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Monday, 8 December 2014

Circular dichroism

Circular dichroism (CD) is the difference in light 
absorbance between left- (L-CPL) and right-circularly 
polarised light (R-CPL) and circular dichroism 
spectrometers (spectrophotometers) are highly 
specialised variations of the absorbance 
spectrophotometer.
A circular dichroism spectrophotometer is also commonly 
termed a circular dichroism spectropolarimeter or a 
circular dichrograph. Most modern circular dichroism 
instruments operate on the same principles, which is 
demonstrated in the slide show at the bottom of the page. 
There is a source of monochromatic linearly polarised light 
which can be turned into either left- or right-circularly 
polarised light by passing it through a quarter-wave plate 
whose unique axis is at 45 degrees to the linear polarisation 
plane as described in the section about polarised light.
Instead of a static quarter-wave plate, a circular dichroism 
spectrophotometer has a specialised optical element called 
a photo-elastic modulator (PEM). This is a piezoelectric 
element cemented to a block of fused silica. At rest, when 
the piezoelectric element is not oscillating, the silica block is 
not birefringent; when driven, the piezoelectric element 
oscillates at its resonance frequency (typically around 50 
kHz), and induces stress in the silica in such a way that it 
becomes birefringent. The alternating stress turns the fused 
silica element into a dynamic quarter-wave plate, retarding 
first vertical with respect to horizontal components of the 
incident linearly polarised light by a quarter-wave and then 
vice versa, producing left- and then right- circularly polarised 
light at the drive frequency. The amplitude of the oscillation 
is tuned so that the retardation is appropriate for the 
wavelength of light passing through the silica block.
On the other side of the sample position there is a light 
detector. When there is no circularly dichroic sample in the 
light path, the light hitting the detector is constant. If there is a 
circularly dichroic sample in the light path, the recorded light 
intensity will be different for right- and left-CPL. Using a lock-
in amplifier tuned to the frequency of the PEM, it is possible 
to measure the difference in intensity between the two 
circular polarisations (vAC). The average total light intensity 
across many PEM oscillations (vDC) can be used to scale 
the size of the lock-in amplifier signal to take into account 
variations in total light level. Both signals can be recorded 
and from them the circular dichroism signal can be 
calculated easily by dividing the vAC component by the vDC 
signal.
CD calculation
G is a calibration-scaling factor to provide either ellipticity or 
differential absorbance. The section about CD Units and 
their inter-conversion explains how ellipticity and differential 
absorbance are related.


























 
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NORWAY\




Image result for NORWAY


Map of norway

















Norway: Oslo to Bergen by train










ALESUND




Stave church Heddal, Norway






Norway Bergen Tramway







At the top of Preikestolen with view over the Lysefjord, Norway 





Norway - Bergen Cityscape by AgiVega










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