反射率
- 与 反射率 相关的网络例句 [注:此内容来源于网络,仅供参考]
-
In this paper,using numerical solution method of vector diffraction theory,we discuss the dependence of reflectivity upon structural parameters of subwavelength grating,particularly upon substrate thickness.It can be used as the basis for design and fabrication of binary optical element with proper antireflection property.
文摘:利用矢量衍射理论的数值求解方法,研究了亚波长光栅结构参数对反射率的影响,特别是基底厚度对反射率的影响,这些为设计和制作具有优良的抗反射性能的二元光学元件提供了设计依据。
-
Charged to the complete absorption of red light, prints on the incident light reflection at 3%, it's ideal for the bar code coloring; white ink on hongguang you will be completely reflectionthe the printing on the incident light reflectivity of close to 1 0 0%, is the most secure blank coloring, so in General, the bar code printed in black and white monochrome.
黑墨可完全吸收红光,印品对入射光的反射率在3 %以下,是最安全理想的条形码用色;白墨对红光则会完全反射,其印品对入射光的反射率接近1 0 0 %,是最安全的空白用色,因此条形码一般都印成黑白相间的单色。
-
The test results indicate that Lambert cosine radiation characteristic of the new method has a distinct improvement, and the incidence normalized curve approaches to the standard cosine curve in the 0° and 45°.
测试结果表明,新工艺的朗伯余弦辐射特性得到明显改善,在0°与45°入射时,归一化曲线接近标准余弦曲线;300 nm处半球反射率均匀度从0.77提高到0.98;200~400 nm处半球反射率平均提高33%;将其应用于紫外-真空紫外遥感仪器上进行了角度响应测试,漫反射特性明显优于美国2002年发射的同类仪器SBUV/2。
-
The test results indicate that Lambert cosine radiation characteristic of the new method has a distinct improvement, and the incidence normalized curve approaches to the standard cosine curve in the 0° and 45°. Moreover,with the new mehtod, hemisphere index of reflection uniformity increases from 0.77 to 0.98 at 300 nm and the hemisphere index of reflection averagely enhances by 33% at 200~400 nm.
测试结果表明,新工艺的朗伯余弦辐射特性得到明显改善,在0°与45°入射时,归一化曲线接近标准余弦曲线;300 nm处半球反射率均匀度从0.77提高到0.98;200~400 nm处半球反射率平均提高33%;将其应用于紫外-真空紫外遥感仪器上进行了角度响应测试,漫反射特性明显优于美国2002年发射的同类仪器SBUV/2。
-
The transmission, reflection and absorption spectra of the cyanine thin films were measured by the spectrophotometer and the reflection and the absorption of this cyanine thin film are high enough for optical recording at 780 nm.
通过染料薄膜光谱的分析,发现该染料薄膜在780 nm波长处有较大的吸收和较高的反射,多层膜的反射率达到75%,这符合橙皮书对反射率大于70%的要求。
-
The correlative relationship between three hyperspectral parameters and chlorophyll content of Festuca arundinacea, Lolium perenne, and Agrostis stoloni fera was studied. The result indicated that the hyperspectral parameters were significantly correlated with the chlorophyll content, especially for GNDVI.
通过3种草坪草高羊茅,多年生黑麦草和匍匐翦股颖反射光谱曲线特征,研究了高光谱参数绿峰反射率Rg、红谷反射率Ro和GNDVI与叶绿素含量的相关性,结果表明:3种高光谱参数与叶绿素含量的相关性均达到显著水平,尤其是GNDVI与叶绿素含量之间的相关性最好。
-
Taking use of the reflectometer which is installed on the 3B1 line in BSRF, two kinds of measurements of reflectivity versus wavelength and reflectivity versus incident angle are carried out.
利用安装在北京同步辐射装置3B1束线上的一台小型反射率计,对磁控溅射方法制备的软X多层膜进行了R~θ、R~λ两种反射率测量,得到实测反射率高达32%的满意结果,同时给出了理论计算对实验的拟合,二者符合的很好。
-
The experimental result shows, Morpho butterfly's wing micro-structure forms the reflecting rate higher than the reflecting rate of other butterflies, so regard Morpho butterfly as and transfer to the micro-structure of printing, is observed by SEM and transfered to the vein micro-structure printed, demonstrate the same array scale as Morpho butterfly and carinate fin slice, small in more quantity than Morpho butterfly in the slight branch form structure, but metal micro-structure of color and luster printed off to transfer to raise reflect, it is it print off by AFM array carinate fin of alternate size nearly the width of 1.5μm to transfer to measure.
实验以高解析光学显微镜及紫外光/可见光光谱仪分析虎斑蝶、碧翠凤蝶、锯粉蝶、摩浮尔蝶蝶翼表面的光学反射、穿透与吸收特性,实验结果显示,转印的Morpho蝶翼微结构与真实摩浮尔蝶反射率较相近,故将Morpho蝶作为转印微结构,由SEM观察转印的翅脉微结构,呈现出与Morpho蝶相同的阵列鳞片与脊状的鳍片,虽细微的树枝状结构少,但转印出的微结构溅镀20nm的金属膜提高反射率,而由AFM检测转印出阵列脊状的鳍片间隔尺寸约为1.5μm的宽度。
-
The absorption spectrum center wavelength of dolomite is near 232 μm is shorter than 235 μm of limestone,and thus RBD7 and RBD8 can be employed effectively to identify dolomite and limestone,respectively. Felsic rocks show AlOH and Fe3+ absorption characteristics in the VNIRSWIR region,while the maficultramafic rocks show Fe2+ and Fe,MgOH absorption features,hence the use of different valence state of iron and secondary minerals can distinguish them:ASTER band2/band1 represent Fe3+ distribution,ASTER band2/band1 represent the Fe2+ distribution,RBD6 can estimate the AlOH mineral abundance. Psammitic/pelitic schist containing phengite,chlorite,stilpnomelane,as well as the weathered surface covered by clay minerals,exist characteristic absorption spectrum in the 221 μm(band 6),and has a high reflectance in 165 μm(band 4),while the blueschist/greenschist show high reflectance in the 221 μm(band 6),and it exit low reflectance in 165 μm(band 4),and blueschist/greenschist appear low ASTER band4/band6 ratio.
白云岩的CO2-3吸收谱带中心波长位于232〖KG*3〗μm,与灰岩的CO2-3 吸收谱带中心波长位置235 μm相比,具有向短波长方向移动的特点,据此可以利用RBD7、RBD8分别有效的识别白云岩和灰岩;长英质岩石显示AlOH和Fe3+ VNIRSWIR吸收特征,而基性超基性岩石显示Fe2+和Fe、MgOH特征,利用不同的铁价态和次要矿物可以区分它们:ASTER band2/band1代表了含Fe3+矿物分布信息、ASTER band5/band4代表了含Fe2+矿物分布信息、RBD6可以估计AlOH矿物的丰度;砂质/泥质片岩含较多的多硅白云母、绿泥石、黑硬绿泥石以及风化后表面覆盖的其它粘土矿物,在221 μm(band 6)存在有特征的吸收谱带,并且在165 μm(band 4)具有较高的反射率,而蓝片/绿片岩在221 μm(band 6)反射率较高,不具有明显特征吸收谱带,同时其在165 μm(band 4)反射率较低,因此蓝片/绿片岩ASTER band4/band6 比值低。
-
The time-resolved hemispherical reflectance and transmittance of the slabs with linearly varying refractive index are obtained for various optical thicknesses, scattering albedos and substrate reflectances.
接著,求各种光学厚度、散射比和基底反射率的线性可变折射系数平板的时间分解半球反射率与半球穿透率。
- 推荐网络例句
-
Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
-
Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
-
This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。