EEG Journal - February 2020 Vol. XXVI, No. I (2)

Page 137

Discerning Erionite from Other Zeolite Minerals during Analysis ROBYN RAY* EMSL Analytical, Inc., 200 Route 130 North, Cinnaminson, NJ 08070

Key Terms: Erionite, Transmission Electron Microscopy, Liquid Nitrogen Cryogenic Holder, Cold Stage, Offretite, Quantitative EDS, Asbestos ABSTRACT Erionite, a naturally occurring fibrous mineral that belongs to the zeolite group has been designated by the International Agency for Research on Cancer (IARC) as a Group 1 Carcinogen on the basis of mesothelioma, a disease also resulting from the inhalation of asbestos fibers. Significant outcrops of fibrous erionite have been reported in California, North Dakota, Nevada, Oregon, and other states. For geologists and industrial hygienists dealing with mining, construction, or various aspects of community protection, it is vital to understand the basics of detecting and handling erionite, since it is similar to asbestos and can cause similar disease. There are many fibrous zeolites, and discerning erionite from these other minerals requires modifications to current asbestos analysis methods. Without these modifications, identification and quantification are questionable and could increase the likelihood of both false negatives and false positives. There is currently no published method specific to erionite analysis; without guidance standards, each laboratory has approached erionite analysis independently. With a few small but significant changes to asbestos analysis methodologies, we developed a reproducible analytical procedure for rapid identification of erionite fibers in air, bulk, and soil samples by transmission electron microscopy (TEM). Using specialized preparation techniques, energy dispersive Spectrometry (EDS) calibrations, and a liquid nitrogen cryo-holder (cold stage), we were able to overcome the difficulties associated with erionite analysis. By incorporating these changes, commercial analytical laboratories can contribute reliable data to air-exposure studies and characterization guidelines, which may help in determining regulations and further understanding the health risks of erionite.

*Corresponding author email: rray@emsl.com

INTRODUCTION Erionite is a member of a large group of hydrated aluminosilicate minerals called zeolites. Zeolites are found in altered volcanic tuffs, ash, and the soils derived from them. In Turkey, these volcanic tuffs are used as building stone for houses (Carbone et al., 2011). Similar to asbestos mineral fibers, erionite mineral fibers have been shown to cause to cancer (International Agency for Research on Cancer [IARC], 2012; Saracci, 2015). Internationally, there are areas in Turkey (Dogan et al. (2008)) and Mexico (Ilgren et al., 2008; Kliment et al., 2009) where malignant mesothelioma has been attributed to erionite that was found in the local environment. There are several occurrences of erionite worldwide. In the United States, it is predominately found in the intermountain west: California, North Dakota, Nevada, Oregon, and other states (Van Gosen et al., 2013, Van Gosen et al. (1996), USGS (1996)). Erionite has not been mined for commercial use since the late 1980s (National Toxicology Program [NTP], 2004). Therefore, many commercial laboratories focusing on asbestos in bulk building material are inexperienced in handling erionite. In fact, in 2009, when erionite was provided as an unknown sample on the transmission electron microscopy (TEM) proficiency round for the National Voluntary Laboratory Accreditation Program (NVLAP), only 3 out of 76 accredited laboratories identified it as erionite (National Institute of Standards and Technology, 2009). Erionite is not regulated as an asbestos mineral in the United States, and no exposure limits have been published. The potency of erionite has been shown in animal studies, where erionite is 500–800 times more tumorigenic than chrysotile and 200 times more tumorigenic than crocidolite (Carbone et al., 2011). Exposure to erionite may occur during mining and production of other zeolites where erionite is found as a contaminant (Rom et al., 1983). Erionite-related diseases are being studied among road construction and maintenance workers who may have been exposed to erionite containing gravel used in road surfacing (National Institute of Occupational Safety and Health [NIOSH], 2014). In 2017, the Nevada Department of Transportation (NDOT) started conducting

Environmental & Engineering Geoscience, Vol. XXVI, No. 1, February 2020, pp. 133–139

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Articles inside

Discerning Erionite from Other Zeolite Minerals during Analysis

18min
pages 137-144

New Tools for the Evaluation of Asbestos-Related Risk during Excavation in an NOA-Rich Geological Setting

22min
pages 117-124

Sampling, Analysis, and Risk Assessment for Asbestos and Other Mineral Fibers in Soil

17min
pages 125-132

Refinement of Sampling and Analysis Techniques for Asbestos in Soil

7min
pages 133-136

Geological Model for Naturally Occurring Asbestos Content Prediction in the Rock Excavation of a Long Tunnel (Gronda di Genova Project, NW Italy

15min
pages 111-116

Geologic Investigations for Compliance with the CARB Asbestos ATCM

24min
pages 103-110

Identification and Preliminary Toxicological Assessment of a Non-RegulatedMineral Fiber: Fibrous Antigorite from New Caledonia

20min
pages 93-102

Management of Naturally Occurring Asbestos Area in Republic of Korea

15min
pages 83-92

Fibrous Tremolite in Central New South Wales, Australia

8min
pages 77-82

Regulations Concerning Naturally Occurring Asbestos (NOA) in Germany—Testing Procedures for Asbestos

11min
pages 71-76

Naturally Occurring Asbestos in France: a Technical and Regulatory Review

17min
pages 65-70

Naturally Occurring Asbestos in France: Geological Mapping, Mineral Characterization, and Technical Developments

14min
pages 57-64

Naturally Occurring Asbestiform Minerals in Italian Western Alps and in Other Italian Sites

17min
pages 43-50

Asbestiform Minerals of the Franciscan Assemblage in California with a Focus on the Calaveras Dam Replacement Project

12min
pages 25-32

Naturally Occurring Asbestos in Valmalenco (Central Alps, Northern Italy): From Quarries and Mines to Stream Sediments

13min
pages 51-56

Does Exposure to Naturally Occurring Asbestos (NOA) During Dam Construction Increase Mesothelioma Risk?

12min
pages 33-38

NOA Air-Quality Lessons Learned during Calaveras Dam Replacement Project

12min
pages 39-42

Overview of Naturally Occurring Asbestos in California and Southwestern Nevada

14min
pages 13-18

Naturally Occurring Asbestos: A Global Health Concern? State of the Art and Open Issues

23min
pages 7-12

Clastic Sedimentary Rocks and Sedimentary Melanges: Potential Naturally Occurring Asbestos Occurrences (Amphibole and Serpentine

11min
pages 19-24

Foreword to the Environmental & Engineering Geoscience Special Edition on Naturally Occurring Asbestos

4min
pages 5-6
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