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Authordc.contributor.authorCaraballo Monge, Manuel 
Authordc.contributor.authorMichel, F. Marc 
Authordc.contributor.authorHochella, Michael 
Admission datedc.date.accessioned2015-09-08T18:29:11Z
Available datedc.date.available2015-09-08T18:29:11Z
Publication datedc.date.issued2015
Cita de ítemdc.identifier.citationAmerican Mineralogist, Volume 100, pages 14–25, 2015en_US
Identifierdc.identifier.otherDOI: 10.2138/am-2015-4749
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/133488
General notedc.descriptionArtículo de publicación ISIen_US
Abstractdc.description.abstractEnvironmental mineralogy is rapidly expanding in technological directions that allow for the detection, characterization, and understanding of non-crystalline and poorly crystalline phases, crystalline-amorphous mixed phases, and nanosized naturally occurring materials. Specifically, this article provides a perspective view of the broad range of structural complexity/heterogeneity observed in environmental minerals and amorphous materials, as well as our current understanding of how these materials can be best observed, evaluated, and described, and why this is important in the mineralogical sciences. The discussion is broken down into the assessment of short-and medium-range order in amorphous materials, and the nature of nanominerals and mineral nanoparticles, amorphous-nanocrystalline transitional phases, and mesocrystals. These materials do not fit one or more aspects of the most commonly used definitions of a mineral (although some of them are formally recognized as minerals, such as ferrihydrite and schwertmannite), yet they do fit other portions of these current definitions. Nevertheless, because these phases can be exceptionally minute in size, and/or not highly crystalline, and/or generally much less abundant than other mineral components in the system, they may be underappreciated and/or understudied, or, apparently as is often the case, completely missed. Yet they are often highly relevant to, and in many cases dominant in, important aspects of how the (bio)geochemistry of an environmental system operates. Furthermore, although it is important to analytically and experimentally characterize synthetic equivalent phases in the laboratory, often under conditions intended to mimic one or a few aspects of the real environment, we argue that it is imperative to study natural, intact (as much as possible) samples and make field measurements with much greater frequency than is currently practiced.en_US
Patrocinadordc.description.sponsorshipSpanish Ministry of Education; Post-doctoral International Mobility Sub-program I+D+i; U.S. Department of Energy DE-FG02-06ER15786; Institute for Critical Technology and Applied Sciences at Virginia Tech; National Science Foundation (NSF); Environmental Protection Agency through the Center for Environmental Implications of NanoTechnology (CEINT) - NSF EF-0830093en_US
Lenguagedc.language.isoen_USen_US
Publisherdc.publisherMineralogical Soc Ameren_US
Type of licensedc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
Keywordsdc.subjectEnvironmental mineralogyen_US
Keywordsdc.subjectSynchrotron radiationen_US
Keywordsdc.subjectFree electron laseren_US
Keywordsdc.subjectTransmission electron microscopyen_US
Keywordsdc.subjectNanomineralen_US
Keywordsdc.subjectMineral nanoparticleen_US
Keywordsdc.subjectPolyphasic nanomineralen_US
Keywordsdc.subjectPrenucleation clusteren_US
Keywordsdc.subjectNon-classical crystallizationen_US
Keywordsdc.subjectMesocrystalen_US
Títulodc.titleThe rapid expansion of environmental mineralogy in unconventional ways: Beyond the accepted definition of a mineral, the latest technology, and using nature as our guideen_US
Document typedc.typeArtículo de revista


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Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 Chile