Physical Principles of Sedimentology is a textbook devoted to the physics of sedimentological processes. The applicability of fundamental principles, such as Newton's Three Laws of Motion, Law of Conservation of Energy, First and Second Laws of Thermodynamics, and of other physical relations in hydraulics and groundwater hydrology is illustrated by discussions of natural processes which form sediments or sedimentary rocks. The author's educational background as a major in physics and geology, and his 40-year experience in teaching and research help him bring together physics and geology in this enjoyable and highly readable form.

apparatus is generally not required for the making of My aim in this book is simple. It is to set out in a logical useful sedimentological experiments. Most of the equip way what I believe is the minimum that the senior undergraduate and beginning postgraduate student in ment needed for those I describe can be found in the kit the Earth sciences should nowadays know of general chen, bathroom or general laboratory , and the materials most often required - sand, clay and flow-marking physics, in order to be able to understand (rather than form merely a descriptive knowledge of) the smaller substances - are cheaply and widely available. As described, the experiments are for the most part purely scale mechanically formed features of detrital sedi ments. In a sense, this new book is a second edition of qualitative, but many can with only little modification my earlier Physical processes of sedimentation (1970), be made the subject of a rewarding quantitative exer which continues to attract readers and purchasers, inas cise. The reader is urged to tryout these experiments much as time has not caused me to change significantly and to think up additional ones. Experimentation the essence of my philosophy about the subject. Time should be as natural an activity and mode of enquiry for has, however, brought many welcome new practitioners a physical sedimentologist as the wielding of spade and hammer.

This textbook explains sedimentological processes via the fundamental physics that underlies the actual mechanisms involved. Demonstrates the applicability of fundamental principles, such as Newton's Three Laws of Motion, the Law of Conservation of Energy, the First and Second Laws of Thermodynamics, and of other physical relations in hydraulics and groundwater hydrology by discussions of natural processes which form sediments and sedimentary rocks. In this second edition several chapters have been updated and amended to reflect progress in the field

Physical Principles of Sedimentology is a textbook devoted to the physics of sedimentological processes. The applicability of fundamental principles, such as Newton's Three Laws of Motion, Law of Conservation of Energy, First and Second Laws of Thermodynamics, and of other physical relations in hydraulics and groundwater hydrology is illustrated by discussions of natural processes which form sediments or sedimentary rocks. The author's educational background as a major in physics and geology, and his 40-year experience in teaching and research help him bring together physics and geology in this enjoyable and highly readable form.

A user-friendly, thorough introduction to quantitative modelling of sedimentary basins, illustrated throughout with real-world examples, applications and test exercises.

Review of physical chemistry. Ion activities in natural waters. Calcium carbonate chemistry in surface waters. Evaporite formation. Diagenetic processes. Diagenetic redox reactions in the system C-N-S-H-O. Diagenesis of Ca-Mg carbonates. Formation and alteration of silica and clay minerals. Diagenesis of iron minerals.

apparatus is generally not required for the making of My aim in this book is simple. It is to set out in a logical useful sedimentological experiments. Most of the equip way what I believe is the minimum that the senior ment needed for those I describe can be found in the kit undergraduate and beginning postgraduate student in the Earth sciences should nowadays know of general chen, bathroom or general laboratory , and the materials most often required - sand, clay and flow-marking physics, in order to be able to understand (rather than substances - are cheaply and widely available. As form merely a descriptive knowledge of) the smaller described, the experiments are for the most part purely scale mechanically formed features of detrital sedi ments. In a sense, this new book is a second edition of qualitative, but many can with only little modification my earlier Physical processes oj sedimentation (1970), be made the subject of a rewarding quantitative exer which continues to attract readers and purchasers, inas cise. The reader is urged to tryout these experiments much as time has not caused me to change significantly and to think up additional ones. Experimentation the essence of my philosophy about the subject. Time should be as natural an activity and mode of enquiry for has, however, brought many welcome new practitioners a physical sedimentologist as the wielding of spade and to the discipline of sedimentology, thrown up a hammer.