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Further, the selection process not only places the obvious limitations on the generalizability of the results to other groups, but may also be the source of other interpretive limitations For example, the validity of self-reports of negative psychosocial characteristics may be suspect among individuals who underwent such assessments as part of college admissions or similar procedures Hence, the scienti c value of studies of such convenience samples involves a trade-off between a more rapid development of the literature versus more de nitive studies Sampling in clinical studies of psychosocial risk factors as predictors of the course of established disease pose other potential limitations For example, if a risk factor (eg, depression) exerts an effect on the initial development of a life-threatening disease (eg, CHD), persons who survive long enough to be recruited into clinical studies will not provide a representative sample for studying this risk factor.

A company might have other assets that do not fit into either current assets or fixed assets. Some of the more common ones are discussed here. China, Glass, Silver, Linen, and Uniforms This amount is made up from two figures. The estimated value of items in use is added to the cost of those items still new and in storage. Deposits If the deposit is refundable at some future time, it can be considered an asset. An example of this would be a deposit with a utility company. Investments Long-term investments in other companies or in property or plant not connected with the day-to-day running of the business are shown as a separate category of asset. This category does not include short-term investments, such as a separate building that is owned and rented to another organization. Leasehold Costs or Leasehold Improvements It is reasonably common for land or the building to be leased. Where a longterm lease is paid in advance, the unexpired portion of this cost should be shown as an asset. Similarly, if improvements are made to a leased building, these

Persons who survive despite a high level of the risk factor are likely to be more resilient to its negative effects than are those who did not survive the initial presentation of the disease (T Q Miller, Turner, Tindale, Posavac, & Dugoni, 1991; R B Williams, 2000) Of course, questions about the psychosocial predictors of the course of a disease are important in and of themselves, and the appropriate sample consists by de nition of those who survived its initial presentation However, if a risk factor has a signi cant effect in initially healthy samples and not among those with established disease, this may re ect moderation of its effects by the nonrandom selection into clinical populations Effect Sizes Valid evidence of reliable associations between psychosocial risk factors and subsequent disease or mortality raises a.

relative contributions of direct and indirect recharge, if the direct recharge element has been independently determined using soil moisture budgeting techniques (It should be noted that the logic of determining recharge rate from water table rise is simply the inverse application of the principle presented in Figure 17, where we calculated speci c yield from the observed water level rise corresponding to a known amount of recharge) Geochemical approaches to recharge estimation can also shed some light on the magnitude of localized inputs For instance, the occurrence of localized recharge can be demonstrated from the chemistry of pore waters extracted from rock core samples obtained at various depths in the unsaturated zone (eg Edmunds and Tyler 2002) As was mentioned in Section 22.

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3, the evapotranspirative loss of water during direct recharge leads us to expect the concentration of chloride (and other solutes) to increase with depth through the soil zone, until some approximately steady concentration is reached, which will persist throughout the unsaturated zone (Figure 23a) However, where localized recharge is occurring, marked decreases in chloride concentration at depth may well be detected (Figure 23b) This occurs due to the mixing of dilute, rapidly in ltrated localized recharge waters with the more concentrated, directly recharged waters (eg de Vries and Simmers 2002) Besides tracing the unsaturated zone pro les of chloride and other major ions, the same approach can also be applied to the isotopes of hydrogen and oxygen present in the water molecules themselves (see Hiscock 2005, pp 123 126).

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