This Tutorial Review, aimed at both the novice and the seasoned solid-state chemist, provides a succinct overview of key findings that have, over the last half century, advanced our ability to make molecular crystals with targeted structures and desired properties. The article critically evaluates the efficiency and reliability of the well-established guidelines used by experimentalists in crystal engineering and highlights statistical and computational tools that are both advantageous to crystal design and accessible to experimental solid-state chemists.The systematic development of our subject will be difficult if not impossible until we understand the intermolecular forces responsible for the stability of the crystalline lattice of organic compounds; a theory of the organic solid state is a requirement for the eventual control of molecular packing arrangement. Once such a theory exists we shall, in the present context of synthetic and mechanistic photochemistry, be able to 'engineer' crystal structures having intermolecular contact geometry appropriate for chemical reaction, much as, in other contexts, we shall construct organic conductors, catalysts, etc. In short, any rational development of the physics and chemistry of the solid state must be based upon a theory of molecular packing; since the molecules studied are complex, the theory will most likely be empirical for some time yet. Rules are now becoming available in what I regard as phase three, the phase of crystal engineering.
Non-equilibrium conditions must have been crucial for the assembly of the first informational polymers of early life-by supporting their formation and continuous enrichment in a long-lasting environment. Here we explored how gas bubbles in water subjected to a thermal gradient, a likely scenario within crustal mafic rocks on the early Earth, drive a complex, continuous enrichment of prebiotic molecules. RNA precursors, monomers, active ribozymes, oligonucleotides, and lipids are shown to (1) cycle between dry and wet states, enabling the central step of RNA phosphorylation, (2) accumulate at the gas-water interface to drastically increase ribozymatic activity, (3) condense into hydrogels, (4) form pure crystals, and (5) encapsulate into protecting vesicle aggregates that subsequently undergo fission. These effects occurred within less than 30 minutes. The findings unite physical conditions in one location which were crucial for the chemical emergence of biopolymers.They suggest that heated microbubbles could have hosted the first cycles of molecular evolution.Life is a non-equilibrium system. By evolution, modern life has created a complex protein machinery to maintain the nonequilibrium of crowded molecules inside dividing vesicles. Based on entropy arguments, equilibrium conditions were unlikely to trigger the evolutionary processes during the origin of life 1 . External non-equilibria had to be provided for the accumulation, encapsulation, and replication of the first informational molecules. They can locally reduce entropy, give rise to patterns 2 , and lean the system towards a continuous, dynamic self-organization 3 . Non-equilibrium dynamics can be found in many fluid systems, including gravity-driven instabilities in the atmosphere 4 , the accumulation of particles in nonlinear flow 5,6 , and shear-dependent platelet activation in blood 7 . Our experiments discuss whether gas-water interfaces in a thermal gradient could have provided such a nonequilibrium setting for the emergence of life on early Earth.Non-equilibrium systems in the form of heat flows were a very common and simplistic setting, found ubiquitously on the planet 8 . Hydrothermal activity is considered abundant on early Earth and intimately linked to volcanic activity 9 . Water is thereby circulating through the pore space of the volcanic rocks, which is formed by magmatic vesiculation (primary origin) and fractures (secondary origin). These systems have been studied as non-equilibrium driving forces for biological molecules in a variety of processes 10-17 .Gases originating from degassing of deeper magma bodies percolate through these water-filled pore networks. At shallow depths bubbles are formed by gases dissolved in water and formation of vapor where sufficient heat is supplied by the hydrothermal system. The bubbles create gas-water interfaces, which previously have been discussed in connection with atmospheric bubble-aerosol-droplet cycles 18 , the adsorption of lipid monolayers and DNA to the interface 19,20 , or the formation of pep...
We present the synthesis and characterization of a series of encapsulated diketopyrrolopyrrole red-emitting conjugated polymers. The novel materials display extremely high fluorescence quantum yields in both solution (>70%) and thin film (>20%). Both the absorption and emission spectra show clearer, more defined features compared to their naked counterparts demonstrating the suppression of inter and intramolecular aggregation. We find that the encapsulation results in decreased energetic disorder and a dramatic increase in backbone colinearity as evidenced by scanning tunnelling microscopy. This study paves the way for diketopyrrolopyrrole to be used in emissive solid state applications and demonstrates a novel method to reduce structural disorder in conjugated polymers.
A series of cocrystals involving theophylline and fluorobenzoic acids highlights the difficulty of predicting supramolecular interactions in molecular crystals.
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