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Carlos Rodriguez-Navarro

Researcher at University of Granada

Publications -  115
Citations -  8623

Carlos Rodriguez-Navarro is an academic researcher from University of Granada. The author has contributed to research in topics: Calcite & Crystallization. The author has an hindex of 49, co-authored 109 publications receiving 7244 citations. Previous affiliations of Carlos Rodriguez-Navarro include Getty Conservation Institute.

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Salt weathering: influence of evaporation rate, supersaturation and crystallization pattern

TL;DR: In this paper, it was shown that salt damage due to crystallization pressure appears to be largely a function of solution supersaturation ratio and location of crystallization, which are constrained by solution composition, environmental conditions, substrate properties, and salt crystallization growth patterns.
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Carbonate and silicate phase reactions during ceramic firing

TL;DR: In this article, a detailed analysis of clay-rich materials following firing is presented, showing that initial mineralogical differences between two raw materials (one with carbonates and the other without) influence the texture and mineralogical evolution of the ceramics as T increases from 700 to 1100°C.
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Conservation of ornamental stone by Myxococcus xanthus-induced carbonate biomineralization.

TL;DR: It is reported that Myxococcus xanthus-induced calcium carbonate precipitation efficiently protects and consolidates porous ornamental limestone and forms new carbonate crystals that are more stress resistant than the calcite grains of the original stone.
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How does sodium sulfate crystallize? Implications for the decay and testing of building materials

TL;DR: In this paper, it was shown that both thenardite and mirabilite (Na2SO4·10H2O) precipitate directly from a saturated sodium sulfate solution at room temperature (20°C).
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Thermal decomposition of calcite: Mechanisms of formation and textural evolution of CaO nanocrystals

TL;DR: In this paper, a model for the thermal decomposition of calcite was proposed to explain how decarbonation occurs at the atomic scale via a topotactic mechanism, which is independent of the experimental conditions.