1,418 research outputs found

    Rock Fracture Image Segmentation Algorithms

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    GEOMETRIC ANALYSIS TOOLS FOR MESH SEGMENTATION

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    Surface segmentation, a process which divides a surface into parts, is the basis for many surface manipulation applications which include model metamorphosis, model simplifica- tion, model retrieval, model alignment and texture mapping. This dissertation discusses novel methods for geometric surface analysis and segmentation and applications for these methods. Novel work within this dissertation includes a new 3D mesh segmentation algo- rithm which is referred to as the ridge-walking algorithm. The main benefit of this algo- rithm is that it can dynamically change the criteria it uses to identify surface parts which allows the algorithm to be adjusted to suit different types of surfaces and different segmen- tation goals. The dynamic segmentation behavior allows users to extract three different types of surface regions: (1) regions delineated by convex ridges, (2) regions delineated by concave valleys, and (3) regions delineated by both concave and convex curves. The ridge walking algorithm is quantitatively evaluated by comparing it with competing algo- rithms and human-generated segmentations. The evaluation is accompanied with a detailed geometrical analysis of a select subset of segmentation results to facilitate a better under- standing of the strengths and weaknesses of this algorithm. The ridge walking algorithm is applied to three domain-specific segmentation prob- lems. The first application uses this algorithm to partition bone fragment surfaces into three semantic parts: (1) the fracture surface, (2) the periosteal surface and (3) the articular surface. Segmentation of bone fragments is an important computational step necessary in developing quantitative methods for bone fracture analysis and for creating computational tools for virtual fracture reconstruction. The second application modifies the 3D ridge walking algorithm so that it can be applied to 2D images. In this case, the 2D image is modeled as a Monge patch and principal curvatures of the intensity surface are computed iv for each image pixel. These principal curvatures are then used by ridge walking algorithm to segment the image into meaningful parts. The third application uses the ridge walking algorithm to facilitate analysis of virtual 3D terrain models. Specifically, the algorithm is integrated as a part of a larger software system designed to enable users to browse, visualize and analyze 3D geometric data generated by NASAโ€™s Mars Exploratory Rovers Spirit and Opportunity. In this context, the ridge walking algorithm is used to identify surface features such as rocks in the terrain models

    Image-Based Modeling of Porous Media Using FEM and Lagrangian Particle Tracking

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    The study of fundamental flow and transport processes at the pore scale is essential to understanding how the mechanisms affect larger, field-scale, processes that occur in oil and gas recovery, groundwater flow, contaminant transport, and CO2 sequestration. Pore-scale imaging and modeling is one of the techniques used to investigate these fundamental mechanisms. Although extensive development of pore-scale imaging and modeling has occurred recently, some areas still need further advances. In this work, we address two areas: (1) imaging of bulk proppants and proppant-filled fractures under varying loading stress and flow simulation in these systems and (2) nanoparticle (NP) transport modeling in porous media. These are briefly explained below. Rock fracturing, followed by proppant injection, has been used for years to improve oil and gas production rates in low permeability reservoirs and is now routinely used in low-permeability resources such as a shales and tight sands. While field data makes clear the effectiveness of this technique, there is still much room to improve on the science, including how the proppant-filled fracture system responds to changes in loading stress which affect permeability and conductivity. Here, we use high-resolution x-ray computed tomography (XCT) to image two unsaturated rock/fracture/proppant systems under a series of stress levels typical of producing reservoirs: one with shale, one with Berea sandstone. The resulting XCT images were segmented, analyzed for structural and porosity changes, and then used for image-based flow modeling of Stokes flow using both finite element (FEM) and Lattice Boltzmann methods. NPs have been widely used commercially and have the potential to be extensively used in petroleum engineering as stabilizers in enhanced oil recovery operations or as tracers or sensors to detect rock and fluid properties. %In spite of a wide range of applications, many NP transport details are still unknown. In this work, we describe a Lagrangian particle tracking algorithm to model NP transport that can be used to better understand the impact of pore-scale hydrodynamics and surface forces on NP transport. Two XCT images, a Berea sandstone and a 2.5D micromodel, were meshed and used for image-based flow modeling of FEM Stokes flow. The effects of particle size, surface forces, flow rate, particle density, surface capacity, and surface forces mapped to XCT-image based mineralogy were studied

    Model Calibration, Drainage Volume Calculation and Optimization in Heterogeneous Fractured Reservoirs

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    We propose a rigorous approach for well drainage volume calculations in gas reservoirs based on the flux field derived from dual porosity finite-difference simulation and demonstrate its application to optimize well placement. Our approach relies on a high frequency asymptotic solution of the diffusivity equation and emulates the propagation of a 'pressure front' in the reservoir along gas streamlines. The proposed approach is a generalization of the radius of drainage concept in well test analysis (Lee 1982), which allows us not only to compute rigorously the well drainage volumes as a function of time but also to examine the potential impact of infill wells on the drainage volumes of existing producers. Using these results, we present a systematic approach to optimize well placement to maximize the Estimated Ultimate Recovery. A history matching algorithm is proposed that sequentially calibrates reservoir parameters from the global-to-local scale considering parameter uncertainty and the resolution of the data. Parameter updates are constrained to the prior geologic heterogeneity and performed parsimoniously to the smallest spatial scales at which they can be resolved by the available data. In the first step of the workflow, Genetic Algorithm is used to assess the uncertainty in global parameters that influence field-scale flow behavior, specifically reservoir energy. To identify the reservoir volume over which each regional multiplier is applied, we have developed a novel approach to heterogeneity segmentation from spectral clustering theory. The proposed clustering can capture main feature of prior model by using second eigenvector of graph affinity matrix. In the second stage of the workflow, we parameterize the high-resolution heterogeneity in the spectral domain using the Grid Connectivity based Transform to severely compress the dimension of the calibration parameter set. The GCT implicitly imposes geological continuity and promotes minimal changes to each prior model in the ensemble during the calibration process. The field scale utility of the workflow is then demonstrated with the calibration of a model characterizing a structurally complex and highly fractured reservoir

    Automated Rock Fracture Detection Algorithm with Convolutional Neural Networks

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    ํ•™์œ„๋…ผ๋ฌธ(์„์‚ฌ)--์„œ์šธ๋Œ€ํ•™๊ต ๋Œ€ํ•™์› :๊ณต๊ณผ๋Œ€ํ•™ ์—๋„ˆ์ง€์‹œ์Šคํ…œ๊ณตํ•™๋ถ€,2019. 8. ์†ก์žฌ์ค€.์•”๋ฐ˜์— ์กด์žฌํ•˜๋Š” ๊ท ์—ด๊ณผ ์ ˆ๋ฆฌ๋Š” ๊ฐ•๋„, ํƒ„์„ฑ๊ณ„์ˆ˜, ํˆฌ์ˆ˜๊ณ„์ˆ˜ ๋“ฑ์— ํฐ ์˜ํ–ฅ์„ ๋ฏธ์น˜๊ธฐ ๋•Œ๋ฌธ์— ์ด๋“ค์„ ์ž˜ ๊ฒ€์ถœํ•˜๋Š” ๊ฒƒ์€ ์ค‘์š”ํ•œ ๋ฌธ์ œ์ด๋‹ค. ํŠนํžˆ ์‚ฌ์ง„์ธก๋Ÿ‰๋ฒ•์€ ๊ฐ„๋‹จํ•˜๊ณ  ๊ฒฝ์ œ์„ฑ์ด ์žˆ์œผ๋ฏ€๋กœ ์ด๋ฅผ ๊ธฐ๋ฐ˜์œผ๋กœ ํ•˜๋Š” ์—ฐ๊ตฌ๋“ค์ด ์ด๋ฃจ์–ด์กŒ๋‹ค. ๊ทธ ์ค‘, ์ ˆ๋ฆฌ๋Š” ์„ ํ˜•์„ฑ์„ ๋ ๊ธฐ ๋•Œ๋ฌธ์— ๋น„๊ต์  ์ธ์‹์ด ํ‰์ดํ•˜๋‚˜, ๊ท ์—ด์€ ๋น„์ •ํ˜•์„ฑ์„ ๋ณด์ด๊ธฐ ๋•Œ๋ฌธ์— ์ธ์‹์ด ์ƒ๋Œ€์ ์œผ๋กœ ์–ด๋ ค์›Œ ๊ด€๋ จ ์—ฐ๊ตฌ๊ฐ€ ๋ถ€์กฑํ•œ ์‹ค์ •์ด๋‹ค. ๋˜ํ•œ, ๊ธฐ์กด์˜ ์—ฐ๊ตฌ๋“ค์€ ๊ท ์—ด ์ธ์‹์„ ๋ฐฉํ•ดํ•˜๋Š” ๋‹ค์–‘ํ•œ ๋…ธ์ด์ฆˆ๊ฐ€ ์—†๋Š” ์ด๋ฏธ์ง€๋ฅผ ์ฃผ๋กœ ์‚ฌ์šฉํ•˜์˜€๋‹ค. ๊ทธ๋ฆผ์ž, ๊ท ์—ด ์‚ฌ์ด์˜ ์ถฉ์ „๋ฌผ, ์‹์ƒ ๋“ฑ์˜ ๋…ธ์ด์ฆˆ๋Š” ์ „ํ†ต์ ์ธ ์•Œ๊ณ ๋ฆฌ์ฆ˜์˜ ๊ท ์—ด ์ธ์‹ ์ •ํ™•๋„๋ฅผ ๋‚ฎ์ถ”๋Š” ์š”์ธ์ด๋‚˜, ์‚ฌ์ง„์„ ์ดฌ์˜ํ•œ ํ˜„์žฅ์˜ ํ™˜๊ฒฝ์— ๋”ฐ๋ผ ์‚ฌ์ง„์— ํฌํ•จ๋  ์ˆ˜ ์žˆ๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋”ฅ๋Ÿฌ๋‹ ์•Œ๊ณ ๋ฆฌ์ฆ˜์˜ ์ผ์ข…์ธ ํ•ฉ์„ฑ๊ณฑ ์‹ ๊ฒฝ๋ง์„ ์‚ฌ์šฉํ•˜์—ฌ ๋‹ค์–‘ํ•œ ๋…ธ์ด์ฆˆ๊ฐ€ ์กด์žฌํ•˜๋Š” ์ด๋ฏธ์ง€๋กœ๋ถ€ํ„ฐ ์•”์„ ๊ท ์—ด์„ ์ž๋™์œผ๋กœ ์ธ์‹ํ•˜๋Š” ์•Œ๊ณ ๋ฆฌ์ฆ˜์„ ๊ฐœ๋ฐœํ•˜์˜€๋‹ค. ๋”ฅ๋Ÿฌ๋‹ ๊ธฐ๋ฐ˜ ํ•ฉ์„ฑ๊ณฑ ์‹ ๊ฒฝ๋ง ์•Œ๊ณ ๋ฆฌ์ฆ˜์€ ์‚ฌ๋žŒ์ด ์ง์ ‘ ์‹œํ–‰์ฐฉ์˜ค๋ฅผ ํ†ตํ•ด ์ ์ ˆํ•œ ํ”ผ์ฒ˜๋ฅผ ๊ฒฐ์ •ํ–ˆ๋˜ ์ „ํ†ต์ ์ธ ์ด๋ฏธ์ง€ ์ฒ˜๋ฆฌ ๋ฐฉ์‹๊ณผ ๋‹ฌ๋ฆฌ ์‹ ๊ฒฝ๋ง์ด ์Šค์Šค๋กœ ์ด๋ฏธ์ง€์—์„œ ์ ํ•ฉํ•œ ํ”ผ์ฒ˜๋ฅผ ์ถ”์ถœํ•˜์—ฌ ์ด์šฉํ•˜๊ธฐ ๋•Œ๋ฌธ์— ์ธ์‹ ์„ฑ๋Šฅ์ด ํ–ฅ์ƒ๋œ๋‹ค. ๋˜ํ•œ, ๊ธฐ์กด ์—ฐ๊ตฌ๋“ค์€ ๋ชจ๋ธ ๊ฐœ๋ฐœ์— ์‚ฌ์šฉํ•œ ๊ท ์—ด ์ด๋ฏธ์ง€์™€ ๊ฐ™์€ ์ด๋ฏธ์ง€๋กœ ํ…Œ์ŠคํŠธ๋ฅผ ์ˆ˜ํ–‰ํ•˜์˜€๊ธฐ ๋•Œ๋ฌธ์— ๊ทธ๋กœ๋ถ€ํ„ฐ ๊ฐœ๋ฐœ๋œ ๋ชจ๋ธ์€ ๊ทธ ํŠน์ • ์ด๋ฏธ์ง€์— ๋Œ€ํ•ด์„œ๋งŒ ์ข‹์€ ์„ฑ๋Šฅ์„ ๋‚ผ ์ˆ˜ ์žˆ์—ˆ๋‹ค. ๊ทธ๋Ÿฌ๋‚˜, ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ํ…Œ์ŠคํŠธ ๊ณผ์ •์— ์™„์ „ํžˆ ์ƒˆ๋กœ์šด ๊ท ์—ด ์ด๋ฏธ์ง€๋ฅผ ์‚ฌ์šฉํ•จ์œผ๋กœ์จ ์ƒˆ๋กœ์šด ์ด๋ฏธ์ง€์—๋„ ์ข‹์€ ๊ฒฐ๊ณผ๋ฅผ ๋‚ด๋Š” ๊ฒƒ์„ ๋ณด์˜€๋‹ค. ์ข…ํ•ฉ์ ์œผ๋กœ, ๋ณธ ์—ฐ๊ตฌ์—์„œ ๊ฐœ๋ฐœ๋œ ์•Œ๊ณ ๋ฆฌ์ฆ˜์€ ์‚ฌ์ง„์œผ๋กœ๋ถ€ํ„ฐ ์‹ ์†ํ•˜๊ณ  ์ผ๊ด€์ ์œผ๋กœ ๊ท ์—ด ์ธ์‹์„ ํ•  ์ˆ˜ ์žˆ์œผ๋ฉฐ ๋‹ค์–‘ํ•œ ๋น„์ •ํ˜• ๊ท ์—ด ์ด๋ฏธ์ง€๋“ค์— ๋Œ€ํ•ด์„œ๋„ ๋†’์€ ๊ฒ€์ถœ ์„ฑ๋Šฅ์„ ๋ณด์ธ๋‹ค.Detection of rock joint and fracture is important because they have a huge influence on rock mass strength. Photogrammetry technique, especially, has been used for decades due to its simplicity and economic feasibility. Although joints are easy to detected since it has linearity, fractures has irregularity which leads to difficulties in detection and lack of relevant studies. Additionally, previous researches used photographs without various types of noise such as shadow, infill material and vegetation. These kinds of noise reduce the accuracy of conventional algorithms. However, it can be included in the photographs under certain circumstances. In this study, a new algorithm based on convolutional neural networks, which can detect rock fracture from rock images with many kinds of noise, is presented. Furthermore, previous models were evaluated with the same image used in model construction stage. The model performance, therefore, is guaranteed only for that specific data. On the contrary, new rock images are used when testing the model, which shows the data-independent performance of proposed model. As a result, the developed model in this study can detect rock fracture from photographs quickly and consistently, and demonstrate high performance for irregular fractures.๋ชฉ ์ฐจ 1. ์„œ๋ก  1 2. ์ธ๊ณต์‹ ๊ฒฝ๋ง ์ด๋ก  5 2.1 ์™„์ „์—ฐ๊ฒฐ ์‹ ๊ฒฝ๋ง 5 2.2 ํ•ฉ์„ฑ๊ณฑ ์‹ ๊ฒฝ๋ง 8 3. ์‹คํ—˜ ๋ฐฉ๋ฒ• 13 3.1 ๋ฐ์ดํ„ฐ ์ˆ˜์ง‘ 14 3.2 ๋ฐ์ดํ„ฐ ๊ฐ€๊ณต 16 3.2.1 ๋ฐ์ดํ„ฐ ๋ ˆ์ด๋ธ”๋ง 16 3.2.2 ๋ฐ์ดํ„ฐ ๋ถ„๋ฆฌ 18 3.2.3 ๋ฐ์ดํ„ฐ ์ฆ๊ฐ• 20 3.2.4 ๋ฐ์ดํ„ฐ ์ „์ฒ˜๋ฆฌ 23 3.3 ํ•ฉ์„ฑ๊ณฑ ์‹ ๊ฒฝ๋ง ๋ชจ๋ธ ๊ตฌ์กฐ 27 3.4 ํ•™์Šต ์ƒ์„ธ ๊ณผ์ • 30 3.5 ํ›„์ฒ˜๋ฆฌ ๊ณผ์ • 30 4. ๊ฒฐ๊ณผ ๋ฐ ๊ณ ์ฐฐ 33 4.1 ๊ทธ๋ฆผ์ž, ๊ฒ€์€ ํ‘œ๋ฉด ๋“ฑ์ด ์žˆ๋Š” ์‚ฌ์ง„ 34 4.2 ์ค„๋ฌด๋Šฌ ๊ตฌ์กฐ๊ฐ€ ์กด์žฌํ•˜๋Š” ์‚ฌ์ง„ 40 4.3 ์ถฉ์ „๋ฌผ์ด ์กด์žฌํ•˜๋Š” ์‚ฌ์ง„ 43 4.4 ๊ธํžŒ ์ž๊ตญ์ด ์กด์žฌํ•˜๋Š” ์‚ฌ์ง„ 47 4.5 ์‹์ƒ์ด ์กด์žฌํ•˜๋Š” ์‚ฌ์ง„ 49 4.6 ๋ชจ๋ธ ์„ฑ๋Šฅ ๊ณ ์ฐฐ 52 5. ๊ฒฐ๋ก  56 ์ฐธ๊ณ ๋ฌธํ—Œ 58Maste

    Lineament Extraction using Gravity Data in the Citarum Watershed

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    Lineament is one of the most important features showing subsurface elements or structural weakness such as faults. This study aims to identify subsurface lineament patterns using automatic lineament in Citarum watershed with gravity data. Satellite gravity data were used to generate a sub-surface lineament. Satellite gravity data corrected using Bouguer and terrain correction to obtain a complete Bouguer anomaly value. Butterworth filters were used to separate regional and residual anomaly from the complete Bouguer anomaly value. Residual anomaly gravity data used to analyze sub-surface lineament. Lineament generated using Line module in PCI Geomatica to obtain sub-surface lineament from gravity residual value. The orientations of lineaments and fault lines were created by using rose diagrams. The main trends observed in the lineament map could be recognized in these diagrams, showing a strongly major trend in NW-SE, and the subdominant directions were in N-S. Area with a high density of lineament located at the Southern part of the study area. High-density lineament might be correlated with fractured volcanic rock upstream of the Citarum watershed, meanwhile, low-density lineament is associated with low-density sediment. The high-density fracture might be associated with intensive tectonics and volcanism

    Integrated Object-Based Image Analysis for semi-automated geological lineament detection in Southwest England

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    This is the final version. Available on open access from Elsevier via the DOI in this record.Regional lineament detection for mapping of geological structure can provide crucial information for mineral exploration. Manual methods of lineament detection are time consuming, subjective and unreliable. The use of semi-automated methods reduces the subjectivity through applying a standardised method of searching. Object-Based Image Analysis (OBIA) has become a mainstream technique for classification of landcover, however, the use of OBIA methods for lineament detection is still relatively under-utilised. The Southwest England region is covered by high-resolution airborne geophysics and LiDAR data that provide an excellent opportunity to demonstrate the power of OBIA methods for lineament detection. Herein, two complementary but stand-alone OBIA methods for lineament detection are presented which both enable semi-automatic regional lineament mapping. Furthermore, these methods have been developed to integrate multiple datasets to create a composite lineament network. The top-down method uses threshold segmentation and sub-levels to create objects, whereas the bottom-up method segments the whole image before merging objects and refining these through a border assessment. Overall lineament lengths are longest when using the top-down method which also provides detailed metadata on the source dataset of the lineament. The bottom-up method is more objective and computationally efficient and only requires user knowledge to classify lineaments into major and minor groups. Both OBIA methods create a similar network of lineaments indicating that semi-automatic techniques are robust and consistent. The integration of multiple datasets from different types of spatial data to create a comprehensive, composite lineament network is an important development and demonstrates the suitability of OBIA methods for enhancing lineament detection.British Geological Survey (BGS)Natural Environment Research Council (NERC

    The use of contextual techniques and textural analysis of satellite imagery in geological studies of arid regions

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    This Thesis examines the problem of extracting spatial information (context and texture) of use to the geologist, from satellite imagery. Part of the Arabian Shield was chosen to be the study area. Two new contextual techniques; (a) Ripping Membrane and (b) Rolling Ball were developed and examined in this study. Both new contextual based techniques proved to be excellent tools for visual detection and analysis of lineaments, and were clearly better than the 'traditional' spatial filtration technique. This study revealed structural lineaments, mostly mapped for the first time, which are clearly related to regional tectonic history of the area. Contextual techniques were used to perform image segmentation. Two different image segmentation methods were developed and examined in this study. These methods were the automatic watershed segmentation and ripping membrane/Laserscan system method (as this method was being used for the first time). The second method produced high accuracy results for four selected test sites. A new automatic lineament extraction method using the above contextual techniques was developed. The aim of the method was to produce an automatic lineament map and the azimuth direction of these lineaments in each rock type, as defined by the segmented regions. 75-85% of the visually traced lineaments were extracted by the automatic method. The automatic method appears to give a dominant trend slightly different (10ยฐ โ€” 15ยฐ) from the visually determined trend. It was demonstrated that not all the different types of rock could be discriminated using the spectral image enhancement techniques (band ratio, principal components and decorrelation stretch). Therefore, the spatial grey level dependency matrix (SGLDM) was used to produce a texture feature image, which would enable distinctions to be made and overcome the limitations of spectral enhancement techniques. The SGLDM did not produce any useful texture features which can discriminate between every rock type in the selected test sites. It did, however, show some acceptable texture discrimination between some rock types. The remote sensing data examined in this thesis were the Landsat (multispectral scanner, Thematic Mapper), SPOT, and Shuttle Imaging Radar (SIR-B)
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