Crystal structure of the amino acid-vitamin complex lysine pantothenatestar, open

L-Lysine d-pantothenate, a 1:1 amino acid-vitamin complex, crystallizes in the monoclinic space group P21 with Image Full-size image (1K) .The structure has been solved by direct methods and refined to an R value of 0.053 for 1868 observed reflections. The zwitterionic positively charged lysine molecules in the structure assume the sterically most favourable conformation with an all-trans side chain trans to the α-carboxylate group. The pantothenate anion has a somewhat folded conformation stabilised by an intramolecular bifurcated hydrogen bond. The unlike molecules aggregate into separate alternating layers. The molecules in the lysine layers form a head-to-tail sequence parallel to the a-axis. The interactions which hold the adjacent layers together include those between the side chain amino group of lysine and the carboxylate group in the pantothenate anion. The geometry of these interactions is such that each carboxylate group is sandwiched between two amino groups in a periodic arrangement of alternating carboxylate and amino groups.

Conformational analysis of D-pantothenic acid

The conformational analysis of d-pantothenic acid using classical semiempirical methods has been carried out. The pantothenic acid molecule can exist in the neutral form (I) or in the ionised form (II) with a deprotonated negatively charged carboxyl group. The neutral molecule as well as the anion is highly flexible and has an ensemble of several allowed conformations rather than one or two unique conformations. The distribution of allowed conformations indicate that the β-alanine as well as the pantoic acid part of the molecule prefers partially folded conformations. The conformation of the former is greatly affected by the ionisation state of the carboxyl group whereas that of the latter is not. Possibility of intramolecular hydrogen bonding in different allowed conformations has also been explored. A bifurcated hydrogen bond involving a carboxyl (or carboxylate) oxygen atom and a hydroxyl oxygen atom, as acceptors, and the amide nitrogen atom as the donor occurs frequently in both I and II. Amongst the two crystal structures containing pantothenic acid reported so far, the conformation of the molecule in l-lysine d-pantothenate lies in the allowed region and is stabilised by a bifurcated intramolecular hydrogen bond, whereas that in the calcium bromide salt falls in a disallowed region, presumably due to the requirement of tridentate metal coordination.

Le determinanti degli investimenti diretti esteri in Italia nel settore agroalimentare

Gli investimenti diretti esteri (IDE) giocano un ruolo importante nella crescita economica e nello sviluppo territoriale. Con il notevole aumento dei flussi IDE nel settore agroalimentare a livello mondiale l’attenzione si è concentrata sul dibattito relativo alle determinanti che spingono alla scelta di un territorio piuttosto che un altro. Non esiste ancora un lavoro definitivo ed univoco sulle determinanti degli IDE. Alcune delle più frequenti analisi sui fattori che influenzano gli IDE includono: l’entità del mercato, il costo del lavoro, i tassi di interesse, le barriere protezionistiche, tassi di cambio, predisposizione all’export, struttura del mercato, distanze geografiche, stabilità politica e affinità culturale. Questo lavoro si propone di analizzare le determinanti nel settore agroalimentare italiano sia teoricamente che empiricamente. A questo scopo è stata applica come base teorica il paradigma OLI di Dunning e i principi legati agli investimenti orizzontali al settore agroalimentare regionale italiano. Sono state esaminate le determinanti degli investimenti diretti inward in questo settore. Le risultanti suggeriscono una relazione positiva tra la presenza di attività di servizi e la presenza di IDE nelle diverse Regioni. In un Paese ad economia avanzata come l’Italia, strategie territoriali e di impresa basate sui costi e sul mercato non sono caratterizzanti per attrarre multinazionali straniere, mentre la dotazione di servizi e infrastrutture rappresentano un nuovo obiettivo su cui le Regioni devono puntare per aprire i territori alle sfide della globalizzazione. Questa ricerca unisce analisi statistica ed econometria e studio bibliografico per approfondire e comprendere la materia in oggetto e fornire nuovi elementi e spunti su cui discutere.

Chemical composition of ferromanganese concretions and host bottom sediments from the Black Sea

Ferromanganese concretions spread out on the bottom of the shallow northwest part of the Black Sea are mainly represented by Fe and Mn nodules on shells and substituted worm tubes. Element composition of these formations was measured by methods of chemical, atomic absorbtion, neutron activation, and ICP-MS analyses. It was established that Fe and Mn contents and Mn/Fe ratio in the concretions varied considerably and which controlled occurrence of several associated metals and minor elements; some of them have not been studied in Black Sea concretions before.

Letters from Timothy Pickering to his brother and father, 1797-1798

These two handwritten letters by Timothy Pickering were written on February 14, 1797 and June 14, 1798 to his brother John Pickering and his father Timothy Pickering, respectively. The letter to his brother, John, discusses mutual friends, classmate Thomas Lee, and John’s recent attendance at a sermon by Dr. Joseph Priestley. The letter from Timothy to his father includes a discussion of Timothy’s expenses and the amount of money needed to pay his debts, a request for new shoes for commencement, the news of Timothy’s invitation to join honor society Phi Beta Kappa, and a few comments on his forensics course at Harvard.

Uranium in Black Sea bottom sediments

Results of uranium content determinations in 76 samples of surface layer bottom sediments, from sediment cores, and deep-sea drilling cores are reported. These data confirm previously established regularities of uranium distribution in Black Sea bottom sediments. The main factors of its concentration are hydrochemical features of the hydrogen sulfide enrichment zone and enrichment of deep-sea sediments in organic matter resulting to increase (4-6 times) of uranium content in comparison with its average content in sedimentary rocks.