By Imran N Hosein
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A good basic reference to solutions and equilibria is that of Garrels and Christ (1965). ( a ) Hydrogen ion potential. CO, dissolves freely in H,O, creating a bicarbonate ion and a free hydrogen ion. /l (pH = 7), but upon saturation of water with CO, it rises to (pH = 5). \‘ I1 ALKALINE I 10 I 12 Fig. 2-1. Catenary diagram illustrating limits of natural environments in terms of pH and Eh, especially the sites of syn-, ana-, and epidiagenesis. M. ) It is called a “catenary” diagram because the boundary is like a linked chain (“catena”).
Stages 1 and -7 are syndiagenetic. stages 3 to 5 are anadiagenetic, whereas stage 6 is epidiagenetic. was intended only for primary chemical sediment such as oolite, and he used “diagenesis” only as the writer uses “syndiagenesis”. Two stages are recognized in the syndiagenetic phase. These have been called (Dapples, 1959, 1962): initial stage, controlled by the chemistry of the superjacent water, and early burial stage, controlled by the entrapped, connate water, chemically modified by the bacteria and other subsurface organisms.
Oxidation becomes very general and the pH will tend to drop, except where the waters are heavily contaminated by connate reserves or where they encounter precipitated soluble salts. Epidiagenesis of the old, stable cratons is a pervasive process in soil development and landscape control, inasmuch as it is constantly interrupted by transgressions and then reintroduced. A global eustatic rhythm of rise and fall of sea level tends to be superimposed on regional epeirogenic crustal warping. The alternation of stabilization and reactivation is the essence of the theory of biorhexistasy (Erhart, 1956; Termier and Termier, 1963).
A Muslim Response to the Attack on America by Imran N Hosein