科研成果

1993
Wang E. A model for the buffer layer formed on silicon during HFCVD diamond growth. Physica B: Physics of Condensed Matter. 1993;(1-4):85-89.
Tu Y, Levine H, Ridgway D. Morphology transitions in a mean-field model of diffusion-limited growth. Physical Review Letters. 1993;(23):3838-3841.
Tu Y, Levine H, Ridgway D. Morphology transitions in a mean-field model of diffusion-limited growth. Physical Review Letters. 1993;(23):3838-3841.
Yu DH, Jia J. Neural network algorithm with optimized parameters and used to solve TSP. Tien Tzu Hsueh Pao/Acta Electronica Sinica [Internet]. 1993;21:16-22. 访问链接
Yu DH, Jia J, Mori S. New neural network algorithm with the orthogonal optimized parameters to solve the optimal problems. IEICE Transactions on Fundamentals of Electronics, Communications and Computer Sciences [Internet]. 1993;E76-A:1520-1526. 访问链接
Liu C, Niu Q. Nonadiabatic effect in a quantum charge pump. Physical Review B. 1993;(19):13031-13034.
Liu C, Niu Q. Nonequilibrium effect in an electron turnstile. Physical Review B. 1993;(24):18320-18323.
Li SM. PARTICULATE AND SNOW NITRITE IN THE SPRING ARCTIC TROPOSPHERE. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS. 1993;27:2959-2967.Abstract
In the spring of 1986 and 1989, particle nitrite was measured at Barrow, Alaska, by filter sampling and by ion chromatographic analysis. Particle nitrite concentrations averaged 2.9 +/- 3.4 and 2.6 +/- 2.0 ppt (molar ratio) in 1986 and 1989, respectively. Both seasons showed diurnal variations with higher concentrations during the day which might have been caused by daytime down mixing. In 1989, nitrite was determined in several snow samples with concentrations between 0 and 0.18 mu mol l(-1). Particle nitrite was probably in disequilibrium with gas phase, suggesting a heterogeneous source for gaseous HONO. A relationship between particle nitrite and sodium ions suggests that sea salt could be involved in nitrite formation, perhaps through hydrolysis of nitryl halides.
Lee KJ, McCormick WD, Ouyang Q, Swinney HL. Pattern formation by interacting chemical fronts. Science [Internet]. 1993;(5118):192-194. 访问链接
Tang C, Liang S. Patterns and scaling properties in a ballistic deposition model. Physical Review Letters. 1993;(17):2769-2772.
Qu C-xu, Lai L-H, Xu X-jie, Tang Y-qi. Phyletic relationships of protein structures based on spatial preference of residues. Journal of Molecular Evolution [Internet]. 1993;(1):67-78. 访问链接
He S, Sarma DS, Xie XC. Quantized Hall effect and quantum phase transitions in coupled two-layer electron systems. Physical Review B. 1993;(8):4394-4412.
Edwards HL, Niu Q, Lozanne DAL. A quantum-dot refrigerator. Applied Physics Letters. 1993;(13):1815-1817.
Salamon MB, Lee W, Ghiron K, Shi J, Overend N, Howson MA. Reaching the unreachable: critical scaling at the superconducting transition. Physica A: Statistical Mechanics and its Applications. 1993;(1-4):365-373.
Jiang J, Zhou X, Du A, Peng L-M, Wang E, Mu S, Zhong Z. A REM study of inhomogeneous stress fields induced by the interfacial steps at In0.2Ga0.8As/GaAs interface. Superlattices and Microstructures. 1993;(3):379-.
Ouyang Q, Gunaratne GH, Swinney HL. Rhombic patterns: Broken hexagonal symmetry. Chaos. 1993;(4):707-712.
Li SM, Barrie LA, TALBOT RW, HARRISS RC, DAVIDSON CI, JAFFREZO JL. SEASONAL AND GEOGRAPHIC VARIATIONS OF METHANESULFONIC-ACID IN THE ARCTIC TROPOSPHERE. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS. 1993;27:3011-3024.Abstract
Measurements in the Arctic troposphere over several years show that MSA concentrations in the atmospheric boundary layer, 0.08-6.1 parts per trillion (ppt, molar mixing ratio), are lower than those over mid-latitude oceans. The seasonal cycle of MSA at Alert, Canada (82.5 degrees N, 62.3 degrees W), has two peaks of 6 ppt in March-April and July-August and minima of 0.3 ppt for the rest of the year. At Dye 3 (65 degrees N, 44 degrees W) on the Greenland Ice Sheet, a similar seasonal MSA cycle is observed although the concentrations are much lower with a maximum of 1 ppt. Around Barrow, Alaska (71.3 degrees N, 156.8 degrees W), MSA is between 1.0 and 25 ppt in July, higher than 1.5+/-1.0 ppt in March-April. The mid-tropospheric MSA level of 0.6-1 ppt in the summer Arctic is much lower than about 6 ppt in the boundary layer. Al Alert, the ratio of MSA to non-sea-salt (nss) SO42- ranges from 0.02 to 1.13 and is about 10 times higher in summer than in spring. The summer ratios are higher than found over mid-latitude regions and, when combined with reported sulfur isotope compositions from the Arctic, suggest that on average a significant fraction (about 16-23%) of Arctic summer boundary layer sulfur is marine biogenic. The measurements show that the summer Arctic boundary layer has a significantly higher MSA/nss-SO42- ratio than aloft.
Tang C. SOC and the Bean critical state. Physica A: Statistical Mechanics and its Applications. 1993;(1-4):315-320.
Xiao R-P, Spurgeon HA, Capogrossi MC, Lakatta EG. Stimulation of opioid receptors on cardiac ventricular myocytes reduced L type Ca2+ channel current. Journal of Molecular and Cellular Cardiology [Internet]. 1993;(6):661-666. 访问链接
Wang EG, Jiang J, Zhou XC, Du AY, Peng LM. Strain relaxation induced by interfacial steps of GaAs/In0.2Ga0.8As superlattices. Superlattices and Microstructures. 1993;(3):387-.

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