Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain
the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in
Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles
and JavaScript.
High-pressure chemistry is an interdisciplinary science exploring reactions and phenomena occurring at pressures above 100 kPa. Under these extreme conditions, substances undergo remarkable transformations, from quantum state alterations to the emergence of exotic stoichiometries. Beyond its role as a boundless source of scientific fascination, high-pressure chemistry unlocks high-yield processes that can save time and eliminate the need for catalysts, all while working with minuscule quantities of materials. Since the pioneering laboratory syntheses of diamond and cubic boron nitride in the late 20th century, high-pressure chemistry has evolved into an indispensable tool for both fundamental and applied materials chemistry. Recognizing the immense potential of this interdisciplinary field for structural exploration and sustainable material synthesis, this Communications Chemistry Collection seeks to encourage further advancements in this exhilarating realm of research.
We aim to cover a comprehensive range of topics related to chemical research at high-pressure. We welcome submissions exploring:
Design and high-pressure synthesis of new inorganic and organic materials and new material phases, including but not limited to materials that can be recovered at room pressure, finding applications as ultrahard, luminescent, or high-energy-density materials, high-transition-temperature superconductors, etc.
High-pressure phenomena and reaction pathways, structure transformations and transitions between solids, liquids, gases, or supercritical phases.
Theoretical and computational high-pressure chemistry, aiming at synthesis planning as well as at structure exploration or mechanistic elucidation.
Applications of high-pressure chemistry in environmental remediation, sustainable synthesis, and green chemistry.
Advanced monitoring techniques for high-pressure chemical reactions, shedding light on the dynamic evolution of chemical transformations at extreme pressures.
Method development for generating high static and dynamic pressures and for quenching high-pressure phases.
The Collection primarily welcomes original research papers, in the form of both full articles and communications. All submissions will be subject to the same review process and editorial standards as regular Communications Chemistry articles.
Post-spinel transition-metal oxides have emerged as potential candidates for high ionic conductors and materials with strongly correlated electrons. In this Review, the authors discuss recent developments in large-volume high-pressure technology, crystal structural features of post-spinel phases and their geochemical significance, and weigh the challenges and opportunities post-spinel phases entail for material applications.
Most of our knowledge about the chemical composition of the Earth’s interior is primarily retrieved by indirect observations, experiments and calculations that are limited to simple compositions. Here, the authors present the investigation of inclusions trapped in super deep diamonds as an alternative source of a wealth of information on the chemical state of the Earth’s interior through time.
Trimethylamine N-oxide (TMAO) protects organisms from the damaging effects of deep-sea high pressure, but it is not well understood how pressure and TMAO in combination perturb the water structure. Here, the authors use neutron scattering coupled with computational modelling of water at 25 bar and 4 kbar in the presence and absence of TMAO to propose an “osmolyte protection ratio” at which pressure and TMAO-induced energy changes effectively cancel out, which translates across scales to the organism level.
Enzymes may behave differently at high pressures found in environments such as the ocean floor, but molecular dynamics force fields are not well characterized at high pressures. Here the CHARMM36m force field is validated against NMR data at variable pressures up to 2500 bar, using ubiquitin as a model protein.
Fatty acid membranes are implicated in several hypotheses about the origins of life, but whether their stability towards extremes of temperature, pressure, and ionic strength is sufficient to enable primitive biochemistry remains unclear. Here branched and linear alkanes are shown to stabilise a common model primordial membrane towards high temperatures and pressures
CsPbBr3 is a characteristic halide perovskite with extensive optoelectronic application potential. Here, the authors report the pressure modulation of the crystal structure and electronic properties of CsPbBr3 at room temperature and pressures up to 5 GPa.
The Zintl-Klemm concept explains the structure and chemical bonding of intermetallic compounds at high pressures — such as high-temperature superconducting metal superhydrides. Here, the authors elucidate the electronic structures of three high-pressure potassium silver alloys, providing an example of where the Zint-Klemm concept needs to be expanded.
Transition metal dichalcogenides exhibit rich polymorphism, making them promising candidates for superconductors, topological insulators, and electrochemical catalysts. Here, the authors study the metallization of non-hydrostatically compressed ZrS2 up to 45.8 GPa and find that a new high-pressure phase forms under deviatoric stress.
Compression is a common densification method for solid-state materials, but the structural evolution of compressed non-equilibrium oxide materials such as glasses and zeolites remains somewhat elusive. Here, the authors show that siliceous zeolite single-crystals cold-compressed at 20 GPa yield permanently densified glassy silica, while cold-compressed siliceous zeolite powder and glassy silica are metastable.
Water can form a vast number of topological frameworks owing to its hydrogen-bonding ability, with 19 different forms of ice experimentally confirmed at present. Here, the authors comment on open questions and possible future discoveries, covering negative to ultrahigh pressures.
Understanding the mechanical properties of metal–organic frameworks (MOFs) is crucial for their industrial application, but the compressibility of structurally dynamic MOFs under pressure remains unclear. Here, in situ variable pressure powder X-ray diffraction experiments on two families of dynamic MOFs find that increased structural flexibility results in enhanced mechanical resilience.
Antimonite (Sb2S3) has potential applications for solar energy, but how its layered structure changes under pressure is incompletely understood. Here diamond anvil cell experiments supported by first principles calculations offer a structural explanation for experimentally observed phase transitions.
CO2 is prominent in the Earth’s and exoplanetary atmospheres, but its excited state photochemistry is not yet fully understood. Here the authors identify gradual quenching of the diffuse vibrational structure in supercritical CO2 electronic spectra under pressures up to 137 bar.
The lower decomposition barriers of cyclo-N6 anions hinder their application as high-energy-density materials. Here, first-principles calculations reveal that enhancing the covalent component of the interaction between cyclo-N6 anions and cations can effectively improve stability at high pressure.
Recent high-pressure studies have uncovered many types of chemical bonds present in noble gas compounds. Here, by extrapolating what has been found so far, the authors discuss which future discoveries can be expected and recommend further avenues of exploration.
The chemical stability of alkali halides has caused them to be exploited as inert media in high-pressure, high-temperature experiments. Here, NaCl and KCl are unexpectedly found to react with yttrium, dysprosium and iron oxide in a laser-heated diamond anvil cell, producing Y2Cl, DyCl, Y2ClC and Dy2ClC at ~40 GPa and 2000 K and FeCl2 at ~160 GPa and 2100 K.
Hydrogen sulfide and ammonia form molecular mixtures that could open up new routes towards hydrogen-rich high-pressure/high-temperature superconductors, but their mixing propensity under pressure is not well understood. Here, the authors identify stable nitric sulfur hydrides at high pressure using first-principles crystal structure prediction methods.
Collision theory predicts the spectral peak of the sodium D-line to have a red-shift dependent on pressure and temperature. Using the serendipitous presence of sodium in octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX), the authors calibrate the D-line shift up to 1.5 GPa during deflagration.