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At least 19 records
All sourcesNASA NTRSDOE OSTI
DOE OSTI2016

Evaluating the role of re-adsorption of dissolved Hg 2+ during cinnabar dissolution using isotope tracer technique

Cinnabar dissolution is an important factor controlling mercury (Hg) cycling. Recent studies have suggested the co-occurrence of re-adsorption of the released Hg during the course of cinnabar dissolution. However, there is a lack of feasible techniques that can quantitatively assess the amount of Hg re-adsorbed on cinnabar when investigating cinnabar dissolution. In this study, a new method, based on isotope tracing and dilution techniques, was developed to study the role of Hg re-adsorption in cinnabar dissolution. The developed method includes two key components: (1) accurate measurement of both released and spiked Hg in aqueous phase and (2) estimation of re-adsorbed Hg on cinnabar surface via the reduction in spiked 202 Hg 2+ . By adopting the developed method, it was found that the released Hg for trials purged with oxygen could reach several hundred g L –1 , while no significant cinnabar dissolution was detected under anaerobic condition. Cinnabar dissolution rate when considering Hg re-adsorption was approximately 2 times the value calculated solely with the Hg detected in the aqueous phase. Lastly, these results suggest that ignoring the Hg re-adsorption process can significantly underestimate the importance of cinnabar dissolution, highlighting the necessity of applying the developed method in future cinnabar dissolution studies.

07 ISOTOPE AND RADIATION SOURCES↗
DOE OSTI2021

The use and abuse of cinnabar in Late Neolithic and Copper Age Iberia

Abstract In this study, total mercury (THg) was analyzed in archaeological human bone from 23 sites dating to between the Middle Neolithic and the Antiquity. A total of 370 individuals from individual or collective burials was sampled, mostly using cortical bone from the humerus. These individuals were recovered from over 50 different funerary structures ranging from tholoi, pits, caves, and hypogea. Although cinnabar (HgS) is a likely cause of mercury poisoning and toxicity for people exposed to this mineral from mining or use as a paint or pigment, not all sites investigated here had cinnabar associated with the burials or other excavated areas. We found unusual levels of THg in many of the sampled individuals that we assume were caused by exposure to cinnabar in life, and not by diagenetic processes or other exposures to mercury such as through diet, which would only cause negligible accumulation of THg in bone. Our data, based on the largest sampling ever undertaken on contamination of human bone through archaeological evidence, provide a baseline for additional research on cinnabar and its use in Prehistory. Moderate to high levels of THg in human bone are mainly associated with societies dating from the second half of the 4th to late 3rd millennia B.C. (Late Neolithic to Middle Chalcolithic) in southern Iberia. By the Late Chalcolithic and Early Bronze Age, the use of cinnabar decreased significantly and became minimal or absent. The use and abuse of cinnabar appears to have been pervasive throughout the above‐mentioned period and particularly between c. 2900–2300 B.C. This occurred in connection with the high symbolic and probably sacred value of the substance, which was sought after, traded, and extensively used in a variety of rituals and social practices.

Emslie, Steven D.↗
DOE OSTI2018

Native Plants in Floodplain in Controlling Hg Flux into East Fork Poplar Creek of Oak Ridge - 18166

Legacy Hg contamination has been identified as the highest priority clean-up risk on the Oak Ridge Reservation (ORR) by the Department of Energy Office of Environmental Management (DOE-EM), Tennessee Department of Environment and Conservation (TDEC), and the US Environmental Protection Agency (EPA). During the 1950's and early 1960's, elemental mercury (Hg) was used to produce enriched Li isotope at the Y-12 National Security Complex (Y-12 Plant) for manufacturing components of various nuclear weapons systems. It is estimated that 350,000 kg of Hg was released to the environment contaminating facilities, soil, sediment, surface water, and groundwater within the boundaries of the Y-12 Plant and the downstream environment (i.e., East Fork Poplar Creek, EFPC). EFPC is a 23-km stream where the headwaters start in the Y-12 Plant, flows through the city of Oak Ridge, and empties into the Clinch River. Although various remediation efforts have reduced Hg fluxes from the Y-12 Plant over the last 25 years, the Hg concentration in water continue to exceed both the regulatory limit (51 ng/L) and the remediation goal (200 μg/L). Perennial grasses as floodplain plants have been successfully employed to control surface runoff and stabilize the floodplain. Hg has been strongly bound to particles suspended with surface runoff. Miscanthus grass is a perennial, tall grass that is adjusted to coarse, fine and medium textured soils. Although it grows best in deep, well-drained floodplain soils it is tolerant of poor to excessive well-drained soils, has an extensive tolerance for acidic to alkaline soils, and tolerates soil textures ranging from sand to clay. These long tangled root systems can reach moisture more deeply than other grasses during drought thus anchoring the plant into the soil. The fine appearance and branching hairs grow to form a dense mat that helps improve soil structure by increasing porosity and adding organic material that helps to bind soil particles together. In compacted or clay soils, spreading roots increase soil porosity by creating fractures in soil aggregates allowing water to penetrate deeper within the subsoil. This study showed that DOE remediation significantly reduced residual Hg to be <400 mg/kg in floodplain. However the residual Hg was mostly present in non-cinnabar mercury which is more bioavailable than cinnabar. The current study also found that Hg transfer flux from floodplain soils through surface soils with trees and grasses under natural rainfall events was an average of 0.28±0.15 μg/L, which was similar to the Hg concentrations in water of EFPC as reported by ORNL. Total Hg concentrations and Hg and speciation in floodplain soils were strongly affected by particle size distribution. Fine particles had higher Hg concentrations rich in cinnabar Hg. Clay particles contained as high as 2000-1600 mg/kg Hg with most Hg as cinnabar Hg, while coarse particles contained less total Hg, dominated by non-cinnabar Hg. Hg speciation in floodplain soil strongly controls its solubility, mobility, and bioavailability in both terrestrial/ aquatic ecosystems and downstream Hg concentrations. (authors)

12 MANAGEMENT OF RADIOACTIVE AND NON-RADIOACTIVE W↗
DOE OSTI2014

Modeling CO 2 -Brine-Rock Interaction Including Mercury and H 2 S Impurities in the Context of CO 2 Geologic Storage

This study uses modeling and simulation approaches to investigate the impacts on injectivity of trace amounts of mercury (Hg) in a carbon dioxide (CO 2 ) stream injected for geologic carbon sequestration in a sandstone reservoir at ~2.5 km depth. At the range of Hg concentrations expected (7-190 ppbV, or ~ 0.06-1.6 mg/std.m 3 CO 2 ), the total volumetric plugging that could occur due to complete condensation of Hg, or due to complete precipitation of Hg as cinnabar, results in a very small porosity change. In addition, Hg concentration much higher than the concentrations considered here would be required for Hg condensation to even occur. Concentration of aqueous Hg by water evaporation into CO 2 is also unlikely because the higher volatility of Hg relative to H 2 O at reservoir conditions prevents the Hg concentration from increasing in groundwater as dry CO 2 sweeps through, volatilizing both H 2 O and Hg. Using a model-derived aqueous solution to represent the formation water, batch reactive geochemical modeling show that the reaction of the formation water with the CO 2 -Hg mixture causes the pH to drop to about 4.7 and then become buffered near 5.2 upon reaction with the sediments, with a negligible net volume change from mineral dissolution and precipitation. Cinnabar (HgS(s)) is found to be thermodynamically stable as soon as the Hg-bearing CO 2 reacts with the formation water which contains small amounts of dissolved sulfide. Liquid mercury (Hg(l)) is not found to be thermodynamically stable at any point during the simulation. Two-dimensional radial reactive transport simulations of CO 2 injection at a rate of 14.8 kg/s into a 400 m-thick formation at isothermal conditions of 106°C and average pressure near 215 bar, with varying amounts of Hg and H 2 S trace gases, show generally that porosity changes only by about ±0.05% (absolute, i.e., new porosity = initial porosity ±0.0005) with Hg predicted to readily precipitate from the CO 2 as cinnabar in a zone mostly matching the single-phase CO 2 plume. The precipitation of minerals other than cinnabar, however, dominates the evolution of porosity. Main reactions include the replacement of primarily Fe-chlorite by siderite, of calcite by dolomite, and of K-feldspar by muscovite. Chalcedony is also predicted to precipitate from the dissolution of feldspars and quartz. Although the range of predicted porosity change is quite small, the amount of dissolution and precipitation predicted for these individual minerals is not negligible. These reactive transport simulations assume that Hg gas behaves ideally. To examine effects of non-ideality on these simulations, approximate calculations of the fugacity coefficient of Hg in CO 2 were made. Results suggest that Hg condensation could be significantly overestimated when assuming ideal gas behavior, making our simulation results conservative with respect to impacts on injectivity. The effect of pressure on Henry’s constant for Hg is estimated to yield Hg solubilities about 10% lower than when this effect is not considered, a change that is considered too small to affect the conclusions of this report. Although all results in this study are based on relatively mature data and modeling approaches, in the absence of experimental data and more detailed site-specific information, it is not possible to fully validate the results and conclusions.

54 ENVIRONMENTAL SCIENCES↗
DOE OSTI2019

Speciation of Mercury and Heavy Metals in Hg-contaminated Soils from Oak Ridge TN - 19426

Mercury is present in various forms in the environments. Mercuric compounds, Hg(II) are found predominant species in soil and water, while elemental mercury, Hg0 is the major species in the atmosphere, and organo-mercury is present mostly in food-chain. The speciation of Hg is important to understand its mobility, bioavailability in soils, sediments and biota and potential toxicity on human and environmental health. A catastrophic Hg spill occurred at the Y-12 National Security Complex (Y-12 Plant) at the Oak Ridge Reservation of the Department of Energy (DOE) in 1960's that contaminated facilities, soil, sediment, surface water, and groundwater within the boundaries of the Y-12 Plant and the downstream environment along the East Fork Poplar Creek (EFPC) at the city of Oak Ridge. It is estimated that 350,000 kg of Hg was released to the environment. The EFPC floodplain soils were reported to contain predominantly cinnabar (HgS) form, but other inorganic and organic Hg species, including Hg0 , HgCl{sub 2}, Hg{sub 2}Cl{sub 2}, HgO and CH{sub 3}Hg{sup +} have been found within the Y-12 Facility boundaries and the 23-km long contaminated EFPC. Over the last 25 years, Hg fluxes from the Y-12 Plant have been reduced by various remediation efforts, nonetheless Hg concentration in water and fish have not declined due to the persistent leaching of Hg from contaminated floodplain soils and sediments. In this work, we performed total elemental analyses and Hg speciation in the floodplain soils and sediments collected along EFPC in Oak Ridge, TN. The objective of the study was to elucidate the distribution of Hg in floodplain soil fractions and the relation with metals including arsenic, copper, zinc and lead. Total elemental; characterization was performed by ICP-MS analysis after with HNO{sub 3} and HF dissolution. Sequential extractions were carried out to extract water-soluble (F1), cation-exchangeable (F2) fractions and those bound to carbonates (F3), reducible oxides (F4) (Mn-oxides), organic matter (F5), amorphous (F6) and crystalline iron oxides (F7) and the residual fraction (F8) containing elemental Hg, non-cinnabar Hg and humic acid-bound Hg. Preliminary studies were conducted with artificially spiked and incubated soils as well as soils contaminated with enriched {sup 200}Hg isotope. The results indicated that Hg is predominantly associated with organic matter, amorphous iron and crystalline oxides and the residual fraction. The total Hg in the first four fractions (F1, F2, F3, and F4) were about 1% of the total Hg, while Hg was found equally bound to organic matter (F5) and crystalline Fe-oxides (F7) that accounted about 20% of total Hg. The Hg associated with amorphous iron oxides (F6) accounted as much as 26% of the total Hg and non-cinnabar Hg accounted about 24% of total Hg (non-cinnabar Hg). The results also indicated positive correlation for As, Cu, Pb and Zn levels with those of Hg. Most As was associated with amorphous Fe-oxides. Cu and Pb were dominant both in organic matter and amorphous oxide fractions. Zn was mostly bound to amorphous Fe-oxide but significant amount of Zn was also found to be associated with organic matter and crystalline Fe-oxides. (authors)

12 MANAGEMENT OF RADIOACTIVE AND NON-RADIOACTIVE W↗
NASA NTRS1983

Pressure-induced phase transition of HgS

The high pressure phase transition of cinnabar (alpha-HgS) was studied by energy dispersive X-ray diffraction using a synchrotron X-ray source. The cinnabar crystal structure was found to transform to the sodium-chloride structure at about 130 kbar. The lattice parameter of the new phase was determined to be 5.070 + or - 0.005 A at 300 kbar. No further phase transition was observed up to 400 kbar.

Huang, T.↗
DOE OSTI2012

Practical high resolution detection method for laser-induced breakdown spectroscopy

A Fabry-Perot etalon was coupled to a Czerny-Turner spectrometer to acquire high-resolution measurements in laser-induced breakdown spectroscopy (LIBS). The spectrometer was built using an inexpensive etalon coupled to a standard 0.5-m imaging spectrometer. The Hg emission doublet at 313.2 nm was used to evaluate instrument performance because it has a splitting of 29 pm. The 313.2 nm doublet was chosen due to the similar splitting seen in isotope splitting from uranium at 424.437 nm, which is 25 pm. The Hg doublet was easily resolved from a continuous source Hg-lamp with a 2 s acquisition. The doublet was also resolved in LIBS spectra of cinnabar (HgS) from the accumulation of 600 laser shots at rate of 10 Hz, or 1 min, under a helium atmosphere. In addition to observed spitting of the 313.2 nm Hg doublet, the FWHM of the 313.1844 nm line from the doublet is reported at varying He atmospheric pressures. The high performance, low cost, and compact footprint makes this system highly competitive with 2-m double pass Czerny-Turner spectrometers.

37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CH↗
DOE OSTI2015

Final Technical Report: Mercury Release from Organic Matter (OM) and OM-Coated Mineral Surfaces

Chemical reactions between mercury, a neurotoxin, and sulfur, an essential nutrient, in the environment control to a large extent the distribution and amount of mercury available for uptake by living organisms. The largest reservoir of sulfur in soils is in living, decaying, and dissolved natural organic matter. The decaying and dissolved organic matter can also coat the surfaces of minerals in the soil. Mercury (as a divalent cation) can bind to the sulfur species in the organic matter as well as to the bare mineral surfaces, but the extent of binding and release of this mercury is not well understood. The goals of the research were to investigate fundamental relationships among mercury, natural organic matter, and selected minerals to better understand specifically the fate and transport of mercury in contaminated soils downstream from the Y-12 plant along East Fork Poplar Creek, Tennessee, and more generally in any contaminated soil. The research focused on (1) experiments to quantify the uptake and release of mercury from two clay minerals in the soil, kaolinite and vermiculite, in the presence and absence of dissolved organic matter; (2) release of mercury from cinnabar under oxic and anoxic conditions; (3) characterization of the forms of mercury in the soil using synchrotron X-ray absorption spectroscopic techniques; and, (4) determination of molecular forms of mercury in the presence of natural organic matter. We also leveraged funding from the National Science Foundation to (5) evaluate published approaches for determining sulfur speciation in natural organic matter by fitting X-ray Absorption Near Edge Structure (XANES) spectra obtained at the sulfur K-edge and apply optimized fitting schemes to new measurements of sulfur speciation in a suite of dissolved organic matter samples from the International Humic Substances Society. Lastly, in collaboration with researchers at the University of Colorado and the U.S. Geological Survey in Boulder, Colorado, (6) we investigated the biogeochemical controls on the release of mercury in simulated flooding experiments using loose soils and intact soil cores from East Fork Poplar Creek.

54 ENVIRONMENTAL SCIENCES↗
DOE OSTI2025

Mercury sequestration in alkaline salt low-level radioactive waste

Liquid low-level radioactive waste at the Savannah River Site contains several species of mercury, including inorganic, elemental and methylmercury. This waste is solidified and stabilized in a cementitious waste form referred to as saltstone. Soluble mercury is stabilized as β-cinnabar, HgS as the result of reaction between the mercury and sulfur present in blast furnace slag, one of the cementitious regents. In this investigation, Mersorb®, a commercial granular activated carbon impregnated with sulfur, was evaluated as a pretreatment to remove mercury from the solution prior to cementation. Mersorb® was found to remove more than 96 mass percent of the methylmercury in simulated tank waste solution when the mass ratio of Mersorb® to mercury was above 2.5. Slag sequestered relatively more inorganic mercury than organic mercury in simulated tank waste after 24 hours of contact. This is likely due to the mercury-carbon bond being more covalent than the mercury-oxygen bond and therefore more difficult to break and slower to form HgS.

Cementitious Material↗
DOE OSTI2015

Analysis of high-resolution spectra from a hybrid interferometric/dispersive spectrometer

To fully take advantage of a low-cost, small footprint hybrid interferometric/dispersive spectrometer, a math- ematical reconstruction technique was developed to accurately capture the high-resolution and relative peak intensities from complex patterns. A Fabry-Perot etalon was coupled to a Czerny-Turner spectrometer, in- creasing spectral resolution by an order of magnitude without the commensurate increase in spectrometer size. Measurement of the industry standard Hg 313.1555/313.1844 nm doublet yielded a ratio of 0.682 with 1.8%error, which agreed well with an independent measurement and literature values. The doublet separation (29 pm), is similar to the U isotope shift (25 pm) at 424.437 nm that is of interest to monitoring nuclear nonpro-liferation activities. Additionally, the technique was applied to a LIBS measurement of the mineral cinnabar (HgS) and resulted in a ratio of 0.681. In addition, this reconstruction method could enable significantly smaller, portable high-resolution instruments with isotopic specificity, benefiting a variety of spectroscopic applications.

46 INSTRUMENTATION RELATED TO NUCLEAR SCIENCE AND ↗
DOE OSTI2017

Zuotai and HgS differ from HgCl{sub 2} and methyl mercury in Hg accumulation and toxicity in weanling and aged rats

Mercury sulfides are used in Ayurvedic medicines, Tibetan medicines, and Chinese medicines for thousands of years and are still used today. Cinnabar (α-HgS) and metacinnabar (β-HgS) are different from mercury chloride (HgCl{sub 2}) and methylmercury (MeHg) in their disposition and toxicity. Whether such scenario applies to weanling and aged animals is not known. To address this question, weanling (21 d) and aged (450 d) rats were orally given Zuotai (54% β-HgS, 30 mg/kg), HgS (α-HgS, 30 mg/kg), HgCl{sub 2} (34.6 mg/kg), or MeHg (MeHgCl, 3.2 mg/kg) for 7 days. Accumulation of Hg in kidney and liver, and the toxicity-sensitive gene expressions were examined. Animal body weight gain was decreased by HgCl{sub 2} and to a lesser extent by MeHg, but unaltered after Zuotai and HgS. HgCl{sub 2} and MeHg produced dramatic tissue Hg accumulation, increased kidney (kim-1 and Ngal) and liver (Ho-1) injury-sensitive gene expressions, but such changes are absent or mild after Zuotai and HgS. Aged rats were more susceptible than weanling rats to Hg toxicity. To examine roles of transporters in Hg accumulation, transporter gene expressions were examined. The expression of renal uptake transporters Oat1, Oct2, and Oatp4c1 and hepatic Oatp2 was decreased, while the expression of renal efflux transporter Mrp2, Mrp4 and Mdr1b was increased following HgCl{sub 2} and MeHg, but unaffected by Zuotai and HgS. Thus, Zuotai and HgS differ from HgCl{sub 2} and MeHg in producing tissue Hg accumulation and toxicity, and aged rats are more susceptible than weanling rats. Transporter expression could be adaptive means to reduce tissue Hg burden. - Highlights: • Aged rats are more susceptible to HgCl{sub 2} and MeHg toxicity than weanling rats. • Zuotai and HgS differ from HgCl{sub 2} and MeHg in producing toxicity. • Zuotai and HgS differ from HgCl{sub 2} and MeHg in much less tissue Hg accumulation. • Renal transporters are altered by HgCl{sub 2} and MeHg, but unaffected by Zuotai and HgS • Liver transporters are less affected than kidney transporters by HgCl{sub 2} and MeHg.

60 APPLIED LIFE SCIENCES↗
DOE OSTI2018

Spectroscopic and Microscopic Evidence of Biomediated HgS Species Formation from Hg(II)–Cysteine Complexes: Implications for Hg(II) Bioavailability

In this work we investigated the chemistry of Hg(II) during exposure of exponentially growing bacteria ( Escherichia coli , Bacillus subtilis , and Geobacter sulfurreducens ) to 50 nM, 500 nM, and 5 μM total Hg(II) with and without added cysteine. With X-ray absorption spectroscopy, we provide direct evidence of the formation of cell-associated HgS for all tested bacteria. The addition of cysteine (100–1000 μM) promotes HgS formation (>70% of total cell-associated Hg(II)) as a result of the biodegradation of added cysteine to sulfide. Cell-associated HgS species are also detected when cysteine is not added as a sulfide source. Two phases of HgS, cinnabar (α-HgS) and metacinnabar (β-HgS), form depending on the total concentration of Hg(II) and sulfide in the exposure medium. However, α-HgS exclusively forms in assays that contain an excess of cysteine. Scanning transmission electron microscopy images reveal that nanoparticulate HgS (s) is primarily located at the cell surface/extracellular matrix of Gram-negative E. coli and G. sulfurreducens and in the cytoplasm/cell membrane of Gram-positive B. subtilis . Intracellular Hg(II) was detected even when the predominant cell-associated species was HgS. This study shows that HgS species can form from exogenous thiol-containing ligands and endogenous sulfide in Hg(II) biouptake assays under nondissimilatory sulfate reducing conditions, providing new considerations for the interpretation of Hg(II) biouptake results.

54 ENVIRONMENTAL SCIENCES↗
DOE OSTI2012

Exploring the structural basis for selenium/mercury antagonism in Allium fistulosum

While continuing efforts are devoted to studying the mutually protective effect of mercury and selenium in mammals, few studies have investigated the mercury-selenium antagonism in plants. In this study, we report the metabolic fate of mercury and selenium in Allium fistulosum (green onion) after supplementation with sodium selenite and mercuric chloride. Analysis of homogenized root extracts via capillary reversed phase chromatography coupled with inductively coupled plasma mass spectrometry (capRPLC-ICP-MS) suggests the formation of a mercury-selenium containing compound. Micro-focused synchrotron X-ray fluorescence mapping of freshly excised roots show Hg sequestered on the root surface and outlining individual root cells, while Se is more evenly distributed throughout the root. There are also discrete Hg-only, Se-only regions and an overall strong correlation between Hg and Se throughout the root. Analysis of the X-ray absorption near edge structure (XANES) spectra show a 'background' of methylselenocysteine within the root with discrete spots of SeO{sub 3}{sup 2-}, Se{sup 0} and solid HgSe on the root surface. Mercury outlining individual root cells is possibly binding to sulfhydryl groups or plasma membrane or cell wall proteins, and in some places reacting with reduced selenium in the rhizosphere to form a mercury(II) selenide species. Together with the formation of the root-bound mercury(II) selenide species, we also report on the formation of cinnabar (HgS) and Hg{sup 0} in the rhizosphere. The results presented herein shed light on the intricate chemical and biological processes occurring within the rhizosphere that influence Hg and Se bioavailability and will be instrumental in predicting the fate and assisting in the remediation of these metals in the environment and informing whether or not fruit and vegetable food selection from aerial plant compartments or roots from plants grown in Hg contaminated soils, are safe for consumption.

54 ENVIRONMENTAL SCIENCES↗
DOE OSTI2017

Identification of Pigments in Colored Layers of a Painting by Raman Spectroscopy

Using the method of Raman spectroscopy the pigment composition is investigated of, and the brushwork technique used in, the original layer of a 19th century painting is established. It is an overdoor worked, presumably, by Antoine Jean-Etienne Faivre. It is established that the artist used the following pigments: cinnabar and dyes on the basis of goethite and hematite (for red, yellow–orange, and brown shades), ultramarine and Prussian blue (for blue shades), and Emerald green and a mixture of blue and yellow shades (to obtain a green color). It is determined that white lead was used a primer.

37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CH↗
DOE OSTI2020

Materials Data on HgTe by Materials Project

HgTe is Cinnabar structured and crystallizes in the trigonal P3_121 space group. The structure is three-dimensional. Hg2+ is bonded to six equivalent Te2- atoms to form a mixture of distorted edge and corner-sharing HgTe6 octahedra. The corner-sharing octahedra tilt angles range from 17–24°. There are a spread of Hg–Te bond distances ranging from 2.76–3.76 Å. Te2- is bonded in a 6-coordinate geometry to six equivalent Hg2+ atoms.

36 MATERIALS SCIENCE↗
DOE OSTI2020

Materials Data on HgS by Materials Project

HgS is Cinnabar structured and crystallizes in the trigonal P3_121 space group. The structure is one-dimensional and consists of one HgS ribbon oriented in the (0, 0, 1) direction. Hg2+ is bonded in a distorted linear geometry to two equivalent S2- atoms. Both Hg–S bond lengths are 2.39 Å. S2- is bonded in a distorted water-like geometry to two equivalent Hg2+ atoms.

36 MATERIALS SCIENCE↗
DOE OSTI2020

Materials Data on HgO by Materials Project

HgO is Cinnabar structured and crystallizes in the trigonal P3_121 space group. The structure is one-dimensional and consists of one HgO ribbon oriented in the (0, 0, 1) direction. Hg2+ is bonded in a distorted linear geometry to two equivalent O2- atoms. Both Hg–O bond lengths are 2.07 Å. O2- is bonded in a distorted water-like geometry to two equivalent Hg2+ atoms.

36 MATERIALS SCIENCE↗