The term p-process (p for proton) is used in two ways in the scientific literature concerning the astrophysical origin of the elements (nucleosynthesis). Originally it referred to a proton capture process which was proposed to be the source of certain, naturally occurring, neutron-deficient isotopes of the elements from selenium to mercury. These nuclides are called p-nuclei and their origin is still not completely understood. Although it was shown that the originally suggested process cannot produce the p-nuclei, later on the term p-process was sometimes used to generally refer to any nucleos
En un principio se pensó que el Proceso P era un proceso de captura protónica que se da durante las supernovas. Entonces se entendió que las densidades protónicas son demasiado pequeñas y las abundancias isotópicas no pueden ser explicadas mediante esta reacción.
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).