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all geography including DSDP/ODP Sites and Legs
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Historic Concrete Science: Opus Caementicium to “Natural Cements”
RELATING THE CATION EXCHANGE PROPERTIES OF THE BOOM CLAY (BELGIUM) TO MINERALOGY AND PORE-WATER CHEMISTRY
Clay mineralogical constraints on weathering in response to early Eocene hyperthermal events in the Bighorn Basin, Wyoming (Western Interior, USA)
Susceptibility of mineral phases of steel slags towards carbonation: mineralogical, morphological and chemical assessment
Lessons from a lost technology: The secrets of Roman concrete
Supplementary Cementitious Materials
Raw materials used in ancient mortars from the Cathedral of Notre-Dame in Tournai (Belgium)
The pozzolanic reaction between clinoptilolite and portlandite: a time and spatially resolved IR study
Portland Cement and other Calcareous Hydraulic Binders: History, Production and Mineralogy
Abstract Portland cement has become a cornerstone of modern society and the present-day cement and concrete industry is one of the largest consumers of industrial minerals. The historical evolution of early calcareous hydraulic binders into the present standard Portland cement is a typical example of a product-performance-optimization process driven by the gradual accumulation of empirical know-how and fundamental process understanding. The early observation that a hydraulic binder may be formed when impure limestone is burnt at temperatures above the decomposition temperature of limestone led to the development of a wide range of early hydraulic binders throughout the 18th and 19th centuries. Initially, burning at relatively low temperatures (1000– 11008C) of impure limestone resulted in the production of fast-setting natural cements and hydraulic limes. Eventually, over the course of the 19th and 20th centuries, sintering at increasingly higher burning temperatures of natural impure limestones and artificial mixes of ground limestone and clay was introduced to produce slow-setting natural cement and finally (proto-)Portland cement with superior strength development. Today, the Portland cement-production process consists of an energy-intensive, high-temperature sintering phase (14508C) of the raw materials, followed by fast cooling and fine intergrinding of the clinker product with gypsum to produce the Portland cement. The mineralogy of the clinker phases is relatively complex. C 3 S and C 2 S show several high- and low-temperature polymorphs, whereas C 3 A and C 4 AF allow considerable compositional solid solution. The addition of water to Portland cement initiates a complex scheme of hydration reactions to form a hardened cement paste. The advent of novel analytical techniques prompted recent advances in the understanding of the structures of the hydration products and the hydration mechanism. Nevertheless many aspects of the hydration reactions remain unsolved. The necessary future developments towards less energy intensive, low-CO 2 cements may take advantage of the historical knowledge acquired in the production of a wide range of alternative hydraulic binders.