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around 10,000 m3/day) single-well installations may indeed suf ce. However, where the aquifer is to be called upon for substantially greater yields (e.g. to feed a large industrial plant, or to supply water to a large town), it is more common to use a group of wells located in relatively close proximity to each other. Such groups of wells are termed well elds.iv The key concept behind the design of well elds is that if a number of wells each pump at modest rates, the resultant drawdown will be far more evenly spread through a given area of aquifer than would be the case were we to obtain the same total ow rate by overpumping a single well. As noted above, the more heavily we pump any one well, the greater will be its well loss. Thus even if the aquifer is more than capable of supplying the demand which we wish to place on it, there will come a point at which two or more wells will be able to extract the water much more ef ciently (i.e.

Effects of Changes Sales revenue (decreased) Operating expense (increased) Net Income (decreased) $5,000 $2,000 $3,000

However, in most hydrogeological settings, water does not in ltrate very far into the unsaturated zone before it encounters signi cant quantities of geochemically reactive solids, which proceed to dissolve in the water and alter its chemistryx In many cases, the pH will be promptly raised by dissolution of calcite or (where calcite is lacking) by incongruent dissolution of silicate minerals (Section 423) Biogenic production of carbon dioxide is also an important process in the soil zone (Section 424), which can add further bicarbonate alkalinity to neutralize recharge waters The concomitant microbial activity can strip much of the original dissolved oxygen from the waters as well.

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Of course in some soils further acidi cation of in ltrating water can occur, for instance if pyrite is present in the soil pro le (as occurs in acidsulfate soils which ank the coastlines of many mid-latitude countries; see Section 935) However, in most hydrogeological settings recharge arrives at the water table pre-neutralized and relatively low in dissolved oxygen 442 Rock water interactions in the saturated zone Given the generally low velocities typical of ow in the saturated zone, there is normally ample time for even relatively slow geochemical reactions to substantially alter groundwater chemistry For instance, dissolution of calcite under laboratory conditions normally requires no more than 24 hours to approach equilibrium In a limestone aquifer, groundwater will typically be in contact with calcite for many years or even centuries, so that equilibrium is the norm rather than the exception.

can be formulated so that tests of selected parameters of the regression model provide tests of null hypotheses for A, B, and A B in the weight-loss experiment. Tests of the following null hypotheses for this regression model are of particular interest: H0: H0: H0:

Only where very rapid, preferential ow pathways exist below the water table (for instance, where there are caves) are we ever likely to nd groundwaters at depth which have not equilibrated with the carbonate minerals in the overlying sequence The dissolution of silicate minerals generally occurs millions of times more slowly than carbonate minerals (see Younger et al 2002a, p 104) However, where groundwater residence times are of the order of.

TABLE 25.1 (Continued) Congresses Societies The French-Speaking Neuropsychological Society was established. The Chinese Psychological Society was reopened and remains open to date (see 1950). The Colombian Society of Psychology was founded. The International Society for Political Psychology was established. The French-Language Association of Work Psychology was established. The Professional Union of Psychologists was established in Spain (see 1952). 1980 1978 The Venezuelan government enacted the Law of Psychological Practice. 1977 Events Publications The German Journal of Psychology, featuring English-language abstracts and review articles, was launched by C. J. Hogrefe Verlag under the auspices of the International Union of Psychological Science.

When such an experiment is carried out the results presented in Fig. 4.10 are obtained. They demonstrate that conditioning results in higher motor neuron activity in the US-CS condition. But how does this happen Stimulation of the tail causes the stimulation of the modulatory interneuron, which forms synapses with the sensory neurons from both the siphon and the mantle. This stimulation triggers the release of seratonin at these synapses. If one of the sensory neurons res at the same time as this seratonin release occurs (as would happen in our CS-US condition), a relatively permanent change in the sensory neuron synapse occurs with the result that it will subsequently release higher than normal amounts of neurotransmitter. When this happens the response of the motor neuron is ampli ed and the strength of the re ex will increase. So in this example learning is brought about via an increase in the effectiveness of the neural pathway.

Another way to set the default value is to take advantage of the UserForm s Initialize event. You can write code in the UserForm_Initialize procedure, which is located in the code module for the UserForm. Here s an example:

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