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Synthetic, structural, spectroscopic and aging studies conclusively show that the main colorant of historical iron gall ink (IGI) is an amorphous form of Fe(III) gallate• xH 2 O (x = ∼1.5−3.2). Comparisons between experimental samples and historical documents, including an 18th century hand-written manuscript by George Washington, by IR and Raman spectroscopy, XRD, X-ray photoelectron spectroscopy, and Mossbauer spectroscopy confirm the relationship between the model and authentic samples. These studies settle controversy in the cultural heritage field, where an alternative structure for Fe(III) gallate has been commonly cited.P rior to the 20th century, historical iron gall ink (IGI) was by far the most common writing material of the western world, and a plethora of recipes from which to produce the ubiquitous dark, brown-black ink can be found starting from at least the Middle Ages. This ink has been used to pen many of the most important documents and drawings in human history, including unique, hand-written works such as Thomas Jefferson's original draft of the Declaration of Independence, Abraham Lincoln's first draft of the Emancipation Proclamation, and Beethoven's original scores. While the virtue of IGI lies in its relative permanence, the great vice of this medium lies in its well-known tendency to degrade paper and parchment substrates. 1−7 Despite its historical importance, there is little consensus on the chemical structure or composition of the iron-gallate complex, the main species responsible for the color of the IGI. We describe here a series of synthetic, structural, spectroscopic, and aging studies, which unequivocally demonstrate that the primary colorant in IGI is an amorphous form of an octahedral Fe(III) gallate metal organic framework structure that has previously been described by Wunderlich 8−10 and Feller. 11 Unlike the majority of prior studies, we use authentic IGI precursors to prepare both crystalline and amorphous forms of the IGI precipitate and study the crystal-to-amorphous transition by way of XRD, thermal gravimetric analysis (TGA), IR and Raman, Mossbauer, and X-ray photoelectron spectroscopy (XPS). Spectroscopic comparisons with historical documents prove the relevance of the synthetic crystalline and amorphous forms of the model IGI materials to those found in the authentic manuscripts.

The pH-dependence and solvent isotope effects of dealkylation in diastereomeric adducts of Electric eel (Ee) and fetal bovine serum (FBS) acetylcholinesterase (AChE) inactivated with P(-)C(+) and P(-)C(-) 2-(3,3-dimethylbutyl) methylphosphonofluoridate (soman) were studied at 4.0 +/- 0.2 degrees C. The rate constant versus pH profiles were fit to a bell-shaped curve for all adducts. Best fit parameters are pK1 4.4-4.6 and pK2 6.3-6.5 for Ee AChE and pK1 4.8-5. 0 and pK2 5.8 for FBS AChE. The pKs are consistent with catalytic participation of the Glu199 anion and HisH+440. Maximal rate constants (kmax) are 13-16 x 10(-3) s-1 for Ee AChE and 8 x 10(-3) s-1 for FBS AChE. The solvent isotope effects at the pH maxima are 1.1-1.3, indicating unlikely proton transfer at the enzymic transition states for the dealkylation reaction. Slopes of log rate constant versus pH plots are near 1 at 25.0 +/- 0.2 degrees C between pH 7.0 and 10.0. In stark contrast, the corresponding adducts of trypsin are very stable even at 37.0 +/- 0.2 degrees C. The rate constants for diastereomers of soman-inhibited trypsin at 37.0 +/- 0.2 degrees C are pH independent and approximately 10(4) times smaller than kmax for analogous adducts with AChE. Dealkylation in soman-inhibited AChEs is estimated to occur at >10(10) times faster than a plausible nonenzymic reaction. Up to 40% of the catalytic acceleration can be attributed to an electrostatic push, and an electrostatic pull provides much of the balance. The results of this work together with results of a product analysis by Michel et al. (1969) can be explained by an initial and rate-determining methyl migration from Cbeta to Calpha. This is driven by the high electron density of residues (Glu199 and Trp84) at a crowded active site and may be concerted with C-O bond breaking. The positive charge at the rate-determining transition state is distributed between Cbeta and His440. A tertiary carbocation may have a fleeting existence before it is trapped by water or neighboring electrons which is likely to be promoted by Glu199 as the proton acceptor.