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For those of you listening to this, youamp;#39;ve just missed 10 minutes of me speaking at the start. Um, so basically weamp;#39;ve identified all of the peaks. Now each of these peaks, the the relative intensity of them, uh corresponds to the number of atoms which are present in the surface. So each peak is proportional to the number of atoms of carbon, the number of atoms of oxygen. And So what we want to do, of course we want to use those peaks to quantify. The carbon to quantify the oxygen. But what youamp;#39;ll notice is where we have we have these peaks, but we also have the this. A docHub background which forms after each peak. So the right hand side have quite a flat low background, but after each peak we have this relatively docHub background that increases in intensity after each peak. And that background is formed by, for example, carbon 1S electrons being inelastically scattered. On the way out of the surface or 01 S electrons being inelastically scattered all
