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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
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 70 (1991), S. 5045-5048 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The magneto-optical polar Kerr rotation spectra and reflectivity spectra in the wavelength region 400–700 nm are studied for Fe/PbTe and Fe/Pb bilayer films. Large Kerr rotation enhancement with high reflectivity was observed. The experimental data of reflectivity are nearly consistent with theoretical calculation using Fresnel's equations. However, the observed Kerr rotation spectra behavior is quite different from that expected by macroscopic optical theory.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 63 (1988), S. 3116-3117 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The Kerr rotation spectra of polycrystalline garnets BixY2−xCa1.0V0.5In0.7Fe3.8O12 (x=0–1.6) were measured in the range 1.8–3.4 eV to study the effect on Bi on the magneto-optical effect of polycrystalline YCaVIn garnets with a narrow linewidth of ferromagnetic resonance at 9 GHz (ΔH=1.6 Oe). Negative peaks appear on the Kerr rotation spectra of the samples containing Bi. The absolute value of the peak increases with the concentration of Bi, while the saturation magnetization at room temperature does not vary much and the Curie temperature increases. The Kerr rotation of the sample without Bi is much smaller, with its spectrum similar to that of yttrium iron garnet as reported in the literature. The reflectivity spectra for all samples are similar, showing a transition at about 2.8 eV, but the transition frequency shifts with Bi incorporation.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 66 (1995), S. 430-432 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: We report a novel method for fullerene formation during diamond synthesis via a hot filament, chemical vapor deposition (CVD) procedure. The fullerenes occur in the soot that forms as a by-product on the edges and rear surface of the substrate holder, where the temperature does not favor diamond deposition. Mass spectrometry of the soot shows a peak having a mass to charge ratio corresponding to C60. From typical concentrations of gaseous species in the diamond-growing CVD chamber, we conclude that hydrocarbon species such as CH3 or C2H2 may be the precursors for the fullerene in the CVD chamber. The atomic hydrogen in the gaseous species is believed to play an important role in removing the hydrogen from hydrocarbon to form the all-carbon fullerene. Our observations also suggest that fullerenes produced in the CVD diamond growth chamber play a role in diamond nucleation on foreign substrates. © 1995 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 69 (1996), S. 1074-1076 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: By electrolysis of the methanol solution, an attempt was made to deposit diamondlike carbon (DLC) films on silicon substrate at temperature of less than 60 °C. Substrates were negatively biased with a dc potential of 0 to −3000 V. IR spectra showed that the O–H, C–H, and C–O vibration bands of electrolyte decreased remarkably after electrolysis and a new peak characterized as the C=C bond appeared. The deposited films were characterized as DLC films by Raman spectroscopy. © 1996 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The dielectric properties of amorphous silicon nitride (SiNx) films that were prepared by microwave electron cyclotron resonance plasma chemical vapor deposition at low temperature in the frequency range 5 Hz–1 MHz have been investigated. The dielectric dispersion in the frequency range exhibits two fractional power laws of (ε′−ε∞′)∝ω−p1 and (ε′−ε∞′)∝ωn1−1 with p1=0.12–0.18 and n1=0.95–0.96. These are close to the result predicted by the many-cluster anomalous conduction theory of fractal structure. © 1997 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 111 (1999), S. 4827-4838 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: The structure of a colloidal suspension under shear flow was studied by in situ small angle neutron scattering (SANS). This suspension exhibited shear thinning at low shear rates and shear thickening at high shear rates. Under quiescent conditions, the SANS profiles were azimuthally symmetric and contained a well-defined scattering maximum. This is due to local, liquidlike correlations between neighboring particles. Increasing shear rate lead to changes in the interparticle correlations. These changes are quantified by obtaining the anisotropic structure factor of the suspension under shear flow. We found an increased probability for the formation of inter-particle clusters in the gradient-vorticity plane. This results in an increase in the low angle scattering intensity in the flow direction, and the scattering peak, observed under quiescent conditions, is reduced to a shoulder. We found no evidence for a shear-induced phase transition in our experimental window. At low shear rates (γ(overdot)), the microstructure is relatively insensitive to shear rate. On the other hand, a pronounced shear rate dependence of microstructure is observed when γ(overdot)(approximate)1/τ, where τ is the characteristic time for the decay of concentration fluctuations. Dynamic light scattering was used to measure τ. The onset of shear thickening occurs when γ(overdot)τ is of order unity suggesting an intimate relationship between quiescent dynamics, and shear-induced microscopic and macroscopic changes. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 72 (2001), S. 2450-2454 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: The camber deformations of the flapping insect wing provide important information for lift force analysis. Recent measurements are nearly all based on the hypothesis of the rigid wing, neglecting the camber deformation. In this article, a measurement system based on fringe pattern projection is introduced. Projected comb fringes, whose intensity function is near a comb function, were used instead of conventional sine fringes because of their high intensity and sharpness, allowing us to take the distorted fringes on the transparent dragonfly wing easily. The camber deformation and torsion angle of a flapping dragonfly wing can be measured without hypothesizing that the wing is a rigid plate. The experimental result shows that the camber deformation is different during upstroke and downstroke. It is very important for the explanation of the lift force. © 2001 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2014-10-21
    Description: The photocarrier relaxation dynamics of EuTiO 3 films have been investigated using femtosecond transient absorption spectroscopy. Two kinds of EuTiO 3 films, with and without strain, have been included. In both films, the decay dynamics of 2 p -3 d t2g transition has a fast (∼2 ps) and slow (ns) components which are independent of the strain. Remarkably, the transient photobleaching of 4 f -3 d t2g transition is found to be enhanced considerably in the strained film, accompanied with a subnanosecond carrier lifetime. This behavior can be linked to the strain induced band structure modulation. Our results reveal the dynamical interactions in EuTiO 3 , identifying the critical roles of strain in photo induced phenomena.
    Print ISSN: 0003-6951
    Electronic ISSN: 1077-3118
    Topics: Physics
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