A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows

Trace intensity is defined as mean total trace length of discontinuities per unit area, which is an important geometric parameter to describe fracture networks. The probability of each trace appearing in the sampling surface is different since discontinuity orientation has a scatter and is probabili...

Full description

Saved in:
Bibliographic Details
Main Authors: Xiaoxue Huo, Qiong Wu, Huiming Tang, Zhen Meng, Di Wang, Yuxin Liu, Shiyu Li
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2020/8834861
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832547690506878976
author Xiaoxue Huo
Qiong Wu
Huiming Tang
Zhen Meng
Di Wang
Yuxin Liu
Shiyu Li
author_facet Xiaoxue Huo
Qiong Wu
Huiming Tang
Zhen Meng
Di Wang
Yuxin Liu
Shiyu Li
author_sort Xiaoxue Huo
collection DOAJ
description Trace intensity is defined as mean total trace length of discontinuities per unit area, which is an important geometric parameter to describe fracture networks. The probability of each trace appearing in the sampling surface is different since discontinuity orientation has a scatter and is probabilistically distributed, so this factor should be taken into account in trace intensity estimation. This paper presents an approach to estimate the two-dimensional trace intensity by considering unequal appearing probability for discontinuities sampled by rectangular windows. The estimation method requires the number of discontinuities intersecting the window, the appearing probability of discontinuities with both ends observed, one end observed, and both ends censored, and the mean trace length of discontinuities intersecting the window. The new estimator is validated by using discontinuity data from an outcrop in Wenchuan area in China. Similarly, circular windows are used along with Mauldon’s equation to calculate trace intensity using discontinuity trace data of the same outcrop as a contrast. Results indicate that the proposed new method based on rectangular windows shows close accuracy and less variability than that of the method based on circular windows due to the influence of finite sample size and the variability of location of the window and has advantage in application to sampling surfaces longer in one direction than in the other such as tunnel cross sections and curved sampling surfaces such as outcrops that show some curvature.
format Article
id doaj-art-23cf900021a448b58dc5bc63219e4968
institution Kabale University
issn 1687-8086
1687-8094
language English
publishDate 2020-01-01
publisher Wiley
record_format Article
series Advances in Civil Engineering
spelling doaj-art-23cf900021a448b58dc5bc63219e49682025-02-03T06:43:37ZengWileyAdvances in Civil Engineering1687-80861687-80942020-01-01202010.1155/2020/88348618834861A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling WindowsXiaoxue Huo0Qiong Wu1Huiming Tang2Zhen Meng3Di Wang4Yuxin Liu5Shiyu Li6Faculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaFaculty of Engineering, China University of Geosciences, Wuhan 430074, ChinaTrace intensity is defined as mean total trace length of discontinuities per unit area, which is an important geometric parameter to describe fracture networks. The probability of each trace appearing in the sampling surface is different since discontinuity orientation has a scatter and is probabilistically distributed, so this factor should be taken into account in trace intensity estimation. This paper presents an approach to estimate the two-dimensional trace intensity by considering unequal appearing probability for discontinuities sampled by rectangular windows. The estimation method requires the number of discontinuities intersecting the window, the appearing probability of discontinuities with both ends observed, one end observed, and both ends censored, and the mean trace length of discontinuities intersecting the window. The new estimator is validated by using discontinuity data from an outcrop in Wenchuan area in China. Similarly, circular windows are used along with Mauldon’s equation to calculate trace intensity using discontinuity trace data of the same outcrop as a contrast. Results indicate that the proposed new method based on rectangular windows shows close accuracy and less variability than that of the method based on circular windows due to the influence of finite sample size and the variability of location of the window and has advantage in application to sampling surfaces longer in one direction than in the other such as tunnel cross sections and curved sampling surfaces such as outcrops that show some curvature.http://dx.doi.org/10.1155/2020/8834861
spellingShingle Xiaoxue Huo
Qiong Wu
Huiming Tang
Zhen Meng
Di Wang
Yuxin Liu
Shiyu Li
A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
Advances in Civil Engineering
title A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
title_full A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
title_fullStr A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
title_full_unstemmed A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
title_short A New Approach for Estimating Rock Discontinuity Trace Intensity Based on Rectangular Sampling Windows
title_sort new approach for estimating rock discontinuity trace intensity based on rectangular sampling windows
url http://dx.doi.org/10.1155/2020/8834861
work_keys_str_mv AT xiaoxuehuo anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT qiongwu anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT huimingtang anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT zhenmeng anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT diwang anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT yuxinliu anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT shiyuli anewapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT xiaoxuehuo newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT qiongwu newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT huimingtang newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT zhenmeng newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT diwang newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT yuxinliu newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows
AT shiyuli newapproachforestimatingrockdiscontinuitytraceintensitybasedonrectangularsamplingwindows