11 research outputs found

    Processual antecedents of perceived channel conflict in franchising

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    In this study, we develop and examine the network of relationships explaining perceived conflict in franchise relationships from a franchisee perspective. Our research contributes to the current knowledge of asymmetric exchange relationships through demonstrating the importance of a franchisee's expectations confirmation, relational trust and relationship satisfaction in franchisee assessments of network conflict. The goal of this paper is to empirically examine (1) the relationship between franchisee perceptions of information quality (information dissemination and information search) and the confirmation of franchisee performance expectations, (2) franchisee characterizations of their relationships with their franchisors in terms of relational sentiments such as trust and relational satisfaction, communication and conflict management, (3) the relationship between franchisee satisfaction and perceived conflict, and (4) the moderating effect of franchisee experience on the relationship between franchisee satisfaction and franchisee perceptions of conflict. Empirical results, utilizing a sample of 345 franchisees in Australia, present strong evidence for the support of nine of the ten hypotheses drawn from the conceptual model. Specifically, data reveal that in an effort to cultivate a network of cooperative and satisfied franchisees, franchisors should adopt strategies that promote the timely dissemination of relevant and meaningful pre- and post-entry information, open communication exchange, transparent conflict management systems and personalized support in accommodating individual franchisee needs

    Characterization of magnetic nanoparticles using programmed quadrupole magnetic field-flow fractionation

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    Quadrupole magnetic field-flow fractionation is a relatively new technique for the separation and characterization of magnetic nanoparticles. Magnetic nanoparticles are often of composite nature having a magnetic component, which may be a very finely divided material, and a polymeric or other material coating that incorporates this magnetic material and stabilizes the particles in suspension. There may be other components such as antibodies on the surface for specific binding to biological cells, or chemotherapeutic drugs for magnetic drug delivery. Magnetic field-flow fractionation (MgFFF) has the potential for determining the distribution of the magnetic material among the particles in a given sample. MgFFF differs from most other forms of field-flow fractionation in that the magnetic field that brings about particle separation induces magnetic dipole moments in the nanoparticles, and these potentially can interact with one another and perturb the separation. This aspect is examined in the present work. Samples of magnetic nanoparticles were analysed under different experimental conditions to determine the sensitivity of the method to variation of conditions. The results are shown to be consistent and insensitive to conditions, although magnetite content appeared to be somewhat higher than expected

    Palaeomagnetism of the 1.89?Ga Boonadgin dykes of the Yilgarn Craton: Possible connection with India

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    A palaeomagnetic study was carried out on the newly identified 1888 ± 9 Ma Boonadgin dyke swarm of the Yilgarn Craton in Western Australia. The Bonnadgin dykes yield a mean direction of magnetisation of D = 143°, I = 13°, k = 37 and a 95 = 8°, based on samples from 10 diabase dykes, with a corresponding palaeopole at 47° S, 235° E, A 95 = 6°. A positive baked contact test establishes the primary nature of the magnetisation. The ca. 1.89 Ga palaeopole suggests that the Yilgarn Craton was near the equator at this time, and the Boonadgin dyke swarm can be interpreted to represent an arm of a radiating dyke swarm that shared the same plume centre with coeval mafic dykes in the Dharwar and Bastar cratons of southern India. We therefore propose that the West Australian Craton (WAC, consisting of the Yilgarn and Pilbara cratons) and the South Indian Block (SIB, consisting of the Dharwar, Bastar, and Singhbhum cratons) were connected ca. 1.89 Ga. Globally, available high-quality palaeopoles of similar age allow the West Australian Craton to be placed northwest of proto-Laurentia during the assembly of the supercontinent Nuna
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