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regular polyphosphazenes that have been synthesized are given in Table 1.3. The trends in the glass transition temperature (Tg , above which the polymer has exibility to reorient its chains) show some interesting variations related to intraand interchain interactions. Wide-ranging properties (e.g., crystallinity vs. amorphous behavior and hydrophilicity vs. hydrophobicity) can be introduced into the polyphosphazenes through substituent variations. This leads to a wide variety of potential uses. The cost of the polymers has limited their practicality, but the innocuous nature of their hydrolysis products in biological systems provides impetus for biomedical uses of these polymers where cost is less important than effectiveness and lack of toxicity. Early attempts to commercialize the polyphosphazenes were economically unsuccessful, but new ventures are underway as this book is being written not too surprising given their potential as elastomers, solid polymer electrolytes, hydrogels, microencapsulators, bioerodibles, adhesives, liquid crystalline polymers, nonlinear optical materials, and re-resistant materials. More details on the potential usefulness of these polymers will be found in 4. The structures of typical polyphosphazenes are approximately cis, trans planar structures as shown in Figure 1.3c for the chloride derivative. This structural

(2001) A new estimate for present-day Cocos Caribbean plate motion: implications for slip along the Central American volcanic arc Geophys Res Lett 28, 4043 6 DeMets, C & Dixon, TH (1999) New kinematic models for Paci c North America motion from 3 Ma to present: 1 Evidence for steady motion and biases in the NUVEL 1A model Geophys Res Lett 26, 1921 4 DeMets, C et al (1990) Current plate motions Geophys J Int 101, 425 78 DeMets C et al (1994) Effect of recent revisions to the geomagnetic time scale on estimates of current plate motions Geophys Res Lett 21, 2191 94 de Ronde, CEJ, Channer, DM DeR & Spooner, ETC (1997) Archaean Fluids In De Wit, MJ & Ashwal, LD (eds) Greenstone Belts, pp 309 35 Clarendon Press, Oxford.

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locating and fetching the appropriate transform So, the SchemaAdaptor API must take a partner identifier as a parameter, supplied by the caller This implies that the initial recipient of the document (for example, the Web Service servlet) must be able to identify the sending client partner, usually by extracting the required information from the SOAP header Thus, the effort associated with adding a new partner amounts to defining a new XSL transform for it and storing it in the standard, retrievable location 2 Define and organize partner-specific XSL transforms Each exchange partner will need an XSL transform document (for example, an xsl file) to facilitate transforming the document from its format to the one, internal format.

The following is a list of steps which must be followed in order to apply the Best of Both Worlds refactoring. These steps outline a strategy for incrementally introducing CMP into a BMP application. Specifically, new CMP equivalents to existing BMP beans can be added to the application. The existing BMP beans can be modified to extend their new CMP counterparts. Finally, the EJB deployment descriptor can be modified to select which implementation to use. 1. Create CMP beans. Provide a CMP implementation for each BMP bean. 2. Let BMP beans extend their CMP counterparts. Modify the BMP bean implementation class so that it extends the new CMP bean implementation class. 3. Select the implementation in the deployment descriptor. Modify the bean deployment descriptor, selecting which implementation to use. 4. Compile, deploy, and test.

DESERT Group (2004) The crustal structure of the Dead Sea Transform Geophys J Int 156, 655 81 Detrick, RS et al (1987) Multi-channel seismic imaging of a crustal magma chamber along the East Paci c Rise Nature 326, 35 41 Detrick, RS et al (1990) No evidence from multi-channel re ection data for a crustal magma chamber in the MARK area on the Mid-Atlantic Ridge Nature 347, 61 4 Detrick, RS, White RS & Purdy, GM (1993a) Crustal structure of North Atlantic fracture zones Rev Geophys 31, 439 57 Detrick, RS et al (1993b) Seismic structure of the southern East Paci c Rise Science 259, 499 503 Detrick, R et al (1994) In situ evidence for the nature of the seismic layer 2/3 boundary in oceanic crust Nature 370, 288 90 Dewey, JF (1969) Evolution of the Appalachian/Caledonian orogen.

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