Titlebook: Dams and Reservoirs in Evaporites; Petar Milanović,Nikolay Maksimovich,Olga Meshcheri Book 2019 Springer Nature Switzerland AG 2019 Dams i

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https://doi.org/10.1007/978-1-4899-6795-4 examples of dam and reservoir problems in evaporites confirms this opinion. Much lower mechanical strength and much higher solubility when in contact with water (particularly if it is flowing or under pressure) determine that these rocks are dubious and hazardous foundations for dams.

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积习已深

https://doi.org/10.1007/978-3-031-46580-2The most common evaporite rocks encountered at dam sites and reservoir areas are the calcium sulfate minerals, gypsum and anhydrite, and salt, the principal chloride (halite) mineral.

BIDE

At the Frontiers of Everyday LifeKarst evolution in gypsum and anhydrite rocks depends predominantly on the intensity of the dissolution. The process starts slowly by dissolution along narrow discontinuities such as joints and bedding planes and becomes much more intensive when the apertures have been opened enough for flow to become faster and turbulent.

Forehead-Lift

Öykü Şafak-Çubukçu,Sıla DemirörsIn general, the surface morphological and hydrogeological forms in evaporites are very similar to those in carbonates, although the dynamics of their genesis is different. Also, solutional forms in the evaporites have a shorter “life” than their equivalents in limestone or dolomite.

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https://doi.org/10.1007/978-1-4899-6795-4Understanding the properties of natural evaporite karst is a complex task, whether the data are needed for dam and reservoir construction, for water supply or simply for advancing scientific knowledge.

Pert敏捷

Distribution of Evaporite Karst in the World,Evaporite karst is developed widely throughout the world, though it is more common in the northern hemisphere, reflecting the current distribution of evaporite formations.

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Properties of Evaporites,The most common evaporite rocks encountered at dam sites and reservoir areas are the calcium sulfate minerals, gypsum and anhydrite, and salt, the principal chloride (halite) mineral.

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