1) absorb losses
吸收亏损
2) unabsorbed loss
未吸纳亏损
3) farm income or loss
农业收入或亏损
4) absorption loss
吸收损失
1.
The results indicated that after the Nd,Cr:GSGG crystal was annealed in the oxidation atmosphere,the absorption spectrum exist two absorption bands near 1μm due to some Cr~(4+) ions in the crystal,which are called 1μm absorption loss.
氧化气氛下退火后的吸收光谱中,在1μm处出现了由于晶体中存在Cr4+离子所引起的两个吸收带,被称为1μm吸收损失。
2.
Titanium oxide and silicon dioxide were used as thinfilm materials and deposition parameters were optimized to minimize the absorption loss,so there could be effective reflection reducing and protection for fluorinated magnesium substrates.
经过实验,选取氧化钛与二氧化硅作为薄膜材料,并优化沉积工艺参数,尽可能减少吸收损失,对氟化镁基底实现有效的增透和保护。
5) Absorption loss
吸收损耗
1.
Absorption loss due to high harmonics of C-H vibrations, the primary loss factor in PMMA POF, was analyzed and calculated.
随着波长的增加 ,C -H谐波吸收损耗增加 ,而伸缩振动的吸收损耗比弯曲振动高一个数量级 ,且两者分别与量子数呈线性关
2.
A quarter-wave conventional film system was adopted to analyze the main effect of the distribution of electric field intensity,absorption loss and the scattering loss on the properties of 193 nm HR mirror.
采用1/4规整膜系,从电场强度、吸收损耗及散射损耗的分布几个方面,对影响193 nm反射膜性能的因素进行了分析。
3.
According to the absorption properties of erbium-doped optical fiber, there would appear a sharp absorption loss, which brought more difficulties to the actual measurement of slow light and its application in communications.
由掺铒光纤的吸收特性可知,此时必伴随着强烈的吸收损耗,这势必会给实际的慢光信号测量及光通信领域带来诸多的困难。
6) Reflection Loss
吸收损耗
1.
In order to reduce the pollution, which the electromagnetic wave being reflected back into air will pollute again the electromagnetic environment, in this paper, the double gradient model for shielding functionally gradient materials (SFGM) was put forward to realize low reflection loss and high absorption loss for electromagnetic wave.
制备的镍/镍锌铁氧体/环氧树脂梯度电磁屏蔽材料,其结果表明:在频率<1GHz时,双梯度材料对电磁波的反射损耗比非梯度材料平均降低了6～8dB;而吸收损耗平均提高了6～14dB。
补充资料：鑀亏损法
分子式：
CAS号：
性质：鑀即230Th。根据处于亏损状态的鑀随时间增长以测定珊瑚、软体动物化石或壳体的地质年龄的方法。此法测定的年龄范围为1万～25万年。
CAS号：
性质：鑀即230Th。根据处于亏损状态的鑀随时间增长以测定珊瑚、软体动物化石或壳体的地质年龄的方法。此法测定的年龄范围为1万～25万年。
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