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THE FIRST ONLINE EVENT OF THE ITALIAN YOUNG CRYSTALLOGRAPHERS

28th-30th September 2020

Book of Abstracts

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Steering Commitee

Chair Paolo P. Mazzeo – Università di Parma, IT Giorgia Confalonieri – Università di Modena, IT Andrea Giaccherini – Università di Firenze, IT Marta Morana – Università di Pavia, IT

Scientific Commitee

Chair Andrea Giaccherini - Università di Firenze, IT Matteo Alvaro – Università di Pavia, IT

Danilo Belviso – CNR, IT

Luca Catalano – University of Liverpool, UK Davide Comboni – ESRF, FR

Simona Fermani – Università di Bologna, IT Carlotta Giacobbe – ESRF, FR

Annalisa Guerri – Università di Firenze, IT Andrea Ienco – CNR, IT

Lucia Maini – Università di Bologna, IT

Silvia Onesti – ELETTRA sincrotrone, IT

Emanuele Priola – Università di Torino, IT

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Video

MS1 Materials and Minerals

Luca Catalano Switchable supramolecular trajectories in techanosynthesis of a halogen-bonded

borromean network: it is about the journey, not the destination. 4 Davide Comboni High-pressure behaviour and phase stability of kernite, Na2B4O6(OH)2·3H2O 5 Gregorio Dal Sasso Designing N- and P- smart nanofertilizers based on nitrate-doped calcium phosphate

Nanoparticles 6

Michela La Bella Understanding the hydration process of gypsum plaster using a combined approach of

diffraction and phase contrast tomography 7

Giovanni O. Lepore Local chemical ordering in the Al8Cr17Co17Cu8Fe17Ni33 compositionally complex alloy 8 Francesco Marin Polymorphism of perylene diimides, thermal and mechanical analysis and role of the

alkyl chains 9

Sabrina Nazzareni Magma water content of pico volcano (azores islands, portugal): clinopyroxoxene

perspective 10

Elena Possenti Potential of non-conventional analytical methods to study inorganic treatments applied

to CH stone artefacts 11

Rebecca Scatena Formate-mediated Magnetic Superexchange in the Model Hybrid Perovskite

[(CH3)2NH2]Cu(HCOO)3 12

Anna Vivani Wide angle X-ray Total Scattering analysis of highly stable CsPbBr3 Nanoplatelets 13

MS2 Materials and Minerals

Isabella Bolognino Enantiorecognition of dihydropyrimidine-based antagonists of adenosine A2B receptor by teicoplanin-based chiral stationary phases

14 Sara Chiarugi Insights into human membrane NAPE-PLD interactions 15 Ludovica Lopresti Structural insight into YAP-TEAD4 protein-protein interactions as target for cancer

treatment

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Giusy Tassone Identification of phosphate-containing compounds as new inhibitors of 14-3-3/c-Abl protein–protein interaction

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MS3 Crystal Growth

Mattia La Fortezza Epiaxial match drives the Growth of magnetite microinclusions in mlivine in rocks

recording deserpentinization under mantle Conditions 18

Francesco Pagliaro Crystal chemistry and behavior at non-ambient conditions of natural REE–arsenates and

–phosphates 19

Emanuele Priola Cocrystallization, high pressure/low temperature behaviour and vapochromism in a

family of aurophilic Copper-Gold Supramolecular networks. 20

MS4 Theory and methods

Laura Contini Using the Cambridge Structural Database to study the role of the halide in the formation

of argentophilic interaction in XAgL compounds 21

Laura Dall’Olio Direct derivation of the crystalline fraction of highly potent active pharmaceutical

ingredients via X-ray powder diffraction 22

Pietro Sacchi Same or different – that is the question: identification of crystal forms from crystal

structuredata 23

Laura Samperisi Exploring molecular gigantism with continuous rotation electron diffraction 24

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Video - MS3 Crystal growth

Crystal chemistry and behavior at non-ambient conditions of natural REE–arsenates and –phosphates

Francesco Pagliaro [1], Paolo Lotti [1], Alessandro Guastoni [2], Davide Comboni [3], Nicola Rotiroti [1], Giacomo Diego Gatta [1]

[1] Università degli Studi di Milano [2] Università degli Studi di Padova

[3] European Synchrotron Radiation Facility, Grenoble

Rare earth elements (REE) represent a group of 15 elements, divided into LREE (La-Eu) and HREE (Gd- Lu) on the basis of their atomic weight coupled with decreasing atomic radii from La to Lu. REE are classified as critical raw materials by the European Commission, due to their elevated supply risk and high economic importance. Several studies have been dedicated to the chemical and physical properties of REE-bearing natural compounds, in order to better understand the conditions at which these minerals form, as well as to identify new strategies useful for mining and exploitation of mineral resources.

The present contribution belongs to a larger project, focusing on four mineralogical species occurring within the REE-enriched pegmatitic dikes and alpine fissures that crop out at Mt. Cervandone (Western Alps, Italy):

monazite-(Ce), xenotime-(Y), chernovite-(Y) and gasparite-(Ce). These minerals have the general formula ABO4, where A is populated by Y or a REE metal and B by P or As. Monazite-(Ce) (ideally REEPO4) and gasparite- (Ce) (REEAsO4) crystallize in the monoclinic P21/n space group, whereas xenotime-(Y) [(Y,REE)PO4] and chernovite-(Y) [(Y,REE)AsO4] show tetragonal symmetry (s.g.: 41/amd). We aim to characterize: the crystal chemistry and crystal structures, (P,T)-phase stability and possible phase transitions, thermo-elastic behaviors and structural re-arrangements at non-ambient conditions of these minerals.

Here we present the preliminary data obtained so far, which include: 1) the crystal-chemical and structural charac- terization of samples of monazite-(Ce), xenotime-(Y), chernovite-(Y) and gasparite-(Ce) from Mt. Cervandone, by means of WDS-EPMA and single-crystal X-ray diffraction analyses; 2) the isothermal high-P behavior of gasparite-(Ce) (at ambient-T, investigated for the first time) up to 10 GPa, by means of in situ single-crystal synchrotron X-ray diffraction using a diamond anvil cell. Gasparite-(Ce) does not experience any P-induced phase transition within the P-range investigated. A II-order Birch-Murnaghan equation of state was fitted on the V-P data, yielding a refined bulk modulus KP0,T0 = 106.7(9) GPa and V0= 323.8(1) Å3. P-induced struc- tural deformation mechanisms at the atomic scale will be discussed.

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