ALBERT

Description / Table of Contents: I. Introduction --- 1. Computer Experiments of Space Plasmas --- II. Simulation Techniques --- 2. KEMPO1 --- 3. TRISTAN --- 4. MACRO-EM --- 5. HYBRID CODES --- 6. TWO-DIMENSIONAL MHD CODE --- 7. HIGH-PRECISION MHD SIMULATION --- 8. TUTORIAL FOR UNIX OPERATIONS --- III. Simulation Software --- 9. KEMPO1 --- 10. TRISTAN --- 11. MACROEM --- 12. HYBRID1 --- 13. MHD2 --- 14. WAVE

Description / Table of Contents: Pages 1-13 / Maars of the Westeifel, Germany / G. Büchel --- Pages 15-60 / Syn- and post-eruptive mechanism of the Alaskan Ukinrek Maars in 1977 / G. Büchel, V. Lorenz --- Pages 61-80 / Maars and maar lakes of the Westeifel Volcanic Field / Jörg F. W. Negendank, Bernd Zolitschka --- Pages 81-94 / Maars of northern Auvergne (Massif Central, France): State of knowledge / E. Juvigné, G. Camus, A. de Goër de Herve --- Pages 95-107 / Palaeoenvironmental investigations on long sediment cores from volcanic lakes of Lazio (central Italy)—An overview / Maria Follieri, Donatella Magri, Biancamaria Narcisi --- Pages 109-116 / Geophysical mapping of organic sediments / Stefan Wende, Reinhard Kirsch --- Pages 117-118 / Preliminary uniboom survey of the Monticchio Lakes (southern Italy) / A. Stefanon --- Pages 119-128 / Sonar investigations in the Laghi di Monticchio (Mt. Vúlture, Italy) / Ralph B. Hansen --- Pages 129-148 / Climatic and tectonic effects on sedimentation in central Italian volcano lakes (Latium)—Implications from high resolution seismic profiles / F. Niessen, A. Lami, P. Guilizzoni --- Pages 149-161 / Sediments and basin analysis of Lake Schalkenmehrener Maar / T. Heinz, B. Rein, J. F. W. Negendank --- Pages 163-171 / Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator / B. Rein, J. F. W. Negendank --- Pages 173-194 / Basin analysis for selected time-frames using sedimentation rates in Lake Meerfelder Maar (Westeifel FRG) / F. Wegner, J. F. W. Negendank --- Pages 195-208 / Turbidites in the sediments of Lake Meerfelder Maar (Germany) and the explanation of suspension sediments / D. Drohmann, J. F. W. Negendank --- Pages 209-222 / Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany) / D. Poth, J. F. W. Negendank --- Pages 223-235 / Paleoenvironmental reconstruction of the Late- and Postglacial sedimentary record of Lake Weinfelder Maar / A. Brauer, J. F. W. Negendank --- Pages 237-275 / Sedimentology and paleoenvironment from the Maar Lac du Bouchet for the last climatic cycle, 0-120,000 years (Massif Central, France) / Elisabeth Truze, Kerry Kelts --- Pages 277-288 / Lago Grande di Monticchio (southern Italy) a high resolution sedimentary record of the last 70,000 years / Bernd Zolitschka, Jörg F. W. Negendank --- Pages 289-304 / A multidisciplinary study of the Vico Maar sequence (Latium, Italy): Part of the last cycle in the Mediterranean area. Preliminary results / P. Francus, S. Leroy, I. Mergeai, G. Seret, G. Wansard --- Pages 305-316 / Environmental geology and geochemistry of lake sediments (Holzmaar, Eifwl, Germany) / B. G. Lottermoser, R. Oberhänsli, B. Zolitschka, J. F. W. Negendank, U. Schütz… --- Pages 317-332 / Geochemistry of Lago Grande di Monticchio, S. Italy / C. Robinson, G. B. Shimmield, K. M. Creer --- Pages 333-348 / Tephrochronology of core C from Lago Grande di Monticchio / Anthony J. Newton, Andrew J. Dugmore --- Pages 349-365 / A palaeomagnetic study of maar-lake sediments from the Westeifel / B. Haverkamp, Th. Beuker --- Pages 367-376 / Preliminary 50m palaeomagnetic records from Lac du Bouchet, Haute Loire, France / T. Williams, K. M. Creer, N. Thouveny --- Pages 377-392 / Palaeomagnetic investigations of Lago Grande di Monticchio, southern Italy / Ian Turton --- Pages 393-420 / Late-Glacial/Holocene changes of the climatic and trophic conditions in three Eifel maar lakes, as indicated by faunal remains. I. Cladocera / Wolfgang Hofmann --- Pages 421-433 / Late-glacial/Holocene changes of the climatic and trophic conditions in three Eifel maar lakes, as indicated by faunal remains. II. Chironomidae (Diptera) / Wolfgang Hofmann --- Pages 435-439 / Ostracoda (Crustacea) and trichoptera (Insecta) from Late-and Postglacial sediments of some European maar lakes / Burkhard W. Scharf --- Pages 441-446 / Oligocence dinoflagellate-cysts in Quaternary freshwater sediments of Eifel maars / H. Weiler --- Pages 447-465 / Tertiary maars of the Hocheifel Volcanic Field, Germany / G. Büchel, M. Pirrung --- Pages 467-476 / Some aspects of Cenozoic maar sediments in Europe: the source-rock potential and their exceptionally good fossil preservation / W. Zimmerle --- Pages 477-484 / Palaeoecological implications from the sedimentary record of a subtropical maar lake (Eocene Eckfelder Maar; Germany) / Bernd Zolitschka --- Pages 485-489 / Arthropods from the Eocene Eckfelder Maar (Eifel, Germany) as a source for paleoecological information / H. Lutz --- Pages 491-497 / Flowers from the Middle Eocene of Eckfeld (Eifel, Germany)— First results / H. Frankenhäuser, V. Wilde --- Pages 499-503 / Initial results on the importance of a flora from the Middle Eocene of Eckfeld (Eifel, W.-Germany) / V. Wilde, H. Frankenhäuser --- Pages 505-509 / International Maar Deep Drilling Project (MDDP) a challenge for earth sciences? / Jörg F. W. Negendank, Bernd Zolitschka

Description / Table of Contents: INTRODUCTION The study is essentially empirical, since it portrays and appraises two different water management systems, and relates them to one another. Yet the analysis has also been made with definite research aims in mind. Its focus has been narrowed down to the environmental assessment of urban water management systems in arid and semi-arid regions, especially with an eye to deal with information problems in the Developing World. The study addresses a set of very critical issues of global concern, and, thus, delineates a crucial topic for international research. The fact that a wide range of critical issues usually complicates and aggravates the given problem setting provides the comparative analysis with a special practical incentive to explore the opportunities for joint strategies and comprehensive solutions. However, the complexities involved between water management and the environment and the relative lack of a joint theory in that field pose certain difficulties to such an undertaking. In order to fully appreciate the underlying purpose of the study and the scope of its implications, the various facets of the problem setting and the essential ingredients of the general line of approach have first to be unravelled and expounded at some length. Above all, it needs to be shown how these facets combine to produce the complex, burning issues which in turn seem to, both in theory and practice, require correspondingly intricate, strategic approaches for their solutions...

Description / Table of Contents: PREFACE Turbidity currents have been comprehensively studied in the past although much remains unknown about both their flow characteristics and resultant sedimentary deposits. Much of this uncertainty arises from the catastrophic nature of their formation which makes them difficult to study in the environment, and has resulted in the majority of studies being experimental or theoretical. Experiments have shown that reversals in the flow of density currents can be associated with the generation of internal solitary waves. This is in contrast to the belief held by many workers that the reversal of a turbidity current simply generates an identical flow travelling in the opposite direction. This book arose from the need for a detailed experimental study to examine the effects and to consider the consequences of density current reversals from a variety of obstructions to their flow. The first part of this book comprises a detailed review of literature covering the fluid dynamics and sedimentology relevant to the experimental study (chapter one). Chapter two presents the results from the comprehensive experimental programme which are discussed and compared with appropiate theoretical hypotheses. This permits the synthesis of a model for the general features of flows that result from the incidence of density currents upon obstructions to the flow. The application of this model to both modern and ancient turbidite systems is then discussed in chapter three. This book is suitable for earth scientists with an interest in the dynamics of turbidity currents. In addition, workers from other fields such as applied maths, meteorology and engineering who have an interest in density currents and bores in practical situations may find it useful...

Description / Table of Contents: INTRODUCTION --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 3-22 --- 1.1 The Nature of Shock Waves, pp. 3-5 --- 1.2 Compaction of Powders and Shock Activation, pp. 6-9 --- 1.3 First-Order Phase Transitions and Chemical Reactions, pp. 10-12 --- 1.4 Time Scales and Interactions of Basic Mechanisms, p. 12 --- 1.4.1 Shock propagation in a particle assemblage, p. 12 --- 1.4.2 Energy localization, pp. 12-13 --- 1.4.3 Thermal relaxation of hot spots, p. 14 --- 1.4.4 Mass diffusion in solids, p. 14 --- 1.4.5 Kinetic constants, pp. 14-16 --- 1.5 Some Roles of Shock Compression Techniques in Material Sciences Study, p. 16 --- 1.5.1 Shock compression technique as a tool of high pressure production, p. 16 --- 1.5.2 Appearance of diamond anvil-type high-pressure apparatus, pp. 16-18 --- 1.5.3 New roles of shock compression technology as a unique method of very high temperature production, pp. 18-19 --- 1.5.4 Development of conventional hypervelocity impact techniques for precise measurement of materials under shock compression, pp. 19-21 --- FUNDAMENTALS OF SHOCK WAVE PROPAGATION --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 23-78 --- 2.1 Hydrodynamic Jump Conditions and the Hugoniot Curve, pp. 23-32 --- 2.2 Shock Transition in Hydrodynamic Solids, pp. 32-42 --- 2.3 Non-Hydrostatic Deformation of Solids, p. 42 --- 2.3.1 Elastic-ideally-plastic solids, pp. 42-53 --- 2.3.2 Experimental observations of elastic-plastic behavior, pp. 53-56 --- 2.4 Wave-body interactions, pp. 56-57 --- 2.4.1 Preliminaries, pp. 57-60 --- 2.4.2 Planar impact of similar and dissimilar bodies, pp. 60-61 --- 2.4.3 Shock wave interaction with material boundaries, pp. 61-64 --- 2.4.4 Wave-wave interactions, pp. 65-66 --- 2.4.5 Detonation wave and interaction with a solid surface, pp. 66-77 --- SHOCK COMPRESSION TECHNOLOGY --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 79-115 --- 3.1 Gun Techniques, p. 80 --- 3.1.1 Single stage gun, p. 80 --- 3.1.2 Conventional two stage light gas gun, pp. 80-83 --- 3.1.3 Velocity measurement of projectile, p. 83 --- 3.1.4 Magnetoflyer method, pp. 83-84 --- 3.1.5 CW x-ray velocity meter, pp. 84-86 --- 3.1.6 Measurement of interior projectile motion, pp. 86-87 --- 3.1.7 Recovery experiments, pp. 87-89 --- 3.2 Explosive Techniques, p. 89 --- 3.2.1 Plane shock wave generation and recovery fixture, pp. 89-91 --- 3.2.2 Numerical simulaation of shock compression in the recovery capsule, pp. 91-94 --- 3.2.3 Cylindrical recovery fixture, pp. 94-95 --- 3.3 In-situ Measurements, p. 95 --- 3.3.1 Manganin pressure gauge, pp. 95-98 --- 3.3.2 Particle velocity gauge, pp. 99-100 --- 3.3.3 Observations of multiple shock reverberations by using a manganin pressure gauge and particle velocity gauge, pp. 100-106 --- 3.3.4 Shock temperature measurement, pp. 106-111 --- 3.3.5 Copper-Constantan thermocouple as a temperature and pressure gauge, pp. 111-113 --- THERMOMECHANICS OF POWDER COMPACTION AND MASS MIXING --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 117-170 --- 4.1 A One Dimensional Particulate Model, pp. 117-123 --- 4.2 Continuum Models, p. 123 --- 4.2.1 Hydrodynamic models, pp. 124-141 --- 4.2.2 Continuum plasticity theory, pp. 141-148 --- 4.2.3 Application, pp. 148-154 --- 4.3 Particle Bonding and Heterogeneous Processes, pp. 154-160 --- 4.4 Mass Mixing, pp. 160-169 --- THERMOCHEMISTRY OF HETEROGENEOUS MIXTURES --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 171-225 --- 5.1 Thermodynamic Functions of Heterogeneous Mixtures, pp. 172-187 --- 5.2 Analytical Equations of State, pp. 187-191 --- 5.3 Hugoniots of Inert Mixtures, p. 191 --- 5.3.1 Thermodynamically equilibrium models, pp. 191-197 --- 5.3.2 Mechanical models, pp. 197-199 --- 5.4 First-Order Phase Transitions, pp. 199-206 --- 5.5 Chemical Equilibria, pp. 206-212 --- 5.6 Reaction Kinetics, p. 212 --- 5.6.1 Rate equations, pp. 212-214 --- 5.6.2 Nucleation, pp. 214-216 --- 5.6.3 Growth, pp. 216-217 --- 5.6.4 Pressure effects, pp. 217-218 --- 5.7 Shock-Induced Reactions in Powder Mixtures, pp. 218-224 --- HYDRODYNAMICAL CALCULATIONS --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 227-276 --- 6.1 Conservation Equations of Continuum Flow, pp. 227-228 --- 6.1.1 Mass conservation, pp. 228-230 --- 6.1.2 Conservation of linear momentum, pp. 230-231 --- 6.1.3 Enegy conservation, pp. 231-234 --- 6.2 Constitutive Modeling of Inorganic Shock Chemistry, pp. 234-235 --- 6.2.1 VIR model, pp. 235-239 --- 6.2.2 Pore collapse, p. 239 --- 6.2.3 Chemical kinetics, pp. 239-240 --- 6.2.4 Computational constitutive reactions, pp. 240-245 --- 6.3 Applications of the VIR Model, p. 245 --- 6.3.1 Shock wave profiles in Ni/Al powder mixtures, pp. 245-250 --- 6.3.2 Compaction of diamond with Si and graphite, pp. 250-257 --- 6.4 Continuum Mixture Theory and the VIR Model, p. 257 --- 6.4.1 Continuum mixture theory, pp. 257-263 --- 6.4.2 Derivation of the VIR model using the CMT, pp. 263-269 --- 6.4.3 A model of heterogeneous flow, pp. 269-275 --- SHOCK CONDITIONING AND PROCESSING OF CERAMICS --- Shock Compression Chemistry of materials, Y. Horie and A. B. Sawaoka, pp. 277-360 --- 7.1 Shock Conditioning of Powder of Inorganic Materials, p. 227 --- 7.1.1 Brief review of shock conditioning studies, p. 227 --- 7.1.2 Aluminum oxide powder, pp. 277-281 --- 7.2 Shock Synthesis of Inorganic Materials, p. 281 --- 7.2.1 Shock synthesis studies, p. 281 --- 7.2.2 High dense forms of carbon, pp. 281-285 --- 7.2.3 High dense forms of boron nitride, pp. 285-287 --- 7.2.4 Shock treatment of boron nitride powders, pp. 287-301 --- 7.3 Shock Consolidation of Ceramic Powders, p. 301 --- 7.3.1 Why non-oxide ceramics?, pp. 301-302 --- 7.3.2 Dynamic consolidation of SiC powders, pp. 302-304 --- 7.3.3 Approach to the fabrication of crack free compacts, pp. 304-305 --- 7.3.4 Shock consolidation of SiC powder utilizing post shock heating by exothermic reaction, pp. 305-310 --- 7.4 Dynamic Compaction of Zinc Blende Type Boron Nitride and Diamond Powders, p. 310 --- 7.4.1 Background, pp. 310-311 --- 7.4.2 Cubic boron nitride, pp. 311-318 --- 7.4.3 Diamond, pp. 318-326 --- 7.4.4 Diamond composites obtained by utilizzing exothermic chemical reaction, pp. 326-332 --- 7.5 Very High Pressure Sintering of Shock Treated Powders, pp. 332-334 --- 7.5.1 Silicon nitride, pp. 334-336 --- 7.5.2 w-BN, pp. 336-346 --- 7.6 Rapid Condensation of High Temperature Ultrasupersaturated Gas, p. 346 --- 7.6.1 Silicon nitride, pp. 346-352 --- 7.6.2 Carbon, pp. 352-357

Description / Table of Contents: K. Pye: Introduction: the nature and significance of aeolian sedimentary systems / Geological Society, London, Special Publications, 72:1-4, doi:10.1144/GSL.SP.1993.072.01.01 --- Aeolian Mechanics and Dune Morphodynamics --- Ian K. McEwan and Brian B. Willetts: Sand transport by wind: a review of the current conceptual model / Geological Society, London, Special Publications, 72:7-16, doi:10.1144/GSL.SP.1993.072.01.02 --- Jack Hardisty, Helen L. Rouse, and Samantha Hart: Gain function analysis of sand transport in a turbulent air flow / Geological Society, London, Special Publications, 72:17-23, doi:10.1144/GSL.SP.1993.072.01.03 --- Jennifer R. Burkinshaw, Werner K. Illenberger, and Izak C. Rust: Wind-speed profiles over a reversing transverse dune / Geological Society, London, Special Publications, 72:25-36, doi:10.1144/GSL.SP.1993.072.01.04 --- Giles F. S. Wiggs: Desert dune dynamics and the evaluation of shear velocity: an integrated approach / Geological Society, London, Special Publications, 72:37-46, doi:10.1144/GSL.SP.1993.072.01.05 --- Desert Dunefields --- Ann G. Wintle: Luminescence dating of aeolian sands: an overview / Geological Society, London, Special Publications, 72:49-58, doi:10.1144/GSL.SP.1993.072.01.06 --- Stephen R. Edwards: Luminescence dating of sand from the Kelso Dunes, California / Geological Society, London, Special Publications, 72:59-68, doi:10.1144/GSL.SP.1993.072.01.07 --- H. M. Rendell, A. Yair, and H. Tsoar: Thermoluminescence dating of periods of sand movement and linear dune formation in the northern Negev, Israel / Geological Society, London, Special Publications, 72:69-74, doi:10.1144/GSL.SP.1993.072.01.08 --- Stephen Stokes and Carol S. Breed: A chronostratigraphic re-evaluation of the Tusayan Dunes, Moenkopi Plateau and southern Ward Terrace, Northeastern Arizona / Geological Society, London, Special Publications, 72:75-90, doi:10.1144/GSL.SP.1993.072.01.09 --- Ian Livingstone and David S. G. Thomas: Modes of linear dune activity and their palaeoenvironmental significance: an evaluation with reference to southern African examples / Geological Society, London, Special Publications, 72:91-101, doi:10.1144/GSL.SP.1993.072.01.10 --- Mary Crabaugh and Gary Kocurek: Entrada Sandstone: an example of a wet aeolian system / Geological Society, London, Special Publications, 72:103-126, doi:10.1144/GSL.SP.1993.072.01.11 --- Tapan Chakraborty and A. K. Chaudhuri: Fluvial-aeolian interactions in a Proterozoic alluvial plain: example from the Mancheral Quartzite, Sullavai Group, Pranhita-Godavari Valley, India / Geological Society, London, Special Publications, 72:127-141, doi:10.1144/GSL.SP.1993.072.01.12 --- Coastal Dunefields --- Norbert P. Psuty: Foredune morphology and sediment budget, Perdido Key, Florida, USA / Geological Society, London, Special Publications, 72:145-157, doi:10.1144/GSL.SP.1993.072.01.13 --- Abhilasha Wal and John McManus: Wind regime and sand transport on a coastal beach-dune complex, Tentsmuir, eastern Scotland / Geological Society, London, Special Publications, 72:159-171, doi:10.1144/GSL.SP.1993.072.01.14 --- R. W. G. Carter and Peter Wilson: Aeolian processes and deposits in northwest Ireland / Geological Society, London, Special Publications, 72:173-190, doi:10.1144/GSL.SP.1993.072.01.15 --- Lluisa Cros and Jordi Serra: A complex dune system in Baix Empordà (Catalonia, Spain) / Geological Society, London, Special Publications, 72:191-199, doi:10.1144/GSL.SP.1993.072.01.16 --- Kenneth Pye and Adrian Neal: Late Holocene dune formation on the Sefton coast, northwest England / Geological Society, London, Special Publications, 72:201-217, doi:10.1144/GSL.SP.1993.072.01.17 --- Rita A. M. Gardner and Susan J. McLaren: Progressive vadose diagenesis in late Quaternary aeolianite deposits? / Geological Society, London, Special Publications, 72:219-234, doi:10.1144/GSL.SP.1993.072.01.18 --- Susan J. McLaren: Use of cement types in the palaeoenvironmental interpretation of coastal aeolianite sequences / Geological Society, London, Special Publications, 72:235-244, doi:10.1144/GSL.SP.1993.072.01.19 --- Temperate and Cold Climate Continental Dunes --- Eduard A. Koster, Ilona I. Y. Castel, and Ron L. Nap: Genesis and sedimentary structures of late Holocene aeolian drift sands in northwest Europe / Geological Society, London, Special Publications, 72:247-267, doi:10.1144/GSL.SP.1993.072.01.20 --- Matti Seppälä: Climbing and falling sand dunes in Finnish Lapland / Geological Society, London, Special Publications, 72:269-274, doi:10.1144/GSL.SP.1993.072.01.21 --- Dust and Loess --- Geneviève Coudé-Gaussen and Pierre Rognon: Contrasting origin and character of Pleistocene and Holocene dust falls on the Canary Islands and southern Morocco: genetic and climatic significance / Geological Society, London, Special Publications, 72:277-291, doi:10.1144/GSL.SP.1993.072.01.22 --- Pei-Ying Li and Li-Ping Zhou: Occurrence and palaeoenvironmental implications of the Late Pleistocene loess along the eastern coasts of the Bohai Sea, China / Geological Society, London, Special Publications, 72:293-309, doi:10.1144/GSL.SP.1993.072.01.23 --- Timothy C. Rolph, John Shaw, Edward Derbyshire, and Wang Jingtai: The magnetic mineralogy of a loess section near Lanzhou, China / Geological Society, London, Special Publications, 72:311-323, doi:10.1144/GSL.SP.1993.072.01.24

Description / Table of Contents: Image sequence processing is becoming a tremendous tool to analyze spatio-temporal data in all areas of natural science. It is the key to studythe dynamics of of complex scientific phenomena. Methods from computer science and the field of application are merged establishing new interdisciplinary research areas. This monograph emerged from scientific applications and thus is an example for such an interdisciplinaryapproach. It is addressed both to computer scientists and to researchers from other fields who are applying methods of computer vision. The results presented are mostly from environmental physics (oceanography) but they will be illuminating and helpful for researchers applying similar methods in other areas.

Description / Table of Contents: The Third International Symposium on Large Spatial Databases (SSD '93) was held at the National University of Singapore in June 1993. The previous meetings of the series were at Sanata Barbara (1989) and Zurich (1991). The meetings are planned as a forum for researchers and practitioners specializing in database theory for and advanced applications of Spatial Information Systems. This volume constitutes the proceedings of the symposium. It contains 25 selected papersand three keynotes papers: "Spatial data management in database systems: research directions" (W. Kim), "From extensible databases to interoperability between multiple databases and GIS applications" (H.-J. Schek), and "The SEQUOIA 2000 project" (M. Stonebraker). The selectedpapers are collected into sections on: data modeling, spatial indexing, indexing mechanisms, handling of raster and vector data, spatial database systems, topology, storage management, query retrieval,knowledge engineering in SDS, and 3-dimensional data handling.

Description / Table of Contents: This book bridges the gap between system theory and global climate change research, and benefits both. A representative set of systems problems is listed indicating how such cross-fertilization would enhance present understanding of global problems while assisting the extension of systems theory. The goal is a comprehensive conceptual model of global change which encompasses atmosphere, lithosphere, ocean, biosphere and cryosphere. The systems model is developed in two steps using a "block diagram" approach. First, causality flows among principal components are identified and a block diagram representation is constructed. Second, mathematical description of the mappings represented by the blocks is derived from the physical principles and known disciplinary models. The generation of the complete block diagram is believed to be the first of its kind. A number of helpful features characterize the book. Chapter 1 provides the basic framework and organization of the book. Chapter 2 is a primer to global climate systems for the reader unfamiliar with the subject of the scientific aspects of global warning. A list of notation in Appendix B, a glossary of global climate change research search terminology, and a detailed index for cross referencing are included. Additionally, a representative set of relevant systems problems in global change is listed at the end of the book.

Description / Table of Contents: PREFACE Sedimentation as a Three-Component System describes the most common styles of deposition in marine environments as they relate to sediment composition. Three components, organic matter, carbonate, and siliciclastic sediment, may settle concurrently, but at different rates, intermixing on the sea floor to form a particular sediment composition. A change in the flux of one component is capable of relatively diluting or concentrating the other two components, which can be expressed in the characteristic ratio of organic carbon to carbonate in the resulting sediment. The basic concept of this book is to address organic carbon-carbonate associations in terms of depositional inputs and time spans. In addition, the three-component system describes organic carbon changes related to major facies transitions. Examples include models of the genesis of carbonaceous sediments, with their various laminated to bioturbated lithotypes, and numerical organic carbon prediction. I hope that this book will encourage stimulating discussions and promote a new approach to quantitative stratigraphy...

Description / Table of Contents: INTRODUCTION The International Summer School of Theoretical Geodesy on Satellite Altimetry in Geodesy and Oceanography was held in Trieste (Italy) from May 25 to June 6, igg2. It was organized by Prof. R. Rummel of the Delft University of Technology and by Prof. F. Sansò of the Politecnico di Milano and was attended by 63 participants and 7 lecturers from 17 countries. The School was hosted by the International Centre of Theoretical Physics of Trieste. Satellite altimetry provides a lot of data that require more and more sophisticated models in order to be interpreted and exploited. One of the main problems related to the practical treatment of the data can be summarized as follows: oceanographers would like to ask geodesists to compute precise orbits and a precise geoid in order to put into evidence the Sea Surface Topography that can be interpreted as an oceanographic signal related to currents and to several physical parameters; on the other hand, geodesists would like to ask oceanographers to a-priori determine the Sea Surface Topography, in order to be able to extract from the altimeter data the geoid and the orbit errors to be used in the gravity field modelling. The solution to this dilemma can only be found in a cooperative frame. An integrated model to be used for a single-step treatment of altimetry is probably far to be defined, so at present geodesists and oceanographers must cooperate to obtain step-wise and iterative modelling of the gravity field and of the oceanographic phenomena. This is precisely the reason why the school on Satellite Altimetry was organized on an interdisciplinary basis...

Description / Table of Contents: PREFACE Some of the major ecological and social problems of the present and future are the production, treatment, and disposal of anthropogenic wastes. Iaais is equally true for sparsely and densely populated industrial areas, including large countries in which sites for waste disposal would seem to be readily available. Especially nonradioactive hazardous wastes with their long-term toxicity need to be isolated from the biosphere just as effectively as radioactive substances. The long-term safety required of waste disposal sites can only be assured under specific geological and mineralogical conditions in certain parts of the lithosphere (underground repositories). The subjects related to the production, avoidance, treatment, and disposal of anthropogenic wastes cover a range of knowledge encompassing the natural sciences, engineering, medicine, and law. This work presents some fundamental situations and problems conceming the disposal of toxic hazardous wastes which have been dealt with in several research projects. The individual chapters are related scientifically. Long-term, effective solutions to our waste problems can only be found when interrelationships and possible future developments are considered. Only the current status of this rapidly developing field can be discussed here. The individual chapters contain scientifically founded data and observations. Other aspects for which there are still controversial opinions and arguments are also discussed, which should stimulate further thought. Further developments and scientific advances can only be achieved by constantly challenging previous theories, and not through static observation and narrow-mindedness. The most extensive quantification possible of the problems related to disposal of hazardous wastes is an essential aim of our work. This not only involves calculating the volume of waste and available repository space, but also compiling data on the long-term effects and the safe, long-term isolation of anthropogenic wastes from the biosphere. A simple description of conditions and processes without using concrete data, which is still widespread, is rejected since it frequently leads to pure speculation. The scientific fundamentals and results presented in this work are of general validity for many questions concerning waste disposal. One example is the amount of waste produced annually in Germany, in which toxic, hazardous wastes play a major role. FoIlowing this train of thought, available data are used to show how limited the possibilities are for the long-term safe underground deposition of hazardous wastes with respect to the current quantities of waste. Of utmost importance is information on the 10ng-term effects of toxic wastes, as well as criteria which have to be considered with respect to the long-term safe deposition of hazardous waste. The natural chemical cycles and material transport in the various zones of the earth are the focus of interest here. They are the scientific basis for assessing every repository for anthropogenic wastes in geological systems. Therefore the significance of material transport and geochemical cycles is emphasized regarding all questions concerning the long-term safety of repositories on the earth's surface and in the lithosphere. Thus, our concept for the scientific evaluation of the long-term safety of underground repositories in geological systems differs from all other models presently under discussion in Germany. In this work, marine evaporites are discussed with respect to the underground deposition of hazardous wastes and the long-term safety of underground repositories in salt rocks. The isolation of hazardous materials from the biosphere can above all be influenced by fluid phases. Fluid phases can mobilize and transport hazardous materials through rocks in the biosphere. This is true, without exception, for all magmatic, sedimentary, and metamorphic rocks, and for marine evaporites, too! In Germany evaporites have commonly been considered to be completely impermeable with respect to fluid phases (solutions and gases). This erroneous view stems from a complete lack of knowledge or misestimation of the dynamic evolution of the composition of evaporite bodies. Unfortunately, this is still true today for parts of some state agencies which deal with repositories. However, all observations of evaporite bodies made over the last more than 100 years have clearly shown that under certain conditions fluid and gaseous components are mobile in evaporites as well. Solutions in marine evaporites have been the object of personal interest and scientific research of A.G. Herrmann for 40 years. The occurrence and formation of salt solutions in the various salt mining districts of Germany are presently being restudied and reevaluated on an extended scientific basis (e.g., v. BORSTEL 1992). A presentation of the current knowledge on salt solutions is beyond the scope of this publication. However, in the interest of continuing research a research project proposed by A.G. Herrmann (1987b) will be introduced here. The direct quantitative analysis of the chemical composition (quatemary and quinary systems) of small fluid inclusions in rocks of the salt deposits of Hessen and Niedersachsen are the primary focus of this project. Information important to fundamental research on the formation and alteration of salt rocks and on the long-term safety of underground repositories should be gained from these studies (e.g., HERRMANN & v. BORSTEL 1991). In addition to salt solutions, gases are also fluid components which occur in practically all marine evaporite deposits. Hence, both salt solutions and gases must be carefully considered when planning underground repositories in an evaporite body and evaluating their long-term safety. This publication contains an up-to-date overview of the gas occurrences in the marine evaporites of Central Europe. Despite previous studies, there is still a considerable deficit in scientific information regarding the distribution and formation of gases in the evaporites occurring in Germany. A detailed research program on the geochemical relationships involving the formation of evaporites and gases will draw attention to this situation. One aspect must be emphasized in the planning and construction of repositories for anthropogenic wastes: their long-term safety. This publication deals precisely with this subject, and in Part III of this work we will present the concept that we have developed. This concept is based on the fact that evaporite bodies are subject to a dynamic evolution and that the chemical and mineralogical composition provides important information on the effect of fluid phases on salt rocks. Previous works contain the testing of methods and presented initial results using the Gorleben salt dome as an example. However, we are just at the beginning of our research project on the long-term safety of underground repositories (e.g., HERRMANN & KNIPPING 1989, HERRMANN 1992). The information contained in this publication is based on years of experience in evaporite research and underground repositories for anthropogenic wastes. Examples are presented which can be applied to similar situations and problems in other countries. Waste disposal is not just a national problem, it has long become an international one for all types of anthropogenic wastes...

Description / Table of Contents: Chapter 1. Primitive Solar Nebula --- Evolution of Magnetized Dense Clouds / T. Nakano, T. Nakamura, T. Terasawa, and Y. Sano / pp. 1-28 --- Molecular Outflows—Observational Signature for the Earliest Phase of Stellar Evolution— / Y. Fukui, A. Mizuno, H. Ogawa, and K. Kawabata / pp. 29-45 --- Observational Evidence of Transition between Protostellar Objects and T Tauri Stars / S. Sato / pp. 47-57 --- Jet Formation and Enhanced Accretion due to Magnetic Effects in Protostellar Objects / Y. Uchida / pp. 59-77 --- Shear Instability of the Solar Nebula / M. Sekiya, S. M. Miyama, and Y. Nakagawa / pp. 79-88 --- Magnetic Fossil of the Solar Nebula Observed in Meteorites / T. Nagata / pp. 89-103 --- Experimental Demonstration of Formations of Tetrataenite and Pyrrhotite / C. Kaito and Y. Saito / pp. 105-112 --- Synthesis of Carbonaceous and Siliceous Materials / A. Sakata and S. Wada / pp. 113-127 --- Chapter 2. Origin of Giant Planets --- Scenario of Formation Processes of the Giant Planets / H. Oya / pp. 129-134 --- Giant Planetary Systems—A Review— / H. Oya / pp. 135-193 --- Accumulation of Materials for the Formation of the Giant Planets—Ring Model under the Flow-out Motion of Disc Gas— / H. Oya / pp. 195-220 --- Nonlinear Evolution of the Accumulation Processes of the Material for Formation of the Giant Planets in the Primeval Solar System / H. Oya and M. Iizima / pp. 221-240 --- Simulation Studies on the Formation Processes of the Saturnian Ringlets / H. Oya, M. Miyauchi, T. Imai, and M. Iizima / pp. 241-164 --- Chapter 3. Origin of the Terrestrial Planets --- Elementary Processes in Planetary Accretion / K. Nakazawa, S. Ida, and K. Ohtsuki / pp. 265-280 --- Experimental Simulation of Collisions / A. Fujiwara, A. Nakamura, M. Kato, and Y. Takagi / pp. 281-295 --- Scaling Law on Impact Phenomena / H. Mizutani / pp. 297-317 --- Numerical Simulation of Planetary Growth / M. Hayakawa and H. Mizutani / pp. 319-340 --- Deformation of Porous Ice-Rock Mixtures and an Application to the Densification of Icy Satellites / N. Maeno, M. Arakawa, and J. Leliwa-Kopystynski / pp. 341-353 --- Chapter 4. Origin of Meteorites --- Precise Determination of the Age of Formation of Meteorites / K. Takahashi and A. Masuda / pp. 355-373 --- Chemical Differentiation during Collision and Accretion of Meteorite Parent Bodies / H. Takeda / pp. 375-394 --- Isotope Variations of Light Elements in Chondrites—Ion Microprobe Studies— / C. Uyeda, H. Nishimura, and J. Okano / pp. 395-408 --- Trace Element Fractionation during the Formation of Chondrules / N. Nakamura / pp. 409-425 --- Vaporization and Condensation of Chondritic Materials—Experimental Studies— / H. Nagahara, 1. Kushiro, and B. O. Mysen / pp. 427-446 --- Metamorphic Processes in New CI Carbonaceous Chondrites from Antarctica: Mineralogy and Petrology / K. Tomeoka / pp. 447-464 --- Evolution and Alteration Process of the CM Carbonaceous Chondrites / H. Kojima and K. Yanai / pp. 465-477 --- Structure and Chemistry of Carbon in Meteorites / T. Murae, H. Kagi, and A. Masuda / pp. 479-501 --- Chapter 5. Origin and Evolution of the Terrestrial Atmosphere --- 244Pu Fission Xe in the Mantle and Mantle Degassing Chronology / M. Ozima, S. Azuma, S. Zashu, and H. Hiyagon / pp. 503-517 --- The Noble Gases in the Venusian Atmosphere and the Fukutomi Chondrite / N. Takaoka / pp. 519-526 --- Formation of Atmospheres of Terrestrial Planets from Volatiles in Solid (Meteoritelike) Material / N. Sugiura / pp. 527-543 --- Early Evolution of the Terrestrial Planets: Accretion, Atmosphere Formation, and Thermal History / T. Matsui / pp. 545-559 --- Existence of Life and Creation of Atmospheric Environment / S. Moriyama / pp. 561-577 --- Chapter 6. Exploration of the Solar System—Halley Mission— --- Interaction of Plasma of Halley's Comet with the Solar Wind / H. Oya / pp. 579-614 --- Plasma Environment of Comet Hally Observed by Suisei / T. Terasawa and S. Takahashi / pp. 615-628 --- Modelling Study of the Cometary Ly α Brightness from a Time-varying H2O Source / O. Ashihara / pp. 629-643 --- Cometary Dust / T. Mukai / pp. 645-662 --- The Origin of Comets as Viewed from the Gaseous Composition / T. Yamamoto / pp. 663-677

Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains

Description / Table of Contents: Owing to the maturity of exploration in the North Sea Basin, reservoir geology will increasingly focus on the exploitation of smaller and technically more demanding hydrocarbon accumulations and the need to maximize reserves from the established producing fields. More refined geological reservoir interpretation and modelling are therefore required. This book details new methods, and the improved use of existing methods in such areas as sequence stratigraphy, petrography, sedimentology, inorganic geochemistry, production logging, quantitative image analysis of pore structure, the dipmeter tool and permeability imaging; and the integration of data from a variety of these sources, including outcrop-derived data.