De Relatie tussen Hechting en Welbevinden bij Ouderen: De mediërende Invloed van Mindfulness en Zingeving

Empirische studies hebben aangetoond dat bij ouderen een veilige hechting positief samenhangt met het niveau van welbevinden. Hechting is een relatief stabiel en moeilijk te beïnvloeden persoonlijk kenmerk en daarom is het belangrijk om mediatoren van het verband tussen hechting en psychologische uitkomstmaten te vinden die met interventies te beïnvloeden zijn. De vraagstelling van de studie luidde: ‘Welk verband bestaat er tussen hechting en welbevinden bij ouderen en wordt dit verband gemedieerd door mindfulness en zingeving?’. De huidige studie was een survey met één meetmoment. De 210 respondenten waren 65 jaar of ouder (M = 71.25, SD = 5.42) en thuiswonend. Daarnaast mochten ze geen ernstige geheugenproblemen of een psychiatrische stoornis hebben. Via de sneeuwbalmethode werden de respondenten mondeling of schriftelijk door de onderzoeker benaderd. De vragenlijst kon anoniem online of op papier worden ingevuld. Hechting werd gemeten met de Experiences in Close Relationships-Revised (ECR-R), mindfulness met de Five Facet Mindfulness Questionnaire (FFMQ), zingeving met de Meaning in Life Questionnaire, subschaal ‘Presence of meaning in life’ (MLQ-P) en welbevinden met de Positive Affect Negative Affect Scale (PANAS) en de Satisfaction With Life Scale (SWLS). Zowel hechtingsgerelateerde angst (‘angst’) als hechtingsgerelateerde vermijding (‘vermijding’) bleek in correlatieanalyses negatief samen te hangen met mindfulness, zingeving en welbevinden. Tussen mindfulness, zingeving en welbevinden werden positieve verbanden gevonden. De (seriële) mediatieanalyse werd uitgevoerd met behulp van de macro PROCESS 2.13. Zowel het verband tussen ‘angst’ en welbevinden als tussen ‘vermijding’ en welbevinden werd volledig (serieel) gemedieerd door mindfulness en zingeving.

Relation entre la représentation de la maladie et le bien-être subjectif et psychologique chez des patients atteints de cancer

L’annonce d’un diagnostic de cancer a un impact important sur l’individu. En se basant sur des informations sociales, environnementales et personnelles, celui-ci tentera de se représenter la maladie. Cette représentation constitue une grille d’informations cognitives et émotionnelles servant à donner un sens à la maladie et y réagir. Le modèle d’autorégulation de Leventhal propose qu’en fonction de sa représentation de la maladie, un individu mettra de l’avant différentes stratégies d’adaptation; ultimement, ces stratégies auront un impact sur l’issue de la maladie dont le niveau de bien-être. La présente recherche propose de considérer l’avenue tant hédonique qu’eudémonique du bien-être, en y incluant le bien-être subjectif, correspondant aux affects positifs et négatifs et à la satisfaction de vie et le bien-être psychologique correspondant à un état d’épanouissement personnel. L’étude a pour objectif principal de documenter les liens entre les dimensions cognitives et émotionnelles de la représentation de la maladie et les dimensions du bien-être subjectif (avenue hédonique) et le bien-être psychologique (avenue eudémonique). Plus précisément, les hypothèses postulent qu’une représentation plus positive de la maladie a pour effet d’augmenter le bien-être subjectif et psychologique. Les hypothèses postulent que la dimension de la représentation émotionnelle de la maladie joue un rôle médiateur entre les dimensions cognitives de la représentation de la maladie et le bien-être subjectif et psychologique. Pour atteindre ces objectifs, 70 participants âgés entre 31 et 75 ans ayant été atteints de cancer dans les cinq dernières années ont été recrutés. Les données ont été recueillies à l’aide de questionnaires autorapportés : un questionnaire sociodémographique, les versions francophones du Revised Illness Perception Questionnaire (IPQ-R : Moss-Morris et al., 2002), du Positive and Negative Affect Scale (PANAS ; Watson, Clark, & Tellegen, 1988), du Satisfaction with Life Scale (Diener, Emmons, Larsen, & Griffin, 1985) et du The Scales of Psychological Well-Being (Ryff & Essex, 1992). Des analyses statistiques de régressions multiples et de médiation ont été réalisées à l’aide du logiciel Statistical Package for Social Sciences (SPSS). Les résultats indiquent que seulement certaines dimensions de la représentation de la maladie exercent un effet unique sur le bien-être subjectif et/ou psychologique soit le contrôle personnel perçu, la représentation émotionnelle de la maladie, les conséquences perçues de la maladie et le cours aigu/chronique de la maladie. La représentation émotionnelle de la maladie semble exercer un effet médiateur complet entre certaines dimensions cognitives de la représentation de la maladie et les niveaux de bien-être. C’est le cas pour l’identité, le cours aigu/chronique de la maladie, le cours cyclique de la maladie, les conséquences perçues de la maladie et l’efficacité perçue du traitement, lorsque mis en lien avec les affects négatifs. C’est aussi le cas pour l’identité et le cours cyclique de la maladie, lorsque mis en lien avec la satisfaction de vie, et pour le cours cyclique de la maladie et les conséquences perçues de la maladie, lorsque mis en lien avec le bien-être psychologique. Les affects positifs associés au volet affectif du bien-être subjectif ne sont pas affectés par la représentation de la maladie.

Qualidade de vida e suporte social em doentes com esquizofrenia

A Esquizofrenia é considerada pela OMS como uma das dez doenças mais incapacitantes. Sendo uma perturbação complexa e de caráter crónico, gera prejuízos significativos na qualidade de vida dos pacientes. O interesse por este tema surge aquando da desinstitucionalização dos doentes psiquiátricos, contudo os avanços no tratamento desta patologia nem sempre vêm acompanhados de melhora na qualidade de vida, fator este que levou a ter também em consideração, aspetos psicossociais. Assim, pretende-se com este estudo contribuir para a compreensão do nível de satisfação com o suporte social e qualidade de vida destes doentes, comparando-os com indivíduos sem psicopatologia. A amostra é composta por 202 participantes, os quais se dividem em dois grupos, indivíduos com esquizofrenia, que frequentam hospitais na zona norte, centro e sul do país (n=101) e indivíduos sem psicopatologia (n=101), com idades compreendidas entre os 20 e os 75 anos. Os participantes responderam a um protocolo de investigação composto por quatro instrumentos: um questionário sociodemográfico; o WHOQOL-Bref, que avalia a qualidade de vida; a escala de satisfação com o suporte social; e a escala de afeto positivo e negativo. Os resultados principais evidenciam a pouca literatura existente, mostrando que existem diferenças significativas no que refere à qualidade de vida e satisfação com o suporte social entre os indivíduos com esquizofrenia e indivíduos sem patologia psiquiátrica, sendo que os valores mais baixos destas variáveis se concentram nos indivíduos com esquizofrenia. Para estes doentes, verificou-se que a qualidade de vida está positivamente correlacionada com o suporte social e com o afeto positivo, estando também correlacionada negativamente com o afeto negativo. Contudo, não se verificaram correlações da qualidade de vida com a escolaridade, o número de internamentos e o tempo de doença. A satisfação com o suporte social e o afeto positivo e negativo revelaram-se preditores de qualidade de vida nos indivíduos com esquizofrenia. No sentido de promover a melhoria da qualidade de vida destes doentes deverão ser tidas em consideração em vários contextos, intervenções psicossociais.

A formação de adultos, aquisição de competências e empregabilidade

Dissertação de Mestrado, Psicologia da Educação, especialidade de Contextos Educativos, 29 abril de 2016, Universidade dos Açores.

O bem-estar subjetivo, a esperança, o otimismo e a resiliência em famílias com filhos com NEE

Dissertação de Mestrado, Psicologia da Educação, Faculdade de Ciências Humanas e Sociais, Universidade do Algarve, 2016

The relationship between perceived training and development and employee retention:the mediating role of work attitudes

This paper considers how utilizing a model of job-related affect can be used to explain the processes through which perceived training and development influence employee retention. We applied Russell’s model of core affect to categorize four different forms of work attitude, and positioned these as mediators of the relationship between perceived training and development and intention to stay. Using data from 1,191 employees across seven organizations, multilevel analyses found that job satisfaction, employee engagement, and change-related anxiety were significantly associated with intention to stay, and fully mediated the relationship between perceived training and development and intention to stay. Contrary to our hypotheses, emotional exhaustion was not significantly associated with intention to stay nor acted as a mediator when the other attitudes were included. These findings show the usefulness of Russell’s model of core affect in explaining the link between training and development and employee retention. Moreover, the findings collectively suggest that studies examining employee retention should include a wider range of work attitudes that highlight pleasant forms of affect.

The contribution of leadership attributes to large scale, complex project success

Mismanagement of large-scale, complex projects has resulted in spectacular failures, cost overruns, time blowouts, and stakeholder dissatisfaction. We focus discussion on the interaction of key management and leadership attributes which facilitate leaders’ adaptive behaviors. These behaviors should in turn influence adaptive team member behavior, stakeholder engagement and successful project outcomes, outputs and impacts. An understanding of this type of management will benefit from a perspective based in managerial and organizational cognition. The research question we explore is whether successful leaders of large-scale complex projects have an internal process leading to a display of administrative, adaptive, and enabling behaviors that foster adaptive processes and enabling behaviors within their teams and with external stakeholders. At the core of the model we propose interactions of key attributes, namely cognitive flexibility, affect, and emotional intelligence. The result of these cognitive-affective attribute interactions is leadership leading to enhanced likelihood of complex project success.

The Evolving Roles of the Human Resource Function: Understanding Role Changes in the Context of Large-Scale Mergers

The human resource (HR) function is under pressure both to change roles and to play a large variety of roles. Questions of change and development in the HR function become particularly interesting in the context of mergers and acquisitions when two corporations are integrated. The purpose of the thesis is to examine the roles played by the HR function in the context of large-scale mergers and thus to understand what happens to the HR function in such change environments, and to shed light on the underlying factors that influence changes in the HR function. To achieve this goal, the study seeks first to identify the roles played by the HR function before and after the merger, and second, to identify the factors that affect the roles played by the HR function. It adopts a qualitative case study approach including ten focal case organisations (mergers) and four matching cases (non-mergers). The sample consists of large corporations originating from either Finland or Sweden. HR directors and members of the top management teams within the case organisations were interviewed. The study suggests that changes occur within the HR function, and that the trend is for the HR function to become increasingly strategic. However, the HR function was found to play strategic roles only when the HR administration ran smoothly. The study also suggests that the HR function has become more versatile. An HR function that was perceived to be mainly administrative before the merger is likely after the merger to perform some strategically important activities in addition to the administrative ones. Significant changes in the roles played by the HR function were observed in some of the case corporations. This finding suggests that the merger integration process is a window of opportunity for the HR function. HR functions that take a proactive and leading role during the integration process might expand the number of roles played and move from being an administrator before the merger to also being a business partner after integration. The majority of the HR functions studied remained mainly reactive during the organisational change process and although the evidence showed that they moved towards strategic tasks, the intra-functional changes remained comparatively small in these organisations. The study presents a new model that illustrates the impact of the relationship between the top management team and the HR function on the role of the HR function. The expectations held by the top management team for the HR function and the performance of the HR function were found to interact. On a dimension reaching from tactical to strategic, HR performance is likely to correspond to the expectations held by top management.

The motion and the core structure of a geostrophic vortex - one-time scale inner solution and the motion of the vortex

By means of the matched asymptotic expansion method with one-time scale analysis we have shown that the inviscid geostrophic vortex solution represents our leading solution away from the vortex. Near the vortex there is a viscous core structure, with the length scale O(a). In the core the viscous stresses (or turbulent stresses) are important, the variations of the velocity and the equivalent height are finite and dependent of time. It also has been shown that the leading inner solutions of the core structure are the same for two different time scales of S/(ghoo)1/2 and S/a (ghoo)1/2. Within the accuracy of O(a) the velocity of a geostrophic vortex center is equal to the velocity of the local background flow, where the vortex is located, in the absence of the vortex. Some numerical examples demonstrate the contributions of these results.

Seismic structure above and below the core-mantle boundary

Seismic structure above and below the core-mantle boundary (CMB) has been studied through use of travel time and waveform analyses of several different seismic wave groups. Anomalous systematic trends in observables document mantle heterogeneity on both large and small scales. Analog and digital data has been utilized, and in many cases the analog data has been optically scanned and digitized prior to analysis.

Differential travel times of S - SKS are shown to be an excellent diagnostic of anomalous lower mantle shear velocity (V s) structure. Wavepath geometries beneath the central Pacific exhibit large S- SKS travel time residuals (up to 10 sec), and are consistent with a large scale 0(1000 km) slower than average V_s region (≥3%). S - SKS times for paths traversing this region exhibit smaller scale patterns and trends 0(100 km) indicating V_s perturbations on many scale lengths. These times are compared to predictions of three tomographically derived aspherical models: MDLSH of Tanimoto [1990], model SH12_WM13 of Suet al. [1992], and model SH.10c.17 of Masters et al. [1992]. Qualitative agreement between the tomographic model predictions and observations is encouraging, varying from fair to good. However, inconsistencies are present and suggest anomalies in the lower mantle of scale length smaller than the present 2000+ km scale resolution of tomographic models. 2-D wave propagation experiments show the importance of inhomogeneous raypaths when considering lateral heterogeneities in the lowermost mantle.

A dataset of waveforms and differential travel times of S, ScS, and the arrival from the D" layer, Scd, provides evidence for a laterally varying V_s velocity discontinuity at the base of the mantle. Two different localized D" regions beneath the central Pacific have been investigated. Predictions from a model having a V_s discontinuity 180 km above the CMB agree well with observations for an eastern mid-Pacific CMB region. This thickness differs from V_s discontinuity thicknesses found in other regions, such as a localized region beneath the western Pacific, which average near 280 km. The "sharpness" of the V_s jump at the top of D", i.e., the depth range over which the V_s increase occurs, is not resolved by our data, and our data can in fact may be modeled equally well by a lower mantle with the increase in V_s at the top of D" occurring over a 100 krn depth range. It is difficult at present to correlate D" thicknesses from this study to overall lower mantle heterogeneity, due to uncertainties in the 3-D models, as well as poor coverage in maps of D" discontinuity thicknesses.

P-wave velocity structure (V_p) at the base of the mantle is explored using the seismic phases SKS and SPdKS. SPdKS is formed when SKS waves at distances around 107° are incident upon the CMB with a slowness that allows for coupling with diffracted P-waves at the base of the mantle. The P-wave diffraction occurs at both the SKS entrance and exit locations of the outer core. SP_dKS arrives slightly later in time than SKS, having a wave path through the mantle and core very close to SKS. The difference time between SKS and SP_dKS strongly depends on V_p at the base of the mantle near SK Score entrance and exit points. Observations from deep focus Fiji-Tonga events recorded by North American stations, and South American events recorded by European and Eurasian stations exhibit anomalously large SP_dKS - SKS difference times. SKS and the later arriving SP_dKS phase are separated by several seconds more than predictions made by 1-D reference models, such as the global average PREM [Dziewonski and Anderson, 1981] model. Models having a pronounced low-velocity zone (5%) in V_p in the bottom 50-100 km of the mantle predict the size of the observed SP_dK S-SKS anomalies. Raypath perturbations from lower mantle V_s structure may also be contributing to the observed anomalies.

Outer core structure is investigated using the family of SmKS (m=2,3,4) seismic waves. SmKS are waves that travel as S-waves in the mantle, P-waves in the core, and reflect (m-1) times on the underside of the CMB, and are well-suited for constraining outermost core V_p structure. This is due to closeness of the mantle paths and also the shallow depth range these waves travel in the outermost core. S3KS - S2KS and S4KS - S3KS differential travel times were measured using the cross-correlation method and compared to those from reflectivity synthetics created from core models of past studies. High quality recordings from a deep focus Java Sea event which sample the outer core beneath the northern Pacific, the Arctic, and northwestern North America (spanning 1/8th of the core's surface area), have SmKS wavepaths that traverse regions where lower mantle heterogeneity is pre- dieted small, and are well-modeled by the PREM core model, with possibly a small V_p decrease (1.5%) in the outermost 50 km of the core. Such a reduction implies chemical stratification in this 50 km zone, though this model feature is not uniquely resolved. Data having wave paths through areas of known D" heterogeneity (±2% and greater), such as the source-side of SmKS lower mantle paths from Fiji-Tonga to Eurasia and Africa, exhibit systematic SmKS differential time anomalies of up to several seconds. 2-D wave propagation experiments demonstrate how large scale lower mantle velocity perturbations can explain long wavelength behavior of such anomalous SmKS times. When improperly accounted for, lower mantle heterogeneity maps directly into core structure. Raypaths departing from homogeneity play an important role in producing SmKS anomalies. The existence of outermost core heterogeneity is difficult to resolve at present due to uncertainties in global lower mantle structure. Resolving a one-dimensional chemically stratified outermost core also remains difficult due to the same uncertainties. Restricting study to higher multiples of SmKS (m=2,3,4) can help reduce the affect of mantle heterogeneity due to the closeness of the mantle legs of the wavepaths. SmKS waves are ideal in providing additional information on the details of lower mantle heterogeneity.

Geological evolution of two crustal scale shear zones. Part I. The Rand thrust complex, northwestern Mojave Desert, California. Part II. The Magdalena metamorphic core complex, north central Sonora, Mexico

The geology and structure of two crustal scale shear zones were studied to understand the partitioning of strain within intracontinental orogenic belts. Movement histories and regional tectonic implications are deduced from observational data. The two widely separated study areas bear the imprint of intense Late Mesozoic through Middle Cenozoic tectonic activity. A regional transition from Late Cretaceous-Early Tertiary plutonism, metamorphism, and shortening strain to Middle Tertiary extension and magmatism is preserved in each area, with contrasting environments and mechanisms. Compressional phases of this tectonic history are better displayed in the Rand Mountains, whereas younger extensional structures dominate rock fabrics in the Magdalena area.

In the northwestern Mojave desert, the Rand Thrust Complex reveals a stack of four distinctive tectonic plates offset along the Garlock Fault. The lowermost plate, Rand Schist, is composed of greenschist facies metagraywacke, metachert, and metabasalt. Rand Schist is structurally overlain by Johannesburg Gneiss (= garnet-amphibolite grade orthogneisses, marbles and quartzites), which in turn is overlain by a Late Cretaceous hornblende-biotite granodiorite. Biotite granite forms the fourth and highest plate. Initial assembly of the tectonic stack involved a Late Cretaceous? south or southwest vergent overthrusting event in which Johannesburg Gneiss was imbricated and attenuated between Rand Schist and hornblende-biotite granodiorite. Thrusting postdated metamorphism and deformation of the lower two plates in separate environments. A post-kinematic stock, the Late Cretaceous Randsburg Granodiorite, intrudes deep levels of the complex and contains xenoliths of both Rand Schist and mylonitized Johannesburg? gneiss. Minimum shortening implied by the map patterns is 20 kilometers.

Some low angle faults of the Rand Thrust Complex formed or were reactivated between Late Cretaceous and Early Miocene time. South-southwest directed mylonites derived from Johannesburg Gneiss are commonly overprinted by less penetrative north-northeast vergent structures. Available kinematic information at shallower structural levels indicates that late disturbance(s) culminated in northward transport of the uppermost plate. Persistence of brittle fabrics along certain structural horizons suggests a possible association of late movement(s) with regionally known detachment faults. The four plates were juxtaposed and significant intraplate movements had ceased prior to Early Miocene emplacement of rhyolite porphyry dikes.

In the Magdalena region of north central Sonora, components of a pre-Middle Cretaceous stratigraphy are used as strain markers in tracking the evolution of a long lived orogenic belt. Important elements of the tectonic history include: (1) Compression during the Late Cretaceous and Early Tertiary, accompanied by plutonism, metamorphism, and ductile strain at depth, and thrust driven? syntectonic sedimentation at the surface. (2) Middle Tertiary transition to crustal extension, initially recorded by intrusion of leucogranites, inflation of the previously shortened middle and upper crustal section, and surface volcanism. (3) Gravity induced development of a normal sense ductile shear zone at mid crustal levels, with eventual detachment and southwestward displacement of the upper crustal stratigraphy by Early Miocene time.

Elucidation of the metamorphic core complex evolution just described was facilitated by fortuitous preservation of a unique assemblage of rocks and structures. The "type" stratigraphy utilized for regional correlation and strain analysis includes a Jurassic volcanic arc assemblage overlain by an Upper Jurassic-Lower Cretaceous quartz pebble conglomerate, in turn overlain by marine strata with fossiliferous Aptian-Albian limestones. The Jurassic strata, comprised of (a) rhyolite porphyries interstratified with quartz arenites, (b) rhyolite cobble conglomerate, and (c) intrusive granite porphyries, are known to rest on Precambrian basement north and east of the study area. The quartz pebble conglomerate is correlated with the Glance Conglomerate of southeastern Arizona and northeastern Sonora. The marine sequence represents part of an isolated arm? of the Bisbee Basin.

Crosscutting structural relationships between the pre-Middle Cretaceous supracrustal section, younger plutons, and deformational fabrics allow the tectonic sequence to be determined. Earliest phases of a Late Cretaceous-Early Tertiary orogeny are marked by emplacement of the 78 ± 3 Ma Guacomea Granodiorite (U/Pb zircon, Anderson et al., 1980) as a sill into deep levels of the layered Jurassic series. Subsequent regional metamorphism and ductile strain is recorded by a penetrative schistosity and lineation, and east-west trending folds. These fabrics are intruded by post-kinematic Early Tertiary? two mica granites. At shallower crustal levels, the orogeny is represented by north directed thrust faulting, formation of a large intermontane basin, and development of a pronounced unconformity. A second important phase of ductile strain followed Middle Tertiary? emplacement of leucogranites as sills and northwest trending dikes into intermediate levels of the deformed section (surficial volcanism was also active during this transitional period to regional extension). Gravitational instabilities resulting from crustal swelling via intrusion and thermal expansion led to development of a ductile shear zone within the stratigraphic horizon occupied by a laterally extensive leucogranite sill. With continued extension, upper crustal brittle normal faults (detachment faults) enhanced the uplift and tectonic denudation of this mylonite zone, ultimately resulting in southwestward displacement of the upper crustal stratigraphy.

Strains associated with the two ductile deformation events have been successfully partitioned through a multifaceted analysis. R_f/Ø measurements on various markers from the "type" stratigraphy allow a gradient representing cumulative strain since Middle Cretaceous time to be determined. From this gradient, noncoaxial strains accrued since emplacement of the leucogranites may be removed. Irrotational components of the postleucogranite strain are measured from quartz grain shapes in deformed granites; rotational components (shear strains) are determined from S-C fabrics and from restoration of rotated dike and vein networks. Structural observations and strain data are compatable with a deformation path of: (1) coaxial strain (pure shear?), followed by (2) injection of leucogranites as dikes (perpendicular to the minimum principle stress) and sills (parallel to the minimum principle stress), then (3) southwest directed simple shear. Modeling the late strain gradient as a simple shear zone permits a minimum displacement of 10 kilometers on the Magdalena mylonite zone/detachment fault system. Removal of the Middle Tertiary noncoaxial strains yields a residual (or pre-existing) strain gradient representative of the Late Cretaceous-Early Tertiary deformation. Several partially destrained cross sections, restored to the time of leucogranite emplacement, illustrate the idea that the upper plate of the core complex bas been detached from a region of significant topographic relief. 50% to 100% bulk extension across a 50 kilometer wide corridor is demonstrated.

Late Cenozoic tectonics of the Magdalena region are dominated by Basin and Range style faulting. Northeast and north-northwest trending high angle normal faults have interacted to extend the crust in an east-west direction. Net extension for this period is minor (10% to 15%) in comparison to the Middle Tertiary detachment related extensional episode.

The orbital scale evolution of regional climate recorded in a long sediment core from Heqing；China

IEECAS SKLLQG

Does grammatical aspect affect motion event cognition? A cross-linguistic comparison of English and Swedish speakers

In this article, we explore whether cross-linguistic differences in grammatical aspect encoding may give rise to differences in memory and cognition. We compared native speakers of two languages that encode aspect differently (English and Swedish) in four tasks that examined verbal descriptions of stimuli, online triads matching, and memory-based triads matching with and without verbal interference. Results showed between-group differences in verbal descriptions and in memory-based triads matching. However, no differences were found in online triads matching and in memory-based triads matching with verbal interference. These findings need to be interpreted in the context of the overall pattern of performance, which indicated that both groups based their similarity judgments on common perceptual characteristics of motion events. These results show for the first time a cross-linguistic difference in memory as a function of differences in grammatical aspect encoding, but they also contribute to the emerging view that language fine tunes rather than shapes perceptual processes that are likely to be universal and unchanging.