane roughness coefficient stable threshold L that step (5) is determined
n *As mechanics quality stable threshold of rock structural face.
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CNB2005100489540A CN1296697C (en) | 2005-01-12 | 2005-01-12 | Determining method for mechanics quality stable threshold of rock structural face |
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CNB2005100489540A CN1296697C (en) | 2005-01-12 | 2005-01-12 | Determining method for mechanics quality stable threshold of rock structural face |
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CN1645101A true CN1645101A (en) | 2005-07-27 |
CN1296697C CN1296697C (en) | 2007-01-24 |
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Cited By (4)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102900062A (en) * | 2012-10-17 | 2013-01-30 | 三峡大学 | Comprehensive analysis method for stability of excavation unloading rock mass |
CN105004662A (en) * | 2015-07-08 | 2015-10-28 | 中国科学院力学研究所 | Method for testing contact rigidity of rock discontinuity structural plane, and apparatus thereof |
CN106546189A (en) * | 2016-11-14 | 2017-03-29 | 绍兴文理学院 | A kind of anisotropic evaluation methodology of array of sizes rock mass discontinuity relief intensity |
CN107228929A (en) * | 2017-06-07 | 2017-10-03 | 绍兴文理学院 | The accurate value field operation method of mine slope rock mass structural plane shearing strength |
Family Cites Families (3)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
FR2605746B1 (en) * | 1986-10-28 | 1989-06-09 | Elf Aquitaine | METHOD FOR DETECTING HETEROGENEITIES AND / OR DETERMINING PETROPHYSICAL CHARACTERISTICS OF GEOLOGICAL LAYERS OF AN ENVIRONMENT TO BE EXPLORED |
JP2002213943A (en) * | 2001-01-16 | 2002-07-31 | Mitsutoyo Corp | System and method for measuring surface property |
CN1462865A (en) * | 2002-05-30 | 2003-12-24 | 浙江工业大学 | Multirange ruler of roughness |
-
2005
- 2005-01-12 CN CNB2005100489540A patent/CN1296697C/en not_active Expired - Fee Related
Cited By (4)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102900062A (en) * | 2012-10-17 | 2013-01-30 | 三峡大学 | Comprehensive analysis method for stability of excavation unloading rock mass |
CN105004662A (en) * | 2015-07-08 | 2015-10-28 | 中国科学院力学研究所 | Method for testing contact rigidity of rock discontinuity structural plane, and apparatus thereof |
CN106546189A (en) * | 2016-11-14 | 2017-03-29 | 绍兴文理学院 | A kind of anisotropic evaluation methodology of array of sizes rock mass discontinuity relief intensity |
CN107228929A (en) * | 2017-06-07 | 2017-10-03 | 绍兴文理学院 | The accurate value field operation method of mine slope rock mass structural plane shearing strength |
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