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In earlier chapters, an architecture for mobile services ( 3), several enabling technologies (s 4, 5 and 6) as well as different reference applications ( 7) have been described. However, if one wants to reach mass markets, one needs a good understanding of the needs and requirements coming from the users and other stakeholders (as discussed in 2), as well as continuous evaluation and validation of the intermediate and nal results. Large R&D projects, covering heterogeneous areas from enabling technologies to end-user applications, need a very strong process in order to enable evaluation and validation of the results from different points of view, requiring therefore expertise in different areas. The key areas of the evaluation are as follows: Evaluation and validation from the end-users points of view, using the approach and methodologies typical of the user-centred design process (see 2). Technical evaluation, looking at the key technological aspects, highlighting the major innovative aspects of the technical results, and analysing them against the requirements and speci cations set at the beginning. User evaluation is an integral part of a process to ensure the user centricity of the overall process, which in turn will result in better user acceptance and better assessment of the market

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very costly to implement. Seriously, I happen to like the AppleTalk protocol. AppleTalk was actually the software and LocalTalk was the hardware. It was Apple s version of networking Mac computers, and, except for the wiring, it was free. The protocol was simple to install and use. It was built into every Mac. Cables were simply needed to hook up Apple computers to a simple network, and file and print services were built in as well. It was known as true peer to peer, for each workstation could see every other workstation, and each workstation could be a server and share any of its resources. Each node ran the name service. Each node picked its own physical address. Even dialing in to an AppleTalk network was easy using the AppleTalk Remote Access (ARA) protocol, and it made it look like you were a local node on the AppleTalk network. It soon became a very popular method of hooking together Mac computers into a network. However, AppleTalk was not envisioned as a protocol to handle large internets of Apple computers, and the inefficiencies of the protocol soon arose. It was about as close as you could come to a network operating system that allowed for simplicity and ingenuity. AppleTalk had one problem: scalability. Try building a large AppleTalk network, not an easy task, if not impossible. TCP/IP eliminated proprietary network operating systems; however, not intentionally. Again, it was built for a different purpose. TCP s beginnings were rough (interoperability issues) and, in fact, TCP/IP was not the original protocol of the

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authorities, user groups and individual users interact and co-operate to create and provide the services effectively, timely, and securely while balancing the various interests and values of the different players To ful l the requirements of the different actors, many technology enablers have been introduced by different initiatives and organisations focusing on one of the requirement subsets.

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The relative positions of such groundwater discharge features within the landscape exert a profound in uence on patterns of groundwater ow (Box 3.2). Where a river is functioning as a groundwater discharge zone, for instance, groundwater owing within the adjoining aquifer will converge towards both banks. In some cases, the patterns of surface-water features incised into aquifers will have been determined by external geological forces. For instance, the usual explanation for meanders incised deeply into bedrock is that the channel pattern must have been established by downcutting through previously overlying soft sediments, since removed. Similarly, erosion along lines of weakness such as faults can result in the incision of linear river reaches into aquifers. In other cases, patterns of groundwater out ow can themselves strongly in uence the patterns assumed by river systems (e.g. LaFleur 1984; Higgins and Coates 1990). Where groundwater out ow has greatly contributed to valley development, characteristic landforms can often be recognized, including:

As described by Graham et al. [6], soil-dust elements (Al, Si, Ca, Ti, Mn and Fe) ranged from 0.2 ng m 3 (Mn) to 25 ng m 3 (Si). They were found in various wet season eld campaigns in both the ne and coarse aerosol fractions in comparable amounts, which hint towards signi cant long-range transport. Crustal enrichment factors close to unity indicate soil dust as the main source. Wind erosion is minimal in the Amazon Basin due to the dense vegetation, and hence, concentrations of these species are very low. A major fraction of soil dust in the basin originates from the Sahara. Coarse-mode P, S, K, Cu and Zn enrichment factors are larger than unity and thus typical for primary biogenic emissions at tropical forest sites. Na and Cl derive mainly from sea salt from the Atlantic, although Cl is also emitted from plants. Ni, Cr, Pb and V were observed in very low concentrations, often below the detection limit.

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