From: Robin Shirley To: uppw@cristal.org Date: Mon, 10 Nov 2003 13:59:48 -0000 Subject: UPPW-4 solution Dear Armel ** UPPW-4 Solution ** Again not a difficult problem, which proves to belong to the expected STF zeolite family and can be solved by judicious refinement starting from the published STF cell. Even if it could not, all six automatic indexing programs that were tried solved it easily at their first attempt. I am very confident that the resulting cell is correct, and would expect that, given profile data, it would not be difficult to proceed to a Rietveld refinement using the published STF structure as starting point. The following C2/m cell, with standard deviations in brackets, was refined against 2Theta values using Celref (within Chekcell) and includes a 2Theta zero correction: a = 13.9656 (0.0068) A b = 18.3743 (0.0107) A c = 7.4377 (0.0034) A beta = 99.400 (0.004) degrees giving V = 1882.96 (0.15) A(3) 2Theta zero correction (to be added) = +0.0080 (0.0067) degrees This cell indexes all 25 observed lines using only 35 calculated lines, with figures of merit (including the C-lattice absences): M1(20) = 43.9, M1(25) = 35.8. Although the 2Theta zero correction is small, omitting it has a significant worsening effect on the standard deviations reported by Celref, in particular increasing the esd of beta from 0.004 to 0.12 degrees. No significant improvement was found by treating the correction as due to specimen displacement. ** Discussion ** A quick (5 to 10 minutes) session with Crysfire showed that many indexing programs would solve this dataset very easily using their Crysfire defaults (1V and 2V refers to volume multiples of the correct C2/m cell: ITO12 1V cell, "M20" = 47.2 (C-centred) FJZN6 1V cell, "M20" = 46.6 (C-centred) (twice) TREOR90 1V cell, "M20" = 20, "M25" = 17. F25 = 45 (0.0084, 67) KOHL (TMO) 1V cell, "M20" = 46.6 (C-centred), plus two 2V cells DICVOL91 1V cell, "M20" = 22.9 plus two equivalent 1V settings LZON 1V cell, "M20" = 46.5 (C-centred) (3 times) plus two 2V cells With such a clear indication there did not seem any need to run further programs such as TAUP, LOSH, HMAP and McMaille, though I have little doubt that they would also have succeeded. The Crysfire version actually used was Crysfire 2003 (32-bit), but Crysfire 2002 would have produced exactly the same outcomes. Since the resulting cell is quite close to the published STF type cell, and clearly belongs to the same family, the question arises as to why the original author did not have sufficient confidence to propose an indexing. Perhaps the reason that a cell was not reported is that, although UPPW-4 is clearly at least closely related to the type-structure given in the zeolite database, it is not quite straightforward to proceed directly to its cell simply by least-squares refinement, taking the published STF cell as starting point. Thus attempts to refine directly from the STF cell in the database (C2/m; 14.104, 18.205, 7.477; 98.989; V=1896.25) using all 25 lines, at least with Celref, stick in a local minimum in which 19 lines fit reasonably well (if not all to the expected accuracy of the data). However, although apparently not far from the correct minimum, the remaining 6 lines (lines 4, 10, 12, 14, 19 & 22) remain unindexed and even look a little as if they might come from a second phase. This local minimum can be escaped by starting the refinement at lower resolution by using only the first 8 observed lines. The STF cell then converges with Celref to what is effectively the correct cell in just one cycle: a = 13.978, b = 18.391, c = 7.444 A, beta = 99.44 deg with the following shifts: -0.12 (-9%) +0.19 (10%) -0.03 (-0.4%) -0.55° Introducing the rest of the data and including a 2Theta zero correction then gives the fully refined C2/m cell, as reported above. Robin Shirley