Mineral Dissolution Kinetics: New Perspectives
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A01=Jim E Greenwood
A01=Tim G Southern
A01=Victor W Truesdale
AB Salt
ABC Salt
Activation Complex
Albite
Alkalinity
Alpha Functions
Aluminate
Analytic Integral
Author_Jim E Greenwood
Author_Tim G Southern
Author_Victor W Truesdale
Bolas Equation
Bolas(1st)
Bolas(2nd)
Calcareous Sediment Dissolution
Calcite Gypsum
Calcium Carbonate
Calcium Fluoride
Cape Verde Plateau
Carbonate Alkalinity
Carbonate Thermodynamics
Category=PNC
Category=PNV
Chemical Control
Chemo-Stat
Common Ion Effect
Complex Reaction
Differential Equation Approach
Diffusion Limited
Diffusivity
Disciplinal Differences
Dissolution
Dissolution Kinetics
Elementary Reaction
eq_bestseller
eq_isMigrated=1
eq_isMigrated=2
eq_nobargain
eq_non-fiction
eq_science
Finite-Difference Method
First Order Back Reaction
Fluorite
Free Energy Diagram
Gypsum
Hydrodynamic Boundary Layer
Hydrodynamics
Initial Rates
Ion-Exchange
Kinetic Aggregate
Kinetics Modelling
Labradorite
Laminar Flow
Mineral Dissolution Kinetics
Nernst Layer
Phenomenology
PWP Equation
Rate Determining
Rate Equation
Sanidine
Second Order Back Reaction
Sierra Leone Rise
Sigmoidal Plot
Sigmoids
Spinning Cylinder Reactor
Spinning Disc Reactor
Standard Integral
Stirred Reactor
Stirring Rate
Stoichiometric Dissolution
Surface Morphology
Templating
Titration Theory
Transition State Theory
Transport Control
Turbulent Flow
Weathering Sequence
Zeolite
Product details
- ISBN 9781800616691
- Publication Date: 20 Jun 2025
- Publisher: World Scientific Europe Ltd
- Publication City/Country: GB
- Product Form: Hardback
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Mineral Dissolution Kinetics: New Perspectives is, at its core, a search for a universal rate equation for mineral dissolutions. It documents and details the journey undertaken by its authors, appealing not only to specialists and experts in related fields but also to novice readers seeking to learn more about this unique subject. The book reveals how the compounding of many otherwise subtle misunderstandings has resulted in the under-development of fundamental concepts in mineral dissolution kinetics, despite its long history of study. By examining a wide cross-section of existing studies, it uncovers these misunderstandings and forges a new way forward.Although mineral dissolution kinetics has been immensely important in explaining continental weathering, landform development, and the maintenance of water supplies for agricultural and human use, it remains a critically undervalued field of chemistry. It is also foundational to our understanding of the marine environment and serves as an essential tool in the long-term storage of CO2 and radionuclide waste. More recently, it has helped address the human-induced rise in tropospheric CO2, a key cause of global warming and ocean acidification.Complex subjects such as the hydrodynamics of dissolution, the thermodynamics of the aqueous carbonate system, and central omissions at the very core of homogeneous kinetics are explained clearly and simply, while still remaining at the cutting edge of the field.
