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  • 1
    Keywords: Mine water. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (194 pages)
    Edition: 1st ed.
    ISBN: 9783030401160
    Series Statement: Springer Theses Series
    DDC: 622.5
    Language: English
    Note: Intro -- Supervisor's Foreword -- Parts of this thesis have been published in the following journal articles: -- This research was supported by the following projects: -- Contents -- Executive Summary -- 1 Introduction -- 1.1 Research Background and Significance -- 1.2 Current Research Status -- 1.2.1 Research on Water-Bearing and Water-resisting Properties of the TOL in NCCs -- 1.2.2 Pertinent Research on Grouting Reconstruction of the TOL -- 1.3 Major Limitations of Current Research -- 1.4 Research Content and Technical Approach -- 1.4.1 Research Content -- 1.4.2 Research Method and Technical Approach -- References -- 2 Paleosedimentary Environments and Karst Characteristics of Ordovician Limestone in North China Coalfields -- 2.1 Paleotectonic Movement in NCCs -- 2.2 Evolution of the Paleosedimentary Environments in NCCs -- 2.3 Characteristics of Karst Development of Ordovician Limestone in NCCs -- References -- 3 Water-Bearing and Water-resisting Properties of Top of Ordovician Limestone in North China Coalfields -- 3.1 Research on Planar Division of Water Yield Property of TOL in NCCs -- 3.1.1 Analysis on the Influencing Factors of Water Abundance of the TOL -- 3.1.2 Comprehensive Evaluation Method of Water Abundance of the TOL -- 3.1.3 Case Study of Water Abundance of the TOL -- 3.2 Research on Vertical Zonation of Water-Bearing and Water-resisting Properties of the TOL in NCCs -- 3.2.1 Three Vertical Zones in the TOL -- 3.2.2 Case Study of Vertical Zoning of Water-Bearing and Water-resisting Properties of the TOL -- References -- 4 Utilizability of Weathered and Filled Zone of Top of Ordovician Limestone in North China Coalfields -- 4.1 Formation, Evolution, and Spatial Distribution Characteristics of the Weathered and Filled Zone of the TOL -- 4.2 Experimental Study on the Utilizability of the Weathered and Filled Zone of TOL as Aquifuge. , 4.2.1 Rock Strength Test -- 4.2.2 Rock Permeability Test -- 4.2.3 Water-resisting Capacity and Rock Strength Test of TOL -- 4.3 Utilizability of the Weathered and Filled Zone of the TOL as Aquifuge -- References -- 5 Criterion for Utilization and Grouting Reconstruction of Top of Ordovician Limestone -- 5.1 Criterion for Utilization and Grouting Reconstruction of the TOL -- 5.2 Thickness of Grouting Reconstruction of the TOL -- 5.3 Prediction Methods of Damage Depth in Coal Seam Floor -- References -- 6 Technical System of Grouting Reconstruction of Top of Ordovician Limestone -- 6.1 Experimental Study on Grouting Material Formula Using Pulverized Coal Ash -- 6.2 Dispersion Properties of Grout in Karst Fractures of the TOL -- 6.3 Surface Automatic Grouting System Using Fly Ash-Based Grouting Materials -- References -- 7 Case Study of Utilization and Grouting Reconstruction of Top of Ordovician Limestone -- 7.1 Background of Tested Working Face 3105 in Sangshuping Coal Mine, Hancheng Mining Area -- 7.2 Karst Characteristics and Water Yield Properties of TOL in Sangshuping Coal Mine -- 7.3 Utilization of the TOL in Working Face 3105 -- Reference -- 8 Conclusions and Innovation Points -- 8.1 Conclusions -- 8.2 Innovation Points.
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Mine water-Prevention. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (521 pages)
    Edition: 1st ed.
    ISBN: 9783030670597
    Series Statement: Professional Practice in Earth Sciences Series
    DDC: 622.5
    Language: English
    Note: Intro -- Preface -- Contents -- 1 Water Hazards in Coal Mines and Their Classifications -- 1.1 Introduction -- 1.2 Water Inrush Conceptual Site Models for Coal Mines of China -- 1.2.1 Development of Water Inrush Conceptual Site Models -- 1.2.2 Benefits of Water Inrush Conceptual Site Models -- 1.3 Classification of Water Inrush for Coal Mines of China -- 1.3.1 Principles for Classification of Mine Water Inrush -- 1.3.2 Types of Mine Water Inrush -- 1.3.3 Characteristics of Mine Water Inrushes -- 1.4 Hydrogeological Classification for Mine Water Hazard Control -- 1.4.1 Criteria of Hydrogeological Classification -- 1.4.2 Hydrogeological Classification of Coal Mines in China -- 1.4.3 Hydrogeological Characteristics of Mines -- 1.5 Advances in Prevention and Control Technologies of Mine Water Hazards -- 1.5.1 Updated Mining Principles -- 1.5.2 Evolution of Water Inrush Coefficient -- 1.5.3 Supplemental Investigation and Water Inrush Prediction -- 1.5.4 Advanced Detection and Dewatering Technologies -- 1.5.5 Early Warning Technique -- 1.5.6 Innovated Grouting Technique -- References -- 2 Mine Water Inrush Mechanisms and Prediction Methods -- 2.1 Overview of Water Inrush Studies -- 2.2 Water Inrush Mechanisms in North China's Coalfields -- 2.2.1 Hydrogeological Background -- 2.2.2 Relationship Between Aquiclude Thickness and Groundwater Pressure -- 2.2.3 Impact of Mining Activities on Geologic Barrier -- 2.2.4 Laboratory Experiments on Failure of Geologic Barrier -- 2.2.5 Initial Conductive Zone in Geologic Barrier -- 2.2.6 In-Situ Hydrofracturing Tests -- 2.3 Water Inrush Mechanism Through Karst Collapse Columns -- 2.3.1 Karst Collapse Columns and Their Relationship with Mining -- 2.3.2 Hydrogeological Characteristics of Karst Collapse Columns -- 2.3.3 Water Inrushes Through Karst Collapse Columns -- 2.4 Prediction Methods. , 2.4.1 Water Inrush Coefficient Method -- 2.4.2 Vulnerability Index Method -- 2.4.3 Three-Map and Two-Prediction Method -- 2.4.4 Five-Map and Two-Coefficient Method -- References -- 3 Modeling of Groundwater Flow in Karst Aquifers for Mine Water Control -- 3.1 Inputs to Karst Hydrogeological Systems -- 3.1.1 Discharge-Storage Method -- 3.1.2 Recession-Curve-Displacement Method -- 3.1.3 Meteorological Model -- 3.2 Groundwater Flow in Karst Hydrogeological Systems -- 3.2.1 Groundwater Flow Patterns in Karst Aquifers -- 3.2.2 Influenced Flow Patterns -- 3.2.3 Confluent Flow in Karst Aquifers -- 3.2.4 Siphon Karst Flow -- 3.3 Water Budget Analyses -- 3.3.1 Discharge Hydrograph -- 3.3.2 Discharge Recession Analysis -- 3.3.3 Discharge Chemograph -- 3.3.4 Groundwater Level Hydrograph -- 3.4 Statistical and Stochastic Methods -- 3.4.1 Regression Analysis -- 3.4.2 Kernel Analysis -- 3.4.3 Threshold Autoregressive Analysis -- 3.5 Mixing-Cell Models -- 3.5.1 Discrete-State-Compartment Model -- 3.5.2 Water Tank Models -- 3.6 Physics-Based Models -- 3.6.1 Equivalent-Porous-Medium Models -- 3.6.2 Discrete-Fracture Models -- 3.6.3 Double-Continuum Models -- 3.6.4 Determination of Hydraulic Parameters at Respective Scales -- 3.7 Quantitative Analysis of Tracer Tests -- 3.7.1 Tracer-Breakthrough Curves -- 3.7.2 Estimation of Hydraulic Parameters of Karst Conduits -- 3.7.3 Evaluation of Dynamic Dispersion in Karst Aquifers -- 3.8 Application of Dual-Porosity Model to Groundwater Simulation in the Ordovician Limestone in Jiaozuo Coalfield, China -- 3.8.1 Introduction to Jiaozuo Coalfield -- 3.8.2 Karst Conduit Distribution -- 3.8.3 Calibration of the Dual-Porosity Model -- References -- 4 Prevention and Control of Mine Water Hazards from Underlying Aquifers. , 4.1 Water Prevention and Control Technology in Mining Lower Coal Seams Under Potentiometric Pressure in Xingtai Dongpang Mine -- 4.1.1 Mine Background -- 4.1.2 Application of Water Prevention and Control Technology to Mining Under Potentiometric Pressure -- 4.2 Grouting Technology in Thin-Bedded Limestone to Prevent Water Inrushes from Underlying Aquifers in Zhuzhuang Coal Mine of Huaibei Coalfield -- 4.2.1 Background -- 4.2.2 Large-Scale Advance Grouting Technology in Transforming Limestone into Water Barrier -- 4.3 Utilization of the Top of the Ordovician Limestone in the Sangshuping Mine of Hancheng and the Underground Grouting Transformation Technology -- 4.3.1 Mine Background -- 4.3.2 Utilization of Top of the Ordovician Limestone and Underground Grouting Transformation Technology -- 4.4 Emergency Mitigation Technology of Water Inrush Induced Mine Flooding in Luotuoshan Coal Mine in Wuhai Energy Co., Ltd. -- 4.4.1 Overview -- 4.4.2 Emergency Water-Plugging Technology in #16 Coal Seam Air Return Lane -- 4.4.3 Comprehensive Investigation Technology of Water Inrush Point -- 4.5 Characterization and Remediation of Karst Collapse Columns in Renlou Coal Mine, China -- 4.5.1 Mine Background -- 4.5.2 Water Source Discrimination by Temperature and Hardness Measurements -- 4.5.3 Geophysical Investigations -- 4.5.4 Borehole Exploration and Grouting -- 4.5.5 Summary -- 4.6 Design and Construction of Watertight Plugs in Permeable Karst Collapse Columns in Restoration of Flooded Dongpang Mine, China -- 4.6.1 Mine Background -- 4.6.2 Construction of the Watertight Plug -- 4.6.3 Completion Criteria of Grouting -- 4.6.4 Grout Intake Distribution -- 4.6.5 Evaluation of Plug Effectiveness -- 4.6.6 Summary -- 4.7 Utilization of Paleokarst Crust of Ordovician Limestone in Water Inrush Control in Sihe Coal Mine, Shanxi Province. , 4.7.1 Introduction to Paleokarst Crust -- 4.7.2 Characteristics of Paleokarst Crust at Sihe Mine -- 4.7.3 Hydrogeogical Properties of Fengfeng Formation -- 4.7.4 Thickness of Aquifuge in Fengfeng Formation -- 4.7.5 Summary -- 5 Prevention and Control of Mine Water Hazards from Overlying Aquifers -- 5.1 Water Control Technology for Overlying Thick-Bedded Sandstone Fissure Aquifer in Hujiahe Mine, Binchang, Shaanxi -- 5.1.1 Mine Background -- 5.1.2 Exploration and Prevention Techniques for Water Hazards Posed by the Overlying Thick Sandstone Fissure Aquifer -- 5.1.3 Exploration and Prevention Technologies of Water Hazards from Overlying Thick Sandstone Fissure Aquifers -- 5.2 Prevention and Control Technology for Water Disaster from Bed-Separation Voids of Overlying Formations in Hongliu Coal Mine, Ningdong Coalfield -- 5.2.1 Mine Background -- 5.2.2 Investigation and Mitigation of Bed-Separation Water Inrush -- 5.2.3 Summary of Bed-Separation Groundwater Control -- 5.3 Prevention Technology on Water and Sand Inrush in Halagou Coal Mine, Shendong Coalfield -- 5.3.1 Mine Background -- 5.3.2 Mechanism and Conditions of Water and Sand Inrush -- 5.3.3 Prevention and Control Technology of Water and Sand Inrush -- 6 Investigation and Prevention of Water Hazards from Old Mine Pools in Ordos -- 6.1 Background of Mining Area -- 6.2 Technical Approaches -- 6.3 Geophysical Methods -- 6.3.1 High-Density Electrical Resistivity Imaging -- 6.3.2 Transient Electromagnetic Method -- 6.3.3 Shallow Seismic Method -- 6.3.4 EH4 Magnetotelluric Method -- 6.3.5 Control-Source Audio Magnetotelluric Method -- 6.3.6 Magnetic Method -- 6.4 Achievements by Electrical and Magnetic Imaging -- 6.4.1 Geophysical Survey Layout -- 6.4.2 Results of Electrical Resistivity Imaging Survey -- 6.4.3 Results of Transient Electromagnetic Survey -- 6.4.4 Results of Magnetic Survey. , 6.5 Experience with Reconnaissance of Coal Mine Goafs in Ordos -- 6.5.1 Unified Organization and Implementation Led by Government -- 6.5.2 Reliance on Technical Institutions to Improve Reconnaissance Effectiveness -- 6.5.3 Active Cooperation of Coal Mine Enterprises -- 6.5.4 Concerted Efforts from All Parties -- 7 Technologies in Sealing Massive Karst Conduits in Restoration of a Flooded Open Pit Quarry in West Virginia, United States -- 7.1 Mine Background -- 7.2 Water Source and Pathway Investigations -- 7.3 Concept of Remediation Design -- 7.3.1 Selection of Cut off Methodology -- 7.3.2 Selection of Grouting Concepts -- 7.3.3 Evolution of the Remediation Program -- 7.4 Execution of Mitigation -- 7.4.1 Drilling -- 7.4.2 Grouting -- 7.5 Drilling and Grouting Quantities -- 7.6 Impact of Grouting Program on Quarry Inflow Characteristics -- 7.7 Summary -- References -- 8 Environmental Impact Assessment in Hongliulin Coal Mine -- 8.1 Mine Background Setting -- 8.1.1 Geographical Location -- 8.1.2 Mining History -- 8.1.3 Resources and Reserves -- 8.2 Geoenvironmental Background -- 8.2.1 Physical Geography -- 8.2.2 Topography -- 8.2.3 Stratum Lithology and Geological Structure -- 8.2.4 Aquifer and Aquiclude -- 8.2.5 Groundwater Flow, Recharge, and Discharge -- 8.2.6 Analysis of Groundwater Recharge Conditions in the Mine -- 8.2.7 Geotechnical Conditions -- 8.2.8 Characteristics of Coal Seam -- 8.2.9 Other Human Engineering Activities in the Mine and its Vicinity -- 8.3 Geoenvironmental Impact Assessment -- 8.3.1 Evaluation Scope and Level -- 8.3.2 Assessment of Background Conditions -- 8.3.3 Soil Erosion Intensity -- 8.3.4 Vegetation and Coverage -- 8.3.5 Summary -- 8.4 Predictive Geoenvironmental Assessment -- 8.4.1 Predictive Assessment of Geological Disasters -- 8.4.2 Predictive Assessment of Aquifers. , 8.4.3 Evaluation of Impact on Topography and Landscape.
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  • 3
    Electronic Resource
    Electronic Resource
    Stamford, Conn. [u.a.] : Wiley-Blackwell
    Polymer Engineering and Science 31 (1991), S. 1301-1309 
    ISSN: 0032-3888
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: This paper reports both experimental and numerical investigations on delamination mechanisms in [05, 905, 05] carbon fiber(CF)/poly(etheretherketone) (PEEK) laminate subjected to low-velocity impact. It was found that the CF/PEEK composite exhibits the same damage mechanisms as epoxy-based composites, but superior delamination resistance. For the crossply laminate, the impact delamination results from a Mode II interlaminar fracture process, and a close association exists between the interlaminar shear stress field and the delamination growth. The prediction of impact-induced delamination sizes is discussed.
    Additional Material: 15 Ill.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2015-05-07
    Description: Two copper coordination polymers (CPs) [Cu(1,2-BIYB) 2 (AQ-2,6-DA)] n · nH 2 O ( 1 ) and [Cu(1,4-BIYB) 2 (AQ-2,7-DA)] n · 3 n H 2 O ( 2 ) were obtained by reactions of pentahydrate copper sulfate with corresponding sulfonate and imidazole ligand under hydrothermal conditions, respectively [Na 2 AQ-2,7-DA = anthraquinone-2,7-disulfonic acid disodium salt, Na 2 AQ-2,6-DA = anthraquinone-2,6-disulfonic acid disodium salt, 1,4-BIYB = 1,4-bis(imidazol-1-ylmethyl)benzene, 1,2-BIYB = 1,2-bis(imidazol-1-ylmethyl)benzene]. CPs 1 and 2 show different structures: CP 1 has a 2D architecture, which is further extended into a 3D supramolecular structure through hydrogen bonding interactions, whereas CP 2 has a 1D architecture, which generates a 3D supramolecular structure via hydrogen bonding and strong π ··· π interaction. Notably, CPs 1 and 2 feature rare examples of CPs based visible-light-driven photocatalysts and reveal good stability toward photocatalysis.
    Print ISSN: 0044-2313
    Electronic ISSN: 1521-3749
    Topics: Chemistry and Pharmacology
    Published by Wiley-Blackwell
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  • 5
    Publication Date: 2014-10-26
    Print ISSN: 0270-9139
    Electronic ISSN: 1527-3350
    Topics: Medicine
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  • 6
    Publication Date: 2013-04-30
    Description: A novel catalyst for bisphenol-A synthesis was prepared by bis (2-mercapto-ethyl) amine adsorbed on macroporous sulfonic resin through neutralization reaction. The physicochemical properties of two resin catalysts before and after bis (2-mercapto-ethyl) amine absorption were compared by scanning electron microscope and nitrogen adsorption. The kinetic of the new catalyst preparation process was studied and found this is a chemical adsorption and endothermic process. The adsorption rate is mainly controlled by the intra-particle diffusion, affected by boundary layer diffusion and chemical reaction as well. The thermodynamic activation parameters were calculated. Compared with unmodified catalyst, the modified resin catalyst showed higher selectivity and acetone conversion in the continuous bisphenol-A synthesis process. © 2013 American Institute of Chemical Engineers AIChE J, 2013
    Print ISSN: 0001-1541
    Electronic ISSN: 1547-5905
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 7
    Publication Date: 2014-02-16
    Description: [1]  Stress relaxation experiments are reported that culminate in energetic failure in rocks analogous to the loading cycle and subsequent localization or reactivation on brittle faults embedded in an elastic medium. Universally, rapid primary deformation arrests and transitions into a long secondary deformation phase that ultimately accelerates to catastrophic rupture. Primary deformation ( u ) conforms to Andrade's law as d u /d t ~  ( t c - t 0 ) θ with a standard exponent of 2/3 . In the long, and readily observable, secondary phase the samples both deform and analogously shed load near-linearly in time. This stress relaxation rate exhibits a robust power-law dependency with time-to-rupture and exhibits the same 2/3 power-law exponent observed in the primary phase. Similarly, the brittle strain energy released in the tertiary collapse scales with a normalized secondary stress relaxation rate. Together, these observations suggest a way to predict both the timing of rupture and its energetics from the observed stress (or strain) rate during the secondary relaxation stage.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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  • 8
    Publication Date: 2014-03-19
    Description: BACKGROUND Although SDF-1/CXCR4 pathway is a potential mechanism of tumor proliferation and progression, the mechanism of controlling CXCR4 expression is not fully understood. This study was to confirm that miR-494-3p might be a potentially post-transcriptional regulator of CXCR4 and over-expression of miR-494 might suppress prostate cancer progression and metastasis. MATERIALS AND METHODS We firstly postulated the post-transcriptional regulation of CXCR4 by miR-494-3p through bioinformatics analysis, and then it was demonstrated that miR-494-3p could regulate the CXCR4 mRNA post-transcriptionally by binding to the predicted site by dual reporter gene assays. The biological effect of miR-494-3p on prostate cancer cells proliferation, apoptosis, migration, and invasion was measured by MTT, TUNEL, flow cytometry, migration, and invasion assays. RESULTS It was shown that the mRNA and protein expression levels of CXCR4 were significantly up-regulated in PC-3 and DU145, whereas barely detected in LNCaP and RWPE-1. However, the CXCR4 protein levels were inversely related to the mature miR-494-3p expression levels in RWPE-1 and prostate cancer cells. The constitutive over-expression of miR-494-3p could down-regulate the protein level of CXCR4 in PC-3 and DU145. MiR-494-3p also could bind to the seed sequences in the 3′-UTR of the CXCR4 gene. Artificial over-expression of miR-494-3p could inhibit the growth, promote the apoptosis, and inhibit the migration and invasion of PC-3 and DU145 cells in vivo. CONCLUSIONS Our results suggested that miR-494-3p might play crucial role in prostate cancer by post-transcriptional regulation to CXCR4 mRNA. MiR-494-3p/CXCR4 pathway may be a potential therapeutic target to prevent prostate cancer progression and metastasis. Prostate © 2014 Wiley Periodicals, Inc.
    Print ISSN: 0270-4137
    Electronic ISSN: 1097-0045
    Topics: Medicine
    Published by Wiley-Blackwell
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  • 9
    Publication Date: 2017-12-08
    Description: Understanding the magnitude of intra-Asian crustal shortening and the collision age of Lhasa–Qiangtang terranes requires quantitative constraints on the crustal motion. The key to this is defining the palaeogeography of the Tibetan Plateau, which constitutes a poorly known factor over the entire convergence history. New detrital zircon U–Pb geochronological and palaeomagnetic data from the terrestrial Abushan Formation in the Qiangtang terrane demonstrate that central Tibet was located at 27.5 ± 3.0°N during the time interval of ~111–83 Ma. Our results suggest 7.5 ± 2.9° continental shortening has occurred between central Qiangtang and Mongolia during the India–Asia convergence. Declination anomaly indicates the central Qiangtang terrane has experienced significant clockwise rotation (57.3 ± 3.9°) relative to stable Eurasia. The compilation of palaeomagnetic results since the Cretaceous reveals ~8.5° northward drift of the Lhasa terrane from 123 ± 9 to 97 ± 7 Ma and the palaeolatitudinal overlap between the Lhasa and Qiangtang terranes after ~111–103 Ma. Together with the onset age of the terrestrial Abushan Formation, our results provide the youngest timing ( ca. ~111–103 Ma) for the closure of the Bangong Meso-Tethys Ocean, as well as for the final collision of the Lhasa and Qiangtang terranes.
    Print ISSN: 0072-1050
    Electronic ISSN: 1099-1034
    Topics: Geosciences
    Published by Wiley-Blackwell
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  • 10
    Publication Date: 2017-11-21
    Description: Hydrogen band electromagnetic ion cyclotron (EMIC) waves have received much attention recently because they are found to frequently span larger spatial areas than the other band EMIC waves. Using test particle simulations, we study the nonlinear effects of hydrogen band EMIC waves on ring current H + ions. A dimensionless parameter R is used to characterize the competition between wave-induced and adiabatic motions. The results indicate that there are three regimes of wave-particle interactions for typical 35 keV H + ions at L =5: diffusive (quasi-linear) behavior when α eq ≤ 35° ( R ≥ 2.45), the nonlinear phase trapping when 35° 〈 α eq 〈 50° (0.75 〈 R 〈 2.45), and both the nonlinear phase bunching and phase trapping when α eq ≥ 50° ( R ≤ 0.75). The phase trapping can transport H + ions towards large pitch angle, while the phase bunching has the opposite effect. The phase trapped H + ions can be significantly accelerated (from 35 keV to over 500 keV) in about 4 minutes, and thus contribute to the formation of high energy components of ring current ions. The results suggest that the effect of hydrogen band EMIC waves is not ignorable in the nonlinear acceleration and resonance scattering of ring current H + ions.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
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