Sediment evolution and habitat function of organic-rich muds within the Albemarle estuarine system,North Carolina

The analyses of 248 samples have revealed that the composition and distribution patterns of sediments within the Albemarle estuarine system (AES) represent a complex interaction between multiple sediment sources, basin morphology and evolution, and associated estuarine processes. Three sediment end-member types are dominant: sand, peat, and organic-rich mud (ORM). Throughout the AES, shallow perimeter platforms and associated sediment-bank shorelines are eroded into Pleistocene units. Shoreline recession supplies sand to the platforms and mud to the central basins; these sediments mix with suspended sediment from the fluvial drainages. Swamp forest-peat and marsh-peat shorelines are actively eroding and supply fine organic detritus to produce the dominant ORM sediment in the central basins. Perimeter platform sands grade into ORM on the platform slope. ORM constitutes about 70% of the benthic habitats within the AES and has an average composition of 76.2% inorganic mud, 13.1% sand, and 10.7% organic matter. The characteristics of ORM greatly affect the benthic community structure, chemical quality of the sediments, and the water quality of the estuary. ORM readily moves in and out of the water column in response to natural and anthropogenic activities, affecting water column turbidity and trace and major element geochemistry. Organic matter and clay minerals in ORM are chemically reactive and interact with the water column to adsorb or release contaminants, nutrients, and gases. Thus, ORM acts as both a sink and source for many different chemical constituents in the water column and plays important, but poorly understood, functions in the physical and chemical dynamics of estuarine ecosystems.     

Assessment of Historical Thunderstorm Data for Urban Effects: The Chicago Case

Altered incidences of thunderstorms resulting fromthe influence of large urban areas on the atmosphere can biasefforts to assess the long-term behavior of regional stormactivity. Past studies of selected cities have defined increasedthunderstorm activity downwind (generally east) of urban areas,but few have documented in-city changes in storm activity.Comparison of the sites where historical thunder records werecollected with areas with potential urban influences on stormactivity is important to identify quality records and to deletedata from questionable urban sites. An investigation of thisissue was conducted using unique, quality long records from twostations at Chicago. This study compared storm activity using40-years of data from a station in central Chicago and one on thecity's western boundary. The city site averaged 4.5 morethunderstorm days a year, an increase of 12%, than theadjacent rural site. In-city increases occurred in all fourseasons with the greatest differences in spring and summer andleast in fall, and enhanced storm activity occurred in all hoursbut was greatest in the afternoon and evening. The resultsestablished that sizable and statistically significant increasesin storm activity occurred over the central portions of Chicago. This has major implications for the selection of stations foruse in climate change assessments of storm activity. This studyrevealed that the official thunderstorm records that had beentaken within the city since 1896 were likely urban influenceduntil the station was moved to the city's western edge in 1959. The Chicago data should not be used in regional and nationalstudies of historical fluctuations of storm activity during the20th century. Results from Chicago and studies of othercities suggest that most storm enhancement occurs to thenortheast, east, and southeast of cities with populations of 1 to2 million, whereas in larger cities like New York and Chicago,storm modification also occurs well within the confines of thecity.     

A crack-like rupture model for the 19 September 1985 Michoacan,Mexico, earthquake

Evidence supporting a smooth crack-like rupture process of the Michoacan earthquake of 1985 is obtained from a major earthquake for the first time. Digital strong motion data from three stations (Caleta de Campos, La Villita, and La Union), recording near-field radiation from the fault, show unusually simple ramped displacements and permanent offsets previously only seen in theoretical models. The recording of low frequency (0 to 1 Hz) near-field waves together with the apparently smooth rupture favors a crack-like model to a step or Haskell-type dislocation model under the constraint of the slip distribution obtained by previous studies. A crack-like rupture, characterized by an approximated dynamic slip function and systematic decrease in slip duration away from the point of rupture nucleation, produces the best fit to the simple ramped displacements observed. Spatially varying rupture duration controls several important aspects of the synthetic seismograms, including the variation in displacement rise times between components of motion observed at Caleta de Campos. Ground motion observed at Caleta de Campos can be explained remarkably well with a smoothly propagating crack model. However, data from La Villita and La Union suggest a more complex rupture process than the simple crack-like model for the south-eastern portion of the fault.     

Geochemistry and petrology of dredged basalts from the Bouvet triple junction,South Atlantic

Basalts dredged from the Bouvet triple junction (South Atlantic), from the Mid-Atlantic Ridge near the triple junction, and from a spreading center east of Bouvet Island differ from normal mid-ocean ridge tholeiites by having higher concentrations of K and other large-ion-lithophile elements, higher ${}^{87}\text{Sr}\text{:}{}^{86}\text{Sr}$ ratios, and rare earth element distributions which show relative enrichment in the lighter rare earths. The basalts are more fractionated than typical oceanic tholeiites, however, fractional crystallization does not fully account for their chemical characteristics, and it appears that they were derived from special source materials, contaminated perhaps by a mantle plume rising beneath Bouvet Island.     

New dimensions in world shipbuilding

New classes of bulk carriers and general cargo vessels are becoming more specialized and larger. The trend towards containerizing cargo has spurred construction of the large cellular containership, the roll-on/roll-off vessel, and the barge carrying ship (LASH). Bulk vessels, especially tankers, have undergone tremendous increases in size until few of the newer ones can pass through the Suez Canal. Crews have not increased primarily because of greater use of shipboard automation devices. Few ports have sufficient water depths to accommodate supertankers, necessitating more off-loading at sea and construction of new deep water terminals. Japanese yards dominate world supership construction, with Scandinavian shipyards most important in Europe. Substantial supership construction is taking place in southern Europe and is an indication of the recent economic growth of Italy, Spain and Yugoslavia. Supership construction in Great Britain has declined relative to Scandinavian and Japanese production and that in the United States is of little significance worldwide.