Four novel polymeric metal complexes with a D–A–π–A motif, BDTT-PY-Cd, BDTT-PY-Zn, BDTT-PY-Cu and BDTT-PY-Ni, were designed, synthesized and characterized. These polymeric metal complexes were made up with Cd(II), Zn(II), Cu(II), Ni(II) complexes, thienylbenzo-[1,2-b:4,5-b'] dithiophene (BDTT) and the 8-quinolinol derivative, which were used severally as dye sensitzers’ auxiliary electron acceptors (A), electron donor (D) and π bridges as well as the acceptors (A). Under AM 1.5 irradiation (100 mW cm?2), the devices of dye sensitized solar cells (DSSC) based on four polymer complexes exhibited short-circuit photocurrent densities (Jsc) of 17.45 mA cm?2, 14.75 mA cm?2, 13.94 mA cm?2 and 12.00 mA cm?2, as well as attractive power conversion efficiencies (PCE) of were 9.73%, 8.02%, 6.82% and 6.12%, respectively. The photovoltaic conversion efficiency (PCE) and short-circuit photocurrent density (Jsc) of BDTT-PY-Cd, BDTT-PY-Zn, BDTT-PY-Cu and BDTT-PY-Ni decrease in order because the radius and charge number of the metal ion affect the strength of the coordination bond between the metal ion and the ligand. These results provides a new way of development for efficient and stable dye sensitizers in the future.
Retiming is a technique for optimizing sequential circuits.In this paper,we discuss this problem and propose an improved retiming algorithm based on varialbes bounding.Through the computation of the lower and upper bounds on variables,the algorithm can significantly reduce the number of constratints and speed up the execution of retiming.Furthermore,the elements of matrixes D and W are computed in a demand-driven way,which can reduce the capacity of memory,It is shown through the experimental results on ISCAS89 benchmarks that our algorithm is very effective for large-scale seuqential circuits. 相似文献
The movement of bottom high-sediment sea water under water waves, especially that of the high-sediment water layer close to
the sea bottom, is important to the resuspension and settlement of sediment. Supposing that the high-sediment sea water is
a Newtonian fluid, based on Navier-Stokes (N-S) theory, the movement of the interfaces of air-water and water-sediment water
was tracked by the volume of fluid (VOF) method. The velocity field of sediment water was simulated by considering the effect
of water waves. The results show that the movement of sediment water is very different from that of sea water, which provides
a solid basis for understanding the resuspension and settlement of sediment and the formation of bottom stripe, and the VOF
method can trace the movement of the two interfaces simultaneously; the movement of the air-water interface has a strong effect
on that of the water-sediment water interface, while the effect of the water-sediment water interface movement on the air-water
interface is not obvious.
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Translated from Journal of Tianjin University, 2008, 41(2): 285-290 [译自: 天津大学学报] 相似文献