Aging in Charged Colloidal SystemsColloidal <strong>di</strong>spersions are a very interesting class ofmatter. Due to their rich phenomenology andproperties they can be used to test a large variety oftheoretical models, or vice versa theories can besubjected to stringent experimental tests. In somecases in fact the inter-particle interactions can betuned almost ad-hoc, e. g. by changing the ionicstrength in the system. In this context the study ofLaponite system is particularly intriguing. LaponiteRD is a <strong>di</strong>sk like clay particle with a well definedthickness of 2H=1 nm and a <strong>di</strong>ameter of about2R=30 nm (fig. 1A). When laponite is <strong>di</strong>spersed inwater a strong negative charge appears on faceswhile, depen<strong>di</strong>ng on the pH of the solution, a weakpositive or negative charge appears on the rim.Therefore in this colloidal system long rangeelectrostatic repulsion and short range attractiveinteractions are both present and the competitionbetween the two interactions makes Laponitesuspensions even more interesting.In particular a new phase <strong>di</strong>agram has shown as wecan be in presence of phase separation, liquid,attractive gel, attractive or repulsive glass, justchanging the clay amount and/or the presence ofsalt in the solutions [2]. For this reasons we canconsider Laponite suspensions as a model system todescribe <strong>di</strong>sk like charged particles in presence ofboth short range attraction and long range repulsion.We performed a dynamic light scattering study of theaging phenomenology in laponite <strong>di</strong>spersions inwater, varying clay and salt concentrations. Allsamples stu<strong>di</strong>ed, surprisingly also those pre<strong>di</strong>cted tobe in a liquid stable phase, experience aging (fig.1B).After a certain waiting time, starting when thesample is filtered, a non ergo<strong>di</strong>c state is reached asshown from an incomplete decay of theautocorrelation function (fig.1B). More the sample isconcentrated less is the waiting time necessary toobtain an arrested phase. Moreover, at a fixedlaponite concentration, this time decreases withad<strong>di</strong>ng salt, reflecting the screening of the repulsivepart of the interaction between particles. All theautocorrelation data show two dynamical regimes.The fast “<strong>di</strong>ffusive” behavior is described by a singleexponential decay with a fast relaxation time τ 1. Theslow one is well described by a stretched exponentialdecay defined by the relaxation time τ 2 and thestretching exponent β. From the analysis of thewaiting time behavior of the slow dynamics it ispossible to identify two dynamical routes to reach afinal arrested state, one at "low" (open circles in fig.1C) and one at "high" (full circles in fig. 1C) clayconcentrations. This dynamical <strong>di</strong>fference should bea signature of two <strong>di</strong>fferent structuralrearrangements of the system realized because ofthe competition between the repulsive and theattractive parts of the potential. These new resultsdetermines a redrawn of a part of the phase <strong>di</strong>agram(fig. 1C). In particular the pre<strong>di</strong>cted liquid region (ILin fig. 1C) is found not to be a stable phase, aspreviously determined, but an arrested phase.Moreover the presence of two <strong>di</strong>fferent arrestedstates, one at "low" and one at "high" clayconcentrations, and a transition line between themare identified [3],[4] .References[1] A. Mourchid, A. Delville, J. Lambard, E. Lecolier,and P. Levitz, Langmuir 11, 1942 (1995).[2] H. Tanaka, J. Meunier, and D. Bonn, Phys. Rev. E69, 031404 (2004).[3] B. Ruzicka, L.Zulian and G. Ruocco, Phys. Rev.Lett. 93, 258301 (2004).[4] B. Ruzicka, L.Zulian and G. Ruocco, Langmuir,22, 1106 (2006).Fig.1: (A) Laponite crystal. (B) Agingphenomenon in sample with C w=1.0%, C s=2x10 -3 M. (C) Phase <strong>di</strong>agram of Laponite <strong>di</strong>spersion, thered line in<strong>di</strong>cates the hypothesized new transitionline between two <strong>di</strong>fferent arrested states.AuthorsB. Ruzicka (a), L. Zulian (b,a), G. Ruocco (c,a)(a) CRS SOFT-CNR-INFM, c/o Universita’ <strong>di</strong> Roma« La <strong>Sapienza</strong> » P.le A. Moro 2, 00185 Roma.(b) <strong>Dipartimento</strong> <strong>di</strong> <strong>Fisica</strong> Universita’ degli stu<strong>di</strong> <strong>di</strong>Perugia, via A. Pascoli 06123, Perugia, Italy.(c) <strong>Dipartimento</strong> <strong>di</strong> <strong>Fisica</strong>, Universita’ Roma « La<strong>Sapienza</strong> », P.le A. Moro 2, 00185, Roma, Italy.79SOFT Scientific <strong>Report</strong> 2004-06
Scientific <strong>Report</strong> – Non Equilibrium Dynamics and ComplexityMatter Under High PressureHigh pressure amorphyzation of carbon <strong>di</strong>oxideAmong the group IV elements, carbon is the uniquethat at ambient con<strong>di</strong>tion forms stable double bondswith oxygen. In contrast to the cases of SiO2 andGeO2 the nonmolecular tetrahedral crystalline formof CO2, phase V, only exists at high pressure.Similarly, while the amorphous phases of SiO2 (asilica)and GeO2 (a-germania) are well known andstable at room con<strong>di</strong>tion, the amorphous,nonmolecular, phase of CO2, although pre<strong>di</strong>cted byab-initio simulations, had not yet been <strong>di</strong>scovered.Byusing a resistive heated Diamond Anvil Cell we couldsynthesize amorphous, silica-like, carbon <strong>di</strong>oxide.The non molecular amorphous phase of carbon<strong>di</strong>oxide, a-CO2, that for similarity with othera-CO 2100 µmFig. 1. Photograph of Carbonia at 61 GPa. androom temperature. The sample is transparent andspatially homogeneous.amorphous oxide of the group IV we have called a-carbonia, was attained by compressing molecularphase III above 47 GPa at room temperature.In situ infrared spectra, measured with raisingtemperature up to 680 K, probe the progressiveformation of C-O single bonds and the simultaneous<strong>di</strong>sappearing of the molecular signatures. State-ofthe-artRaman and synchrotron x-ray <strong>di</strong>ffractionmeasurements on the temperature quenched sampleshow the amorphous character of this material. Thecomparison with vibrational and <strong>di</strong>ffraction patternsof amorphous silica and germania, shows that a-carbonia is homologous to those glasses. The staticstructure factor of a-CO2 has also been calculated byab initio techniques (Sandro Scandolo), reproducingthe main features of the experimental pattern.These fin<strong>di</strong>ngs do extend the scenario of archetypalnetwork-forming <strong>di</strong>sordered systems such as a-silica,a-germania, a-Si and a-Ge, and water.References[1] M.Santoro, F.Gorelli, G.Ruocco, R.Bini,S.Scandolo and W.Crichton, “Carbonia: theamorphous silicalike carbon <strong>di</strong>oxide” (in preparation)AuthorsM.Santoro (a,b), F.A.Gorelli (a,b), , G.Ruocco (a,d),R. Bini (b,e), S.Scandolo (f) and W.Crichton (g).(a) INFM-CRS-<strong>Soft</strong> Matter (CNR), Univ. la <strong>Sapienza</strong>.(b) LENS, Univ. <strong>di</strong> Firenze. (c) Dip. <strong>di</strong> <strong>Fisica</strong>, Univ. <strong>di</strong>Firenze. (d) Dip. <strong>Fisica</strong>, Univ. La <strong>Sapienza</strong>, Roma. (e)Dip. Chimica, Univ. <strong>di</strong> Firenze. (f) ICTP-DNSC,Trieste, Italy (g) ESRF, Grenoble, FranceInelastic scattering of X rays from overcriticalfluids at high pressureThe possibility of performing inelastic X rayscattering measurements on low Z materials in theDiamond Anvil Cell has been recently demonstratedwith an experiment on liquid water (Krisch et alPhys. Rev. Lett. 89, 125502 (2002)). We performedan inelastic X ray scattering experiment on ID 28beamline of ESRF on overcritical fluid Oxygen at highpressure using a Diamond Anvil Cell. As the criticaltemperature of Oxygen is about 155 K and weperformed the measurements at room temperature,it implies a value of T/T c equal to about 2. Wecollected data at about 1, 3 and 5 GPa and comparedthe sound velocity with the a<strong>di</strong>abatic one measuredby Abramson et al (J. Chem. Phys. 110, 10493(1999)). It results a positive <strong>di</strong>spersion of about 20%at all pressures which has never been reported for anovercritical fluid, and on the contrary it is an or<strong>di</strong>narybehaviour of liquids.This result has been compared to previous data onNitrogen, Neon and Mercury in<strong>di</strong>cating that themetastable extension of the liquid-vapourcoexistence line beyond the critical point splits the PT<strong>di</strong>agram in two regions correspon<strong>di</strong>ng to two<strong>di</strong>fferent regimes for what concerns the positive<strong>di</strong>spersion.This experiment has to be followed by similar oneson under/overcritical fluids at high pressure in orderto better elucidate this result.AuthorsF.A.Gorelli (a,b), M.Santoro (a,b), G.Ruocco (a,d),T.Scopigno (a,d) and A. Beraud (e).(a) INFM-CRS-<strong>Soft</strong> Matter (CNR), Univ. la <strong>Sapienza</strong>.(b) LENS, Univ. <strong>di</strong> Firenze. (c) Dip. <strong>di</strong> <strong>Fisica</strong>, Univ. <strong>di</strong>Firenze. (d) Dip. <strong>Fisica</strong>, Univ. La <strong>Sapienza</strong>, Roma. (e)ESRF (Grenoble), France (f) ICTP-DNSC, Trieste.Phase <strong>di</strong>agram and vibrational spectroscopy ofpolymers at high pressurePolyethylene is the most widely used polymericmaterial but very little is known about its propertiesat high pressure. We performed an infraredabsorption and Raman scattering study ofpolyethylene at high pressure and temperatures inthe range 0-60 GPa e 300-650 K. We also performedan X ray <strong>di</strong>ffraction experiment in the same PT rangein order to have structural information to couple tovibrational data. The whole data sets are alsocompared with simulations provided by a theoreticalgroup in Trieste (Sandro Scandolo, ICTP)AuthorsL.Fontana (a), M.Santoro (a,b), F.A.Gorelli (a,b),S.Scandolo (c), R. Bini (a,d) and M.Hanfland (e).(a) LENS, Univ. <strong>di</strong> Firenze. (b) INFM-CRS-<strong>Soft</strong> Matter(CNR), Univ. la <strong>Sapienza</strong>. (c) ICTP-DNSC, Trieste.(d) Dip. Chimica, Univ. <strong>di</strong> Firenze. (e) ESRF(Grenoble), France.SOFT Scientific <strong>Report</strong> 2004-0680
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