Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico

Calcium sulfate (CaSO<sub>4</sub>) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO<sub>4</sub>∙2H<sub>2</sub>O), bassanite (CaSO<sub>4</sub>∙0.5H<sub>2</sub>O), soluble...

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Main Authors: Iván Jalil Antón Carreño-Márquez, Isaí Castillo-Sandoval, Bernardo Enrique Pérez-Cázares, Luis Edmundo Fuentes-Cobas, Hilda Esperanza Esparza-Ponce, Esperanza Menéndez-Méndez, María Elena Fuentes-Montero, María Elena Montero-Cabrera
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/3/292
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author Iván Jalil Antón Carreño-Márquez
Isaí Castillo-Sandoval
Bernardo Enrique Pérez-Cázares
Luis Edmundo Fuentes-Cobas
Hilda Esperanza Esparza-Ponce
Esperanza Menéndez-Méndez
María Elena Fuentes-Montero
María Elena Montero-Cabrera
author_facet Iván Jalil Antón Carreño-Márquez
Isaí Castillo-Sandoval
Bernardo Enrique Pérez-Cázares
Luis Edmundo Fuentes-Cobas
Hilda Esperanza Esparza-Ponce
Esperanza Menéndez-Méndez
María Elena Fuentes-Montero
María Elena Montero-Cabrera
author_sort Iván Jalil Antón Carreño-Márquez
collection DOAJ
description Calcium sulfate (CaSO<sub>4</sub>) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO<sub>4</sub>∙2H<sub>2</sub>O), bassanite (CaSO<sub>4</sub>∙0.5H<sub>2</sub>O), soluble anhydrite, and insoluble anhydrite (CaSO<sub>4</sub>), being the key difference the hydration state of the sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow up to 11–12 m long. The growth rates are reported to be as slow as (1.4 ± 0.2) × 10<sup>−5</sup> nm/s, taking thousands of years to form crystals with a unique smoothness and diaphaneity, which may or may not include solid or liquid inclusions. Conservation efforts can be traced back to other gypsum structures found prior to Naica’s. Furthermore, in the last two decades, several authors have explored the unique requirements in which these crystals grow, the characterization of their environment and microclimatic conditions, and the prediction of deterioration scenarios. We present a state-of-the-art review on the mentioned topics. Beyond the findings on the origin, in this work we present the current state and the foreseeable future of these astounding crystals.
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spelling doaj.art-ba7627ce07aa4ff19a1ba80d2fd830252023-11-21T10:02:47ZengMDPI AGMinerals2075-163X2021-03-0111329210.3390/min11030292Evolution of the Astonishing Naica Giant Crystals in Chihuahua, MexicoIván Jalil Antón Carreño-Márquez0Isaí Castillo-Sandoval1Bernardo Enrique Pérez-Cázares2Luis Edmundo Fuentes-Cobas3Hilda Esperanza Esparza-Ponce4Esperanza Menéndez-Méndez5María Elena Fuentes-Montero6María Elena Montero-Cabrera7Department of Engineering, Universidad La Salle Chihuahua, Chihuahua 31625, MexicoDepartment of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, MexicoDepartment of Computational Chemistry, Universidad Autónoma de Chihuahua, Chihuahua 31125, MexicoDepartment of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, MexicoDepartment of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, MexicoDepartment Physicochemical Assays, Instituto Eduardo Torroja de Ciencias de la Construcción, 28033 Madrid, SpainDepartment of Computational Chemistry, Universidad Autónoma de Chihuahua, Chihuahua 31125, MexicoDepartment of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, MexicoCalcium sulfate (CaSO<sub>4</sub>) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO<sub>4</sub>∙2H<sub>2</sub>O), bassanite (CaSO<sub>4</sub>∙0.5H<sub>2</sub>O), soluble anhydrite, and insoluble anhydrite (CaSO<sub>4</sub>), being the key difference the hydration state of the sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow up to 11–12 m long. The growth rates are reported to be as slow as (1.4 ± 0.2) × 10<sup>−5</sup> nm/s, taking thousands of years to form crystals with a unique smoothness and diaphaneity, which may or may not include solid or liquid inclusions. Conservation efforts can be traced back to other gypsum structures found prior to Naica’s. Furthermore, in the last two decades, several authors have explored the unique requirements in which these crystals grow, the characterization of their environment and microclimatic conditions, and the prediction of deterioration scenarios. We present a state-of-the-art review on the mentioned topics. Beyond the findings on the origin, in this work we present the current state and the foreseeable future of these astounding crystals.https://www.mdpi.com/2075-163X/11/3/292Naicagypsumgiant crystalsnucleation
spellingShingle Iván Jalil Antón Carreño-Márquez
Isaí Castillo-Sandoval
Bernardo Enrique Pérez-Cázares
Luis Edmundo Fuentes-Cobas
Hilda Esperanza Esparza-Ponce
Esperanza Menéndez-Méndez
María Elena Fuentes-Montero
María Elena Montero-Cabrera
Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
Minerals
Naica
gypsum
giant crystals
nucleation
title Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
title_full Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
title_fullStr Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
title_full_unstemmed Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
title_short Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
title_sort evolution of the astonishing naica giant crystals in chihuahua mexico
topic Naica
gypsum
giant crystals
nucleation
url https://www.mdpi.com/2075-163X/11/3/292
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