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Pyrite (P), marcasite (M), and arsenopyrite (A) are of significant historical and contemporary interest. Compounds adopting these structure types are studied for their crystallographic properties and potential applications in energy storage and conversion. Despite numerous investigations since the 1970s, understanding the chemical behaviour of pyrite, marcasite, and arsenopyrite remains limited. This study proposes a new structure determining electron (SDE) rule to systematise these compounds without relying on formal charge assignments. The SDE rule predicts structure types based on the distribution of non-localised electrons around transition metals, providing a framework for identifying and categorising related compounds. We observe good agreement with literature data and furthermore synthesised nine new ternary compounds within the Pt/Ir-Ge-As/Sb systems, demonstrating the applicability of SDE. Our findings reveal that these compounds can be seen as layer configurations of P, M and A, enhancing our understanding of their chemical diversity. This work not only categorises existing compounds, but also paves the way for future exploration of new materials, highlighting the structural potential of P, M, A-related compounds beyond traditional frameworks. Preliminary results indicate that the type of layers influences physical properties, such as electrical conductivity, warranting further investigation into the relationship between structure and function in these compounds.
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http://dx.doi.org/10.1002/anie.202502322 | DOI Listing |
Sci Rep
May 2025
Department of Electrical Engineering, Khalifa University of Science and Technology, Abu Dhabi, 127788, United Arab Emirates.
Iron pyrite (FeS) has emerged as a promising photovoltaic material due to its high absorption coefficient, earth abundance, and non-toxicity. However, its low power conversion efficiency, largely attributed to structural defects and phase impurities, has limited its application in solar cells. This study explores the solvothermal synthesis of iron pyrite under varying reaction conditions to optimize its phase purity and optical properties.
View Article and Find Full Text PDFAngew Chem Int Ed Engl
June 2025
Department of Chemistry, Ludwig-Maximilians-Universität München, Butenandtstrasse 5-13 (D), 81377, München, Germany.
Pyrite (P), marcasite (M), and arsenopyrite (A) are of significant historical and contemporary interest. Compounds adopting these structure types are studied for their crystallographic properties and potential applications in energy storage and conversion. Despite numerous investigations since the 1970s, understanding the chemical behaviour of pyrite, marcasite, and arsenopyrite remains limited.
View Article and Find Full Text PDFDalton Trans
March 2025
Department of Quantum Matter Physics, University of Geneva, CH-1211 Geneva, Switzerland.
We present an investigation of the prototypical polymorphic structural transformation from marcasite to pyrite FeS studied by combining annealing experiments and theoretical calculations. These experiments have become possible due to the availability of laboratory-synthesized high-purity marcasite samples. We constructed an annealing temperature, time, and phase composition map of marcasite based on a series of isothermal annealing experiments at different temperatures and heating times.
View Article and Find Full Text PDFDalton Trans
October 2024
Key Laboratory of Cluster Science, Ministry of Education of China, Beijing Key Laboratory of Photoelectronic/Electrophotonic Conversion Materials, School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, P. R. China.
FeS is a promising electrode material for alkali metal ion storage due to its high theoretical capacity. However, it still faces critical issues such as suboptimal rate and cycling performances owing to sluggish charge transport and significant volume variations. Herein, we constructed FeS (m-FeS) and pyrite FeS (p-FeS) nanocomposites embedded in N,S-doped carbon nanoboxes (m/p-FeS@NSCN) to conquer such challenges.
View Article and Find Full Text PDFEnviron Sci Process Impacts
March 2024
Centre for Earth Observation Science, Department of Environment and Geography, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada.
Mercury-bearing nano-mineral assemblages (Hg-NMAs) are chemically and mineralogically heterogeneous, micrometer-sized aggregates of nanoparticles (NPs) found in contaminated soils and sediments. Although these NMAs control sequestration and release of Hg that is a global contaminant, our understanding is limited with respect to the conditions of different types of Hg-NMAs, the diversity of its minerals, the size distribution of its NPs and whether mineral replacement and alteration reactions in these NMAs result in the release of Hg-bearing NPs. For this purpose, Hg-NMAs in four sediment samples from the Guanajuato Mining District (GMD) in Mexico, a region that was polluted by Hg and silver (Ag) due to historical mining involving Hg amalgamation, are characterized at the micro- and nanoscale.
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