Introduction to Anatomy and Physiology is a brand new, beautifully illustrated anatomy and physiology textbook program written and designed for high school students. The text includes thorough, accurate coverage of all the body systems in an inviting, accessible format that chunks chapter information into manageable lessons for the beginning anatomy and physiology student. An abundance of study aids, such as learning objectives, lesson summaries, vocabulary-building exercises, hands-on activities, real-world applications, and extensive assessment opportunities increase students' ability to succeed in this challenging course. An outstanding supplement package that includes a robust companion website, ExamView Assessment Suite CD, PowerPoint lecture slides, detailed lesson plans, and a variety of enrichment labs and activities, will minimize your preparation time.
The combustion of fossil fuels remains a key technology for the foreseeable future. It is therefore important that we understand the mechanisms of combustion and, in particular, the role of turbulence within this process. Combustion always takes place within a turbulent flow field for two reasons: turbulence increases the mixing process and enhances combustion, but at the same time combustion releases heat which generates flow instability through buoyancy, thus enhancing the transition to turbulence. The four chapters of this book present a thorough introduction to the field of turbulent combustion. After an overview of modeling approaches, the three remaining chapters consider the three distinct cases of premixed, non-premixed, and partially premixed combustion, respectively. This book will be of value to researchers and students of engineering and applied mathematics by demonstrating the current theories of turbulent combustion within a unified presentation of the field.
Clay minerals form in a wide variety of crustal environments, e.g. in soil profiles, in sediments at the surface and in deeply buried sedimentary deposits, and under regional, contact and hydrothermal metamorphism conditions. The book provides information about the dynamics of isotope systems in clays and helps us to understand the physical and chemical parameters in the transfer of masses within the crustal domain. Written for graduate students taking courses in sedimentary geochemistry, clay mineralogy, and soil mineralogy, the book will also appeal to scientists carrying out research on clay genesis and mass transfer in crustal environments.
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