Programming nonreciprocity and reversibility in multistable mechanical metamaterials

Nonreciprocity can be passively achieved by harnessing material nonlinearities. In particular, networks of nonlinear bistable elements with asymmetric energy landscapes have recently been shown to support unidirectional transition waves. However, in these systems energy can be transferred only when the elements switch from the higher to the lower energy well, allowing for a one-time signal transmission. Here, we show that in a mechanical metamaterial comprising a 1D array of bistable arches nonreciprocity and reversability can be independently programmed and are not mutually exclusive. By connecting shallow arches with symmetric energy wells and decreasing energy barriers, we design a reversible mechanical diode that can sustain multiple signal transmissions. Further, by alternating arches with symmetric and asymmetric energy landscapes we realize a nonreciprocal chain that enables propagation of different transition waves in opposite directions

La produzione di ceramica a pareti sottili di Poggio alle Fonti a Santa Cristina in Caio. Tipologie, cronologie e quantificazioni

The excavation of a large furnace discharge and the study of the thin walled pottery of Santa Cristina in Caio has allowed to propose a typology of this kind of pottery and to identify some original forms, perhaps produced only in this settlement: likely, the production of this fine ware takes inspiration from glass products, especially during the 1st century AD. The statistical study on chronologies has allowed to identify two periods of increased activity of the furnace, which can be framed in the construction phase of the thermal implant and in a phase of restoration of the structure. The circumstance suggests that there may be a correlation between pottery production and architectural constructions. It is possible that there was a locatio-conductio contract between ceramists and the owner of production structures and raw materials. In this perspective, it is quite obvious to observe a superior income of the owner in the times of more intense production and, therefore, a bigger spending capacity. The presence of the baths and of the kiln probably had a striking impact on Santa Cristina in Caio landscape: within its topographic basin, between the end of the 1st century B.C. and the 1st century AD., it is likely that a process of deforestation took place, fostering the creation of new agricultural areas in order to support the vicus, the La Befa and Casalone villas and the farms located in the Ombrone valley

Geometric charges and nonlinear elasticity of soft metamaterials

Problems of flexible mechanical metamaterials, and highly deformable porous solids in general, are rich and complex due to nonlinear mechanics and nontrivial geometrical effects. While numeric approaches are successful, analytic tools and conceptual frameworks are largely lacking. Using an analogy with electrostatics, and building on recent developments in a nonlinear geometric formulation of elasticity, we develop a formalism that maps the elastic problem into that of nonlinear interaction of elastic charges. This approach offers an intuitive conceptual framework, qualitatively explaining the linear response, the onset of mechanical instability and aspects of the post-instability state. Apart from intuition, the formalism also quantitatively reproduces full numeric simulations of several prototypical structures. Possible applications of the tools developed in this work for the study of ordered and disordered porous mechanical metamaterials are discussed.Comment: 12 pages, 5 figure

A new statistical method to assess potential debris flow erosion

Debris-flow erosion patterns were investigated for two adjacent catchments, Molinara and Val del Lago creeks (Eastern Alps, Trento Province, Italy), where two debris flows were triggered by an intense storm in the summer of 2010. Both basins have been inactive over the last two centuries. The debris flows were activated by channel and bank erosion under stable bed conditions before the event. The erosive process was analysed by combining a field campaign (two hundred cross sections were surveyed along the creeks) and pre- and post-event LiDAR surveys. Data were analysed by selecting morphologically-homogenous channel reaches and deriving for each reach: erosion depth, creek width, eroded volume and peak discharge. Investigating the frequency distribution of the erosion depth we found out that it follows an EV1 probability distribution. On this basis, a new approach has been proposed to predict event volumes when the expected maximum potential depth erosion is known. The procedure would be of high interest in predicting debris flow volume in mountain channels characterized by long silent periods