polarizing beam splitter
"
UV Fused Silica Optical Beam Splitters 20Hz Plate Beam Splitter
Plate Beamsplitter, Wide Variety Of Splitting Ratios Over 400-1200nm Overview: Plate Beamsplitters consist of a thin, flat glass plate that has been coated on the first surface to split incident light by a specified ratio that is independent of the light's wavelength or polarization state, while the back surface AR coated in order to improve efficiency and minimize ghosting and interference effects.Plate beamsplitters are often designed for a 45° AOI. General Specifications
Διαχωριστής δέσμης πολωτικής πλάκας 45 μοιρών
45 Degree Plate Polarizing Beamsplitter, High Damage Threshold Overview: Plate beamsplitter is the most common type of beamsplitter which reflects and transmit light at 45° angle. Our 45 Deg Polarizing plate beamsplitter separates the input beam into two orthogonal components such as P-polarized light, which is transmitted while S-polarized light is reflected at a 45°angle. Plate beamsplitter has different benefits over cube beamsplitters such as high tolerance over advanced
Calcite YVO4 Optical Polarizer Glan Taylor 3000nm για VIS-IR
Glan Taylor Polarizer, a-BBO, Calcite and YVO4, Air-spaced Medium power for VIS-IR Overview: A Glan-Taylor prism reflects s-polarized light at an internal air-gap, transmitting only the p-polarized component. The optical axes are vertical in the plane of the diagram. A Glan–Taylor prism is a type of prism which is used as a polarizer or polarizing beam splitter. It is one of the most common types of modern polarizing prism. The prism is made of two right-angled prisms of
Ευρύ οπτικό πεδίο ορθής γωνίας Calcite Glan Thompson Polarizer Prism 500nm
Glan Thompson Polarizer, Calcite, Wide Field of View Overview: A Glan–Thompson prism consists of two right-angled calcite prisms that are cemented together by their long faces. The optical axes of the calcite crystals are parallel and aligned perpendicular to the plane of reflection. Birefringence splits light entering the prism into two rays, experiencing different refractive indices; the p-polarized ordinary ray is totally internally reflected from the calcite–cement
