یادداشتهای مربوط به کتابنامه ، واژه نامه و نمایه های داخل اثر
متن يادداشت
Includes bibliographical references and index.
یادداشتهای مربوط به مندرجات
متن يادداشت
Intro; Preface; Curriculum vitae; Contents; Preparatory Aspects of the Methodology of Analysis; 1 Genesis and Structures of Cohesive Soils; 1.1 Introduction; 1.2 Mineralogic Composition of Clays; 1.3 Electrostatic Characteristics of Clays; 1.4 Genesis of Clayey Soils; References; 2 Causes of Lanslides in Cohesive Soils; 2.1 Introduction; 2.2 The Principle of Effective Stresses; 2.3 Equilibrium Conditions; 2.3.1 Passive Thrust; 2.3.2 Active Thrust; 2.4 The Failure Process (from Bles and Feuga 1981); 2.4.1 Failure of Rocks Under Tension; 2.4.2 Failure of Rocks Under Compression.
متن يادداشت
2.5 The Influence of Pore-Water PressureReferences; 3 The Dating of Landslides; 3.1 Introduction; 3.2 General Overview of Quaternary Subdivisions in Marine Environment; 3.3 Chronostratigraphic Evaluations of Landslide Units; 3.4 Analytical Procedure for the Chronological Evaluation of Pre-Existing Landslides by Means of Tables 3.1 and 3.2-Example Referring to Würm; 3.5 The Importance of a Correct Site Analysis; References; 4 The Pre-failure Deformation; 4.1 Introduction; 4.2 Development of Cracks Under Compression; 4.3 Analysis of Brittle Deformation.
متن يادداشت
4.4 Definition and Description of the Various Types of Fractures4.4.1 Diaclases and Joints; 4.4.2 Extension Fractures (Fentes); 4.4.3 Faults; 4.5 Interpretation of the Mechanisms of Fractures Formation; 4.5.1 Introduction; 4.5.2 Formation of Diaclases and Joints; 4.5.3 Formation of Extension Fractures and Fentes; 4.5.4 Formation of Faults; 4.6 The Stress Field; 4.6.1 Identification of the Stress Field; 4.6.2 Stress Field in a Continuous Medium; 4.6.3 Stress Field in a Discontinuous Medium; 4.6.4 Method of the Minimum Dihedral (or Quick Method); 4.7 The Analysis Process; References.
متن يادداشت
6.4 The North-Eastern Slope of Tricarico6.4.1 Location; 6.4.2 Lithology of the Slope; 6.4.3 Morphological Processes in Place; 6.4.4 Instrumental Monitoring; 6.4.5 Discussion; 6.5 Hydraulic Conductivity and Hydraulic Potential at Failure; References; 7 Landslides Types and Their Failure Mechanisms; 7.1 Introduction; 7.2 Monotype Landslides; 7.3 Composite Landslides; 7.4 The Great Ancona Landslide; 7.4.1 Chronicle Notes (from Carciofi 1983); 7.4.2 Summary of Damages (from Carciofi 1983); 7.4.3 Geological-Structural Framework of the Landslide; 7.4.4 Morphological Aspects of the Slope.
متن يادداشت
Methodological and Analytical Aspects5 The Dynamics of Disruptions; 5.1 Introduction; 5.2 Dynamics of Recent Landslides; 5.2.1 First Environment; 5.2.2 Second Environment; 5.2.3 Third Environment; 5.3 Pre-existing Landslides; 5.3.1 Relation Between Stress and Strain; 5.3.2 Causes of Deformation at Failure; 5.3.3 Reactivation of Pre-existing Landslides; References; 6 The Role of the Coefficient of Permeability K; 6.1 Introduction; 6.2 The Effect of Ground Anisotropy on Permeability; 6.3 Consequence of Slopes Erosion on the Variations of the Coefficient of Permeability K.
بدون عنوان
0
بدون عنوان
8
بدون عنوان
8
بدون عنوان
8
بدون عنوان
8
یادداشتهای مربوط به خلاصه یا چکیده
متن يادداشت
This book discusses techniques for predicting, preventing and controlling the hydrogeological instability of slopes consisting of cohesive soils. The proposed methodology is practical and innovative, and assumes a dynamic valence in defining the deformation process of underground failure as well as its activation through the assumption of a four-dimensional space-time continuum. This latter aspect is crucial for predicting a landslide in time to control it. At present, predicting, preventing and controlling hydrogeological instability in cohesive soils relies on mathematical modelling using specific software, the predictive reliability of which is rather deficient. Such modelling is based upon deterministic processes, which are entirely unsuitable for dealing with the complexity of vital processes occurring during the genesis of a landslide. In this work, the three-dimensional vision of a landslide as a set of distinct and independent phenomena is abandoned and the prediction and prevention of hydrogeological instability is pursued through the alternative of an indivisible totality of natural phenomena that includes the time factor. The book is of interest to graduates and researchers of applied geology, geotechnical, environmental and civil engineering, as well as professionals in the fields of hydrogeology and natural hazards.
یادداشتهای مربوط به سفارشات
منبع سفارش / آدرس اشتراک
Springer Nature
شماره انبار
com.springer.onix.9783319743318
ویراست دیگر از اثر در قالب دیگر رسانه
عنوان
Hydrogeological instability in cohesive soils.
شماره استاندارد بين المللي کتاب و موسيقي
9783319743301
موضوع (اسم عام یاعبارت اسمی عام)
موضوع مستند نشده
Landslide hazard analysis.
موضوع مستند نشده
Landslides.
موضوع مستند نشده
Scour (Hydraulic engineering)
موضوع مستند نشده
Soil mechanics.
موضوع مستند نشده
Economic geology.
موضوع مستند نشده
Environmental monitoring.
موضوع مستند نشده
Hydrology & the hydrosphere.
موضوع مستند نشده
Landslide hazard analysis.
موضوع مستند نشده
Landslides.
موضوع مستند نشده
Meteorology & climatology.
موضوع مستند نشده
Natural disasters.
موضوع مستند نشده
Scour (Hydraulic engineering)
موضوع مستند نشده
Soil mechanics.
موضوع مستند نشده
TECHNOLOGY & ENGINEERING-- Civil-- General.
مقوله موضوعی
موضوع مستند نشده
RB
موضوع مستند نشده
TEC-- 009020
رده بندی ديویی
شماره
624
.
151363
ويراست
23
رده بندی کنگره
شماره رده
TA710
نام شخص به منزله سر شناسه - (مسئولیت معنوی درجه اول )