California State University, Long Beach

About: California State University, Long Beach is a education organization based out in Long Beach, California, United States. It is known for research contribution in the topics: Population & Poison control. The organization has 10036 authors who have published 13933 publications receiving 377394 citations. The organization is also known as: Cal State Long Beach & Long Beach State.

Individual and Crew Level Determinants of Collective Efficacy in Rowing

Abstract: The purpose of this study was to examine individual (i.e., task self-efficacy, rowing experience, and goal orientations) and group/boat level (perceptions of motivational climate and boat size) determinants of collective efficacy in the sport of rowing. Participants were 154 male and female rowers ages 13 to 18 years (M = 16.19, SD = 1.29). Approximately 24 hours prior to the regional championship regatta, participants completed a demographic measure, the Task and Ego Orientation in Sport Questionnaire, the Perceived Motivational Climate in Sport Questionnaire-2, and sport-specific individual and collective efficacy measures developed for the current study. Multilevel modeling revealed that task self-efficacy significantly predicted individual perceptions of collective efficacy, while perceptions of a mastery climate significantly predicted average collective efficacy scores at the group level.

Super-scale failure of the southern Oregon Cascadia margin

Abstract: —Using SeaBeam bathymetry and multichannel seismic reflection records we have identified three large submarine landslides on the southern Oregon Cascadia margin. The area enclosed by the three arcuate slide scarps is approximately 8000 km2, and involves an estimated 12,000–16,000 km3 of the accretionary wedge. The three arcuate slump escarpments are nearly coincident with the continental shelf edge on their landward margins, spanning the full width of the accretionary wedge. Debris from the slides is buried or partially buried beneath the abyssal plain, covering a subsurface area of at least 8000 km2. The three major slides, called the Heceta, Coos Basin and Blanco slides, display morphologic and structural features typical of submarine landslides. Bathymetry, sidescan sonar, and seismic reflection profiles reveal that regions of the continental slope enclosed by the scarps are chaotic, with poor penetration of seismic energy and numerous diffractions. These regions show little structural coherence, in strong contrast to the fold thrust belt tectonics of the adjacent northern Oregon margin. The bathymetric scarps correlate with listric detachment faults identified on reflection profiles that show large vertical separation and bathymetric relief. Reflection profiles on the adjacent abyssal plain image buried debris packages extending 20–35 km seaward of the base of the continental slope. In the case of the youngest slide, an intersection of slide debris and abyssal plain sediments, rather than a thrust fault, mark the base of slope. The age of the three major slides decreases from south to north, indicated by the progressive northward shallowing of buried debris packages, increasing sharpness of morphologic expression, and southward increase in post-slide reformation of the accretionary wedge. The ages of the events, derived from calculated sedimentation rates in overlying Pleistocene sediments, are approximately 110 ka, 450 ka, and 1210 ka. This series of slides traveled 25–70 km onto the abyssal plain in at least three probably catastrophic events, which may have been triggered by subduction earthquakes. The lack of internal structure in the slide packages, and the considerable distance traveled suggest catastrophic rather than incremental slip, although there could have been multiple events. The slides would have generated large tsunami in the Pacific basin, possibly larger than that generated by an earthquake alone. We have identified a potential future slide off southern Oregon that may be released in a subduction earthquake. The occurrence of the slides and subsequent subduction of the slide debris, along with evidence for margin subsidence implies that basal subduction erosion has occurred over at least the last 1 Ma. The massive failure of the southern Oregon slope may have been the result of the collision of a seamount province or aseismic ridge with the margin, suggested by the age progression of the slides and evidence for subducted basement highs. The lack of latitudinal offset between the oldest slide debris and the corresponding scarp on the continental slope implies that the forearc is translating northward at a substantial fraction of the margin-parallel convergence rate.

Rheology of a Magnetorheological Fluid

Abstract: We report on experimental investigations of the rheological behavior of aqueous magnetic suspensions. The suspended particles are monodisperse colloidal polystyrene spheres which contain magnetic Fe203-grains. In the absence of a magnetic field these suspensions behave as Newtonian fluids, whereas under the influence of a magnetic field due to the formation of an ordered structure the apparent viscosity of the suspension increases up to three orders of magnitude and they clearly exhibit non-Newtonian properties, such as shear thinning and yield stress. The apparent viscosity depends on the magnetic field according to aq - H2". Increasing the volume fraction of the particles in the range of 0.014 < 0 < 0.12 results in a linear increase in apparent viscosity and yield stress. Both apparent viscosity and yield stress depend also on the particle size as first measurements on particles with diameters ranging from 0.5 Am to 1.0,Am clearly show. All measurements were carried out with a rotation viscometer using ...

Toward a Social Psychology of Social Support

Abstract: An analysis of social psychological aspects of social support examined several stages of the interaction between provider and recipient. In the first stage, the provider may offer support, respond positively to requests for support, or decline requests for support, whereas the recipient may seek, accept, or reject support. In the second stage, after support is exchanged, attributions about its effect may occur for each member, which in turn affects the extent to which the support is continued and the nature of its effect. Attributional errors about the effect may occur, especially if factors other than support—such as external factors—alter the problem status. The final stage follows the resolution of the problem and may involve reciprocation of support when roles are reversed, although such reciprocity may not be a necessary condition for social support. Possible mechanisms for both positive as well as negative effects of support were postulated. Assessing the effects of support is complicated by factors...