Role In Decay Processes Research Articles

Diffusion dynamics of valley excitons by transient grating spectroscopy in monolayer WSe2

The transient grating spectroscopy is widely used to determine the diffusion coefficients of valley excitons or spins in low-dimensional semiconductor materials. Here, we present the investigation on the diffusion dynamics of the valley excitons in a high-quality large-scale mechanically exfoliated tungsten diselenide (WSe2) monolayer by this technique at room temperature. Collinearly polarized laser excitation (at a photon energy of 1.66 eV resonant to the energy of valley A-excitons) was used to introduce a spatially periodic density of valley excitons. Through probing the spatial and temporal evolution of the initial density of valley excitons, we find that the signals of transient grating exhibit an nonexponential decay, and its decay rate is independent of the period of optical grating Λ. Combined with the transient reflection measurements, we show that the exciton-exciton annihilation plays a key role in decay processes of the transient grating spectroscopy, which results in the distortion of sinusoidal gratings. Based on Einstein relationship, we estimate the diffusion coefficient of valley exciton DX = 0.7 cm2/s.

Micro-porosity and minero-petrographic features influences on decay: Experimental data from four dimension stones

Sedimentary stones have been used since long as dimension stones, constituting the primary building material of several monumental structures all over the world. The understanding of their behaviour when exposed to weathering factors is crucial for preservation, replacement and restoration intervention. Although not directly involved with decay mechanisms, micro-pores (i.e. open pores with radius <0.1 µm) and their interconnection to the wider ones are important for air and water flow inside rocks. In fact, micro-pores are not directly the site of ice or salt crystallization, nor of oil and gas entrapment, but are the main pathway for fluids during both adsorption and evaporation processes. The study of narrow pores is therefore crucial to predict e.g. stone durability and physical properties. This study presents the study on four different sedimentary lithotypes vastly employed as dimension or ornamental stones in Italy, both sound and artificially weathered. In particular, coupled MIP and hygroscopic sorption based micro-porosimetry were used to uncover liability to relative humidity variation, in association with a thorough mineralogical characterization. The MIP intrusion pattern attained pore shapes and typology description for the different rock types; but only the hygroscopic sorption helped deciphering the on-going processes. Moreover, the coupling of petrography and petro-physical analyses (i.e. MIP and hygroscopic sorption based micro-porosimetry) pointed out that phyllosilicates have a role in decay processes of rocks due to swelling and/or suturing of the adjacent voids.

Porosity as key factor in the durability of two historical building stones: Neapolitan Yellow Tuff and Vicenza Stone

Porosity plays a decisive role in decay processes of stones, as the pore network allows the water penetration responsible for the several physical and chemical deterioration processes affecting stone materials. In this paper two stones (with porosity from high to medium) used in Naples and Vicenza architectures have been considered to investigate the effects produced by the application of an ethyl silicate consolidant and an anti-swelling protective agent on pore space and therefore on stone durability.A deep characterization of the pore system has been carried out as considered crucial to evaluate the effectiveness of conservation treatments and their performance through time. To this purpose, petrophysical and physico-mechanical measurements have been carried out before and after aging tests, on both untreated and treated stones.Conservation treatments, strongly affecting pore size distribution and the behavior towards water absorption, do not always improve the durability of stone, especially in Neapolitan Yellow Tuff (herafter NYT) where a set of meso-macropores was totally annealed as well as a relevant portion of ultramacropores. Such treatments favor the persistence of water in NYT rock structure still after a long time, further contributing to a fast decay of this stone after aging tests. By contrast, treatments in Vicenza Stone (hereafter VS) prevailingly occlude micro- and mesopores and only slightly affect larger pores thus again favoring the flow rate during water desorption test. Moreover, the increase of the average pore radii after treatments also improves the features of this stone that accounts for almost negligible effects after accelerated aging tests.