Aixecament topogràfic en tres dimensions de l'Arborètum Dr. Pius Font i Quer de Lleida

Amb el nou jardí botànic de Lleida, l’Arborètum, s’ha aconseguit un gran jardí botànic amb gran variabilitat d’espècies, ja que en 7ha de terreny hi podem trobar fins a 16 ambients amb diferents biodiversitats. En total hi ha uns 1.500 arbres de 225 espècies diferents i 90.000 arbustos de 300 espècies repartits en el territori. Tenint en compte la importància d’aquest jardí botànic, i relacionant-lo amb la topografia, volem aconseguir veure’l en tres dimensions. A través de la visió 3D intentarem donar un tomb virtual dins d’aquest Arborètum, intentant plasmar amb exactitud el seu relleu i recorregut, així com cada un dels seus biomes.

Deposits of the sandy braided South Saskatchewan River: Implications for the use of modern analogs in reconstructing channel dimensions in reservoir characterization

Estimation of the dimensions of fluvial geobodies from core data is a notoriously difficult problem in reservoir modeling. To try and improve such estimates and, hence, reduce uncertainty in geomodels, data on dunes, unit bars, cross-bar channels, and compound bars and their associated deposits are presented herein from the sand-bed braided South Saskatchewan River, Canada. These data are used to test models that relate the scale of the formative bed forms to the dimensions of the preserved deposits and, therefore, provide an insight as to how such deposits may be preserved over geologic time. The preservation of bed-form geometry is quantified by comparing the Alluvial architecture above and below the maximum erosion depth of the modem channel deposits. This comparison shows that there is no significant difference in the mean set thickness of dune cross-strata above and below the basal erosion surface of the contemporary channel, thus suggesting that dimensional relationships between dune deposits and the formative bed-form dimensions are likely to be valid from both recent and older deposits. The data show that estimates of mean bankfull flow depth derived from dune, unit bar, and cross-bar channel deposits are all very similar. Thus, the use of all these metrics together can provide a useful check that all components and scales of the alluvial architecture have been identified correctly when building reservoir models. The data also highlight several practical issues with identifying and applying data relating to cross-strata. For example, the deposits of unit bars were found to be severely truncated in length and width, with only approximately 10% of the mean bar-form length remaining, and thus making identification in section difficult. For similar reasons, the deposits of compound bars were found to be especially difficult to recognize, and hence, estimates of channel depth based on this method may be problematic. Where only core data are available (i.e., no outcrop data exist), formative flow depths are suggested to be best reconstructed using cross-strata formed by dunes. However, theoretical relationships between the distribution of set thicknesses and formative dune height are found to result in slight overestimates of the latter and, hence, mean bankfull flow depths derived from these measurements. This article illustrates that the preservation of fluvial cross-strata and, thus, the paleohydraulic inferences that can be drawn from them, are a function of the ratio of the size and migration rate of bed forms and the time scale of aggradation and channel migration. These factors must thus be considered when deciding on appropriate length:thickness ratios for the purposes of object-based modeling in reservoir characterization.

Facing the broader dimensions of biological invasions

Invasive species are an excellent opportunity to think about the nature society desires, particularly in the face of global changes. Nature and human views of nature are rapidly evolving; our approach to bio- logical invasions through biosecurity institutions and land management policies must evolve in tandem with these changes. We review three dimensions that are insufficiently addressed. First, biological inva- sions are culturally shaped and interpreted. Humans play a major role in the movement and nurturing of alien life, and esthetics, perception, and emotion are deeply implicated in the management of invasive species. What people fear or regret with invasive species are not their effects on nature per se, but their effects on a particular desired nature, and policymaking must reflect this. Second, biological invasions are not restricted to negative impacts. Invasions take place in landscapes where many natural condi- tions have been altered, so policy tools must recognize that invasive species are a functional, structural, and compositional part of transformed ecosystems. In some cases, native species benefit from changes in resource availability caused by invasions or from protections provided by an invasive plant. Finally, invasive species can help ecosystems and people to adapt to global change by maintaining ecosystem processes such as productivity, carbon storage, and nutrient cycling in a context of climate change or land cover transformations. While recognition is growing among ecologists that novel, invaded ecosystems have value, and while the on-the-ground application of biosecurity policies has of necessity adjusted to local contexts and other agendas, invasion biology could aid policymaking by better addressing the three complexities inherent in the three dimensions highlighted above.

Noves i velles migracions: dimensions de la integració sociocultural dels immigrants a Lleida

En aquest article sobre Noves i velles migracions: dimensions de la integració sociocultural dels immigrants a Lleida (1999), s'analitza de forma concisa aquest fenòmen per identificar les principals característiques diferenciadores dels immigrants de la zona lleidatana. L'article consta de tres apartats. En el primer, la introducció, es resumeixen breument els continguts del treball que donen títol a l'article. El segon apartat tracta sobre la integració dels immigrants i comença per una breu reflexió sobre els canvis d'enfocament a l'hora d'estudiar el fenòmen migratori que ajuda a entendre, per exemple, perquè avui parlem d'integració i no d'assimilació. Posteriorment, s'analitza el model migratori català del qual destaca la inexistència de fractura social malgrat l'elevada arribada d'immigrants a Catalunya, i valora els diferents nivells d'integració assolida en cada onada immigratòria del segle XX. Finalment, es detallen els diferents factors relacionats amb la integració sociocultural (impacte en el creixement demogràfic, sistema educatiu, integració en el mercat laboral i adopció de la llengua catalana) de la població immigrada a la ciutat de Lleida i comarques. El treball conclou que el repte és trobar el model d'integració sociocultural adient per al col•lectiu extracomunitari que integra, majoritàriament, l'onada migratòria iniciada en la dècada dels noranta.