A crystal structure with N atoms in its unit cell can be solved starting from a model with atoms 1 to j − 1 being located. To locate the next atom j , the method uses a modified definition of the traditional R 1 factor where its dependencies on the locations of atoms j + 1 to N are removed. This modified R 1 is called the single-atom R 1 ( sR 1), because the locations of atoms 1 to j − 1 in sR 1 are the known parameters, and only the location of atom j is unknown. Finding the correct position of atom j translates thus into the optimization of the sR 1 function, with respect to its fractional coordinates, x j , y j , z j . Using experimental data, it has been verified that an sR 1 has a hole near each missing atom. Further, it has been verified that an algorithm based on sR 1, hereby called the sR 1 method, can solve crystal structures (with up to 156 non-hydrogen atoms in the unit cell). The strategy to carry out this calculation has also been optimized. The main feature of the sR 1 method is that, starting from a single arbitrarily positioned atom, the structure is gradually revealed. With the user's help to delete poorly determined parts of the structure, the sR 1 method can build the model to a high final quality. Thus, sR 1 is a viable and useful tool for solving crystal structures.
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Zhang et al. (2024) studied this question.
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