239 research outputs found

    Mining Safety and Sustainability I

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    Safety and sustainability are becoming ever bigger challenges for the mining industry with the increasing depth of mining. It is of great significance to reduce the disaster risk of mining accidents, enhance the safety of mining operations, and improve the efficiency and sustainability of development of mineral resource. This book provides a platform to present new research and recent advances in the safety and sustainability of mining. More specifically, Mining Safety and Sustainability presents recent theoretical and experimental studies with a focus on safety mining, green mining, intelligent mining and mines, sustainable development, risk management of mines, ecological restoration of mines, mining methods and technologies, and damage monitoring and prediction. It will be further helpful to provide theoretical support and technical support for guiding the normative, green, safe, and sustainable development of the mining industry

    ์นจํˆฌ์‹คํ—˜์„ ํ†ตํ•œ ์ž…๋„๋ถ„ํฌ๊ฐ€ ์ข‹์€ ํ’ํ™”ํ† ์˜ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ ํ‰๊ฐ€

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    ํ•™์œ„๋…ผ๋ฌธ(๋ฐ•์‚ฌ) -- ์„œ์šธ๋Œ€ํ•™๊ต๋Œ€ํ•™์› : ๊ณต๊ณผ๋Œ€ํ•™ ๊ฑด์„คํ™˜๊ฒฝ๊ณตํ•™๋ถ€, 2022. 8. ์ •์ถฉ๊ธฐ.Internal erosion is an important process that affects the stability of a fill dam. Suffusion and suffosion, also known as internal instability, are forms of internal erosion. Suffusion involves the selective erosion of fine particles from the matrix of coarse particles of an internally unstable soil through seepage flow, thereby removing the fine particles through the voids and leaving behind a soil skeleton formed by coarse particles. Suffosion is a similar process but results in volume changes. The erosion of fine particles increases the soil permeability, resulting in a decrease in shear strength and changes in hydraulic conditions. In turn, this scenario may cause various types of dam failures. Generally, gap-graded soil with two distinct grain sizes is vulnerable to internal instability. Such soils show clear manifestations of suffusion, such as the erosion of a significant quantity of fine particles and an increase in permeability and void ratio. Therefore, previous studies on seepage erosion problems commonly focused on gap-graded soils as the target. However, no study has shown whether the well-graded soils, used as fill dam materials in South Korea, are susceptible to suffusion. Moreover, the process and cause of internal instability in well-graded soils have not been investigated. In this dissertation, suffusion tests were performed on gap-graded and well-graded soils with different relative densities by using a newly developed suffusion test apparatus. In short-term tests, hydraulic gradient was increased stepwise, and the occurrence of internal instability were analyzed. In contrast to gap-graded soils, well-graded soils showed a continuous reduction in permeability before the initiation of internal instability. At the onset of internal instability, permeability and soil discharge suddenly increased. Additionally, when the relative density of well-graded soils increased, the hydraulic gradient required to reach an unstable state also increased. Long-term tests were carried out to analyze the progress and cause of the internal instability of well-graded soils at constant hydraulic gradients. Results revealed that well-graded soils in internally stable conditions had clogging of fine particles in the bottom, which reduces the overall permeability. Similar clogging was identified in internally unstable conditions, and subsequent unclogging resulted in a rapid increase in permeability and erosion rate with the collapse of soil structure. Consequently, the internal instability of well-graded soils developed in the form of suffosion. On this basis, the mechanism of internal instability and its progress in well-graded soils were proposed. Seepage tests with pore water pressure transducer were used to verify the above mechanism of internal instability in well-graded soils. The erosion of fine particles increased permeability and decrease the pressure, while the clogging of fine particles decreased permeability and increased pressure. Consequently, the test confirmed that the movement path of fine particles and verified the mechanism of internal instability in well-graded soils. Results indicated that the characteristics and development of the internal instability of well-graded soils differed from those of gap-graded soils. The findings can be used to deepen the understanding of the development of internal instability in well-graded soils.๋‚ด๋ถ€ ์นจ์‹์€ ์„ฑํ† ๋Œ์˜ ์•ˆ์ •์„ฑ์— ์˜ํ–ฅ์„ ๋ฏธ์น˜๋Š” ์ค‘์š”ํ•œ ์›์ธ ์ค‘ ํ•˜๋‚˜์ด๋ฉฐ, ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์œผ๋กœ ์•Œ๋ ค์ง„ suffusion๊ณผ suffosion์€ ๋‚ด๋ถ€ ์นจ์‹์˜ ํ•œ ํ˜•ํƒœ์ด๋‹ค. Suffusion์€ ๋ถ€ํ”ผ ๋ณ€ํ™”์—†์ด ์นจํˆฌ์••์— ์˜ํ•ด์„œ ์„ธ๋ฆฝ์งˆ์ด ์กฐ๋ฆฝ์งˆ ์‚ฌ์ด๋ฅผ ์ด๋™ํ•˜์—ฌ, ์„ ํƒ์ ์œผ๋กœ ์นจ์‹๋˜๋Š” ๊ฒƒ์œผ๋กœ ์ •์˜ํ•˜๊ณ , Suffosion์€ suffusion๊ณผ ๊ฐ™์€ ๋ฉ”์ปค๋‹ˆ์ฆ˜์œผ๋กœ ๋ฐœ์ƒํ•œ, ๋ถ€ํ”ผ๋ณ€ํ™”๋ฅผ ๋™๋ฐ˜ํ•œ๋‹ค๊ณ  ์ •์˜ํ•˜๊ณ  ์žˆ๋‹ค. ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์ด ๋ฐœ์ƒํ•˜๋ฉด ์„ธ๋ฆฝ์งˆ์ด ์œ ์ถœ๋˜์–ด ๊ฐ„๊ทน๋น„๊ฐ€ ์ฆ๊ฐ€ํ•˜๊ณ , ์ด๋กœ ์ธํ•ด ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ์ฆ๊ฐ€ํ•˜๋ฉฐ, ํ™์˜ ์ „๋‹จ๊ฐ•๋„๊ฐ€ ๊ฐ์†Œํ•  ์ˆ˜ ์žˆ๋‹ค. ๋˜ํ•œ, ํ›„๋ฐฉ์นจ์‹, ์นจํ•˜, ์‚ฌ๋ฉด๋ถ•๊ดด์˜ ์›์ธ์ด ๋  ์ˆ˜๋„ ์žˆ๋‹ค๊ณ  ์•Œ๋ ค์ ธ ์žˆ๋‹ค. Gap-graded soil์€ ์–‘๊ทนํ™”๋œ ์„ธ๋ฆฝ์งˆ๊ณผ ์กฐ๋ฆฝ์งˆ๋กœ ์ด๋ฃจ์–ด์ง„ ํ™์œผ๋กœ, ์ผ๋ฐ˜์ ์œผ๋กœ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์— ์ทจ์•ฝํ•˜๋ฉฐ, ์„ธ๋ฆฝ์งˆ์˜ ์œ ์ถœ๊ณผ ํˆฌ์ˆ˜๊ณ„์ˆ˜, ๊ฐ„๊ทน๋น„์˜ ์ฆ๊ฐ€์™€ ๊ฐ™์€ ๋ช…ํ™•ํ•œ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์„ ๋ณด์ธ๋‹ค. ๋”ฐ๋ผ์„œ, ์ฃผ๋กœ gap-graded soil์„ ์ด์šฉํ•˜์—ฌ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์— ๋Œ€ํ•œ ์—ฐ๊ตฌ๋ฅผ ์ˆ˜ํ–‰ํ•˜์˜€๋‹ค. ๊ทธ๋Ÿฌ๋‚˜ ๊ตญ๋‚ด ํ™๋Œ ์ œ์ฒด์žฌ๋ฃŒ์™€ ๊ฐ™์ด ์—ฌ๋Ÿฌ๊ฐ€์ง€ ์ž…๋„๋ถ„ํฌ๊ฐ€ ํ˜ผํ•ฉ๋˜์–ด์žˆ๋Š” well-graded soil์— ๋Œ€ํ•œ ์—ฐ๊ตฌ๋Š” ์ œํ•œ์ ์œผ๋กœ ์ˆ˜ํ–‰๋˜์—ˆ์œผ๋ฉฐ, ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ ๋ฐœ์ƒ ์—ฌ๋ถ€ ๋ฐ ํ˜•ํƒœ, ์›์ธ์— ๋Œ€ํ•œ ๋ถ„์„์ด ๋ถ€์กฑํ•œ ์‹ค์ •์ด๋‹ค. ๋”ฐ๋ผ์„œ, ๋ณธ ๋…ผ๋ฌธ์—์„œ๋Š” ์ƒˆ๋กœ ๊ฐœ๋ฐœํ•œ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ ์‹คํ—˜ ์žฅ์น˜๋ฅผ ์ด์šฉํ•˜์—ฌ, gap-graded soil๊ณผ well-graded soil์— ๋Œ€ํ•˜์—ฌ ๋‹ค์–‘ํ•œ ์ƒ๋Œ€๋ฐ€๋„์™€ ๋™์ˆ˜๊ฒฝ์‚ฌ์—์„œ ์นจํˆฌ์‹คํ—˜์„ ์‹ค์‹œํ•˜์˜€๋‹ค. ๋‹จ๊ธฐ์‹คํ—˜์—์„œ๋Š” ๋™์ˆ˜๊ฒฝ์‚ฌ๋ฅผ ๋‹จ๊ณ„์ ์œผ๋กœ ์ฆ๊ฐ€์‹œํ‚ค๋ฉฐ ์‹คํ—˜์„ ์ˆ˜ํ–‰ํ•˜๊ณ , ํ™์˜ ์œ ์ถœ๋Ÿ‰๊ณผ ํˆฌ์ˆ˜๊ณ„์ˆ˜๋ฅผ ๊ธฐ์ค€์œผ๋กœ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์˜ ๋ฐœ์ƒ์„ ๋ถ„์„ํ•˜์˜€๋‹ค. ์‹คํ—˜ ๊ฒฐ๊ณผ, well-graded soil์€ gap-graded soil๊ณผ๋Š” ๋‹ฌ๋ฆฌ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์ด ์‹œ์ž‘๋˜๊ธฐ ์ „์— ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ๊ฐ์†Œํ•˜๋‹ค ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์ด ์‹œ์ž‘๋  ๋•Œ ๊ธ‰๊ฒฉํ•˜๊ฒŒ ํˆฌ์ˆ˜๊ณ„์ˆ˜์™€ ํ™์˜ ์œ ์ถœ์†๋„๊ฐ€ ์ฆ๊ฐ€ํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์˜€๋‹ค. ๋˜ํ•œ, ์ƒ๋Œ€๋ฐ€๋„๊ฐ€ ์ฆ๊ฐ€ํ• ์ˆ˜๋ก ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์ด ๋ฐœ์ƒํ•˜๋Š” ๋™์ˆ˜๊ฒฝ์‚ฌ๊ฐ€ ์ฆ๊ฐ€ํ•˜์˜€๋‹ค. ์žฅ๊ธฐ์‹คํ—˜์€ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์˜ ์ง„ํ–‰๊ณผ์ •๊ณผ ์›์ธ์„ ๋ถ„์„ํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ๋™์ˆ˜๊ฒฝ์‚ฌ๋ฅผ ์ผ์ •ํ•˜๊ฒŒ ์œ ์ง€ํ•˜๋ฉด์„œ ์ˆ˜ํ–‰ํ•˜์˜€๋‹ค. ๋‚ด๋ถ€์ ์œผ๋กœ ์•ˆ์ •ํ•œ์กฐ๊ฑด์—์„œ well-graded soil์€ ํ•˜๋ถ€์— ์„ธ๋ฆฝ๋ถ„๋“ค์ด ๋ง‰ํžˆ๋ฉด์„œ ์ „์ฒด ํˆฌ์ˆ˜๊ณ„์ˆ˜๋ฅผ ๊ฐ์†Œ์‹œ์ผฐ๊ณ , ๋‚ด๋ถ€์ ์œผ๋กœ ๋ถˆ์•ˆ์ •ํ•œ ์กฐ๊ฑด์—์„œ๋Š” ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ๊ฐ์†Œํ•˜๋‹ค๊ฐ€ ํ™์˜ ์œ ์ถœ๋Ÿ‰๊ณผ ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ๊ฐ‘์ž๊ธฐ ์ฆ๊ฐ€ํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์˜€๋‹ค. ๋˜ํ•œ, ์กฐ๋ฆฝ์งˆ๊ณผ ์„ธ๋ฆฝ์งˆ์ด ๊ฐ™์ด ์œ ์ถœ๋˜๋ฉฐ ์นจํ•˜๊ฐ€ ๋ฐœ์ƒํ•˜๋Š” suffosion์˜ ํ˜•ํƒœ๋กœ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์ด ์ง„ํ–‰๋˜์—ˆ๋‹ค. ์‹คํ—˜๊ฒฐ๊ณผ๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ well-graded soil์˜ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์˜ ์ง„ํ–‰ ๋ฉ”์ปค๋‹ˆ์ฆ˜์„ ์ œ์•ˆํ•˜์˜€๋‹ค. ์ œ์•ˆ๋œ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ ๋ฉ”์ปค๋‹ˆ์ฆ˜์„ ๊ฒ€์ฆํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ๊ฐ„๊ทน์ˆ˜์••๊ณ„๋ฅผ ์„ค์น˜ํ•œ ์นจํˆฌ์‹คํ—˜์„ ์‹ค์‹œํ•˜์˜€๋‹ค. ์„ธ๋ฆฝ์งˆ์ด ์œ ์ถœ๋˜๋Š” ๋ถ€๋ถ„์€ ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ์ฆ๊ฐ€ํ•˜๊ณ , ๊ฐ„๊ทน์ˆ˜์••์ด ๊ฐ์†Œํ•œ ๋ฐ˜๋ฉด, ์„ธ๋ฆฝ์งˆ์ด ์Œ“์ด๋Š” ๋ถ€๋ถ„์€ ํˆฌ์ˆ˜๊ณ„์ˆ˜๊ฐ€ ๊ฐ์†Œํ•˜๊ณ , ๊ฐ„๊ทน์ˆ˜์••์ด ์ฆ๊ฐ€ํ•˜์˜€๋‹ค. ๋”ฐ๋ผ์„œ, ๊ฐ„๊ทน์ˆ˜์••์„ ์ธก์ •ํ•˜์—ฌ ์„ธ๋ฆฝ์งˆ์˜ ์ด๋™์„ ์กฐ์‚ฌํ•˜๊ณ  ๋ฉ”์ปค๋‹ˆ์ฆ˜์„ ๊ฒ€์ฆํ•˜์˜€๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” well-graded soil์˜ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์˜ ํŠน์„ฑ ๋ฐ ์ง„ํ–‰๊ณผ์ •์ด gap-graded soil๊ณผ ๋‹ค๋ฆ„์„ ํ™•์ธํ•˜์˜€๊ณ , ๊ทธ ์›์ธ์— ๋Œ€ํ•˜์—ฌ ๋ถ„์„ํ•˜์˜€๋‹ค. ์ด ์—ฐ๊ตฌ ๊ฒฐ๊ณผ๋Š” well-graded soil์—์„œ ๋‚ด๋ถ€๋ถˆ์•ˆ์ •์„ฑ์˜ ์ง„ํ–‰๊ณผ์ •์„ ์ดํ•ดํ•˜๊ณ , ์•ˆ์ •์„ฑ์„ ํ‰๊ฐ€ํ•˜๋Š” ์ฐธ๊ณ ์ž๋ฃŒ๋กœ ์‚ฌ์šฉ๋  ์ˆ˜ ์žˆ์„ ๊ฒƒ์ด๋‹ค.Chapter 1. Introduction 1 1.1 Research Background 1 1.2 Objective and Scope of Research 7 1.3 Organization and Structure 9 Chapter 2. Literature review 11 2.1 Introduction 11 2.2 Conditions governing the internal instability 13 2.2.1 Geometric condition 13 2.2.2 Hydraulic condition 16 2.3 Previous studies on well-graded soil 22 Chapter 3. Research methods 26 3.1 Introduction 26 3.2 Testing materials 27 3.2.1 Particle size distributions and properties of specimens 27 3.2.2 Assessment of the internal instability 29 3.3 Experimental apparatuses 34 3.3.1 Apparatus for the short-term and long-term tests 34 3.3.2 Apparatus with pore pressure transducer 38 3.4 Experimental procedure and program 42 3.4.1 Short-term tests 42 3.4.2 Long-term tests 45 3.4.3 Tests with pore pressure transducer 46 Chapter 4. Short-term test results and analyses 48 4.1 Introduction 48 4.2 Short-term test results and analyses 49 4.2.1 Gap soil with a relative density of 78% 49 4.2.2 WG soil with a relative density of 50% 51 4.2.3 WG soil with a relative density of 65% 53 4.2.4 WG soil with a relative density of 80% 56 4.3 Assessment of internal instability 59 4.4 Summary 63 Chapter 5. Long-term test results and analyses 65 5.1 Introduction 65 5.2 Amount of eroded soil and erosion rate 68 5.3 Hydraulic conductivity 73 5.3.1 Gap soil 75 5.3.2 Internally stable WG soil 79 5.3.3 Internally unstable WG soil 84 5.4 Settlement 92 5.5 Mechanism of internal instability 98 5.6 Summary 103 Chapter 6. Test results with pore pressure transducer 106 6.1 Introduction 106 6.2 Hydraulic conductivity and pore water pressure 108 6.2.1 Internally unstable result 109 6.2.2 Internally stable result 114 6.3 Verification of mechanism of internal instability in WG soil 118 6.4 Summary 121 Chapter 7. Conclusions and Recommendations 122 7.1 Conclusions 122 7.2 Recommendations for further researches 130 List of References 131๋ฐ•

    Environmental Hydraulics Research

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    This book aims to provide research and engineering applications related to water and hydraulic problems. It is comprised of scientific papers in all topics of hydraulics, in particular, on sustainable water management, environmental hydraulics, ecohydraulics, waterโ€“energy nexus, and systems protection and efficiency. Safety and innovation issues, interdisciplinary problems, and linkage of theory to experimental and field applications can also be found within. Solutions of water problems in the form of prediction models, flow simulations, engineering systems, monitoring, management strategies covering scientific investigations and/or experimental or field studies of flow behaviour, hydrodynamics, and climate changes effects and adaptation, new design solutions, innovative approaches in the field of environment, hydraulics, techniques, methods, and analyses to address the new challenges in environmental hydraulics are alo presented and explored. This topic is studied both from a technical and environmental point of view, with the objective of protecting and enhancing the quality of the environment. In a cross-disciplinary field of study, this book comprises open channel/river flows and pressurised systems, combining, among others, new technological, social, and environmental hydraulic challenges, working in water-related fields with available information, new concepts and tools, new design solutions, eco-friendly technologies, and the advanced materials necessary to address the increasing challenges of ensuring a sustainable water environment by promoting the adaptation, flexibility, integration, and sustainability of recognised environmental solutions

    Corrosion and Degradation of Materials

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    Studies on the corrosion and degradation of materials play a decisive role in the novel design and development of corrosion-resistant materials, the selection of materials used in harsh environments in designed lifespans, the invention of corrosion control methods and procedures (e.g., coatings, inhibitors), and the safety assessment and prediction of materials (i.e., modelling). These studies cover a wide range of research fields, including the calculation of thermodynamics, the characterization of microstructures, the investigation of mechanical and corrosion properties, the creation of corrosion coatings or inhibitors, and the establishment of corrosion modelling. This Special Issue is devoted to these types of studies, which facilitate the understanding of the corrosion fundamentals of materials in service, the development of corrosion coatings or methods, improving their durability, and eventually decreasing corrosion loss

    Advanced Underground Space Technology

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    The recent development of underground space technology makes underground space a potential and feasible solution to climate change, energy shortages, the growing population, and the demands on urban space. Advances in material science, information technology, and computer science incorporating traditional geotechnical engineering have been extensively applied to sustainable and resilient underground space applications. The aim of this Special Issue, entitled โ€œAdvanced Underground Space Technologyโ€, is to gather original fundamental and applied research related to the design, construction, and maintenance of underground space

    Experimental, Numerical and Field Approaches to Scour Research

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    This book presents fourteen state-of-the-art research papers prepared by research scientists and engineers around the world. They explore the subject of scour related to bridge piers, monopiles, propellers, turbines, weirs, dams, grade-control structures, and pipelines. Their works are based on three different research methodologies, namely experimental, numerical, and field approaches

    River Ecological Restoration and Groundwater Artificial Recharge

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    Three of the eleven papers focused on groundwater recharge and its impacts on the groundwater regime, in which recharge was caused by riverbed leakage from river ecological restoration (artificial water replenishment). The issues of the hydrogeological parameters involved (such as the influence radius) were also reconsidered. Six papers focused on the impact of river ecological replenishment and other human activities on river and watershed ecology, and on groundwater quality and use function. The issues of ecological security at the watershed scale and deterioration of groundwater quality were of particular concern. Two papers focused on water resources carrying capacity and water resources reallocation at the regional scale, in the context of the fact that ecological water demand has been a significant topic of concern. The use of unconventional water resources such as brackish water has been emphasized in the research in this issue

    SYMPOSIUM ON ENGINEERING WITH NUCLEAR EXPLOSIVES, LAS VEGAS, NEVADA, JANUARY 14--16, 1970. PROCEEDINGS.

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