The Excitation Filters will convert the Macropod into a system that is capable of capturing fluorescence. They will work with any camera utilizing the MT-24 EX Dual twin lite flash by Canon. It is recommended that the Macropod be used for magnifications greater than 5x due to the reduced levels of light being emitted.
Blue excitation fluorescence filters are designed with a narrow passband excitation range (20 nanometers) in order to minimize autofluorescence and photobleaching. The longpass barrier (emission) filter is capable of transmitting signals from green, yellow, and red fluorophores that have significant absorption in the upper blue wavelength region. The filters have a longpass dichromatic mirror with a cut-on wavelength of 505 nanometers.
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The device is made to work with specific flash units. We have options from the Yongnuo YN-24EX, Canon MT-26EX-RT, Canon MT 24EX and Godox MF12 (Recommended). We strongly recommend using the Godox MF12 Flash units as they are wireless and allow for seamless control with the flash unit. Flash units are not required, but recommended when imaging. The analyzers are equipped with LED lights.
If a hardware component of the Macropod product line is in need of repair and out of warranty, please purchase a repair request and send your part to:
Macroscopic Solutions
ATTN: Repairs
222 Pitkin St
East Hartford, CT 06108
The total cost covers component repair, testing, cleaning and return postage. If additional parts or repairs are necessary, we will inform you of any balance due prior to starting the work.
Description of Problem/Symptoms
Camera shows Error 20 or Error 30. Camera needs Mirror Box Ass’y. Camera will be checked, cleaned and repaired to good working order and functional test. If additional parts are needed, an updated balance will be sent subsequent to payment.
Send with the following accessories: Body Cap, Eyecup, No Battery, No Media Card
Metashape is a proprietary software solution by AgiSoft. The software and documentation are supplied electronically. You will receive a registration code by e-mail after your order is processed. This registration code allows a demo Metashape version to convert into a fully featured registered version.
Floating license allows to install the program on as many computers as desired and run it, at any one time, on as many systems as the number of licenses purchased indicates. One computing machine shall be designated as the “license server”; the license server utility installed on it will manage license distribution across the network of computers where the program has been installed. Floating license is available for Agisoft Metashape Professional Edition only.
Agisoft provides node-locked licenses, i.e. one license allows to activate the program at one machine only. MetaShape license is NOT time-limited. Metashape license includes 12 month of e-mail based technical support and entitles the licensee to free updates of the software up to the version 1.9.x (see the current released version number at Installer page). To support education in the field of photogrammetry, Agisoft offers educational licenses to educational institutions.
* Package price is valid only for sale to one End User at a time
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Gneiss ( /ˈnaɪs/) is a common distributed type of rock formed by high-grade regional metamorphic processes from pre-existing formations that were originally either igneous or sedimentary rocks. It is often foliated (composed of layers of sheet-like planar structures). The foliations are characterized by alternating darker and lighter colored bands, called “gneissic banding”.
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A drop or droplet is a small column of liquid, bounded completely or almost completely by free surfaces. A drop may form when liquid accumulates at the lower end of a tube or other surface boundary, producing a hanging drop called a pendant drop. Drops may also be formed by the condensation of a vapor or by atomization of a larger mass of liquid. Liquid forms drops because the liquid exhibits surface tension.[1]
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A snowflake is a single ice crystal that has achieved a sufficient size, and may have amalgamated with others, then falls through the Earth’s atmosphere as snow.[1][2][3] Each flake nucleates around a dust particle in supersaturated air masses by attracting supercooled cloud water droplets, which freeze and accrete in crystal form. Complex shapes emerge as the flake moves through differing temperature and humidity zones in the atmosphere, such that individual snowflakes differ in detail from one another, but may be categorized in eight broad classifications and at least 80 individual variants. The main constituent shapes for ice crystals, from which combinations may occur, are needle, column, plate and rime. Snowflakes appear white in color despite being made of clear ice. This is due to diffuse reflection of the whole spectrum of light by the small crystal facets.[4]
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A snowflake is a single ice crystal that has achieved a sufficient size, and may have amalgamated with others, then falls through the Earth’s atmosphere as snow.[1][2][3] Each flake nucleates around a dust particle in supersaturated air masses by attracting supercooled cloud water droplets, which freeze and accrete in crystal form. Complex shapes emerge as the flake moves through differing temperature and humidity zones in the atmosphere, such that individual snowflakes differ in detail from one another, but may be categorized in eight broad classifications and at least 80 individual variants. The main constituent shapes for ice crystals, from which combinations may occur, are needle, column, plate and rime. Snowflakes appear white in color despite being made of clear ice. This is due to diffuse reflection of the whole spectrum of light by the small crystal facets.[4]
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This product has multiple variants. The options may be chosen on the product page
A snowflake is a single ice crystal that has achieved a sufficient size, and may have amalgamated with others, then falls through the Earth’s atmosphere as snow.[1][2][3] Each flake nucleates around a dust particle in supersaturated air masses by attracting supercooled cloud water droplets, which freeze and accrete in crystal form. Complex shapes emerge as the flake moves through differing temperature and humidity zones in the atmosphere, such that individual snowflakes differ in detail from one another, but may be categorized in eight broad classifications and at least 80 individual variants. The main constituent shapes for ice crystals, from which combinations may occur, are needle, column, plate and rime. Snowflakes appear white in color despite being made of clear ice. This is due to diffuse reflection of the whole spectrum of light by the small crystal facets.[4]
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This product has multiple variants. The options may be chosen on the product page
A snowflake is a single ice crystal that has achieved a sufficient size, and may have amalgamated with others, then falls through the Earth’s atmosphere as snow.[1][2][3] Each flake nucleates around a dust particle in supersaturated air masses by attracting supercooled cloud water droplets, which freeze and accrete in crystal form. Complex shapes emerge as the flake moves through differing temperature and humidity zones in the atmosphere, such that individual snowflakes differ in detail from one another, but may be categorized in eight broad classifications and at least 80 individual variants. The main constituent shapes for ice crystals, from which combinations may occur, are needle, column, plate and rime. Snowflakes appear white in color despite being made of clear ice. This is due to diffuse reflection of the whole spectrum of light by the small crystal facets.[4]
