Two companies are involved in the industrial extraction and processing of gellant-grade attapulgite clay within the same Attapulgus deposit: Active Minerals International, LLC, and BASF Corp. In 2008, BASF acquired the assets of Zemex Attapulgite, leaving only two gellant-grade producers. Active Minerals operates a dedicated factory to produce the patented product Actigel 208 and built a new state-of-the-art production process in early 2009 involving portable plant processing at the mine site.[11]
Attapulgite clays are a composite of smectite and palygorskite. Smectites are expanding lattice clays, of which bentonite is a commonly known generic name for smectite clays. The palygorskite component is an acicular bristle-like crystalline form that does not swell or expand. Attapulgite forms gel structures in fresh and salt water by establishing a lattice structure of particles connected through hydrogen bonds.
Attapulgite, unlike some bentonite (sodium-rich montmorillonites), can gel in seawater,[12] forming gel structures in salt water and is used in special saltwater drilling mud for drilling formations contaminated with salt. Palygorskite particles can be considered as charged particles with zones of positive and negative charges. The bonding of these alternating charges allows them to form gel suspensions in salt and fresh water.
Studies thus far on the possibility of Palygorskite being a carcinogen has been mixed. Some studies show that cytotoxicity in rats, mice, livestock, hamsters, and even humans have caused malignant mesothelioma. In rats specifically, studies have ranged from 2.5-94% mesothelioma rates. Differences in palygorskite fiber length and purity (i.e., presence of other carcinogenic mineral fibers) may have been responsible for the disparate results observed in those experiments.[16]
Specifically in Nevada, there is a strong link between Palygorskite and mesothelioma. In 2011, medical Geologist Brenda Buck of The University of Nevada Las Vegas (UNLV) was looking for arsenic minerals in Nellis Dunes. What she found was fibrous Palgorskite in her sample.[17] Further research found that more women and children than men had higher rates of malignant mesothelioma; with the ratio being as high as 3:1. Palygorskite samples were taken from 4 different locations in southern Nevada, and scanned by electron microscopy (SEM). The results showed that Palygorskite fibrous physical features similar to those of asbestos minerals.[16][18]
Until 2003, Kaopectate marketed in the US also contained attapulgite. However, at that time, the U.S. Food and Drug Administration retroactively rejected medical studies showing its efficacy, calling them insufficient.[20][21] The manufacturer also settled with the State of California over toxic levels of lead in the attapulgite component. Part of this settlement was a reformulation to remove attapulgite in the liquid version in the US.[22]
Kaopectate's U.S. formula was changed to bismuth subsalicylate (pink bismuth). The next year (2004), an additional change in labeling was made; from then on, Kaopectate was no longer recommended for children under 12 years old.[23] Nevertheless, Kaopectate with attapulgite is still available in Canada and elsewhere. Until the early 1990s, Kaopectate used the similar clay product kaolinite with pectin (hence the name).
Construction
Palygorskite can be added to lime mortar with metakaolin for period-correct restoration of mortar at cultural heritage sites.[24]
In human culture
Palygorskite is known to have been a key constituent of the pigment called Maya blue, which was used notably by the pre-ColumbianMaya civilization of Mesoamerica on ceramics, sculptures, murals, and (most probably) Maya textiles. The clay mineral was also used by the Maya as a curative for certain illnesses, and evidence shows it was also added to pottery temper.
A Maya region source for palygorskite was unknown until the 1960s, when one was found at a cenote on the Yucatán Peninsula near the modern township of Sacalum, Yucatán. A second possible site was more recently (2005) identified, near Ticul, Yucatán.[25]
The Maya blue synthetic pigment was also manufactured in other Mesoamerican regions and used by other Mesoamerican cultures, such as the Aztecs of central Mexico. The blue coloration seen on Maya and Aztec codices, and early colonial-era manuscripts and maps, is largely produced by the organic-inorganic mixture of añil leaves and palygorskite, with smaller amounts of other mineral additives.[26] Human sacrificial victims in postclassic Mesoamerica were frequently daubed with this blue pigmentation.[27]
12"Palygorskite (Mg,Al)2 Si4 O10 (OH).4H2O"(PDF). handbookofmineralogy.com. Mineral Data Publishing, version 1.2. 2001. Archived from the original(PDF) on 1 May 2022. Retrieved 29 August 2024. Palygorskite in the Handbook of Mineralogy.
↑Belluso, E.; Cavallo, A; Halterman, D. (January 2017). Gualtieri, A.F. (ed.). Crystal habit of mineral fibres. European Mineralogy Union. pp.65–109. Retrieved 29 November 2025.
↑Andrejkovičová, S.; Velosa, A.; Gameiro, A.; Ferraz, E.; Rocha, F. (2013). "Palygorskite as an admixture to air lime–metakaolin mortars for restoration purposes". Applied Clay Science. 83–84: 368–374. Bibcode:2013ApCS...83..368A. doi:10.1016/j.clay.2013.07.020.
Arnold, Dean E. (2005). "Maya Blue and Palygorskite: A second possible pre-Columbian source". Ancient Mesoamerica. 16 (1): 51–62. doi:10.1017/S0956536105050078. ISSN0956-5361. JSTOR26309393. OCLC9977998608. S2CID162864157. Maya Blue is an unusual blue pigment used on pottery, sculpture, and murals from the Preclassic to the Colonial period. Until the late 1960s, its composition was unknown, but chemists working in Spain, Belgium, Mexico, and the United States identified Maya Blue as a combination of indigo and the unusual clay mineral palygorskite (also called attapulgite).
Garcia-Rivas, Javier; Sánchez del Río, Manuel; García-Romero, Emilia; Suárez, Mercedes (2017). "An insight in the structure of a palygorskite from Palygorskaja: Some questions on the standard model". Applied Clay Science. 148: 39–47. Bibcode:2017ApCS..148...39G. doi:10.1016/j.clay.2017.08.006. ISSN0169-1317. OCLC7121090747. This palygorskite is consistent with a purely orthorhombic palygorskite, based on good agreement of data with simulations.
Wiersma, J. (1970). Provenance, genesis and paleogeographical implications of microminerals occurring in sedimentary rocks of the Jordan Valley area (PhD thesis). Publicaties van het Fysisch Geografisch en Bodemkundig Laboratorium van de Universiteit van Amsterdam. University of Amsterdam. hdl:11245.1/9c960a65-cab0-44de-9e20-9deae0260fe3. OCLC898805873.
Further reading
Callen, Roger E. (1984). "Clays of the Palygorskite-Sepiolite Group: Depositional Environment, Age and Distribution". In Singer, A.; Galan, E. (eds.). Palygorskite — Sepiolite: Occurrences, Genesis and Uses. Developments in Sedimentology. Vol.37. Amsterdam, New York: Elsevier. pp.1–37. doi:10.1016/S0070-4571(08)70027-X. ISBN978-0-444-42337-5. OCLC10606245.
Kazakov, Alexander Vasilievich (1911). "Материалы к изучению группы палыгорскита" [Materials to the study of the palygorskite group]. Изв. ИАН (Izvestiia Imperatorsko Akademii Nauk, Bulletin of the Imperial Academy of Sciences. 6. 5 (9). Saint Petersburg: 679–694. OCLC212413675.
Weaver, Charles E.; Pollard, Lin D. (1973). The chemistry of clay minerals. Amsterdam: Elsevier Scientific Pub. Co. ISBN978-0-444-41043-6. OCLC713936.
Zelazny L, Calhoun F (1977). "Palygorskite (attapulgite), sepiolite, talc, pyrophyllite, and zeolites". In Dixon JB, Weed SB, Dinauer RC (eds.). Minerals in soil environments. Madison, Wisconsin: Soil Science Society of America. pp.435–470. ISBN978-0-89118-765-3. OCLC3574957. Retrieved 30 August 2024. Abstract. The structural properties and identification, natural occurrence, equilibrium environment and conditions for synthesis, chemical and physical properties, and quantitative determination of these minerals are considered.
Zvyagin, B.B.; Mishchenko, K.S.; Shitov, V.A. (1963). "Electron diffraction data on the structure of sepiolite and palygorskite". Crystallography Reports (Soviet Physics Crystallography, Kristallografya). 8. American Institute of Physics: 148–153. ISSN1063-7745. OCLC26141038.