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ELECTRONICALLY CROSS-LINKED PbS QUANTUM DOT NETWORKS USING POLYMERS AS SURFACE LIGANDS
WEI LÜ,YUE YANG,AKIRA YAMAKATA,ITARU KAMIYA 성균관대학교(자연과학캠퍼스) 성균나노과학기술원 2013 NANO Vol.8 No.2
Bilayer structures of colloidal PbS quantum dots (QDs) with different sizes are fabricated by two methods: chemical bond anchoring and electrostatic adsorption. Unlike the sample prepared by chemical bond anchoring, we find that the electronic connection between different layers is suppressed in the samples prepared by electrostatic adsorption with charged polyelectrolytes. To clarify the electronic coupling between the QDs and the polyelectrolytes, QDs directly stabilized by charged polyelectrolytes were synthesized. Transmission electron microscopy investigation shows that cross-linked QD networks are formed. Time-resolved photoluminescence measurements indicate that the carrier lifetimes of QDs in networks were greatly reduced. The photoluminescence peak energy increases with a third root of the excitation power. All these observations can be consistently explained considering spatially separated photoexcited carriers in a type-II band alignment. The abnormal behaviors of electrostatic adsorption sample are discussed based on these results.
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Wei Mei,Xinbiao Lü,Zhi Liu,Rankun Tang,Zhilong Ai,Xiangdong Wang,Mamady Cisse 한국지질과학협의회 2015 Geosciences Journal Vol.19 No.1
Huanggang skarn Fe-Sn deposit is located in themain ridge Sn-polymetallic metallogenic sub-belt of the SouthernGreat Xing’an Range. A combination of zircon U-Pb age, geochemistryand Hf isotopic composition are reported for the orerelatedgranite (K-feldspar granite) of the Huanggang deposit toconstrain its petrogenesis and tectonic setting. LA-ICP-MS U-PbZircon dating results indicate that the K-feldspar granite wasintruded at 145.3 ± 1.6Ma. The K-feldspar granites belong to high-K calc-alkaline and shoshonite series, mainly peraluminous. Theserocks have a negative slope from La to Lu with strongly negativeEu anomalies, they demonstrate negative Ba, Sr P, Ti and Nbspikes and positive Th, U, Nd spikes on the normalized incompatibleelement diagrams. The regional geological setting togetherwith the geochemistry of the K-feldspar granite indicates that it isformed in a post-orogenic setting. The zircon Hf isotopic compositions(εHf(t): +5.2 to +6.6, 176Hf/177Hf: 0.282837‒0.282876) indicateboth juvenile crust sources that originated from depleted mantleand some ancient continental crust sources contributed to its origin,and there is a significant addition of juvenile crust under theSouthern Great Xing’an Range during the time from Paleo-Neoproterozoicto Phanerozoic.
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Comparison of Two Cases of Strong Increase in the Bottom Temperature in the Yellow Sea in Winter
Lian-Gang Lü,Guang-Bing Yang,Zong-Wei Liu,Ying Jiang,Chunmei Yang,Chao Zhang 한국해양과학기술원 2015 Ocean science journal Vol.50 No.3
Mooring observations were carried out on the western slope of the southern Yellow Sea (YS) to observe the Yellow Sea Warm Current (YSWC). Strong increases in the bottom temperature (about 3°C within 1 day) were observed at mooring M5 (shelf break) on 8 January 2007, and at mooring A2 (mid-slope) on 5 December 2008. The strong temperature increase of bottom water at M5 was closely related to the burst of the YSWC. The bottom temperature at mooring A2 increased and decreased alternately from 7 November to 14 December 2008, and the strong increase (about 3°C within 1 day) occurring on 5 December was one of the four rises during that period. The significant semi-diurnal-oscillation during that period indicated that the thermal fronts outlining the Yellow Sea Cold Water Mass (YSCWM) boundary was very close to location A2. The notable rises in the bottom temperature at A2 were associated with bottom eastward currents, while the distinct falls in temperature coincide with bottom westward currents. The distinctive distribution in the bottom temperature associated with the YSCWM and the bottom eastward currents were mainly responsible for the strong increase in the bottom temperature at A2. The variations in the bottom temperature described here are valuable for understanding the time evolution of the YSWC in winter and the YSCWM from late autumn to early winter.
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Cheng Wang,Gang-Lin Yan,Shao-Wu Lü,Chun-Hong Sui,Yang Zhao,Ya-Wei Xu,Gang Zhao,Jun-jie Xu,Ping-Sheng Gong,Gui-Min Luo,Ying Mu 한국생물공학회 2013 Biotechnology and Bioprocess Engineering Vol.18 No.1
Glutathione peroxidase (GPX) is one of the important members of the antioxidant enzyme family. It can catalyze the reduction of hydroperoxides with glutathione to protect cells against oxidative damage. Single-chain variable fragment (scFv) can be converted into seleniumcontaining single-chain variable fragment (Se-scFv) by chemical modification of the hydroxyl groups in scFv, thus Se-scFv possesses GPX activity and becomes a prodrug. To improve the expression of scFv and simplify its purification steps, Single-protein production (SPP) system was used to express scFv and chemical modification was used to synthesize Se-scFv. Therefore, we must construct a new scFv-WCD1-lessACA gene, which can express its mRNA not containing any ACA sequences and express its amino acid sequence of target protein (scFv) being same to scFv-WCD1. In this way, the scFv-WCD1-lessACA can be only expressed in SPP system and no other background proteins in the cells could be expressed. The expression results showed that high level of scFv-WCD1-lessACA synthesis was at least sustained for 96 h in the virtual absence of background protein synthesis. Then, selenocysteine (Sec) was incorporated into the scFv-WCD1-lessACA by chemical modification and resulted in Se-scFv-WCD1-lessACA. The enzymatic characteristics of Se-scFv-WCD1-lessACA were determined. GPX activity was 2,563 U/μmol,its binding constant for GSH was 0.687 ×105/mol. Moreover,Se-scFv-WCD1-lessACA was confirmed to have a strong antioxidant ability to protect mitochondria against oxidative damage induced by Vc/Fe2+ (mitochondrial damage model),suggesting that Se-scFv-WCD1-lessACA has potential application for protection of mitochondrial damage induced by reactive oxygen species (ROS).
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