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homogeneous and isotropic transmissivity, and to be of in nite areal extent At rst glance, these ideal conditions seem unlikely to apply in many real aquifers However, they are often true enough in practice, particularly where the cone of depression is of modest extent This is because a small cone of depression will not have traversed many zones of different transmissivity during its development, and neither will the radius of in uence have yet come into contact with the outer boundaries of the aquifer Even where boundaries are encountered by the expanding cone of depression, the deviation of real-timedrawdown behavior from the anticipated ideal response predicted by the Theis (1935) method provides powerful evidence for the existence and hydrological functioning of recharge boundaries (ie rivers/lakes connected to the aquifer) or barrier boundaries (eg impermeable faults, outcrop zones, etc).

William McDougall s (1908) Introduction to Social Psychology engaged Darwinian theory to propose the idea of the evolution of social forms and, more speci cally, the construct of instincts or innate predispositions According to McDougall, instincts the springs of human action (p 3) consist of cognitive, emotional, and behavioral components that have evolved to constitute the fundamental dynamics of social behaviors and interactions The same year, Edward A Ross s (1908) Social Psychology, taking a more sociological orientation, proffered an interpretation of society as an aggregate of individual social actions Ross called his combination of sociological and psychological precepts a psycho-sociology Numerous accounts record 1908, the year of the textbooks, as the origin of the discipline In fact, the rst two decades of the century witnessed a proliferation of studies, theories, and pronouncements on the eld.

Furthermore, various adaptations of the basic Theis approach have been developed to allow various types of nonideal conditions to be taken into account (Kruseman and de Ridder 1991), including boundary effects and the depletion of saturated thickness due to drawdown in a thin uncon ned aquifer For the most part, however, it is impressive how often the basic Theis (1935) formulation proves adequate for analysing constant-rate test pumping data in a wide range of eld settings Although the full intricacies of test-pumping interpretation are beyond the scope of this book, it is worthwhile mentioning one of the most powerful adaptations of Theis (1935) basic method, namely the Jacob Method (Cooper and Jacob 1946) At its simplest, it is possible to use the Jacob Method as described in Box 33 to quantify transmissivity.

A further advantage of the Jacob method is that plots of time versus drawdown on semi-logarithmic paper (so-called Jacob plots; Figure 312a) can provide powerful visual evidence for the presence of aquifer boundaries A barrier boundary (eg a fault or some other feature that brings the aquifer into contact with lowpermeability rock) causes drawdown to steepen beyond that which we would expect from extrapolation of the Jacob straight line (Figure 312b)..

Some historians consequently labeled this interval of social psychological work as the age of schools and theories; they list among the new theory perspectives those of instinct, imitation, neo-Hegelian or Chicago, psychoanalytic, behaviorist, and gestalt (Faris, 1937; Frumkin, 1958; Woodard, 1945) Others have depicted the era as con ictual, fraught with major controversies and theoretical.

Proof: This follows directly from the weak law of large numbers. 1 P1 (X1 , X2 , . . . , Xn ) 1 log = log n P2 (X1 , X2 , . . . , Xn ) n

Voltage (E):

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