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Theoretical and Numerical Modeling of Nonlinear Electromechanics with applications to Biological Active Media

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Communications in Computational Physics 2015年第1期17卷 93-126页

作者： Alessio Gizzi Christian Cherubini Simonetta Filippi anna pandolfi Nonlinear Physics and Mathematical Modeling Laboratory ***University Campus Bio-Medico of RomeVia A.del Portillo 2100128 RomeItaly International Center for Relativistic Astrophysics Network ***University Campus Bio-Medico of RomeVia A.del Portillo 2100128 RomeItaly Civil and Environmental Engineering Department Politecnico di Milano Piazza Leonardo da Vinci 3220133 MilanoItaly

We present a general theoretical framework for the formulation of the nonlinear electromechanics of polymeric and biological active *** approach developed here is based on the additive decomposition of the Helmholtz free energy in elastic and inelastic parts and on the multiplicative decomposition of the deformation gradient in passive and active *** describe a thermodynamically sound scenario that accounts for geometric and material *** view of numerical applications,we specialize the general approach to a particular material model accounting for the behavior of fiber reinforced ***,we use the model to solve via finite elements a uniaxial electromechanical problem dynamically activated by an electrophysiological *** for nonlinear solid mechanics and computational electrophysiology are finally discussed.

关键词： Active electromechanical media Helmholtz free energy multiplicative decomposition of the deformation gradient active deformation active stress

Tendril-Based Climbing Plants to Model, Simulate and Create Bio-Inspired Robotic Systems

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Journal of Bionic Engineering 2015年第2期12卷 250-262页

作者： Renato Vidoni Tanja Mimmo Camilla pandolfi Faculty of Science and Technology Free University of Bolzano Piazza universith 3 91 O0 Bolzano Italy European Space Agency-Advanced Concepts Team Estec Noordwjik Netherlands

Bioinspiration can be considered one of the keys for future smart and versatile robotic systems. Plants could be an im- portant source of ideas despite the fact that they have not yet been deeply observed and considered. In this paper, climbing tendril-bearer plants that, by means of irritable filiform organs called tendrils, search for a support, grasp it and climb to gain height, have been used to study and develop an effective climbing robot. The study aimed first to evaluate the main movements and behaviors of the tendril from a biomimetic point of view. The tendril complexity was then simplified, a robotic model was developed and a kinematic simulator was designed and implemented to visualize and evaluate the chosen system. Finally, based on the biological, technical and numerical evaluations, the main tendril behaviors were replicated by proof of concept devices made of smart materials to move towards a practical realization and to replicate the simulated results. The designed proof of concept prototypes showed food repeatability and feasibility.

关键词： climbing plants robotic tendril kinematic model Shape-Memory-Alloy (SMA) grasping

Osteogenic differentiation of amniotic fluid mesenchymal stromal cells and their bone regeneration potential

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World Journal of Stem Cells 2015年第4期7卷 681-690页

作者： Caterina Pipino Assunta pandolfi Department of Medical Oral and Biotechnological Sciences"G.d’ Annunzio"University Aging Research Center Ce.S.I."Gabriele d’Annunzio" University Foundation StemTeCh Group

In orthopedics, tissue engineering approach using stem cells is a valid line of treatment for patients with bone defects. In this context, mesenchymal stromal cells of various origins have been extensively studied and continue to be a matter of debate. Although mesenchymal stromal cells from bone marrow are already clinically applied, recent evidence suggests that one may use mesenchymal stromal cells from extra-embryonic tissues, such as amniotic fluid, as an innovative andadvantageous resource for bone regeneration. The use of cells from amniotic fluid does not raise ethical problems and provides a sufficient number of cells without invasive procedures. Furthermore, they do not develop into teratomas when transplanted, a consequence observed with pluripotent stem cells. In addition, their multipotent differentiation ability, low immunogenicity, and anti-inflammatory properties make them ideal candidates for bone regenerative medicine. We here present an overview of the features of amniotic fluid mesenchymal stromal cells and their potential in the osteogenic differentiation process. We have examined the papers actually available on this regard, with particular interest in the strategies applied to improve in vitro osteogenesis. Importantly, a detailed understanding of the behavior of amniotic fluid mesenchymal stromal cells and their osteogenic ability is desirable considering a feasible application in bone regenerative medicine.

关键词： Mesenchymal stromal cells Amniotic fluid Amniotic fluid mesenchymal stromal cells Amniotic fluidstem cells Osteogenesis Bone regeneration

Lower Continental Crusts Involved in the Alpine Orogeny:New Insight from the Santa Lucia Nappe Metasediments(Corsica,France)

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Acta Geologica Sinica(English Edition) 2024年第4期98卷 904-920页

作者： Chiara FRASSI Maria DI ROSA Luca pandolfi Michele MARRONI Dipartimento di Scienze della Terra Universitàdi PisaVia Santa Maria 5356126 PisaItaly Istituto di Geoscienze e Georisorse IGG-CNRVia Moruzzi50124 PisaItaly

In the Alpine Corsica(France),the Santa Lucia Nappe represents a peculiar unit preserving the unique relicts of Paleozoic lower to medium continental *** consists of composite basement affected by Permian granulite facies metamorphic conditions unconformably covered by a Late Cretaceous clastic sequence(Tomboni Conglomerate and Tralonca Flysch)affected by polyphase deformation and *** this work,we present a new reconstruction of the deformation events registered by the Tralonca Flysch during the Alpine *** D1 phase was testified by rare isoclinal *** D2 phase produced a continuous foliation and a map-scale sheath-fold with a top-to-W sense of *** D3 phase produced E-verging non-cylindrical folds and S3 crenulation cleavage that is not associated to metamorphic *** present the first temperature-pressure-deformation(P-T-d)path for the Tralonca Flysch,demonstrating that the Santa Lucia Nappe underwent accretion and then first stage exhumation in the Alpine wedge during the D1 phase with pressure and temperature peaks both occurred under blueschist metamorphic *** D2 phase occurred at lower pressure-temperature conditions during a second stage *** pressure-temperaturedeformation path is comparable with those of the Lower Units(i.e.,the subducted continental units of Alpine Corsica)suggesting a common geodynamic history.

关键词： blueschist-facies metamorphism P-T-d path Santa Lucia Nappe Corsica Alpine orogeny

Third-line rescue therapy for Helicobacter pylori infection

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World Journal of Gastroenterology 2006年第15期12卷 2313-2319页

作者： Rossella Cianci Massimo Montalto Franco pandolfi Giovan Battista Gasbarrini Giovanni Cammarota Department of Internal Medicine Endoscopy Unit Catholic University of Sacred HeartRomeItaly

H pylori gastric infection is one of the most prevalent infectious diseases worldwide. The discovery that most upper gastrointestinal diseases are related to Hpylori infection and therefore can be treated with antibiotics is an important medical advance. Currently, a first-line triple therapy based on proton pump inhibitor （PPI） or ranitidine bismuth citrate （RBC） plus two antibiotics （darithromycin and amoxicillin or nitroimidazole） is recommended by all consensus conferences and guidelines. Even with the correct use of this drug combination, infection can not be eradicated in up to 23% of patients. Therefore, several second line therapies have been recommended. A 7 d quadruple therapy based on PPI, bismuth, tetracycline and metronidazole is the more frequently accepted. However, with second-line therapy, bacterial eradication may fail in up to 40% of cases. When Hpylori eradication is striclly indicated the choice of further treatment is controversial. Currently, a standard third-line therapy is lacking and various protocols have been proposed. Even after two consecutive failures, the most recent literature data have demonsbated that Hpylori eradication can be achieved in almost all patients, even when antibiotic susceptibility is not tested. Different possibilities of empirical treatment exist and the available third-line strategies are herein reviewed.

关键词： Helicobacter pylori Third-line rescue therapy Antimicrobial resistance Levofloxacin Rifabutin Furazolidone Doxycycline

Deformation history and processes during accretion of seamounts in subduction zones:The example of the Durkan Complex(Makran,SE Iran)

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Geoscience Frontiers 2023年第2期14卷 182-203页

作者： Edoardo Barbero Maria Di Rosa Luca pandolfi Morteza Delavari Asghar Dolati Federica Zaccarini Emilio Saccani Michele Marroni Dipartimento di Fisica e Scienze della Terra Universitàdi Ferrara44123 FerraraItaly Istituto di Geoscienze e Georisorse Consiglio Nazionale delle Ricerche(CNR)10125 TorinoItaly Dipartimento di Scienze della Terra Universitàdi Pisa56126 PisaItaly Istituto di Geoscienze e Georisorse Consiglio Nazionale delle Ricerche(CNR)56124 PisaItaly Faculty of Earth Sciences Kharazmi UniversityTehran 15719-19911Iran Department of Applied Geological Sciences and Geophysics University of Leoben8700 LeobenAustria

The Durkan Complex is a tectonic element of the Makran Accretionary Prism(SE Iran)that includes fragments of Late Cretaceous *** this paper,the results of map-to micro-scale structural studies of the western Durkan Complex are presented with the aim to describe its structural and tectonometamorphic *** Durkan Complex consists of several tectonic units bordered by mainly NNW-striking *** main deformation phases(D_(1),D_(2),and D_(3))are distinguished and likely occurred from the Late Cretaceous to the Miocene–Pliocene.D_(1) is characterized by sub-isoclinal to close and W-verging folds associated with an axial plane foliation and shear zone along the fold *** phase records the accretion of fragments of the seamount within the Makran at blueschist facies metamorphic conditions(160–300℃ and 0.6–1.2 GPa).D_(2) is characterized by open to close folds with subhorizontal axial plane that likely developed during the exhumation of previously accreted seamount *** upper Paleocene–Eocene siliciclastic succession unconformably sealed the D_(1) and D_(2) structures and is,in turn,deformed by W-verging thrust faults typical of D_(3).The latter likely testifies for a Miocene–Pliocene tectonic reworking of the accreted seamount fragments with the activation of out of sequence *** results shed light on the mechanism of accretion of seamount materials in the accretionary prisms,suggesting that seamount slope successions favour the localization and propagation of the basal dé*** study further confirms that the physiography of the subducting plates plays a significant role in the tectonic evolution of the subduction complexes.

关键词： Underplated seamount Makran Accretionary Prism Tectono-sedimentary evolution Tectono-metamorphic evolution Cretaceous Iran

The Intra-Pontide ophiolites in Northern Turkey revisited:From birth to death of a Neotethyan oceanic domain

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Geoscience Frontiers 2020年第1期11卷 129-149页

作者： Michele Marroni M.Cemal Goncüoglu Chiara Frassi Kaan Sayit Luca pandolfi Alessandro Ellero Giuseppe Ottria Dipartimento di Scienze della Terra Universita di Pisavia S.Maria 5356126PisaItaly Istituto di Geoscienze e Georisorse-CNR Via G.Moruzzi 156124PisaItaly Department of Geological Engineering Middle East Technical University06531 AnkaraTurkey

The Anatolian peninsula is a key location to study the central portion of the Neotethys Ocean(s)and to understand how its western and eastern branches were *** of the lesser known branches of the Mesozoic ocean(s)is preserved in the northern ophiolite suture zone exposed in Turkey,namely,the Intra-Pontide suture *** is located between the Sakarya terrane and the Eurasian margin(i.e.,Istanbul-Zonguldak terrane)and consists of several metamorphic and non-metamorphic units containing ophiolites produced in supra-subduction settings from the Late Triassic to the Early *** preserved in the metamorphic units recorded pervasive deformations and peak metamorphic conditions ranging from blueschist to eclogite *** the nonmetamorphic units,the complete oceanic crust sequence is preserved in tectonic units or as olistoliths in sedimentary ***,structural,metamorphic and geochronological investigations performed on ophiolite-bearing units allowed the formulation of a new geodynamic model of the entire"life"of the IntraPontide oceanic basin(s).The reconstruction starts with the opening of the Intra-Pontide oceanic basins during the Late Triassic between the Sakarya and Istanbul-Zonguldak continental microplates and ends with its closure caused by two different subductions events that occurred during the upper Early Jurassic and Middle *** continental collision between the Sakarya continental microplate and the Eurasian margin developed from the upper Early Cretaceous to the *** presented reconstruction is an alternative model to explain the complex and articulate geodynamic evolution that characterizes the southern margin of Eurasia during the Mesozoic era.

关键词： Intra-Pontide suture zone Central Pontides Northern Turkey Ophiolites Neotethys Ocean Geodynamics

The western Durkan Complex(Makran Accretionary Prism,SE Iran):A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style

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Geoscience Frontiers 2021年第3期12卷 503-527页

作者： Edoardo Barbero Luca pandolfi Morteza Delavari Asghar Dolati Emilio Saccani Rita Catanzariti Valeria Luciani Marco Chiari Michele Marroni Dipartimento di Fisica e Scienze della Terra Universitàdi FerraraVia Saragat 144123 FerraraItaly Dipartimento di Scienze della Terra Universitàdi PisaVia S.Maria 5356126 PisaItaly Istituto di Geoscienze e Georisorse CNRPisaVia G.Moruzzi 156124 PisaItaly Faculty of Earth Sciences Kharazmi UniversityShahid Mofatteh St.43TehranIran Istituto di Geoscienze e Georisorse CNRFirenzeVia La Pira 450121 FirenzeItaly

The Durkan Complex is a key tectonic element of the Makran accretionary prism(SE Iran)and it has been interpreted as representing a continental margin *** present here a multidisciplinary study of the western Durkan Complex,which is based on new geological,stratigraphic,biostratigraphic data,as well as geochemical data of the volcanic and meta-volcanic rocks forming this *** data show that this complex consists of distinct tectonic slices showing both non-metamorphic and very low-grade metamorphic deformed *** and biostratigraphic data allow us to recognize three types of ***-Ⅰis composed by a Coniacian-early Campanian pelagic succession with intercalation of pillow lavas and minor volcaniclastic ***-Ⅱsuccession includes a volcanic sequence passing to a volcano-sedimentary sequence with Cenomanian pelagic limestones,followed by a hemipelagic *** succession is characterized by abundant mass-transport ***-Ⅲsuccession includes volcanic and volcano-sedimentary sequences,which are stratigraphically covered by a Cenomanian platform *** latter is locally followed by a hemipelagic *** volcanic rocks in the different successions show alkaline geochemical affinity,suggesting an origin from an oceanic within-plate *** new results indicate that the western Durkan Complex represents fragments of seamounts tectonically incorporated in the Makran accretionary wedge during the latest Late *** propose that incorporation of seamounts in the frontal prism caused a shortening of the whole convergent margin and possibly contributed to controlling the deformation style in the Makran Accretionary Wedge during Late Cretaceous-Paleocene times.

关键词： Tectonically disrupted seamounts Makran Late Cretaceous Iran Neo-Tethys

Geological,Structural and Mineralogical Approach to Investigate the Evolution of Low-and very Low-Grade Metamorphic Units from the Intra-Pontide Suture Zone,Central Pontides,Turkey

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Journal of Earth Science 2021年第6期32卷 1512-1527页

作者： Alessandro Ellero Chiara Frassi Mehmet Cemal Göncüoğlu Marco Lezzerini Michele Marroni Giuseppe Ottria Luca pandolfi Kaan Sayit Marco Tamponi Istituto di Geoscienze e Georisorse-CNR Via G.Moruzzi 156124PisaItaly Dipartimento di Scienze della Terra Universitàdi PisaVia S.Maria 5356126PisaItaly Department of Geological Engineering Middle East Technical University06800AnkaraTurkey

A multidisciplinary approach combining multiscale geological-structural analyses(from field to microscale) and clay mineral transformations(clay mineralogy, illite and chlorite "crystallinity" and b cell dimension(b_(0)) of K-white mica) was adopted to unravel the tectono-metamorphic evolution of low-and very low-grade tectono-metamorphic units from the Intra-Pontide suture zone in northern Turkey. The mineralogical study allowed to better evaluate the structural stacking outlined during the geological mapping, leading to distinguish three tectono-metamorphic units, two in epizone(Daday and Emirkoy units) and one in anchizone(Cifter Unit) metamorphic conditions. The mesostructural and microstructural analyses suggest a polyphase tectonic-metamorphic evolution. The different macroscopic features observed between the two units characterized by the same epizone metamorphism, can be justified by the evidence that these metamorphic conditions were acquired during the last stages of exhumation in the Daday Unit, while they constrained the metamorphic-peak conditions in the Emirkoy Unit. Contemporary analyses and comparison between structural and mineralogical data have thus proven to be a powerful tool to investigate the low-grade and very low-grade metamorphic environments, allowing at the same time to solve the apparent contradictions deriving from the mineralogical study and to significantly improve the detail of the geological mapping in the field.

关键词： clay minerals structural analyses low-temperature metamorphism epizone anchizone diagenesis Intra-Pontide suture zone Turkey