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patterns are oxygen-18 (18O) and deuterium (2H, or simply D ), as both of these isotopes are to be found in the water molecule itself. As water evaporates, the heavier molecules tend to get left behind, so that water which has been subject to much evaporation can be expected to contain higher proportions of 18O and 2H than fresh rainwater. Armed with this information, it is sometimes possible to identify old and new components of groundwater in environments where vigorous mixing can occur, such as in upland stream runoff source areas (Buttle 1994). Another important use of isotope studies is in identifying the in uence of microbial processes on hydrogeochemical reactions. Just as the heavier isotopes tend to get left behind during evaporation, the heavier isotopes of nutrients (especially such as 13C, 34S, and 15N) tend to pass through many metabolic chains more slowly than their lighter counterparts (12C, 32S and 14N). Shifts in the relative proportions of heavy and light isotopes can provide evidence of the extent and rates of microbial intervention in geochemical cycles. 4.2.8 Dissolved gases Direct measurements of the quantities of gases dissolved in groundwater tend to be made only as part of specialized investigations, such as:

Furthermore, the duration of a problem should be assessed via interview, preferably by more than one interviewer, in order to establish reliability of.

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mation. In sophisticated systems, decision circuits regenerate and retime the pulses on the occurrence of a transition. Unlike decision circuits, timing circuits that reshape a pulse when a transition takes place must have a memory in case a long series of marks or spaces is received. Although such periods have no transitions, they carry meaningful information. Likewise, the memory must maintain timing for reasonable periods in case of circuit outage. Note that synchronism pertains to both frequency and phase and that the usual error in high-stability systems is a phase error (i.e., the leading edges of the received pulses are slightly advanced or retarded from the equivalent clock pulses of the receiving device). Once synchronized, high-stability systems need only a small amount of correction in timing (phase). Modem internal timing systems may have a long-term stability of 1 10 8 or better at both the transmitter and receiver. At 2400 bps, before a signi cant timing error can build up, the accumulated time difference between transmitter and receiver must exceed approximately 2 10 4 s. Whenever the circuit of a synchronized transmitter and receiver is shut down, their clocks must differ by at least 2 10 4 s before signi cant errors take place once the clocks start back up again. This means that the leading edge of the receiver clock equivalent timing pulse is 2 10 4 in advance or retarded from the leading edge of the pulse received from the distant end. Often an idling signal is sent on synchronous data circuits during periods of no traf c to maintain the timing. Some high-stability systems need resynchronization only once a day. Note that thus far in our discussion we have considered dedicated data circuits only. With switched (dial-up) synchronous circuits, the following problems exist:

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Sensor nodes typically run on batteries, which makes effective power management a key challenge in operating system design, as described in Section 6.3.4. While

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