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the importance of the external environment both for projects in general and for construction projects in particular. Internal stakeholders, representing the internal exchange, can be de ned as those who are formally connected with the project (e.g. owners, customers and employees), whereas external stakeholders, representing the external exchange, are those affected by the project in some way (Gibson, 2000). Figure 15.1 shows a schematic picture of the potential stakeholders in a construction project, divided into internal and external stakeholders. Construction project managers need to be capable of managing internal and external stakeholder exchange. In a way, it can be argued that more effort and resources should be committed to the management of external stakeholders because there are more of them and relationships with them are more diffuse than in the case of internal stakeholders. For the internal exchange, there is often an agreement or a contract to set the framework of the relationship and the resolution of potential con icts. The stakeholder environment has a strong effect on project implementation. The environment will change in its nature depending on actions taken by different stakeholders and will affect project implementation in a certain way. The stakeholder management process can thus be de ned as having the aim of maintaining the desired implementation of the project and avoiding unnecessary con ict and controversy with stakeholders. The Hallands s project

16 V

Similarly, we can consider the data content for the combined schema and compare it to the data content in each S-DBE If every data value present in the S-DBE DBs is visible to the DDBA in the DDBE, then we have total data visibility (TDV) In other words, TDV means that there is no hidden data content; there is no data value missing from the DDBE but present in one of the CDBE DBs When we have both total schema visibility and total data visibility, we have the rst extreme case for this level, namely, total visibility (TV) TV can happen in the real world, and in fact, it is a requirement for some particular DDBE architectures, some of which we will discuss in 12.

It should be obvious that the other extreme case is not possible if the combined schema was empty and all the data content were hidden, then the DDBE would be completely worthless! If we have some hidden schema, then we have partial schema visibility (PSV) If we have some hidden data, then we have partial data visibility (PDV) Having either PSV, PDV, or both PSV and PDV is referred to as partial visibility (PV) PV is a common occurrence and even a requirement for some particular DDBE architectures We will also discuss some of these architectures in 12 For the sake of completeness, we will mention that there is one more reason why this level is not interesting when we are looking at a single CDBE (as opposed to a DDBE or a Sub-DBE): the TV scenario is really the only possible situation for most CDBEs..

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The work described here has been supported since 1980 by the National Institute on Aging (Grant #AG-07137). This research was made possible by the support of our many friends and colleagues, including Steve Aggen, Dick Bell, Steve Boker, Aki Hamagami, Earl Hishinuma, John Horn, Bill Meredith, Carol Prescott, and Dick Woodcock.

183 Hu, YF and Lee, H Prediction of the surface tension of mixed electrolyte solutions based on the equation of Patwardhan and Kumar and the fundamental Butler equations Journal of Colloid and Interface Science 2004; 269(2): 442 448 184 Hanel, G The properties of atmospheric aerosol particles as functions of the relative humidity at thermodynamic equilibrium with the surrounding moist air Advances in Geophysics 1976; 19: 73 188 185 Chen, JP Theory of deliquescence and modi ed Kohler curves Journal of the Atmospheric Sciences 1994; 51(23): 3505 3516 186 Brechtel, FJ and Kreidenweis, SM Predicting particle critical supersaturation from hygroscopic growth measurements in the humidi ed TDMA Part I: theory and sensitivity studies Journal of the Atmospheric Sciences 2000; 57(12): 1854 1871 187 Brechtel, FJ and Kreidenweis, SM Predicting particle critical supersaturation from hygroscopic growth measurements in the humidi ed TDMA.

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Part II: laboratory and ambient studies Journal of the Atmospheric Sciences 2000; 57(12): 1872 1887 188 Tuckermann, R and Cammenga, HK The surface tension of aqueous solutions of some atmospheric water-soluble organic compounds Atmospheric Environment 2004; 38(36): 6135 6138 189 Facchini, MC, Decesari, S, Mircea, M, Fuzzi, S and Loglio, G Surface tension of atmospheric wet aerosol and cloud/fog droplets in relation to their organic carbon content and chemical composition Atmospheric Environment 2000; 34(28): 4853 4857 190 Poling, BE, Prausnitz, JM and O Connell, JP The Properties of Gases and Liquids McGraw-Hill Professional, New York: 2000 191 Topping, D Modelling the Hygroscopic Properties of Atmospheric Aerosols University of Manchester, Manchester: 2005 192 Lamer, VK and Gruen, R A direct test of Kelvin equation connecting vapour pressure and radius of curvature Transactions of the Faraday Society 1952; 48(5): 410 415.

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