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macrophase separation, leading to visible “protein/RNA” droplets, has been widely studied and suggested to be a mechanism underlying so-called membraneless organelles, potential associative mechanisms
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open questions concerning the role of small droplets, ice surface roughness and influences of rimer rotation, humidity and pressure on the secondary ice formation process. To this end, the existing
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microorganisms catalyze the freezing of cloud droplets. These substances are a significant source of so-called ice-nucleating particles, particularly over remote marine regions. The aim of the advertised PhD
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