33 research outputs found

    How your sexual orientation affects your salary in the UK

    Get PDF
    Research concerning labour market discrimination based on sexual orientation has yielded varying outcomes so far. Studies were usually based on small on unrepresentative samples. Drawing on a large and previously unavailable dataset, Cevat Giray Aksoy, Christopher S. Carpenter and Jefferson Frank find that gay men earn less than straight ones and heterosexual women earn less than lesbians

    Proposing a Tool for Supply Chain Configuration: An Application to Customised Production

    Get PDF
    The full implementation of collaborative production networks is crucial for companies willing to respond to consumer demand strongly focused on product customisation. This chapter proposes an approach to evaluate the performance of different Supply Chain (SC) configurations in a customised production context. The model is based on discrete-event simulation and is applied to the case of supply chain in the fashion sector to support the comparison between mass and customised production. A prototype web-based interface is also developed and proposed to facilitate the use of the model not only for experts in simulation but for any user in the SC management field

    Continuous selections of multivalued mappings

    Full text link
    This survey covers in our opinion the most important results in the theory of continuous selections of multivalued mappings (approximately) from 2002 through 2012. It extends and continues our previous such survey which appeared in Recent Progress in General Topology, II, which was published in 2002. In comparison, our present survey considers more restricted and specific areas of mathematics. Note that we do not consider the theory of selectors (i.e. continuous choices of elements from subsets of topological spaces) since this topics is covered by another survey in this volume

    Melatonin inhibira lipidnu peroksidaciju u jetri štakora uzrokovanu benzenom

    Get PDF
    We studied the antioxidative role of melatonin against benzene toxicity in rat liver. The inhibition of mitochondrial and microsomal lipid peroxidation differed between 24-hour (single-dose), 15-day, and 30-day treatments. Inhibition of mitochondrial lipid peroxidation was the highest after the single dose of melatonin, whereas highest microsomal inhibition was recorded after 30 days of melatonin treatment. No signifi cant difference was recorded between 15-day and 30-day treatments. Cytochrome P4502E1 (CYP4502E1) activity declined after the single-dose and 15-day melatonin treatment in the benzenetreated group, but it rose again, though not signifi cantly after 30 days of treatment. Liver histopathology generally supported these fi ndings. Phenol concentration in the urine samples declined in melatonin and benzene-treated rats. Our results show that melatonin affects CYP4502E1, which is responsible for benzene metabolism. Inhibition of its metabolism correlated with lower lipid peroxidation. In conclusion, melatonin was found to be protective against lipid peroxidation induced by benzene.Istražena je antioksidacijska uloga melatonina u zaštiti protiv toksičnoga djelovanja benzena u jetri štakora. Utvrđeno je da kratkoročno odnosno dugoročnije liječenje štakora melatoninom u različitoj mjeri štiti štakore istodobno izložene benzenu. Inhibicija lipidne peroksidacije mitohondrija i mikrosoma bila je različita nakon 24 h, 15 dana, odnosno 30 dana liječenja melatoninom. Najveća inhibicija lipidne peroksidacije mitohondrija zamijećena je nakon primjene jednokratne doze melatonina, dok je najizraženija inhibicija u mikrosomima zamijećena nakon 30 dana liječenja melatoninom. Slična istraživanja pokazuju da razina glutationa (GSH) najviše raste nakon 24 h liječenja melatoninom. Nije zamijećena razlika između liječenja u trajanju od 15 odnosno 30 dana. U štakora koji su uz benzen istodobno primali i melatonin razine citokroma P4502E1 pale su nakon 24 h odnosno 15 dana izloženosti. U štakora koji su primali samo melatonin te su razine nakon 30 dana statistički neznačajno porasle u odnosu na skupinu izloženu samo benzenu. Histopatološka analiza jetre načelno je potvrdila ove nalaze. Koncentracije fenola u mokraći bile su niže u štakora koji su istodobno primali melatonin i benzen. Ovi rezultati pokazuju da melatonin utječe na citokrom P4502E1, koji je odgovoran za metabolizam benzena. Inhibira li se njegov metabolizam, smanjuje se lipidna peroksidacija. Zaključak je da melatonin štiti od lipidne peroksidacije uzrokovane benzenom

    Oceanographic observations in the Panama Bight, "Askoy" Expedition, 1941. Bulletin of the AMNH ; v. 118, article 3

    No full text
    p. 117-151 : ill., maps ; 27 cm.Includes bibliographical references (p. 150-151)."The Panama Bight may be defined as that part of the eastern tropical Pacific Ocean that lies between the Isthmus of Panama (about latitude 9° N.) and Punta Santa Elena (about latitude 2° S.) and extends westward from the coasts of Panama, Colombia, and Ecuador to about longitude 81° W. Oceanographic observations discussed in this region were made by the 'Askoy' expedition during the period February 9 to May 26, 1941. Bathymetrically the region is part of the Panama Basin which is enclosed by Central and South America, Cocos Ridge, the Galapagos Islands, and Carnegie Ridge. Most of the Panama Bight is deeper than 3000 meters, the shelf being nowhere wider than 30 miles except in the Gulf of Panama which is less than 200 meters deep. Seasonal contrasts in weather within the Bight are related to movement of the Intertropical Convergence. In January-March the Intertropical Convergence is farthest south, offshore northerlies cause upwelling in the Gulf of Panama, and the Gulf experiences its dry season. In July-September the Intertropical Convergence is farthest north, and the region south of Cabo de San Francisco receives its least rain. The central part of the Bight receives heavy rainfall throughout the year. From June to November most of the Panama Bight is dominated by southwest winds. These seasonal changes are reflected in the average surface distribution of temperature and salinity. In February surface temperatures of 26° to 28° C. and salinities of 34 to 35 parts per mille are found in most parts of the Bight, with lower temperatures in the Gulf of Panama. By August low surface temperatures have disappeared in the Gulf, and the whole region is covered with surface waters of low salinity (less than 33°‰). It is estimated that during the rainiest period the salinity of a 10-meter layer of water 300 miles long and 60 miles wide could be reduced by rainfall and runoff from 33 parts per mille to 28 parts per mille in a period of two to three months. During the 'Askoy' expedition, surface temperatures of 26° to 28° C. and surface salinities of somewhat less than 34 parts per mille were observed in most of the region. These high surface temperatures and relatively low surface salinities were characteristic of only a rather thin surface layer (reaching 25 meters or less) which was underlain by a shallow pycnocline. At 100 meters temperatures range from 15.8° to 19.5° C., salinities from 34.87 parts per mille to 35.05 parts per mille. In the Gulf of Panama high surface temperatures, low surface salinities, and the presence of a strong shallow pycnocline suggest that upwelling in early 1941 was less intense than usual. This was confirmed by comparison with 'Hannibal' observations in March, 1933, and by examination of long-term measurements of sea level and surface temperature at Balboa by the Panama Canal Company. Correlation of a northerly wind-stress index for February-March with the average sea level for the same months over a 42-year period gave the significant correlation coefficient of -0.54. However, although the 1941 northerly wind-stress index was somewhat lower than average, it was not low enough to account for the unusually high sea level observed in 1941. Thus it seems likely that some other large-scale process affecting sea temperatures over a large area was operating. During the first half of 1941 El Niño was observed off the coast of northern Peru. Schott's explanation of this phenomenon, based on its characteristics in 1891 and 1925, calls for a cold tongue extending from the Gulf of Panama nearly to the equator. Although this cold tongue was not detected by the 'Askoy,' unusually high temperature, low salinity, and a strong southward surface current measured west of Malpelo Island may be related to the influx of northern waters on the coast of Peru. Observation of a pronounced subsurface temperature discontinuity 200 miles west of Buenaventura, accompanied by other indications at the surface, suggests that a well-developed oceanic front was present on March 24, 1941. Examination of average surface current charts shows a northward coastal surface flow north of Cabo de San Francisco throughout the year, with a mean speed of about 25 cm. per second (0.5 knot) and a width of less than 100 miles. 'Askoy' measurements in the northern part of the Bight show a subsurface distribution of mass consistent with such a current which appears to be the eastern limb of the general counterclockwise circulation in the Panama Bight. It is proposed that it be called the 'Colombia Current'"--P. 149-150
    corecore