Assume the same absorbance measurements are made at the same temperatures. at t=310k fd=0.200 but a folding intermediate exists which has a fraction fx=0.200. similarly at t=340k fd=0.800 and fx=0.100 . furthermore, for uv-vis absorbance measurements dx=0.100. from your values of kapp at t=310k and t=340k, calculate the apparent molar enthalpy of folding δh∘app .

f=ma a/f/m a= 480/60 a = 8m/s/s that is quick wow

co2reflects heat radiation back to earth buning coal and oil emits co2 globe warms

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scattering of light by tiny particles in air to produce the colors we see on sky, is dependent on the following factors:

(i) wavelength of light

(ii) size of the scattering particle  

(iii) distance traveled by light through the atmosphere.

according to rayleigh's law of scattering, the amount of scattering is inversely proportional to the fourth power of its wavelength. shorter the wavelength, greater is its scattering. hence violet/blue light is scattered more than red.

sun's light is a composite light ( visible light) with wavelengths in the range 400 nm (violet) to 700 nm (red). as sunlight passes through our atmosphere, the molecules of air scatter light according to their wavelengths. during sunrise and sunset, the sun's position is below the horizon. hence light from the sun travels a greater distance in the atmosphere when compared to its position a noon.

as sunlight enters the earth's atmosphere, blue light is scattered away and at the end of its journey in the sky, only red and orange wavelengths remain in the beam.

hence at sunrise and sunset, the sky appears reddish orange.