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  • 1
    Online Resource
    Online Resource
    Singapore : Springer
    Keywords: Urban Geography / Urbanism (inc. megacities, cities, towns) ; Architecture ; Urban geography. ; Landscape architecture. ; GNSS ; Erdbeben ; Erdmagnetische Störung ; Elektromagnetismus ; Luftelektrizität ; Fernerkundung ; GNSS ; Ionosphäre ; Aschenwolke ; Detektion
    Description / Table of Contents: Introduction -- Atmospheric Changes and Observations -- Atmospheric Changes and Observations -- GNSS Ionospheric Sounding -- Detection methods for ionospheric disturbances -- Seismic lower-atmospheric anomalies -- Pre-seismic Ionospheric Anomalies -- Co-/Post-seismic Ionospheric Disturbances -- Two-mode seismo-ionospheric disturbances -- Seismo-ionospheric Rayleigh waves -- Epicenter from Ionospheric Disturbances -- Tsunami Ionospheric Disturbances -- Volcano Atmospheric Disturbances -- Volcanic Plumes Detection from GNSS SNR -- Summary and Prospective -- Index
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (XVI, 315 p. 153 illus., 143 illus. in color)
    ISBN: 9789811031786
    Series Statement: Springer eBooks
    Language: English
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  • 2
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 72 S., 10,1 MB) , Ill., graph. Darst.
    Language: German
    Note: Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Förderkennzeichen BMWi 032564A. - Verbund-Nr. 01085445 , Systemvoraussetzungen: Acrobat reader.
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  • 3
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Plastic analysis (Engineering). ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (492 pages)
    Edition: 1st ed.
    ISBN: 9780444598356
    Series Statement: Issn Series ; v.Volume 52
    Language: English
    Note: Front Cover -- Limit Analysis in Soil Mechanics -- Copyright Page -- Table of Contents -- Preface -- Chapter 1. INTRODUCTION -- 1.1 Introduction -- 1.2 A short historical review of soil plasticity -- 1.3 Idealized stress-strain relations for soil -- 1.4 Limit analysis for collapse load -- 1.5 Finite-element analysis for progressive failure behavior of soil mass -- Chapter 2. BASIC CONCEPTS OF LIMIT ANALYSIS -- 2.1 Introduction -- 2.2 Index notation -- 2.3 The perfectly plastic assumption and yield criterion -- 2.4 The kinematic assumption on soil deformations and flow rule -- 2.5 The stability postulate of Drucker -- 2.6 Restrictions imposed by Drucker's stability postulate - convexity and normality -- 2.7 The assumption of small change in geometry and the equation of virual work -- 2.8 Theorems of limit analysis -- 2.9 Limit theorems for materials with non-associated flow rules -- 2.10 The upper-bound method -- 2.11 The lower-bound method -- References -- Chapter 3. VALIDITY OF LIMIT ANALYSIS IN APPLICATION TO SOILS -- 3.1 Introduction -- 3.2 Soil - a multiphase material -- 3.3 Mechanical behaviour of soils -- 3.4 Soil failure surfaces -- 3.5 Validity of limit analysis in application to soils -- 3.6 Friction-dalatation and related energy in cohesionless soils -- 3.7 Effect of friction on the applicability of limit analysis to soils -- 3.8 Some aspects of retaining wall problems and the associated phenomena at failure -- References -- Chapter 4. LATERAL EARTH PRESSURE PROBLEMS -- 4.1 Introduction -- 4.2 Failure mechanism -- 4.3 Energy dissipation -- 4.4 Passive earth pressure analysis -- 4.5 Active earth pressure analysis -- 4.6 Comparisons and discussions -- 4.7 Some practical aspects -- References -- Chapter 5. RIGID RETAINING WALLS SUBJECTED TO EARTHQUAKE FORCES -- 5.1 Introduction -- 5.2 General considerations. , 5.3 Seismic passive earth pressure analysis -- 5.4 Seismic active earth pressure analysis -- 5.5 Numerical results and discussions -- 5.6 Earth pressure tables for practical use -- References -- Appendix A: Seismic earth pressure tables for KA and KP -- Appendix B: Earth pressure tables for NAc and NPc -- Chapter 6. SOME PRACTICAL CONSIDERATIONS IN DESIGN OF RIGID RETAINING STRUCTURES -- 6.1 Introduction -- 6.2 Theoretical considerations of the modified Dubrova method -- 6.3 Some numerical results and discussions of the modified Dubrova method -- 6.4 Evaluation of the modified Dubrova method -- 6.5 Effects of wall movement on lateral earth pressures -- 6.6 Earth pressure theories for design applications in seismic environments -- 6.7 Design recommendations -- References -- Chapter 7. BEARING CAPACITY OF STRIP FOOTING ON ANISOTROPIC AND NONHOMOGENEOUS SOILS -- 7.1 Introduction -- 7.2 Analysis -- 7.3 Results and discussions -- References -- Chapter 8. EARTHQUAKE-INDUCED SLOPE FAILURE AND LANDSLIDES -- 8.1 Introduction -- 8.2 Failure surface -- 8.3 Determination of the critical height for seismic stability -- 8.4 Special spiral-slope configurations -- 8.5 Calculated results and discussions -- 8.6 Concluding remarks -- References -- Chapter 9. SEISMIC STABILITY OF SLOPES IN NONHOMOGENEOUS, ANISOTROPIC SOILS AND GENERAL DISCUSSIONS -- 9.1 Introduction -- 9.2 Log-spiral failure mechanism for a nonhomogeneous and anisotropic slope -- 9.3 Numerical results and discussions -- 9.4 Mechanics of earthquake-induced slope failure -- References -- Chapter 10. ASSESSMENT OF SEISMIC DISPLACEMENT OF SLOPES -- 10.1 Introduction -- 10.2 Failure mechanisms and yield acceleration -- 10.3 Assessment of seismic displacement of slopes -- 10.4 Summary -- References -- Appendix 1: Plane failure surface -- Appendix 2: Logspiral failure surface. , Appendix 3: Limit analysis during earthquake -- Chapter 11. STABILITY ANALYSIS OF SLOPES WITH GENERALIZED FAILURE CRITERION -- 11.1 Introduction -- 11.2 Variational approach in limit analysis and the combined method -- 11.3 Stability analysis of slopes -- 11.4 Layered analysis of embankments -- 11.5 Summary -- References -- Subject index -- Author index.
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  • 4
    Publication Date: 2023-03-16
    Keywords: Archive of Ocean Data; ARCOD; Area/locality; Badain Jaran Desert; Bicarbonate ion; BJD-1; BJD-10; BJD-11; BJD-12; BJD-13; BJD-14; BJD-15; BJD-16; BJD-17; BJD-18; BJD-19; BJD-2; BJD-20; BJD-21; BJD-22; BJD-23; BJD-24; BJD-25; BJD-26; BJD-27; BJD-28; BJD-29; BJD-3; BJD-30; BJD-31; BJD-32; BJD-33; BJD-34; BJD-35; BJD-36; BJD-37; BJD-38; BJD-4; BJD-5; BJD-6; BJD-7; BJD-8; BJD-9; Calcium; Calculated; Carbonate; Chloride; Da Tong River; Elevation of event; Event label; Gu Ri Nai; Hei He River; Helium-3/Helium-4; Helium-4/Neon-20; Huang Shui River; Latitude of event; Longitude of event; Magnesium; Mass spectrometry; Nitrate; pH; Potassium; Ratio; Sample type; Shi Yang River; Shi You River; Shu Le River; Sodium; Sulfate; Tao LaiRiver; Total dissolved solids; Tritium; Tritium, standard deviation; Water sample; Wen Tu Gao Le; WS; δ18O, water; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 601 data points
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  • 5
    Publication Date: 2023-03-16
    Keywords: Archive of Ocean Data; ARCOD; Badain Jaran Desert; BJD-P1; BJD-P2; BJD-P3; Date; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Latitude of event; Longitude of event; Mass spectrometry; SOIL; Soil profile; Water content, wet mass; δ18O, water; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 174 data points
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  • 6
    Publication Date: 2023-03-16
    Keywords: Archive of Ocean Data; ARCOD; Badain Jaran Desert; BJD-P1; BJD-P2; BJD-P3; Chloride; Date; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Ion chromatograph, Dionex Corporation, DX-300; Latitude of event; Longitude of event; SOIL; Soil profile; Sulfate; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 174 data points
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Chen, J S; Sun, X X; Gu, W Z; Tan, H B; Rao, W B; Dong, H Z; Liu, X Y; Su, Z G (2012): Isotopic and hydrochemical data to restrict the origin of the groundwater in the Badain Jaran Desert, Northern China. Geokhimiya, 2012, 50(5), 502-512, Geochemistry International, 50(5), 455-465, https://doi.org/10.1134/S0016702912030044
    Publication Date: 2023-03-16
    Description: Despite its extreme aridity the Badain Jaran Desert is rich in groundwater. In the southeastern part of this desert it is characterized by coexistence of high megadunes and a great number of lakes. Deuterium and oxygen 18 isotope compositions as well as hydrochemistry of groundwater, lake water, soil water and river water were investigated in detail to gain an insight into their relationships and the origin of the groundwater. The results show that the groundwater and the lake water are genetically related, but unrelated to local precipitation and the leakage of Heine River at the northern slope of the Qilian mountain. dD and d18O values of deep soil water (deeper than 40 cm) and groundwater plot on the same evaporation line E11, which shows that they have the same recharge source. The point of intersection between E11 and LMWL suggests that the groundwater originates from a water resource, which has a weighted mean value that is lighter by some 6 per mil d18O than local precipitation in Badain Jaran Desert. 3H data of water samples show that the groundwater in the Badain Jaran Desert originates from water recharged after the nuclear test. The deep fault zone underground maybe a water circulation channel based on helium analysis of groundwater. The result has guiding significance to rational exploitation and utilization of the local groundwater.
    Keywords: Archive of Ocean Data; ARCOD
    Type: Dataset
    Format: application/zip, 3 datasets
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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. 3940-3945 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Photodissociation of the H2S molecule at 157.6 nm was studied experimentally using the Rydberg tagging technique. Translational energy distributions of the H-atom product from the H2S photodissociation were measured, and the SH(X 2Π)+H(2S) channel was found to be the dominant dissociation process. Spin-orbit and rovibrational state distributions were also obtained for the SH product, which was found to be both vibrationally and rotationally excited. An intriguing bimodal rotational distribution in the lowest two vibrational states, v=0 and 1, has been clearly observed for the SH product, indicating that there are two distinctive dissociation mechanisms involved in the photodissociation of H2S at 157 nm excitation. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 111 (1999), S. 1628-1635 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Despite the relevance to most aspects of crystallization, a comprehensive understanding of the kinetics of heterogeneous nucleation has not been well established yet. In this paper, a new kinetic model based on the "steady-state" approach will be put forward to describe both heterogeneous and homogeneous nucleation. As a key point in this model, the effect of foreign particles on both the nucleation barrier, the "chain reaction" process and the transport of structural units is taken into account. Ranging from low to high supersaturations, heterogeneous nucleation plays a more comprehensive role in nucleation than we expected, depending on the size of foreign particles and the interaction and structural matching between foreign particles and the nucleating phase. It follows that genuine homogeneous nucleation may only be possible at very high supersaturations, and can become easier when convection is eliminated. The results have been verified by the CaCO3 nucleation experiments. This general model allows us to describe many unexpected nucleation phenomena for the first time, and will have significant impact on the control of nucleation, understanding of crystallization in microgravity, the measurement of the crystal–fluid interfacial tension, and crystallization in general. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 110 (1999), S. 9174-9178 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Effects of hydrostatic pressure on Raman spectra have been investigated in mixed-valence (MV) gold complexes Cs2Au2X6 (X=Cl and Br). We have observed pressure-induced deactivation of the Raman-active Au-X stretching modes at various temperatures, indicating a pressure-induced phase transition from the MV state to a single-valence (SV) state. The critical pressure at 300 K decreases from 10.6 GPa for X=Cl to 6.8 GPa for X=Br, perhaps due to reduced electron–phonon interaction in Cs2Au2Br6. We further derived comprehensive electronic phase diagrams of Cs2Au2X6 (X=Cl and Br) as a function of pressure and temperature. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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