A territorial approach to firm entry: The effect of city size

This paper concerns the effects of territorial factors on the processes involved in the creation of manufacturing firms in Spanish cities. Most contributions have focused on regional factors rather than urban ones. Here we assume that it is possible to identify certain urban factors that attract new firms. We use data for the entry of firms in Spanish manufacturing industries between 1994 and 2002. This paper contributes to the existing literature on market entry. Key words: cities, regions, firm entry and Spanish economy. JEL: R0, R12, L60

Los mecanismos de cohesión territorial en España: un análisis y algunas propuestas

El presente informe describe y cuantifica los principales mecanismos de cohesión social y territorial existentes en España, analiza su incidencia sobre la distribución regional de la renta y su contribución a la nivelación de la calidad de los servicios básicos, y propone algunos cambios en su diseño con el objetivo de mejorar sus propiedades de eficiencia y su adecuación a los principios constitucionales de igualdad, solidaridad y autonomía. La tesis central del tabajo es que el proceso de reformas autonómicas que ahora se inicia no debería en ningún caso suponer la ruptura de los mecanismos existentes de cohesión y debería aprovecharse para perfeccionarlos.

Industrial location at a local level: some comments about the territorial level of the analysis

This paper contributes to the existing literature on industrial location by discussing some issues regarding the territorial levels that have been used in location analysis. We analyse which could be the advantages and disadvantages of performing locational analysis at a different local levels. We use data for new manufacturing firms located at municipality, county and travel to work areas level. We show that location determinants vary according to the territorial level used in the analysis, so we conclude that the level at which we perform the investigation should be carefully selected. Keywords: industrial location, cities, agglomeration economies, count data models.

Processos participatius, governança ambiental i desenvolupament territorial sostenible

Estudio realizado a partir de una estancia en el Centro de Filosofia e Ciências Humanas de la Universidade Federal de Santa Catarina, Brasil, durant entre septiembre y noviembre del 2005. El intercambio con los grupos de trabajo del Programa de Pós-Graduçao Interdisciplinar em Ciências Humanas (UFSCE-Brasil), se ha llevado a cabo con el objetivo de profundizar en las diferentes perspectivas teóricas y analíticas que orientan la reflexión sobre el papel crítico de los investigadores en el área de sociología del conocimiento ambiental científico. Esto ha permitido conocer experiencias-laboratorios de procesos participativos para planear intervenciones en áreas protegidas. Estas orientaciones conceptuales, epistemológicas y metodológicas ayudaran a la candidata a reforzar la aproximación de investigación participativa del proyecto “Avaluació social multicriteri per a la presa de decisions orientades a una gestió conservativa de sistemes agropecuaris i el desenvolupament sostenible de la zona seca i semi-seca del paisatge terrestre protegit de Miraflor-Moropotente (Nicaragua)” que es la línea del trabajo de PhD de la candidata. En especial, las reflexiones teóricas y metodológicas se han centrado en los siguientes temas: aproximación sistemática y basada en los actores para el análisis de sistemas complejos y incertezas, métodos participativos para las evaluaciones integradas de sustentabilidad que apoyan los procesos de toma de decisiones, o el nuevo papel de los investigadores sobre una perspectiva compleja de análisis y diálogo entre los conocimientos científicos y locales.

Seminar on territorial cooperation in Europe

Contribució al Seminari: "Les Euroregions: Experiències i aprenatges per a l’Euroregió Pirineus-Mediterrània", 15-16 de desembre de 2005

El territori a Noruega, Finlàndia i Catalunya: comparació territorial i sistemes de planejament

Noruega i Finlàndia representen les icones del model de l'estat del benestar, motiu pel qual molt sovint han estat considerades com a exemples a seguir en matèria de política social, econòmica i ecològica. A més, es tracta de països amb una experiència democràtica més dilatada que Catalunya. Per la seva banda, aquesta darrera forma part de la Mediterrània, una regió històricament marcada per la important intervenció humana sobre el medi i en permanent canvi. Els països nòrdics i Catalunya són exemples de realitats totalment diferents, no només per les característiques del territori sinó també a nivell social, cultural, econòmic, polític i ambiental. La comparació territorial i de sistemes de planejament d'uns i altres és l'objecte d'aquest estudi.

The tectonically controlled emplacement of a vertically sheeted gabbro-pyroxenite intrusion: Feeder-zone of an ocean-island volcano (Fuerteventura, Canary Islands)

The Miocene PX1 gabbro-pyroxenite pluton, Fuerteventura, Canary Islands, is a 3.5 x 5.5 km shallow-level intrusion (0.15-0.2 GPa and 1100-1120 degrees C), interpreted as the feeder-zone to an ocean-island volcano. It displays a vertical magmatic banding expressed in five 50 to 100 metre-wide NNE-SSW trending alkaline gabbro sequences alternating with pyroxenites. This emplacement geometry was controlled by brittle to ductile shear zones, generated by a regional E-W extensional tectonic setting that affected Fuerteventura during the Miocene. At a smaller scale, the PX1 gabbro and pyroxenite bands consist of metre-thick differentiation units, which suggest emplacement by periodic injection of magma pulses as vertical dykes that amalgamated, similarly to a sub-volcanic sheeted dyke complex. Individual dykes underwent internal differentiation following a solidification front parallel to the dyke edges. This solidification front may have been favoured by a significant lateral/horizontal thermal gradient, expressed by the vertical banding in the gabbros, the fractionation asymmetry within individual dykes and the migmatisation of the wall rocks. Pyroxenitic layers result from the fractionation and accumulation of clinopyroxene +/- olivine +/- plagioclase crystals from a mildly alkaline basaltic liquid. They are interpreted as truncated differentiation sequences, from which residual melts were extracted at various stages of their chemical evolution by subsequent dyke intrusions, either next to or within the crystallising unit. Compaction and squeezing of the crystal mush is ascribed to the incoming and inflating magma pulses. The expelled interstitial liquid was likely collected and erupted along with the magma flowing through the newly injected dykes. Clinopyroxene mineral orientation - as evidenced by EBSD and micro X-ray tomography investigations - displays a marked pure-shear component, supporting the interpretation of the role of compaction in the generation of the pyroxenites. Conversely, gabbro sequences underwent minor melt extraction and are believed to represent crystallised coalesced magma batches emplaced at lower rates at the end of eruptive cycles. Clinopyroxene orientations in gabbros record a simple shear component suggesting syn-magmatic deformation parallel to observed NNE-SSW trending shear zones induced by the regional tensional stress field. This emplacement model implies a crystallisation time of 1 to 5 years for individual dykes, consistent with PX1 emplacement over less than 0.5 My. A minimum amount of approximately 150 km(3) of magma is needed to generate the pluton, part of it having been erupted through the Central Volcanic Centre of Fuerteventura. If the regional extensional tectonic regime controls the PX1 feeder-zone initiation and overall geometry, rates and volumes of magma depend on other, source-related factors. High injection rates are likely to induce intrusion growth rates larger than could be accommodated by the regional extension. In this case, dyke intrusion by propagation of a weak tip, combined with the inability of magma to circulate through previously emplaced and crystallised dykes could result in an increase of non-lithostatic pressure on previously emplaced mushy dyke walls; thus generating strong pure-shear compaction within the pluton feeder-zone and interstitial melt expulsion. These compaction-dominated processes are recorded by the cumulitic pyroxenite bands. (C) 2010 Elsevier B.V. All rights reserved.

Modeling of in-situ crystallization processes in the Permian mafic layered intrusion of Mont Collon (Dent Blanche nappe, western Alps)

The Mont Collon mafic complex is one of the best preserved examples of the Early Permian magmatism in the Central Alps, related to the intra-continental collapse of the Variscan belt. It mostly consists (> 95 vol.%) of ol+hy-nonnative plagioclase-wehrlites, olivine- and cpx-gabbros with cumulitic structures, crosscut by acid dikes. Pegmatitic gabbros, troctolites and anorthosites outcrop locally. A well-preserved cumulative, sequence is exposed in the Dents de Bertol area (center of intrusion). PT-calculations indicate that this layered magma chamber emplaced at mid-crustal levels at about 0.5 GPa and 1100 degrees C. The Mont Collon cumulitic rocks record little magmatic differentiation, as illustrated by the restricted range of clinopyroxene mg-number (Mg#(cpx)=83-89). Whole-rock incompatible trace-element contents (e.g. Nb, Zr, Ba) vary largely and without correlation with major-element composition. These features are characteristic of an in-situ crystallization process with variable amounts of interstitial liquid L trapped between the cumulus mineral phases. LA-ICPMS measurements show that trace-element distribution in the latter is homogeneous, pointing to subsolidus re-equilibration between crystals and interstitial melts. A quantitative modeling based on Langmuir's in-situ crystallization equation successfully duplicated the REE concentrations in cumulitic minerals of all rock facies of the intrusion. The calculated amounts of interstitial liquid L vary between 0 and 35% for degrees of differentiation F of 0 to 20%, relative to the least evolved facies of the intrusion. L values are well correlated with the modal proportions of interstitial amphibole and whole-rock incompatible trace-element concentrations (e.g. Zr, Nb) of the tested samples. However, the in-situ crystallization model reaches its limitations with rock containing high modal content of REE-bearing minerals (i.e. zircon), such as pegmatitic gabbros. Dikes of anorthositic composition, locally crosscutting the layered lithologies, evidence that the Mont Collon rocks evolved in open system with mixing of intercumulus liquids of different origins and possibly contrasting compositions. The proposed model is not able to resolve these complex open systems, but migrating liquids could be partly responsible for the observed dispersion of points in some correlation diagrams. Absence of significant differentiation with recurrent lithologies in the cumulitic pile of Dents de Bertol points to an efficiently convective magma chamber, with possible periodic replenishment, (c) 2005 Elsevier B.V. All rights reserved.

Local consumption and territorial based accounting for CO2 Emissions

We examine the complications involved in attributing emissions at a sub-regional or local level. Speci cally, we look at how functional specialisation embedded within the metropolitan area can, via trade between sub-regions, create intra-metropolitan emissions interdependencies; and how this complicates environmental policy implementation in an analogous manner to international trade at the national level. For this purpose we use a 3-region emissions extended input-output model of the Glasgow metropolitan area (2 regions: city and surrounding suburban area) and the rest of Scotland. The model utilises data on commuter flows and household consumption to capture income and consumption flows across sub-regions. This enables a carbon attribution analysis at the sub-regional level, allowing us to shed light on the signi cant emissions interdependencies that can exist within metropolitan areas.

Desenvolupament d’una aplicació web del SIG d’accessibilitat territorial per persones de mobilitat reduïda

L’aplicació web del SIG d’accessibilitat territorial per persones amb mobilitat reduïda pretén ser un instrument que, a partir de la localització cartogràfica dels elements analitzats, ens dona a conèixer les barreres arquitectòniques existents i, d’aquesta manera, estudiar les possibilitats d’actuació i millora que s’haurien de proposar en cada cas