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At least 127 records · Page 7

Identifying microbial functional guilds performing cryptic organotrophic and lithotrophic redox cycles in anaerobic granular biofilms

Granular biofilms used in anaerobic digester systems contain diverse microbial populations that interact to hydrolyze organic matter and produce methane within controlled environments. Prior research investigated the feasibility of utilizing granular biofilms obtained from an anaerobic digester to remove nitrate without the addition of exogenous electron donors. These granules possessed a unique structure of alternating light and dark iron sulfide and pyrite rich layers that potentially served as both an electron source and sink, linking carbon, nitrogen, sulfur, and iron cycles. To characterize the functional roles of diverse microbial populations enriched within these layered biofilms, we analyzed metagenomes obtained from three different granules. Comparisons between the functional gene content of forty metagenome assembled genomes (MAGs) identified phylogenetically cohesive functional guilds. Each of these functional MAG clusters was assigned to specific steps in anaerobic digestion (hydrolysis, acidogenesis, acetogenesis, and methanogenesis) and anaerobic respiration (denitrification and sulfate reduction). Comparisons with metagenomes derived from a variety of natural and engineered ecosystems confirmed that the enriched denitrifying bacteria were similar to populations typically found in wetlands and biological nitrogen removal systems. Analysis of read alignments to individual genes within the forty MAGs identified conserved genomic features that were representative of the functions that distinguished functional guilds. Overall, this research illustrates the utility of functional based classification of microorganisms for characterizing ecosystem functions and highlights the potential application of engineered ecosystems to serve as experimental models for complex natural ecosystems.

Ecosystem engineering↗

Core-flood Effluent and Shale Surface Chemistries in Predicting Interaction between Shale, Brine, and Reactive Fluid

We report field and laboratory observations to date indicate that the efficiency of hydraulic fracturing, as it relates to hydrocarbon recovery, depends significantly on geochemical alterations to rock surfaces that diminish accessibility by partial or total plugging of the pore and fracture networks. This is caused by mineral scale deposition such as coating of fracture surfaces with precipitates, particle migration, and/or crack closure due to dissolution under stress. In reactive flow-through experiments, mineral reactions in response to acidic fluid injection significantly reduced system porosity and core permeability. The present study focuses on changes to fluid chemistry and shale surfaces (inlet and fracture walls) resulting from shale-fluid interactions and integrating these findings for an improved estimate of transport-related consequences. The reacted shale surfaces were examined by spatially-resolved scanning electron microscopy - energy dispersive spectroscopy (SEM-EDS) analysis. Importantly, inductively coupled plasma - mass spectrometry/optical emission spectroscopy (ICP-MS/OES) was utilized to probe the chemical evolution of the core-flood effluents. The three study cores selected from the Marcellus formation represent different mineralogies and structural features. In flow-through experiments, lab-generated brine and HCl-based fracture fluid (pH=2) were injected sequentially under effective stress (up to 500 psi) at reservoir temperature (80°C). SEM-EDS results confirmed by the ICP concentration trends showed significant Fe hydroxide precipitates in clay- and pyrite-rich outcrop samples due to partial oxidation of Fe-bearing phases in the case of intrusion of low salinity water-based fluids. Porosity reduction in the MSEEL (Marcellus Shale Energy and Environmental Laboratory) carbonate-rich sample is related to compaction of cores under stress due to matrix softening with substantial dissolution, and pore-filling by hydroxides, as well as barite and salts. Despite the same fluid compositions and experimental conditions used for both MSEEL samples, barite precipitation was much more intense in the MSEEL clay-rich sample due to its greater sorption capacity and additional sulfate source as well as fissile nature with multiple lengthwise cracks. ICP tests revealed time-resolved concentration trends in produced brine and reactive fluids that in turn complemented the pre-/post-reaction SEM-EDS observations.

37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CH↗

Materials Data on FeS2 by Materials Project

FeS2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Fe3+ is bonded to six equivalent S+1.50- atoms to form corner-sharing FeS6 octahedra. The corner-sharing octahedral tilt angles are 64°. All Fe–S bond lengths are 2.25 Å. S+1.50- is bonded in a 3-coordinate geometry to three equivalent Fe3+ atoms.

36 MATERIALS SCIENCE↗

Materials Data on CuS2 by Materials Project

CuS2 is Pyrite-like structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Cu3+ is bonded to six equivalent S+1.50- atoms to form CuS6 octahedra that share corners with twelve equivalent CuS6 octahedra and corners with six equivalent SCu3S tetrahedra. The corner-sharing octahedral tilt angles are 67°. All Cu–S bond lengths are 2.46 Å. S+1.50- is bonded to three equivalent Cu3+ and one S+1.50- atom to form distorted SCu3S tetrahedra that share corners with three equivalent CuS6 octahedra and corners with fifteen equivalent SCu3S tetrahedra. The corner-sharing octahedral tilt angles are 74°. The S–S bond length is 2.03 Å.

36 MATERIALS SCIENCE↗

Materials Data on ThC2 by Materials Project

ThC2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Th4+ is bonded to six equivalent C2- atoms to form ThC6 octahedra that share corners with twelve equivalent ThC6 octahedra and corners with six equivalent CTh3C tetrahedra. The corner-sharing octahedral tilt angles are 74°. All Th–C bond lengths are 2.57 Å. C2- is bonded to three equivalent Th4+ and one C2- atom to form CTh3C tetrahedra that share corners with three equivalent ThC6 octahedra and corners with fifteen equivalent CTh3C tetrahedra. The corner-sharing octahedral tilt angles are 67°. The C–C bond length is 1.35 Å.

36 MATERIALS SCIENCE↗

Materials Data on Te2Ir by Materials Project

IrTe2 is Pyrite-like structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Ir4+ is bonded to six equivalent Te2- atoms to form corner-sharing IrTe6 octahedra. The corner-sharing octahedral tilt angles are 62°. All Ir–Te bond lengths are 2.70 Å. Te2- is bonded in a 4-coordinate geometry to three equivalent Ir4+ and one Te2- atom. The Te–Te bond length is 3.01 Å.

36 MATERIALS SCIENCE↗

Materials Data on Sb2Pd by Materials Project

PdSb2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Pd2+ is bonded to six equivalent Sb1- atoms to form PdSb6 octahedra that share corners with twelve equivalent PdSb6 octahedra and corners with six equivalent SbSbPd3 trigonal pyramids. The corner-sharing octahedral tilt angles are 63°. All Pd–Sb bond lengths are 2.72 Å. Sb1- is bonded to three equivalent Pd2+ and one Sb1- atom to form distorted SbSbPd3 trigonal pyramids that share corners with three equivalent PdSb6 octahedra and corners with fifteen equivalent SbSbPd3 trigonal pyramids. The corner-sharing octahedral tilt angles are 80°. The Sb–Sb bond length is 2.89 Å.

36 MATERIALS SCIENCE↗

Materials Data on MnS2 by Materials Project

MnS2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Mn4+ is bonded to six equivalent S2- atoms to form corner-sharing MnS6 octahedra. The corner-sharing octahedral tilt angles are 64°. All Mn–S bond lengths are 2.30 Å. S2- is bonded in a 3-coordinate geometry to three equivalent Mn4+ atoms.

36 MATERIALS SCIENCE↗

Materials Data on As2Rh by Materials Project

RhAs2 is Pyrite-like structured and crystallizes in the monoclinic P2_1/c space group. The structure is three-dimensional. Rh4+ is bonded to six As2- atoms to form RhAs6 octahedra that share corners with eight equivalent RhAs6 octahedra, corners with six AsAsRh3 tetrahedra, and edges with two equivalent RhAs6 octahedra. The corner-sharing octahedra tilt angles range from 53–60°. There are a spread of Rh–As bond distances ranging from 2.45–2.54 Å. There are two inequivalent As2- sites. In the first As2- site, As2- is bonded to three equivalent Rh4+ and one As2- atom to form distorted AsAsRh3 tetrahedra that share corners with three equivalent RhAs6 octahedra, corners with thirteen AsAsRh3 tetrahedra, and an edgeedge with one AsAsRh3 tetrahedra. The corner-sharing octahedra tilt angles range from 73–78°. The As–As bond length is 2.50 Å. In the second As2- site, As2- is bonded to three equivalent Rh4+ and one As2- atom to form AsAsRh3 tetrahedra that share corners with three equivalent RhAs6 octahedra, corners with thirteen AsAsRh3 tetrahedra, and an edgeedge with one AsAsRh3 tetrahedra. The corner-sharing octahedra tilt angles range from 68–72°.

36 MATERIALS SCIENCE↗

Materials Data on Te2Ru by Materials Project

RuTe2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Ru4+ is bonded to six equivalent Te2- atoms to form corner-sharing RuTe6 octahedra. The corner-sharing octahedral tilt angles are 63°. All Ru–Te bond lengths are 2.68 Å. Te2- is bonded in a 4-coordinate geometry to three equivalent Ru4+ and one Te2- atom. The Te–Te bond length is 2.86 Å.

36 MATERIALS SCIENCE↗

Materials Data on Ca2Mn3O8 by Materials Project

Ca2Mn3O8 is Pyrite-derived structured and crystallizes in the monoclinic C2/m space group. The structure is three-dimensional. Ca2+ is bonded to six O2- atoms to form distorted CaO6 pentagonal pyramids that share corners with seven MnO6 octahedra, edges with three MnO6 octahedra, and edges with two equivalent CaO6 pentagonal pyramids. The corner-sharing octahedra tilt angles range from 20–56°. There are a spread of Ca–O bond distances ranging from 2.28–2.45 Å. There are two inequivalent Mn4+ sites. In the first Mn4+ site, Mn4+ is bonded to six O2- atoms to form MnO6 octahedra that share corners with six equivalent CaO6 pentagonal pyramids, edges with four equivalent MnO6 octahedra, and edges with two equivalent CaO6 pentagonal pyramids. There is four shorter (1.93 Å) and two longer (1.95 Å) Mn–O bond length. In the second Mn4+ site, Mn4+ is bonded to six O2- atoms to form MnO6 octahedra that share corners with four equivalent CaO6 pentagonal pyramids, edges with four MnO6 octahedra, and edges with two equivalent CaO6 pentagonal pyramids. There are a spread of Mn–O bond distances ranging from 1.90–2.03 Å. There are three inequivalent O2- sites. In the first O2- site, O2- is bonded in a distorted trigonal planar geometry to one Ca2+ and two equivalent Mn4+ atoms. In the second O2- site, O2- is bonded to one Ca2+ and three Mn4+ atoms to form a mixture of distorted edge and corner-sharing OCaMn3 trigonal pyramids. In the third O2- site, O2- is bonded to two equivalent Ca2+ and two Mn4+ atoms to form a mixture of distorted edge and corner-sharing OCa2Mn2 trigonal pyramids.

36 MATERIALS SCIENCE↗

Materials Data on RuSe2 by Materials Project

RuSe2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Ru4+ is bonded to six equivalent Se2- atoms to form corner-sharing RuSe6 octahedra. The corner-sharing octahedral tilt angles are 64°. All Ru–Se bond lengths are 2.50 Å. Se2- is bonded in a 4-coordinate geometry to three equivalent Ru4+ and one Se2- atom. The Se–Se bond length is 2.51 Å.

36 MATERIALS SCIENCE↗

Materials Data on As2Pd by Materials Project

PdAs2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Pd4+ is bonded to six equivalent As2- atoms to form PdAs6 octahedra that share corners with twelve equivalent PdAs6 octahedra and corners with six equivalent AsAsPd3 tetrahedra. The corner-sharing octahedral tilt angles are 64°. All Pd–As bond lengths are 2.54 Å. As2- is bonded to three equivalent Pd4+ and one As2- atom to form AsAsPd3 tetrahedra that share corners with three equivalent PdAs6 octahedra and corners with fifteen equivalent AsAsPd3 tetrahedra. The corner-sharing octahedral tilt angles are 78°. The As–As bond length is 2.46 Å.

36 MATERIALS SCIENCE↗

Materials Data on CoS2 by Materials Project

CoS2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Co4+ is bonded to six equivalent S2- atoms to form CoS6 octahedra that share corners with twelve equivalent CoS6 octahedra and corners with six equivalent SCo3S tetrahedra. The corner-sharing octahedral tilt angles are 65°. All Co–S bond lengths are 2.31 Å. S2- is bonded to three equivalent Co4+ and one S2- atom to form distorted SCo3S tetrahedra that share corners with three equivalent CoS6 octahedra and corners with fifteen equivalent SCo3S tetrahedra. The corner-sharing octahedral tilt angles are 77°. The S–S bond length is 2.14 Å.

36 MATERIALS SCIENCE↗

Materials Data on NiSe2 by Materials Project

NiSe2 is pyrite-like structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Ni4+ is bonded to six equivalent Se2- atoms to form corner-sharing NiSe6 octahedra. The corner-sharing octahedral tilt angles are 63°. All Ni–Se bond lengths are 2.46 Å. Se2- is bonded in a 3-coordinate geometry to three equivalent Ni4+ atoms.

36 MATERIALS SCIENCE↗

Materials Data on OsS2 by Materials Project

SSOs is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Os4+ is bonded to six equivalent S2- atoms to form OsS6 octahedra that share corners with twelve equivalent OsS6 octahedra and corners with six equivalent SOs3S tetrahedra. The corner-sharing octahedral tilt angles are 64°. All Os–S bond lengths are 2.37 Å. S2- is bonded to three equivalent Os4+ and one S2- atom to form distorted SOs3S tetrahedra that share corners with three equivalent OsS6 octahedra and corners with fifteen equivalent SOs3S tetrahedra. The corner-sharing octahedral tilt angles are 78°. The S–S bond length is 2.28 Å.

36 MATERIALS SCIENCE↗

Materials Data on SiP2 by Materials Project

SiP2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Si4- is bonded to six equivalent P2+ atoms to form corner-sharing SiP6 octahedra. The corner-sharing octahedral tilt angles are 65°. All Si–P bond lengths are 2.41 Å. P2+ is bonded in a trigonal non-coplanar geometry to three equivalent Si4- atoms.

36 MATERIALS SCIENCE↗

Materials Data on SiAs2 by Materials Project

SiAs2 is Pyrite structured and crystallizes in the cubic Pa-3 space group. The structure is three-dimensional. Si4+ is bonded to six equivalent As2- atoms to form SiAs6 octahedra that share corners with twelve equivalent SiAs6 octahedra and corners with six equivalent AsSi3As tetrahedra. The corner-sharing octahedral tilt angles are 64°. All Si–As bond lengths are 2.55 Å. As2- is bonded to three equivalent Si4+ and one As2- atom to form distorted AsSi3As tetrahedra that share corners with three equivalent SiAs6 octahedra and corners with fifteen equivalent AsSi3As tetrahedra. The corner-sharing octahedral tilt angles are 78°. The As–As bond length is 2.45 Å.

36 MATERIALS SCIENCE↗