Alien Registration- De Grasse, Herbert (Bangor, Penobscot County)

https://digitalmaine.com/alien_docs/15928/thumbnail.jp

Alien Registration- De Grasse, Freda (Bangor, Penobscot County)

https://digitalmaine.com/alien_docs/15927/thumbnail.jp

Alien Registration- De Grasse, Minnie Blle (Bangor, Penobscot County)

https://digitalmaine.com/alien_docs/15929/thumbnail.jp

A study on the use and meaning of maps

This item was digitized by the Internet Archive. Thesis (Ed.M.)--Boston Universityhttps://archive.org/details/studyonusemeanin00deg

Isotopic evidence for complex biogeochemical cycling of Cd in the eastern tropical South Pacific

Over the past decades, observations have confirmed decreasing oxygen levels and shoaling of oxygen minimum zones (OMZs) in the tropical oceans. Such changes impact the biogeochemical cycling of micronutrients such as Cd, but the potential consequences are only poorly constrained. Here, we present seawater Cd concentrations and isotope compositions for 12 depth profiles at coastal, nearshore and offshore stations from 4ºS to 14ºS in the eastern tropical South Pacific, where one of the world’s strongest OMZs prevails. The depth profiles of Cd isotopes display high δ114/110 Cd at the surface and decreasing δ114/110 Cd with increasing water depth, consistent with preferential utilization of lighter Cd isotopes during biological uptake in the euphotic zone and subsequent remineralization of the sinking biomass. In the surface and subsurface ocean, seawater displays similar δ114/110 Cd signatures of 0.47 ±0.23‰ to 0.82±0.05‰ across the entire eastern tropical South Pacific despite highly variable Cd concentrations between 0.01 and 0.84 nmol/kg. This observation, best explained by an open system steady-state fractionation model, contrasts with previous studies of the South Atlantic and South Pacific Oceans, where only Cd-deficient waters have a relatively constant Cd isotope signature. For the subsurface to about 500 m depth, the variability of seawater Cd isotope compositions can be modeled by mixing of remineralized Cd with subsurface water from the base of the mixed layer. In the intermediate and deep eastern tropical South Pacific (>500 m), seawater [Cd] and δ114/110 Cd appear to follow the distribution and mixing of major water masses. We identified modified AAIW of the ETSP to be more enriched in [Cd] than AAIW from the source region, whilst both water masses have similar δ114/110 Cd. A mass balance estimate thus constrains a δ114/110 Cd of between 0.38‰ and 0.56‰ for the accumulated remineralized Cd in the ETSP. Nearly all samples show a tight coupling of Cd and PO4 concentrations, whereby surface and deeper waters define two distinct linear trends. However, seawater at a coastal station located within a pronounced plume of H2S, is depleted in [Cd] and features significantly higher δ114/110 Cd. This signature is attributed to the formation of authigenic CdS with preferential incorporation of lighter Cd isotopes. The process follows a Rayleigh fractionation model with a fractionation factor of α114/110 Cdseawater-CdS = 1.00029. Further deviations from the deep Cd-PO4 trend were observed for samples with O2 < 10 µmol/kg and are best explained by in situ CdS precipitation within the decaying organic matter even though dissolved H2S was not detectable in ambient seawater

Isotopic evidence for complex biogeochemical cycling of Cd in the eastern tropical South Pacific

Over the past decades, observations have confirmed decreasing oxygen levels and shoaling of oxygen minimum zones (OMZs) in the tropical oceans. Such changes impact the biogeochemical cycling of micronutrients such as Cd, but the potential consequences are only poorly constrained. Here, we present seawater Cd concentrations and isotope compositions for 12 depth profiles at coastal, nearshore and offshore stations from 4◦S to 14◦S in the eastern tropical South Pacific, where one of the world’s strongest OMZs prevails. The depth profiles of Cd isotopes display high δ114/110Cd at the surface and decreasing δ114/110Cd with increasing water depth, consistent with preferential utilization of lighter Cd isotopes during biological uptake in the euphotic zone and subsequent remineralization of the sinking biomass. In the surface and subsurface ocean, seawater displays similar δ114/110Cd signatures of 0.47 ± 0.23‰ to 0.82 ± 0.05‰ across the entire eastern tropical South Pacific despite highly variable Cd concentrations between 0.01 and 0.84 nmol/kg. This observation, best explained by an open system steady-state fractionation model, contrasts with previous studies of the South Atlantic and South Pacific Oceans, where only Cd-deficient waters have a relatively constant Cd isotope signature. For the subsurface to about 500 m depth, the variability of seawater Cd isotope compositions can be modeled by mixing of remineralized Cd with subsurface water from the base of the mixed layer. In the intermediate and deep eastern tropical South Pacific (>500 m), seawater [Cd] and δ114/110Cd appear to follow the distribution and mixing of major water masses. We identified modified AAIW of the ETSP to be more enriched in [Cd] than AAIW from the source region, whilst both water masses have similar δ114/110Cd. A mass balance estimate thus constrains a δ114/110Cd of between 0.38‰ and 0.56‰ for the accumulated remineralized Cd in the ETSP. Nearly all samples show a tight coupling of Cd and PO4 concentrations, whereby surface and deeper waters define two distinct linear trends. However, seawater at a coastal station located within a pronounced plume of H2S, is depleted in [Cd] and features significantly higher δ114/110Cd. This signature is attributed to the formation of authigenic CdS with preferential incorporation of lighter Cd isotopes. The process follows a Rayleigh fractionation model with a fractionation factor of α114/110Cdseawater-CdS = 1.00029. Further deviations from the deep Cd–PO4 trend were observed for samples with O2 < 10 μmol/kg and are best explained by in situ CdS precipitation within the decaying organic matter even though dissolved H2S was not detectable in ambient seawater

Slowdown or Crisis? Editorial Introduction

SUMMARY This introduction poses the dilemma of how to characterise the current state of the world economy — is it a mere slowdown, subject to correction by the implementation of better?designed market?orientated strategies, or does it represent a more historically significant crisis, whose resolution depends upon changes in the broader pattern of social relations? The discussion is pursued in three parts. In the first section the dimensions of the current slowdown/crisis are presented. Thereafter a bifurcation is drawn between these two broad framework of analysis. And finally, each of the individual articles in this Bulletin is briefly introduced in the context of the debate between the slowdown and crisis approaches. RESUMEN Introducción editorial Esta introducción plantea el dilema de cómo caracterizar el actual estado de la economía mundial. ¿Se trata de una mera recesión, susceptible de ser rectificada mediante la implementación de estrategias orientadas al mercado, mejor diseñadas o representa una crisis históricamente más significativa, cuya solución depende de cambios en el modelo más amplio de las relaciones sociales? El análisis se realiza en tres partes. En la primera sección se presentan las dimensiones de la crisis/recesión actual. A continuación, se traza una línea divisoria entre ambos marcos de análisis. Finalmente, cada artículo incursiona brevemente en el debate sobre ambos enfoques. RESUME Introduction editoriale Cette introduction pose le problème de savoir comment caractériser l'état actuel de l'économie mondiale — c'est un ralentissement tout simple, sujet à des changements dûs à la mise en pratique de stratégies mieux conçues et orientées vers les marchés, ou est ce que cela représente une crise beaucoup plus importante du point de vue historique, dont la résolution dépend des changements dans la grande structure des relations sociales? Le débat se poursuit en trois parties. Dans la premiere partie est présentée l'étendue du ralentissement/crise actuels. Ensuite une séparation est faite entre ces deux larges charpentes d'analyse. Et pour finir, chaque article dans ce bulletin est introduit brièvement dans le contexe du débat entre les points de vue du ralentissement et de Ja crise

Which bills are lobbied? Predicting and interpreting lobbying activity in the US

Using lobbying data from OpenSecrets.org, we offer several experiments applying machine learning techniques to predict if a piece of legislation (US bill) has been subjected to lobbying activities or not. We also investigate the influence of the intensity of the lobbying activity on how discernible a lobbied bill is from one that was not subject to lobbying. We compare the performance of a number of different models (logistic regression, random forest, CNN and LSTM) and text embedding representations (BOW, TF-IDF, GloVe, Law2Vec). We report results of above 0.85\% ROC AUC scores, and 78\% accuracy. Model performance significantly improves (95\% ROC AUC, and 88\% accuracy) when bills with higher lobbying intensity are looked at. We also propose a method that could be used for unlabelled data. Through this we show that there is a considerably large number of previously unlabelled US bills where our predictions suggest that some lobbying activity took place. We believe our method could potentially contribute to the enforcement of the US Lobbying Disclosure Act (LDA) by indicating the bills that were likely to have been affected by lobbying but were not filed as such