1) Balance of intensities
射线强度平衡
2) intensity balance
强度平衡
1.
The calculation formulas of energy balance and intensity balance from β~-decays are presented here.
论述了β-衰变的能量和强度平衡的计算公式,并以95Nb的β-衰变为例说明其实际应用。
2.
It is introduced to give calculation formula of absolute intensities of γ-ray from α decay on the basis of α decay intensity and γ-transition intensity balance.
根据α衰变的α强度和γ跃迁强度平衡,导出了α衰变的γ射线强度的计算公式,并以实例进行说明,并给出了有关强度平衡的物理自洽检验方法及其讨论。
3.
The calculation of γ-ray emission probability (absolute intensity) for isomeric transition is described on the basis of intensity balance of γ-transition.
文章涉及基于γ跃迁强度平衡的同核异能跃迁γ射线强度的计算方法,并以实例进行说明。
3) scheme balance method
强度平衡法
1.
γ-ray emission probabilities measurement of ~(138)Cs using scheme balance method;
强度平衡法测定~(138)Csγ射线发射概率
2.
This paper described scheme balance method and determined the main γ-ray emission probabilities of 138Cs using the calibrated efficiency curve.
根据母核衰变到子核基态上各种射线强度之和等于母核衰变活度的强度平衡法原理,用已标定好的峰效率曲线的HPCe γ谱仪准确测定了138Cs的γ射线发射概率,Pr(1435。
5) Line Balance Level
线路平衡度
6) the equilibrium line altitude
平衡线高度
1.
Further, utilizing the European Centre for Medium-Range Weather Forecast (ECMWF) reanalysis and the Climate Prediction Center (CPC) precipitation data, the relationship between the variability of the equilibrium line altitude (ELA) over the TP and its associated atmospheric circulation over Eastern Asia was investigated.
8万年前)和小冰期(约400-500年前)冰川在相应外部强迫条件下的分布进行了模拟,对SRES本世纪气候情景下的冰川进行了预测,同时对高原冰川在不同气候环境下的发育进行了模拟;并使用European Centre for Medium-Range Weather Forecast (ECMWF)再分析和美国NOAA Climate Precipitation Centre(CPC)的降水量资料,对青藏高原现代冰川平衡线高度(ELA)的变化与东亚地区大气环流和气候的关系进行了分析。
补充资料：表光合强度(见光合强度)
表光合强度(见光合强度)
forecast of sowing or transplanting time
b iaoguanghe qiangdu表光合强度见光合强度
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条