Study of transmembrane La3+ movement in rat ventricular myocytes by the patch-clamp technique

We have studied transmembrane La3+ movement in rat ventricular myocytes for the first time by using the whole-cell patch-clamp recording mode. La3+ (0.01-5.0 mmol/L) could not bring out inward currents through the L-type calcium channel in rat ventricular myocytes, while it could enter the cells by the same way carried by 1μmol/L ionomycin. When the outward Na+ concentration gradient is formed, La3+ can enter the cells via Na-Ca exchange, and the exchange currentsincrease with the increase of external La3+ concentrations. But compared with Na-Ca exchange currents in the same concentration, the former is only 14%-38% of the latter. The patch-clamp experiment indicates that La3+ normally can not enter ventricular myocytes through L-type calcium channel, but it can enter the cells via Na-Ca exchange.     

The 1997–1998 warm event in the South China Sea

A strong warm event happens during spring 1997 to spring 1999 in the South China Sea. Its intensity and duration show that it is the strongest event on the record over the past decades. It also corresponds with the severe flood over the valley of the Yangtze River and a couple of marine environmental events. This note addressed the evolution process by using several data sets, such as sea surface temperature, height and wind stress in addition to subsurface temperature. The onset of the warm event almost teleconnects with the El Niño event in the tropical Pacific Ocean. Summer monsoon is stronger and winter monsoon is weaker in 1997 so that there are persistent westerly anomalies in the South China Sea. During the development phase, the warm advection caused by southerly anomalies is the major factor while the adjustment of the thermocline is not obvious. Subsequently, the southerly anomalies decay and even northerly anomalies appear in the summer of 1998 resulting from the weaker than normal summer monsoon in 1998 in the South China Sea. The thermocline develops deeper than normal, which causes the downwelling pattern and the start of the maintaining phase of the warm event. Temperature anomalies in the southern South China Sea begin to decay in the winter of 1998–1999 and this warm event ends in the May of 1999.     

0行列式的定义

补充定义 0阶行列式的值 ,从而完善行列式的有关理论并简化行列式的计算与证明     

幂函数和指数函数回归模型参数的无偏估计及应用

本文给出了一类非线性函数、幂函数和指数函数回归模型参数的一种估计方法，用此方法计算幂函数和指数函数参数所得的残差平方和比用化为线性模型计算所得的残差平方和小得多。与精确的高斯－牛顿迭代计算结果相近，它比一般非线性回归迭代计算简单。     

合金钢CCT曲线计算

本工作利用现有的TTT曲线和数据，以及等温转变动力学方程（Avrami方程），计算合金钢CCT曲线。     

极量运动疲劳的研究

本文通过观察与分析极量运动疲劳时某些生理指标的变化,说明过性极量运动外周疲劳的发生机制可能首先不在中枢,而是在外周。     

全膜碳纤维阳极溶出伏安法测定汞

阐述了用金膜碳纤维电极差分脉冲阳极溶出伏安法测定水中微量汞的方法,讨论了支持电解质、镀金方式和金膜厚度对溶出峰电流i_p的影响,方法的线性范围为0.5—10 ppb,检测下限为 0.5 ppb,对标准水样(SB 0901)中汞的测定,变异系数为10.5％,相对误差为 1.3％,t 检验方法可靠。     

不定型Kac-Moody代数的极小虚根

本文描述了不定型Kac—Moody代数的极小虚根的一些性质及判定条件。利用极小虚根刻划虚根系,并证明了严格双曲型李代数有唯一的极小虚根,同时给出其具体表达式。     

霜冻图案与遥感考古研究

研究了历史遗迹的遥感分析方法及其理论依据,发现遥感图像上的霜冻图案经过增强后,可做为历史遗迹的稳定判读标志;用此法确定了唐长安城的位置和规模.同时指出,霜冻图案并非透视信息,而是地表差异在特定时相和波段的遥感图像上被增强了的结果.