(Table 5) Experimental hydrodynamic parameters for different soil types obtained in the Lüchow-Dannenberg district, Lower Saxony

In three typical sandy soils of Northern Germany the mobility of radioactive fission products of technetium, iodine, ruthenium and zirconium have been investigated in dependence of the hydrodynamic and physico-chemical soil properties. The laboratory experiments, which simulated fall-out events, used soil columns (1 m length, 30 cm diameter) taken as undisturbed as possible. By measurements of the breakthrough curves in the percolate and of the depth distribution of radionuclides in the soil columns after 6 months the average transport velocity could be determined. These values could be compared with the average water velocity measured by 3H tagging. Three qualitative mobility relations were observed: Ranker: Tc > Ru > I > Zr; Podsol: Tc > Ru > I > Zr; Brown forest soil: Tc = Ru > I > Zr. Relations between some physico-chemical soil properties and the retardation of radionuclides due to adsorption could be observed (eg. retardation of iodine and technetium by organic substances). The average retardation factors of the radionuclides and the hydrodynamic soil parameters are used in a model which gives a quantitative assessment of the hazard of groundwater contamination by a fall-out event in areas covered with comparable soils.

Hydrochemical and geothermic data on the Caribbean-Mexican region

Results of detailed geophysical, geological and gas- and hydrochemical research in the Caribbean-Mexican Basin and the Western Atlantic obtained during Cruise 4 of R/V Akademik Nikolaj Strakhov are published in the book. Distribution of the thermal field in different tectonic structures of the region is shown. Places of submarine hydrothermal vent discharge in tectonically active structures are described. They are confirmed by geothermal, geological and hydrochemical data. Based on lithofacies analysis of modern sediments installed their Specificity of different genetic types, facies and macrofacies of recent sediments in different geomorphological zones of the sea floor is shown. For description of hydrogeochemical situation of modern sedimentation and primary diagenesis the water column and interstitial sediment waters have been studied.

Geochemical parameters of sediments and water of the Black Sea, data of Cruise 8 of R/V Vityaz-2

The book presents results of comprehensive geological investigations carried out during Cruise 8 of R/V "Vityaz-2" to the western part of the Black Sea in 1984. Systematic studies in the Black Sea during about hundred years have not weakened interest in the sea. Lithological and geochemical studies of sediments in estuarine areas of the Danube and the Kyzyl-Irmak rivers, as well as in adjacent parts of the deep sea and some other areas were the main aims of the cruise. Data on morphological structures of river fans, lithologic and chemical compositions of sediments in the fans and their areal distribution, forms of occurrence of chemical elements, role of organic matter and gases in sedimentation and diagenesis are given and discussed in the book.

Criterio ambiental volumétrico para cálculo de espacios verdes

Los espacios verdes y, en general, la vegetación utilizada para protección, son valorados, medidos y calculados por el área destinada a esa función más que por los elementos vegetales relacionados. Esto significa una simplificación excesiva que no aporta los criterios de cuantificación necesarios tanto para preservar el patrimonio natural existente como para elaborar proyectos de mejoramiento ambiental. En este trabajo se propone un concepto nuevo para la valoración de los elementos vegetales atendiendo a su influencia como mejoradores ambientales. Se determinan dos índices de valoración: el Índice de Vegetación Ambientalmente Activa por unidad de área utilizada y el Índice Ambiental Urbanístico. Ambos permiten cuantificar la importancia urbanística y ambiental de la vegetación. También se introduce un nuevo concepto en el cálculo de la necesidad de espacios verdes en proyectos urbanísticos y en áreas de amortiguación industriales, basado en el volumen vegetativo que debe existir en áreas que normalmente se destinan a espacios verdes.

Comportamiento de clones de álamos en San Carlos : Mendoza, Argentina

Desde hace más de 30 años el Instituto Forestal de la Facultad de Ciencias Agrarias de la Universidad Nacional de Cuyo, Mendoza, Argentina, ha realizado la introducción de clones de álamos de diversos orígenes, con el fin de evaluar sus comportamientos frente a agentes bióticos y abióticos, ampliar la base genética disponible y mejorar los rendimientos volumétricos promedio de las plantaciones comerciales de la región. Como parte de esta línea de investigación, en 1996 se instaló un ensayo en un establecimiento agrícola-forestal ubicado en el Departamento de San Carlos, provincia de Mendoza, a los 33°46' S; 69°02' O y 940 msnm. Se evaluaron 10 clones de álamos: cuatro P. x deltoides (Stoneville 124, EEA Delta 107/68, INTA 69/69, Fierolo) y seis Populus x canadensis (El Campeador, Neva, Luisa Avanzo, B. L. Constanzo, I-42, I-455), que se dispusieron en parcelas de 9 plantas cada una distribuidas al azar con 4 repeticiones. La distancia de plantación fue de 4 x 6 m. Se realizaron mediciones anuales de diámetro altura pecho (DAP) y altura total de los árboles, además de registrar periódicamente el estado sanitario, en particular en lo referido a la presencia de ataques de cancrosis producida por Septoria musiva Peck. Los clones que produjeron un mayor volumen de madera/ha fueron: Stoneville 124 con una producción de 322 m3/ha, EEA Delta 107/68 con 293 m3/ha, INTA 69/69 con 285 m3/ha y Fierolo con 239 m3/ha. El clon Luisa Avanzo y el clon I-42 presentaron una alta susceptibilidad a cancrosis, lo que motivó un altísimo porcentaje de fallas a partir del tercer año, fallas que se repitieron en menor medida en el resto de los clones P. x canadensis. Cabe concluir que los clones con mejor comportamiento bajo las condiciones del ensayo fueron: Stoneville 124, EEA Delta 107/68 e INTA 69/69.

Microfiltración en restauraciones coronarias completas libres de metal

En el presente trabajo se estudió la microfiltración de núcleos de alúmina cementados con cemento de resina autoacondicionante y con cemento de ionómero de vidrio convencional. Una vez preparadas las muestras se sumergieron en azul de metileno, para luego ser cortadas longitudinalmente. Los cortes fueron observados en una lupa estereoscópica, estableciéndose su grado de filtración por penetración del colorante. El análisis estadístico demostró que las muestras cementadas con cemento de resina tuvieron menor filtración que las cementadas con ionómero de vidrio.

Consolidation properties and strength characteristics of ODP Site 204-1244 sediments

Eight whole-core samples from Ocean Drilling Program Site 1244, Hydrate Ridge, Cascadia continental margin, were provided to Massachusetts Institute of Technology (Cambridge, Massachusetts, USA) for geotechnical characterization. The samples were collected from depths ranging from 5 to 136 meters below seafloor (mbsf). Seven of the eight whole-core samples were located within the gas hydrate stability zone, whereas the eighth sample was located in the free gas zone. Atterberg limits testing showed that the average liquid limit of the soil is 81% and the average plastic limit is 38%, giving an average plasticity index of 43%. The liquid limit is sensitive to oven drying, shown by a drop in liquid limit to 64% when tests were performed on an oven-dried sample. Loss on ignition averages 5.45 wt%. Constant rate of strain consolidation (CRSC) tests were performed to obtain the compression characteristics of the soil, as well as to determine the stress history of the site. CRSC tests also provided hydraulic conductivity and coefficient of consolidation characteristics for these sediments. The compression ratio (Cc) ranges from 0.340 to 0.704 (average = 0.568). Cc is fairly constant to a depth of 79 mbsf, after which Cc decreases downhole. The recompression ratio (Cr) ranges from 0.035 to 0.064 (average = 0.052). Cr is constant throughout the depth range. In situ hydraulic conductivity varies between 1.5 x 10**-7 and 3 x 10**-8 cm/s and shows no trend with depth. Ko-consolidated undrained compression/extension (CKoUC/E) tests were also performed to determine the peak undrained shear strength, stress-strain curve, and friction angle. The normalized undrained strength ranges from 0.29 to 0.35. The friction angle ranges from 27 to 37. Because of the limited amount of soil, CRSC and CKoUC/E tests were also conducted on resedimented specimens.

Composition of recent carbonate bottom sediments from the Guiana shelf an off the West Africa

This work was based on a study of the upper layer of recent carbonate bottom sediments of the Atlantic Ocean. Biogenic carbonate of recent sediments is represented by metastable and stable minerals. In the ocean metastable phases can exist indefinitely long, but the structure of polymorphism determines inevitability of transformation of metastable phases into stable ones. This transformation occurs in the solid phase. In the absence of a critical point between the two phases of the transition process is not available for study by microscopic methods. It is estimated indirectly by studying the nature and extent of changes in mineral and chemical compositions. With aging of sediments their mineral composition alters in direction of increasing contents of resistant minerals. Fine grained sediments and fractions are subject to more intensive effects of early diagenesis processes, rather than coarse ones; this is reflected in their mineral composition. Regularities of distribution of carbonate minerals in size fractions consistent with the direction of polymorphic transformations in calcium carbonate. Such transformations can occur in a particular dimension of grains. Concrete grain size depends on environmental conditions. This situation explains presence of metastable biogenic carbonates at different depths of the ocean and suggests presence of diagenetic calcite in sediments occurring below expected for each case depth of the transition.

Contents of major and noble chemical elements in phosphorites and bottom sediments

Ag and Au are typically concentrated in phosphorites; they genetically related to organic matter of bottom sediments that extract these elements from seawater or interstitial water. Consequently, the phosphorites inherit Ag and Au from host sediments that are not always enriched in them. In contrast to other organic-rich sediments, analyzed sample of recent diatom ooze from the Namibian shelf is not enriched in Ag and Au, although some sediments from this region are enriched in Au. In addition to authigenic Au, allochthonous Au associated with quartz grains and micrograins can also be present in shelf phosphorites. This was observed in oceanic phosphorites of various types. Anomalous Au and Fe contents recorded in one seamount phosphorite sample can be related to extraction of Au and nonferrous metals by ferromanganese hydroxides from seawater. This process can serve as one of major mechanisms of Au supply to ferromanganese crusts on seamounts. Phosphorites and sediments are enriched in Ru simultaneously with U. Author's data show that U content varies from 17 (seamount phosphorite) to 887 ppm (Pleistocene phosphorite nodule from the Namibian shelf). This is probably caused by different types of behavior of light and heavy PGEs in the marine environment.

Chemistry and age determination of basement fluids from Juan de Fuca Ridge

The geochemical implications of thermally driven flow of seawater through oceanic crust on the mid-ocean ridge flank have been examined on a well-studied 80 km transect across the eastern flank of the Juan de Fuca Ridge at 48°N, using porewater and basement fluid samples obtained on ODP Leg 168. Fluid flow is recognised by near-basement reversals in porewater concentration gradients from altered values in the sediment section to seawater-like values in basaltic basement. In general, the basement fluids become more geochemically evolved with distance from the ridge and broadly follow basement temperature which ranges from not, vert, similar16° to 63°C. Although thermal effects of advective heat exchange are only seen within 20 km east of where basement is exposed near the ridge crest, chemical reactivity extends to all sites. Seawater passing through oceanic crust has reacted with basement rocks leading to increases in Ca2+ and decreases in alkalinity, Mg2+, Na+, K+, SO42- and delta18O. Sr isotope exchange between seawater and oceanic crust off axis is unequivocally demonstrated with endmember 87Sr/86Sr ~ 0.707. Evidence of more evolved fluids is seen at sites where rapid upwelling of fluids through sediments occurs. Chlorinities of the basement fluids are consistent with post-glacial seawater and thus a short residence time in the crust. Rates of lateral flow have been by estimated by modelling porewater sulphate gradients, using Cl as a glacial chronometer, and from radiocarbon dating of basal fluids. All three methods reveal fluid flow with 14C ages less than 10,000 yr and particle velocities of ~1-5 m/yr, in agreement with thermally constrained volumetric flow rates through a ~600 m thick permeable layer of ~10% porosity. Delta(element)/Delta(heat) extraction ratios are similar to values for ridge-crest hydrothermal systems.