Problemi di consolidamento di matrici lapidee di differente microstruttura esposte a sollecitazioni ambientali e microclimatiche di varia origine

Questa ricerca presenta i risultati di una indagine volta a verificare la reale efficacia di rinforzo corticale su rocce carbonatiche di differenti caratteristiche mineralogiche, utilizzando consolidanti inorganici in soluzione acquosa quali l’Ossalato Ammonico (AmOX) e il Diammonio Fosfato Acido (DAHP). Le matrici carbonatiche scelte sono quelle del marmo invecchiato e una biomicrite. Sui campioni sono state effettuate indagini (SEM,MIP,XRD,MO,TG-DTA) di caratterizzazione prima e dopo i trattamenti volte a valutare eventuali effetti di rinforzo e misure fisiche di suscettività all’acqua. L’efficacia dei consolidanti inorganici è stata comparata con diversi consolidanti organici e ibridi presenti in commercio ed utilizzati in ambito conservativo. L'efficacia si è mostrata fortemente legata al fabric del materiale e alle modalità di strutturazione del prodotto di neomineralizzazione all’interno della compagine deteriorata. Nel caso del trattamento con AmOx il soluzione acquosa al 4%, la whewellite è l’unica fase di neoformazione riscontrata; la sua crescita avviene con un meccanismo essenzialmente topochimico. Nei materiali carbonatici compatti si possono ottenere solo modesti spessori di coating di neoformazione; per le rocce porose, contenenti difetti come lesioni, pori o micro-fratture, l’efficacia del trattamento può risultare più incisiva. Questo trattamento presenta lo svantaggio legato alla rapidissima formazione dei cristalli di whewellite che tendono a passivare le superfici impedendo la progressione della reazione; il vantaggio è connesso alla facile applicazione in cantiere. Nel caso del DAHP sulla matrice carbonatica trattata, si formano cluster cristallini contenenti specie più o meno stabili alcune riconducibili all’idrossiapatite. La quantità e qualità delle fasi, varia fortemente in funzione della temperatura, pH, pressione con conseguenze interferenza nelle modalità di accrescimento dei cristalli. Il trattamento alla stato attuale appare comunque di notevole interesse ma allo stesso tempo difficilmente applicabile e controllabile nelle reali condizioni operative di un cantiere di restauro.

Lateral spreading and associated slope processes in fractured rock slabs

Landslides of the lateral spreading type, involving brittle geological units overlying ductile terrains, are a common occurrence in the sandstone and limestone plateaux of the northern Apennines of Italy. These instability phenomena can become particularly risky, when historical towns and cultural heritage sites built on the top of them are endangered. Neverthless, the mechanisms controlling the developing of related instabilities, i.e. toppling and rock falls, at the edges of rock plateaux are not fully understood yet. In addition, the groundwater flow path developing at the contact between the more permeable units, i.e. the jointed rock slab, and the relatively impermeable clay-rich units have not been already studied in details, even if they may play a role in this kind of instability processes, acting as eventual predisposing and/or triggering factors. Field survey, Terrestrial Laser Scanner and Close Range Photogrammetry techniques, laboratory tests on the involved materials, hydrogeological monitoring and modelling, displacements evaluation and stability analysis through continuum and discontinuum numerical codes have been performed on the San Leo case study, with the aim to bring further insights for the understanding and the assessment of the slope processes taking place in this geological context. The current research permitted to relate the aquifer behaviour of the rocky slab to slope instability processes. The aquifer hosted in the fractured slab leads to the development of perennial and ephemeral springs at the contact between the two units. The related piping erosion phenomena, together with slope processes in the clay-shales led to the progressive undermining of the slab. The cliff becomes progressively unstable due to undermining and undergoes large-scale landslides due to fall or topple.

Abituàti a morire: Uno sguardo sulla scena punk-rock siberiana degli anni '80

Il presente elaborato ha lo scopo di fornire una panoramica sul movimento punk siberiano, nato e sviluppatosi a cavallo fra il 1984 e il 1991. L'analisi della poetica di alcuni fra i musicisti principali del cosiddetto "sibpunk" e la traduzione delle loro canzoni più significative costituiscono una prospettiva inusuale e interessante per osservare la Siberia negli anni della Perestrojka.

Differential requirement for ROCK in dendritic cell migration within lymphatic capillaries in steady-state and inflammation

Dendritic cell (DC) migration via lymphatic vessels to draining lymph nodes (dLNs) is crucial for the initiation of adaptive immunity. We imaged this process by intravital microscopy (IVM) in the ear skin of transgenic mice bearing red-fluorescent vasculature and yellow-fluorescent DCs. DCs within lymphatic capillaries were rarely transported by flow, but actively migrated within lymphatics and were significantly faster than in the interstitium. Pharmacologic blockade of the Rho-associated protein kinase (ROCK), which mediates nuclear contraction and de-adhesion from integrin ligands, significantly reduced DC migration from skin to dLNs in steady-state. IVM revealed that ROCK blockade strongly reduced the velocity of interstitial DC migration, but only marginally affected intralymphatic DC migration. By contrast, during tissue inflammation, ROCK blockade profoundly decreased both interstitial and intralymphatic DC migration. Inhibition of intralymphatic migration was paralleled by a strong up-regulation of ICAM-1 in lymphatic endothelium, suggesting that during inflammation ROCK mediates de-adhesion of DC-expressed integrins from lymphatic-expressed ICAM-1. Flow chamber assays confirmed an involvement of lymphatic-expressed ICAM-1 and DC-expressed ROCK in DC crawling on lymphatic endothelium. Overall, our findings further define the role of ROCK in DC migration to dLNs and reveal a differential requirement for ROCK in intralymphatic DC crawling during steady-state and inflammation.

Role of RhoA/ROCK-dependent actin contractility in the induction of tenascin-C by cyclic tensile strain

In chick embryo fibroblasts, the mRNA for extracellular matrix protein tenascin-C is induced 2-fold by cyclic strain (10%, 0.3 Hz, 6 h). This response is attenuated by inhibiting Rho-dependent kinase (ROCK). The RhoA/ROCK signaling pathway is primarily involved in actin dynamics. Here, we demonstrate its crucial importance in regulating tenascin-C expression. Cyclic strain stimulated RhoA activation and induced fibroblast contraction. Chemical activators of RhoA synergistically enhanced the effects of cyclic strain on cell contractility. Interestingly, tenascin-C mRNA levels perfectly matched the extent of RhoA/ROCK-mediated actin contraction. First, RhoA activation by thrombin, lysophosphatidic acid, or colchicine induced tenascin-C mRNA to a similar extent as strain. Second, RhoA activating drugs in combination with cyclic strain caused a super-induction (4- to 5-fold) of tenascin-C mRNA, which was again suppressed by ROCK inhibition. Third, disruption of the actin cytoskeleton with latrunculin A abolished induction of tenascin-C mRNA by chemical RhoA activators in combination with cyclic strain. Lastly, we found that myosin II activity is required for tenascin-C induction by cyclic strain. We conclude that RhoA/ROCK-controlled actin contractility has a mechanosensory function in fibroblasts that correlates directly with tenascin-C gene expression. Previous RhoA/ROCK activation, either by chemical or mechanical signals, might render fibroblasts more sensitive to external tensile stress, e.g., during wound healing.

Different migration of vascular smooth muscle cells from human coronary artery bypass vessels. Role of Rho/ROCK pathway

BACKGROUND: We examined whether vascular smooth muscle (VSMC) or endothelial cell (EC) migration from internal mammary artery (MA) differed from VSMC or EC migration from saphenous vein (SV). METHODS AND RESULTS: Migration to PDGF-BB (1-10 ng/ml) was lower in VSMC from MA than SV; however, attachment, movement without chemokine, and chemokinesis were identical. Unlike VSMC, migration of EC was similar in response to several mediators. Expression of PDGF receptor-beta was lower in VSMC from MA than SV, while alpha-receptor expression was higher. PDGF-BB-induced RhoA activity was lower in MA than SV, while basal activity was identical. Rosuvastatin and hydroxyfasudil impaired PDGF-BB-induced migration of VSMC from MA and SV. Mevalonate and geranylgeranylpyrophosphate rescued inhibition by rosuvastatin. PDGF-BB induced less stress fiber formation in VSMC from MA than SV. A dominant negative RhoA mutant inhibited stress fiber formation to PDGF-BB, while a constitutively active mutant resulted in maximal stress fiber formation in MA and SV. Rosuvastatin and hydroxyfasudil impaired PDGF-BB-induced stress fiber formation in MA and SV. CONCLUSIONS: VSMC migration to PDGF-BB is lower in MA than SV, which is at least in part related to lower activity of the Rho/ROCK pathway.