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Should users open your files directly (as host) via file sharing rather than through FileMaker s Open Remote dialog, your files are placed at risk (for example, if a network drop-out occurs), and performance is severely compromised Another significant risk presenting itself whenever database files are stored on a volume enabled for file sharing is that multiple copies of the files will be available, and users may make their own copies If they do, users are highly likely to inadvertently open the wrong copy of the database for a given work session Then, when they next log in (to the correct copy of your solution), all the work from their previous work session is absent.

Database tables are part of the organizing principle for your data. When you have things to organize, you group them together, first into broad (but clear) categories and then into finer categories. All your clothes go into a certain closet, but within that closet, the socks go into a certain drawer, the handkerchiefs into another. Tables provide a receptacle for information about a particular kind or class of things, allowing you to establish hierarchies of order and clarity as a framework for management of the information in your solution.

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Even if users realize immediately what has occurred and where all their work from the previous day is located, reconciling the data between the two copies of your solution may present significant challenges (particularly if some users have been updating one version while others were updating another) You can avoid all these problems and potential pitfalls by ensuring that file sharing is never enabled for volumes where copies of your database files are stored and, particularly, for the computer (or computers) you re using to host databases via FileMaker Network Sharing..

Purpose: Use the Set Next Serial Value step to set the next value to be used for an auto-entry serial number field. You can specify a literal value or a calculated result. Options: Specify target field, Specify calculated result If the Specify target field option is not used to select a field, the currently active field (if any) is set. This field must be an auto-entry serial number field; otherwise, this script step has no effect. The Calculated result Specify button is used to specify the literal value or create the formula used by the step. See also: Set Field, Insert Calculated Result

Continental areas of the Earth are typically composed of materials in the following vertical sequence: the A and B soil horizons; the C soil horizon (from which the other soil horizons may have been derived: Madsen and Ghiorse, 1993; Brady and Weil, 1999); an unsaturated (or vadose) zone (that begins with the C soil horizon and ends at the water table); and a capillary fringe zone residing directly above a saturated zone which may extend through many different geologic strata (Figure 4.11). Where does the soil habitat end and the subsurface terrestrial habitat begin In some de nitions, the subsurface terrestrial habitat begins immediately below the B soil horizon where soil scientists traditionally have felt that photosynthesis-based biological activity ceases (Madsen and Ghiorse, 1993; Brady and Weil, 1999). It is important to acknowledge, however, that the transition between soil and subsurface terrestrial habitats is not delineated by soil horizons per se. Indeed, plant roots may penetrate the C soil horizon, thereby supplementing the subsurface with photosynthetic carbon compounds that may stimulate microbial activity (Madsen, 1995). Beneath the soil, which, by de nition, is the zone of pedogenesis (soil formation), lie the unsaturated and saturated subsurface zones. This view of the subsurface habitat as being delineated in terms of the degree to which water occupies voids in a porous matrix (if air has been completely displaced by water, the system is saturated ; if not, the system is unsaturated ) is satisfying, but it is also simplistic. For superimposed upon the degree of water saturation are the geologic, geographic, and climatic characteristics. At a given location on the Earth s surface, the stratigraphy beneath re ects a unique and complex history of geologic

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