4,463 research outputs found

    Lithostratigraphy, sedimentation and evolution of the Volta Basin in Ghana

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    We present a revised lithostratigraphy for the Voltaian Supergroup of Ghana, based on a review of existing literature, interpretations of remotely sensed data and reconnaissance field survey of the Volta Basin. These strata thicken eastwards, to a maximum of between 5 and 6 km adjacent to the Pan-African Dahomeyide orogen. They began to accumulate some time after about 1000 Ma, along the margin of an epicontinental sea. Initial sedimentation, comprising the age-equivalent Kwahu and Bombouaka Groups, shows a cyclical mode of deposition controlled by eustatic changes in sea-level that produced a range of nearshore marine, littoral and terrestrial environments. A major erosional interval was followed by deposition of the 3–4 km thick Oti-Pendjari Group. Basal tillites and associated sandy diamictons are correlated with the Marinoan (end-Cryogenian) glaciation, indicating a maximum depositional age of about 635 Ma. The overlying cap carbonates and tuffs were deposited within a shallow epeiric sea bordered by a volcanically active rift system. The main part of the group records the transition from a rifted passive margin to a fully developed foreland basin receiving marine flysch in the form of argillaceous strata interbedded with highly immature wacke-type sandstones and conglomerates. Maximum accommodation space was developed within a foredeep adjacent to the Dahomeyide belt. Towards the end of the orogenic phase, the foredeep succession became partially inverted and then was buried under coarse terrestrial, red-bed molasse of the Obosum Group

    Wind tunnel results of the low-speed NLF(1)-0414F airfoil

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    The large performance gains predicted for the Natural Laminar Flow (NLF)(1)-0414F airfoil were demonstrated in two-dimensional airfoil tests and in wind tunnel tests conducted with a full scale modified Cessna 210. The performance gains result from maintaining extensive areas of natural laminar flow, and were verified by flight tests conducted with the modified Cessna. The lift, stability, and control characteristics of the Cessna were found to be essentially unchanged when boundary layer transition was fixed near the wing leading edge. These characteristics are very desirable from a safety and certification view where premature boundary layer transition (due to insect contamination, etc.) must be considered. The leading edge modifications were found to enhance the roll damping of the Cessna at the stall, and were therefore considered effective in improving the stall/departure resistance. Also, the modifications were found to be responsible for only minor performance penalties

    EFFECTS OF TASK CONSTRAINTS ON SIDESTEPPING JOINT KINETICS

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    The purpose of this study was to assess the change in lower limb joint kinetics associated with anterior cruciate ligament injury (ACL) risk in sidesteps with and without task constraints. Female athletes (n=21) performed pre-planned and unplanned sidesteps with and without task constraints to the trunk and the preparatory step. Statistical differences in negative peak joint power for the hip, knee and ankle during the execution step, the entry velocity and the sidestep angle between the constrained and unconstrained sidesteps were determined with a linear mixed model. The entry velocity decreased for all unplanned sidesteps compared to pre-planned sidesteps. Trunk constraints increased knee joint loading in pre-planned sidesteps (-24.51 ± 11.27 W·kg-1) compared to unconstrained unplanned sidesteps (-17.69 ± 8.58 W·kg-1). Understanding how constraints can alter the magnitude of lower-body joint loading can help design effective drills to overload single-joint capacities

    Aggresion in terrorism

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    Behavioral scientists have attempted to describe and explain terroristic aggression in various ways. Acts of terrorism have typically been labeled as instrumentally aggressive in nature, however, we argue that this descriptor is insufficient in capturing the complexity of terroristic aggression. In light of this, we propose a new term called “programmatic aggression” that may better serve to capture the multiple levels of influence in generating terroristic aggression. We also review how personality and psychopathological models and theories of aggression, including the frustration-aggression hypothesis, social learning theory, and the General Aggression Model, have been applied and fall short in the explication of terroristic aggression. Finally, we suggest some future directions of research that would likely benefit the study of terrorism and aggression, including analysis of social psychological work on group dynamics and their influence on individual and group behavior, as well as forensic risk and threat assessment research that could inform future efforts at predicting and hopefully, preventing acts of terroristic aggression

    Distinguishing Oceans of Water from Magma on Mini-Neptune K2-18b

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    Mildly irradiated mini-Neptunes have densities potentially consistent with them hosting substantial liquid-water oceans ("Hycean" planets). The presence of CO2 and simultaneous absence of ammonia (NH3) in their atmospheres has been proposed as a fingerprint of such worlds. JWST observations of K2-18b, the archetypal Hycean, have found the presence of CO2 and the depletion of NH3 to 4 ÎĽm region, where CO2 and CO features dominate: magma ocean models suggest a systematically lower CO2/CO ratio than estimated from free-chemistry retrieval, indicating that deeper observations of this spectral region may be able to distinguish between oceans of liquid water and magma on mini-Neptunes
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