Mathematical Problems in Engineering

Mathematical Problems in Engineering / 2019 / Article

Research Article | Open Access

Volume 2019 |Article ID 8718936 | 11 pages | https://doi.org/10.1155/2019/8718936

Neutrosophic Function with NNs for Analyzing and Expressing Anisotropy Characteristic and Scale Effect of Joint Surface Roughness

Academic Editor: Mijia Yang
Received17 Nov 2018
Accepted25 Mar 2019
Published14 Apr 2019

Abstract

The shear behavior of rock mass significantly depends upon the surface roughness of rock joints which is generally characterized by the anisotropy characteristic and the scale effect. The large-scale natural rock joint surfaces, at Qingshi Town, southeast of Changshan County, Zhejiang Province, China, were used as a case study to analyze the roughness characteristics. A statistical assessment of joint roughness coefficient (JRC) indicated the roughness anisotropy of different sized rock joints. The lower limit () was regarded as the determinate information, and the difference between lower and upper limits represented indeterminate information. The neutrosophic number (NN) was calculated to express the various JRC values. The parametric equations for JRC anisotropic ellipse were presented based on the JRC statistical assessment of joint profiles of various orientations. The JRC values of different sized joint samples were then quantitatively described by the neutrosophic function. Finally, a neutrosophic parameter for evaluating the scale effect on the surface roughness anisotropy was introduced using the ratio of maximum directional roughness to minimum directional roughness. The case study indicates that the proposed method has the superiority in moving forward from subjective assessment to quantitative and objective analysis on anisotropy characteristic and scale effect of joint surface roughness.

1. Introduction

Joint roughness is one of the most important parameters for understanding the shear behavior of rock joints [15]. Yet the irregularity or roughness of rock surfaces is difficult to estimate. Thus, during the past few decades, considerable effort has been devoted to estimating the roughness properties of rock joint surfaces. Since Barton [6] first introduced the joint roughness coefficient (JRC) for quantifying rock joint roughness, various roughness parameters have been established for roughness characterization [712]. The scale effect on surface roughness has been proven to be an inherent property of rock joints. Consequently, a large number of researchers have attempted to determine the scale dependency of joint surface roughness by relating the roughness parameters to the joint sample size. Du et al. [13] found that the negative scale effect exists in rock joint roughness by statistical analysis of asperity amplitudes. Furthermore, anisotropy is everywhere in rock engineering, and the joint roughness varies directionally, which is an important source of anisotropic behavior of rock joints. Chen et al. [14] used geological statistics to analyze the anisotropy and the scale effect of rock joints using the sill value and the range of variogram. The statistical analysis of the directional JRC values of different sized rock joint samples may disclose the scale effect of joint roughness. Fardin et al. [15] investigated the scale effect on the surface roughness of rock joints using fractal concepts. The fractal parameters remained almost constant when the sampling windows were larger than the stationarity threshold. Yong et al. [16] analyzed the sampling problem in studying the scale effect of rock joints and proposed a sampling method based on a systematic sampling technique for quantitatively evaluating roughness characteristics and representativeness of different sized rock joints. However, the roughness characteristics are difficult to quantify because of the irregularity and inconsistency of joint roughness of different sized samples in various measurement orientations. Moreover, none of the previous studies considered the scale effect on the surface roughness anisotropy of rock joints.

The real world consists of determinate and/or indeterminate information. A neutrosophic number (NN) presented by Smarandache [1719] seems appropriate for expressing them because a NN consists of a determinate part and an indeterminate part for , where the symbol denotes indeterminacy and represents real numbers. Recently, Ye [20] developed a bidirectional projection model of NNs for a multiple attribute group decision-making problem. Then, Ye [21] proposed a deneutrosophication method and a possibility degree ranking method for neutrosophic numbers and applied these methods to a group decision-making problem under a NN environment. Kong et al. [22] introduced a cosine similarity measure of NNs and applied it to the misfire fault diagnosis of gasoline engine. Further, Ye [23] presented an exponential similarity measure of NNs for the fault diagnosis of steam turbine in a NN environment. To express indeterminate functions in indeterminate problems, Smarandache [24] introduced the interval function (thick function), which is defined as a neutrosophic function h: , where represents all real numbers and is all interval functions, denoted by the form of an interval function for . Smarandache’s neutrosophic function, however, cannot express and deal with functions involving NNs. Ye et al. [25] expressed the joint roughness coefficient and the shear strength in rock mechanics by means of neutrosophic functions (interval functions). It is necessary to introduce new neutrosophic functions containing NNs for statistical assessment of joint roughness, containing both determinate information and indeterminate information. Consequently, NN is appropriate for expressing various JRC values, because it consists of determinate and indeterminate parts.

The objectives of this paper are as follows: (1) presenting some basic operations of NNs and new neutrosophic function with NNs; (2) developing the parametric equations for JRC anisotropic ellipse to characterize the joint profiles in various orientations; (3) presenting a neutrosophic function with NNs to describe the JRC values of different sized joint samples; and (4) developing a neutrosophic parameter to evaluate the scale effect on the surface roughness anisotropy using the ratio of maximum directional roughness to minimum directional roughness.

2. NNs and Neutrosophic Functions

2.1. Some Basic Operations of NNs

In indeterminate environments, Smarandache [1719] presented the concept of NN. It consists of a determinate part and an indeterminate part . Its mathematical expression is for , where is indeterminacy and represents all real numbers. It has been successfully applied to represent determinate and/or indeterminate information in real problems.

When NN is considered as , its determinate value is 2 and its indeterminate value is . In application, a possible interval range of indeterminacy is often specified to satisfy concrete application requirements. For example, if the indeterminacy is considered to fall within an possible interval [0, 0.1], then it is equivalent to , where is within the interval . If is the interval range, then z = [2.2, 2.4].

Yet, may be a possible interval number, where for (Z is all NNs) and . Specially, if for the best case, then equals the determinate part . But if is the worst case, then is the same as the indeterminate part z = bI.

For two NNs z1 = a1 + b1I and z2 = a2 + b2I for z1, z2 Z and I∈ [IL, IU], the basic operational laws are derived as follows:

3. Data Acquisition

A 141.4 cm ×141.4 cm joint surface sample was collected from a large sized, slightly weathered, slate rock surface with an orientation of N40W, 35NW at Qingshi Town, southeast of Changshan County, Zhejiang Province, China. The grayish-green colored slate rock is foliated, very fine-grained, and formed by the metamorphosis of intermediate tuff, and the joint surface is relatively smooth and planar. The surface profiles were measured in 25 different orientations at an interval of 15° (Figure 1). A simple mechanical hand profilograph (Figure 2) was employed to measure the rock joint profiles. The profilograph consists of feeler, drawing pen, balance block, fixed board, bubble levels, and drawing paper. It is easy to operate and correctly records a large number of joint traces with minimal cost. In this study, the number of measured roughness profiles with different orientations and sample sizes was 19,616. These recorded joint profiles were scanned by a large format scanner. On the basis of pixel analysis, the joint profiles were then digitized with a sampling interval of 0.5 mm, which is fairly often used in previous studies on joint roughness determination [26].

Many studies regarding JRC evaluation have been carried out over the past three decades. The most commonly used methods include visual comparison, root mean square method (Z2), roughness profile index method (Rp), and fractal approaches (D). However, none of these studies considered the combined effects of shear direction, the scale of joint surfaces, the inclination angle, and the amplitudes of asperities in joint roughness calculations. To overcome these shortcomings, Zhang et al. [27] developed a logistic function between JRC and the ratio of asperity amplitude to profile length. The inclination angle, the amplitude of asperities, and their directions were considered in this method. This procedure was proved to be accurate and efficient in JRC evaluation via the comparisons with different kinds of test results. Consequently, it was used in this study to calculate the JRC values for different sized and orientated profiles. It is briefly introduced as follows.

First, an arbitrary horizontal reference line was assumed to pass through the digitized profile. The mean vertical distance between the reference line and the points along the roughness profile was calculated by where L is the length of a digitized roughness profile and x and y are the horizontal and vertical coordinates of the points on the profile, respectively.

Those profile segments whose dip-direction is opposite to the shear direction were significant in determining joint roughness in the direction of shearing. The modified root mean square taking into account the positive dilation angles was determined by

A roughness index λ was introduced by Zhang et al. [27] and written as

The JRC value was then calculated based on the following logistic correlation with λ, as

This procedure was repeated to determine the JRC evaluation for all profiles.

4. Neutrosophic Function with NNs for Anisotropy Characteristics of Joint Surface Roughness

The JRC values of joint samples in different orientations were calculated and displayed on the polar plots. For example, Figure 3 shows the JRC values of 10 cm joint samples with various orientations from 0° to 345° at a 15° interval. As can be observed, the JRC values in some orientations (e.g., 0° and 180°) were greater, while the values in the orientations of 90° and 270° were relatively smaller. The JRC values in all orientations were randomly distributed in a range from 0 to 20. The JRC distributions of 10cm joint samples in the orientations of 0°, 90°, 180°, and 270° are illustrated in Figure 4. These frequency distributions can be represented graphically by the characteristic bell-shaped curves, which are close to the “Normal Distribution” or the “Right-skewed Distribution.” The mean value and the standard deviation σ of JRC values in the 0° orientation were 10.536 and 2.233. For those joint samples in the 180° orientation, and σ were 9.850 and 2.144, respectively. The JRC mean values in the 90° and 270° orientations were 7.047 and 6.802, respectively, and the standard deviations were 2.405 and 2.117.

A low standard deviation indicates that the data points tend to approximate the mean value. Here, the JRC values in a range from (lower limit) to (upper limit) were chosen to describe the roughness anisotropy characteristics. As shown in Figure 4, a total of 68.62%, 73.37%, 72.41%, and 71.19% of the directional joint roughness samples fell within the range [, ]. The polar plots of the upper and lower limits of JRC values showed a pattern similar to an ellipse (Figure 5). The parametric equations for each anisotropic ellipse arewhere x, y are the coordinates of any point on the ellipse; a and b are the radius on the x and y axes, respectively, and θ is the orientation, which ranges from 0 to 2π in radians.

For joint samples of each size, two ellipse envelopes can be established to fit the upper and lower limits of JRC values based on the least square method (LSM). The JRC values indicating the anisotropy characteristics should be spread among the two ellipse envelopes. According to the concept of NNs, the parametric equations with NNs for JRC arewhere n1, n2 are the radius of the inside ellipse envelope; μn1, μn2 are twice the difference in radius of the outside and inside ellipse envelopes. For example, n1, n2 of the inside ellipse envelope were 8.655 and 5.808, and n3, n4 of the outside ellipse envelope were 13.074 and 9.924 (Figure 5). Then, the μn1, μn2 terms can be calculated as follows:

Thus, the neutrosophic functions based on the parametric equations with NNs for describing the anisotropy characteristic of 10cm joint samples were

The fitting results of two NN radiuses (a=n1+μn1I and b=n2+μn2I for I∈[0, 0.5]) using the neutrosophic functions based on the parametric equations for the anisotropy characteristics of different sized joint samples are tabulated in Table 1.


Scale (cm)

108.6558.8385.8088.232
208.3327.0095.7106.467
308.0286.4555.5485.477
407.9025.9785.4794.668
507.6385.9255.3434.349
607.4765.6395.5244.976
707.5035.2295.2464.602
807.4014.6935.1374.179
907.2714.2565.0973.735
1007.1783.9465.0453.319

By using (3) and (10), the directional JRC values with NN functions, , within I∈[0, 0.5] can be derived by

According to the fitting results of NNs of different sized joint samples in Table 1, the JRC neutrosophic functions of different sized joint profiles in each orientation can be obtained by using (13). The calculated results are tabulated in Table 2.


Orientation
(°)10 cm20 cm30 cm40 cm50 cm



Orientation
(°)60 cm70 cm80 cm90 cm100 cm