9,438 research outputs found
Low degradation and high annealing effects of amorphous silicon multilayer processed through alternate hydrogen dilution
No full textFabrication of protocrystalline silicon multilayer/protocrystalline silicon multilayer tandem solar cell for low degradation (Submitted)
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Niemcza diorites and moznodiorites (Sudetes, SW Poland): a record of changing geotectonic setting at ca. 340 Ma
No full textGranites sensu lato in the Sudetes intruded in several episodes during the Variscan orogeny recording different stages of crust and mantle evolution. Correlating precise ages with geochemistry of the Variscan granites provides information on the evolution of these sources within the Variscan orogen. The Variscan intrusive rocks from the Niemcza Zone (Bohemian Massif, Sudetes, SW Poland) include undeformed dioritic to syenitic rocks and magmatically foliated granodiorites. In this study we analysed low SiO2 (48–53 wt.%) monzodioritic rocks from Przedborowa and Koźmice. The monzodiorites contain late-magmatic zircons with ages of 341.8 ± 1.9 Ma for Przedborowa and 335.6 ± 2.3 Ma for Koźmice, interpreted as emplacement ages of the dioritic magmas. Older Przedborowa rocks are lower in K, Mg, Rb and Ni than the Koźmice rocks and similar compositional trend is also observed in the Central Bohemian Plutonic Complex. The implication is that the mantle underlying the Niemcza Zone became more enriched from ca. 342 to ca. 336 Ma, probably following the collision of the Saxothuringian and Moldanubian/Lugian domains. The magmatism related to the collision occurred ca. 12 Ma later than that in the Central Bohemian Plutonic Complex, but was accompanied by a similar change in magma chemistry from high-K (Przedborowa) to shoshonitic (Koźmice, Kośmin enclaves) and probably to ultrapotassic (Wilków Wielki)
Geochemistry and grain size analysis of cored sediments from Taiwan Strait and offshore southwestern Taiwan: A comparison
No full textCharacterization of the protocrystalline silicon multilayer
No full textThe protocrystalline silicon (pc-Si:H) multilayer solar cell is very promising owing to its fast stabilization with low degradation against light irradiation. However, the pc-Si:H multilayers have not extensively been investigated in detail on its material characteristics yet. We present the material characteristics of pc-Si:H multilayers using a transmission electron microscopy (TEM), Fourier transform infra (FTIR) spectroscopy, Raman spectroscopy, constant photocurrent method (CPM) and quantum efficiency (QE) measurement. A TEM micrograph shows that a pc-Si:H multilayer has a repeatedly layered structure consisting of low hydrogen-diluted and highly hydrogen-diluted sublayers. FTIR spectra depict the strong vibration mode at 2090 cm(-1) which is attributed to hydrogen-rich amorphous silicon (a-Si:H) regions of highly hydrogen-diluted sublayers. Based on these results, excellent light-soaking behavior of the pcSi:H multilayers is primarily due to the repeatedly layered structure that improves a structural order in the material. (c) 2006 Elsevier B.V. All rights reserved
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