The first paragraph of Section 5.2 mentions one type of prior information that cannot be implemented by a linear equation of the form, Hm = h. What is it?

Usually, we know something about the model parameters, even before we perform any observations. Even before we measure the density of a soil sample, we know that its density will be around 1500 kg/m3 , give or take 500 or so, and that negative densities Even before we measure a topographic profile across a range of hills, we know that it can contain no impossibly high and narrow peaks. Even before we measure the chemical components of an organic substance, we know that they should sum to 100%. Further, even before we measure the concentration of a pollutant in an underground reservoir, we know that its dispersion is subject to the diffusion equation

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