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Depths Greater (depth + greater)
Selected AbstractsElectrical conductivity and crustal structure beneath the central Hellenides around the Gulf of Corinth (Greece) and their relationship with the seismotectonicsGEOPHYSICAL JOURNAL INTERNATIONAL, Issue 3 2000V. N. Pham A deep magnetotelluric sounding (MTS) investigation in the western part of the Gulf of Corinth has revealed a complex electrical image of the crustal structure. The geotectonic structure of the Parnassos unit and the Transition zone in the central Hellenides, overthrusting the Pindos zone both towards the west and towards the south, has been clearly identified by its higher resistivity and its intrinsic anisotropy related to the N,S strike of the Hellenides range. Subsequent N,S extension of the Gulf introduced another heterogeneous anisotropy characteristic that corresponds to E,W-trending normal faults on both sides of the Gulf. The 2-D modelling of the MTS results reveals the existence of a relatively conductive layer about 4 km thick at a depth greater than 10 km in the middle crust. It corresponds to a ductile detachment zone suggested by microseismic and seismic studies (King et al. 1985; Rigo et al. 1996; Bernard et al. 1997a). It may be attributed to the phyllite series lying between the allochthonous Hellenic nappes and the autochthonous Plattenkalk basement. Towards the east, under the Pangalos peninsula, approaching the internal Hellenides, the detachment zone could root deeply into the lower crust. Some strong local electrical anomalies are observed, reaching the conductive layer in the middle crust, such as that under the Mamousia fault and under the front of the overthrust of the Transition zone on the Pindos zone. Other anomalies affect only the shallower zones such as that beneath the Helike fault and in the Psaromita peninsula. These shallower anomalies provide complementary information to the study of spatial and temporal variations of the seismic anisotropy in relation to the short- and long-term tectonic activity of the Gulf (Bouin et al. 1996; Gamar et al. 1999). [source] Periodontal disease in research beagle dogs , an epidemiological studyJOURNAL OF SMALL ANIMAL PRACTICE, Issue 12 2008H. E. Kortegaard Objectives: To estimate the prevalence and describe the extent and severity of periodontal disease and associated periodontal parameters in beagle dogs. Methods: A full-mouth, site-specific examination was performed in 98 beagle dogs. Focus was placed on clinical attachment loss, pocket depth and bleeding on probing. Results: The prevalence of clinical attachment loss greater than equal to 1 mm was 20 per cent in the one-year-old dogs, increasing to 84 per cent of the dogs aged more than three years. The number of sites affected with clinical attachment loss greater than equal to 1 mm showed a skewed distribution. The prevalence of clinical attachment loss greater than equal to 4 mm was only seven per cent. A probing pocket depth of 4+ mm was observed in 44 to 81 per cent of the dogs, depending on age. Also, the distribution of the number of deepened pockets/dog was skewed. The teeth most prone to clinical attachment loss greater than equal to 1 mm were the P2, the P3 and the P4 of the maxilla. The teeth most prone to pocket depth greater than equal to 4 mm were the maxillary canines. Clinical Significance: Periodontal disease in terms of clinical attachment loss greater than equal to 1 mm and pocket depth greater than equal to 4 mm is common in beagle dogs, but the major disease burden is carried by only a few dogs. The prevalence increases with increased age but is high already at the age of two years. [source] A tunable photonic RF notch filter based on opto-VLSI technologyMICROWAVE AND OPTICAL TECHNOLOGY LETTERS, Issue 6 2006Rong Zheng Abstract In this paper, we propose a novel tunable transversal photonic RF notch filter based on opto-VLSI technology. By using an array of fiber Bragg gratings (FBGs) in conjunction with an opto-VLSI processor, the broadband light source can be spectrally sliced and attenuated, hence realizing a two-tap RF notch filter with stepwise true-time delays and variable weights. In addition, the free spectral frequency and notch depth of the RF notch filter can be tuned by driving the opto-VLSI processor with optimized phase-only holograms. We experimentally demonstrate the proposed tunable RF notch filter structure and the results show that a notch depth greater than 40 dB can be attained. © 2006 Wiley Periodicals, Inc. Microwave Opt Technol Lett 48: 1011,1015, 2006; Published online in Wiley InterScience (www.interscience.wiley.com). DOI 10.1002/mop.21586 [source] Transformation of the offshore benthic community in Lake Michigan: recent shift from the native amphipod Diporeia spp. to the invasive mussel Dreissena rostriformis bugensisFRESHWATER BIOLOGY, Issue 3 2009THOMAS F. NALEPA Summary 1. The native amphipod Diporeia spp. was once the dominant benthic organism in Lake Michigan and served as an important pathway of energy flow from lower to upper trophic levels. Lake-wide surveys were conducted in 1994/1995, 2000 and 2005, and abundances of Diporeia and the invasive bivalves Dreissena polymorpha (zebra mussel) and Dreissena rostriformis bugensis (quagga mussel) were assessed. In addition, more frequent surveys were conducted in the southern region of the lake between 1980 and 2007 to augment trend interpretation. 2. Between 1994/1995 and 2005, lake-wide density of Diporeia declined from 5365 to 329 m,2, and biomass (dry weight, DW) declined from 3.9 to 0.4 g DW m,2. The percentage of all sites with no Diporeia increased over time: 1.1% in 1994/1995, 21.7% in 2000 and 66.9% in 2005. On the other hand, total dreissenid density increased from 173 to 8816 m,2, and total biomass increased from 0.4 to 28.6 g DW m,2. Over this 10-year time period, D. r. bugensis displaced D. polymorpha as the dominant dreissenid, comprising 97.7% of the total population in 2005. In 2007, Diporeia was rarely found at depths shallower than 90 m and continued to decline at greater depths, whereas densities of D. r. bugensis continued to increase at depths greater than 50 m. 3. The decline in Diporeia occurred progressively from shallow to deep regions, and was temporally coincident with the expansion of D. polymorpha in nearshore waters followed by the expansion of D. r. bugensis in offshore waters. In addition, Diporeia density was negatively related to dreissenid density within and across depth intervals; the latter result indicated that dreissenids in shallow waters remotely influenced Diporeia in deep waters. 4. With the loss of Diporeia and increase in D. r. bugensis, the benthic community has become a major energy sink rather that a pathway to upper trophic levels. With this replacement of dominant taxa, we estimate that the relative benthic energy pool increased from 17 to 109 kcal m,2 between 1994/1995 and 2005, and to 342 kcal m,2 by 2007. We project that previously observed impacts on fish populations will continue and become more pronounced as the D. r. bugensis population continues to expand in deeper waters. [source] Regional teleseismic tomography of the western Lachlan Orogen and the Newer Volcanic Province, southeast AustraliaGEOPHYSICAL JOURNAL INTERNATIONAL, Issue 2 2002Frank M. Graeber Summary From 1998 May to September a portable array of 40 short-period digital seismograph stations was operated in western Victoria, southeast Australia, across the western end of the mid-Paleozoic Lachlan Foldbelt and the Newer Volcanic Province. Consisting of four parallel, almost W,E-oriented receiver lines, the array covered an area of about 270 × 150 km2. The major aim of the LF98 (Lachlan Foldbelt survey 1998) project is to map lateral variations in P -wave speeds (Vp) in the crust and upper mantle using teleseismic arrival time tomography, primarily in order to investigate whether the major surface structural zones are associated with seismic velocity signatures at depth. Little a priori information from seismic profiling is available. We invert 4067 relative arrival time residuals for a minimum structure Vp model in the upper few hundred km using non-linear iteration and 3-D ray tracing. The most prominent negative anomaly (,3.8 per cent) in Vp is found at a depth of about 45 km underneath the eastern part of the Newer Volcanic Province. It correlates spatially with the highest density of Pliocene and Pleistocene eruption centres northwest of Melbourne, and is therefore interpreted as a hotspot-related high-temperature anomaly causing reduced mantle velocities. The related coherent volume of significantly lower than average velocities extends down to depths greater than 100 km in the east, and extends west underneath the Newer Volcanic Province. A strong velocity contrast, with average velocities ,2 per cent greater in the west, is found down to about 100 km across the Moyston Fault Zone, which forms the major structural boundary between the early-Paleozoic Delamerian Orogen in the west and the Lachlan Orogen in the east. This result suggests that the Moyston Fault Zone should be seen as a major lithospheric boundary. In the south this boundary is also expressed by a distinct discontinuity in Sr-isotopic ratios of xenoliths (the so-called Mortlake discontinuity) and a change in the geochemistry of plutons of similar age. However, if the east to west velocity contrast originally existed in this southern zone, it is now overprinted by the thermally reduced mantle velocities beneath the Newer Volcanic Province. [source] Infiltration, runoff and sediment production in blanket peat catchments: implications of field rainfall simulation experimentsHYDROLOGICAL PROCESSES, Issue 13 2002J. Holden Abstract Blanket peat covers the headwaters of many major European rivers. Runoff production in upland blanket peat catchments is flashy with large flood peaks and short lag times; there is minimal baseflow. Little is known about the exact processes of infiltration and runoff generation within these upland headwaters. This paper presents results from a set of rainfall simulation experiments performed on the blanket peat moorland of the North Pennines, UK. Rainfall was simulated at low intensities (3,12 mm h,1), typical of natural rainfall, on bare and vegetated peat surfaces. Runoff response shows that infiltration rate increases with rainfall intensity; the use of low-intensity rainfall therefore allows a more realistic evaluation of infiltration rates and flow processes than previous studies. Overland flow is shown to be common on both vegetated and bare peat surfaces although surface cover does exert some control. Most runoff is produced within the top few centimetres of the peat and runoff response decreases rapidly with depth. Little vertical percolation takes place to depths greater than 10 cm owing to the saturation of the peat mass. This study provides evidence that the quickflow response of upland blanket peat catchments is a result of saturation-excess overland flow generation. Rainfall,runoff response from small plots varies with season. Following warm, dry weather, rainfall tends to infiltrate more readily into blanket peat, not just initially but to the extent that steady-state surface runoff rates are reduced and more flow takes place within the peat, albeit at shallow depth. Sediment erosion from bare peat plots tends to be supply limited. Seasonal weather conditions may affect this in that after a warm, dry spell, surface desiccation allows sediment erosion to become transport limited. Copyright © 2002 John Wiley & Sons, Ltd. [source] Soil Temperature and Planting Depth Effects on Tef EmergenceJOURNAL OF AGRONOMY AND CROP SCIENCE, Issue 3 2009S. Evert Abstract Tef [Eragrostis tef (Zucc.) Trotter] is an annual C4 grass crop that originated in Ethiopia. It has potential as a grain crop in the Great Plains because of its tolerance to drought and high temperatures. In Ethiopia, tef seed is typically broadcast on the soil surface and lightly incorporated. Shallow planting depths are used because the seed is very small and emergence can be limited by soil crusting. If planting equipment is to be used, planting depth may be important for successful tef production. The objective of this study was to identify optimal depths and soil temperatures to aid in developing tef planting recommendations for the central Plains. Tef was planted at five depths (0, 0.6, 1.3, 2.5 and 5.0 cm) in pots filled with a silt loam soil, and pots were placed in growth chambers at four temperature regimes (day/night: 15/19 °C; 19/23 °C; 23/27 °C and 27/31 °C). No plants emerged from the 5.0-cm depth, so this depth was not included in the analysis. Emergence was greatest for planting depths of 0.6 and 1.3 cm and lower at 0 and 2.5 cm depths. Temperature did not affect final emergence, measured 21 days after planting (DAP), but did influence emergence rates during the first 9 DAP. Plant dry matter production increased as planting depth increased, but plant dry matter per pot was not different among planting depths greater than 0.9 cm, suggesting that compensation between plants across different plant densities began early in the plants' life cycles. Our results show that tef seed can emerge from depths between 0.6 and 1.3 cm and that soil temperatures below 19 °C can slow emergence but should not affect final stands. [source] Accumulation of methylglyoxal in the gingival crevicular fluid of chronic periodontitis patientsJOURNAL OF CLINICAL PERIODONTOLOGY, Issue 4 2003S. Kashket Abstract Background, aims: Methylglyoxal (MG), a toxic product of cellular metabolism, is elevated in tissues and fluids in a number of human diseases. A cross-sectional study was undertaken to determine whether MG accumulates in the gingival crevicular fluid (GCF) of chronic periodontitis patients. Methods: GCF samples were collected for 30 s each from three teeth with pocket depths greater than 3 mm (DD sites), from 14 chronic periodontitis patients. Control samples were taken from three healthy sites (DH sites) in the same patients, as well as from seven subjects who were periodontally healthy (HH sites). Fluid volumes were determined and the strips were placed in 0.5 N perchloric acid. Subsequently, samples were derivatized with o -phenylenediamine and the resulting methylquinoxaline was assayed by high-performance liquid chromatography on Lichrospher® -100 RP-18, with UV detection. Results: Mean pocket depths were 5.7±0.7, 2.7±0.6 and 2.7±0.5 mm (mean±SD) for the DD, DH and HH sites, respectively. Mean MG levels were found to be 208.7±241.7 and 142.9±235.7 pmol/site in the GCF from DD and DH sites, respectively (p=0.0023), but only 11.5±4.4 pmol/site for the HH sites. Bacteroides forsythus has been found to accumulate high levels of MG in culture (unpublished data) and, consistent with this, the sampled diseased sites contained higher levels of B. forsythus than the corresponding healthy sites (2.7±4.2×105 versus 0.7±1.1×105, respectively; p=0.022). Total "red complex" microorganisms were significantly elevated in the DD sites. Conclusions: In view of the known protein- and DNA-modifying effects of MG, the finding of elevated levels of MG in the GCF from chronic periodontitis patients supports the hypothesis that MG may contribute to destructive tissue damage in this disease. Zusammenfassung Hintergrund: Methylglyoxal (MG), ein toxisches Produkt des Zellstoffwechsels, ist bei einer Reihe menschlicher Erkrankungen in Geweben und Körperflüssigkeiten erhöht. Zielsetzung: Querschnittsstudie zur Klärung der Frage, ob sich MG in der Sulkusflüssigkeit (SF) bei Patienten mit chronischer Parodontitis ansammelt. Methoden: Bei 14 Patienten mit chronischer Parodontitis wurde SF für 30 s an 3 Zähnen mit Sondierungstiefen >3 mm (DD-Stellen) gewonnen. Kontrollproben wurden von jeweils 3 gesunden Stellen (DH-Stellen) bei den gleichen Patienten und bei 7 parodontal gesunden Personen gewonnen (HH-Stellen). Die Flüssigkeitsvolumina wurden bestimmt und die Probenstreifen in 0,5 N Perchlorsäure gegeben. Anschließend wurden die Proben mit o-Phenyldiamin versetzt und das resultierende Methylquinoxalin wurde mittels High-Performance-Liquid-Chromatographie in einem Lichrospher®-100 RP-18 bei UV-Detektion nachgewiesen. Ergebnisse: Die mittleren Sondierungstiefen lagen bei 5,7±0,7, an den DD-Stellen, bei 2,7±0,6 (DH) und 2,7±0,5 mm (Mittelwert + Standardabweichung) (HH). Die mittleren MG-Spiegel lagen bei 208,7±241,7 an den DD-Stellen und bei 142,9±235,7 pmol/Stelle an den DH-Stellen (p=0,0023), aber nur bei 11,5±4,4 pmol/Stelle an den HH-Stellen. Es war gezeigt worden, dass Bacteroides forsythus in Kultur hohe Konzentrationen von MG ansammelt (unveröffentlichte Daten) und übereinstimmend damit wurden an den untersuchten DD-Stellen höhere Zahlen von B. forsythus gefunden als an den entsprechenden gesunden Stellen (2,7±4,2×105 versus 0,7±1,1×105; p=0,022). Die Zahl aller Keime des "Roten Komplexes" waren an DD-Stellen signifikant erhöht. Schlussfolgerungen: In Anbetracht der bekannten Proteine und DNS verändernden Effekte von MG unterstützt dieser Nachweis erhöhter MG-Spiegel in der SF bei Patienten mit chronischer Parodontitis die Hypothese, dass MG zur Gewebezerstörung bei Parodontitis beiträgt. Résumé Références et buts: Le méthylglyoxal (MG), un produit toxique du métabolisme cellulaire est retrouvé en quantitéélevée dans les tissus et les fluides lors de nombreuses maladies humaines. Une étude croisée fut réalisée pour déterminer si MG s'accumulait dans le fluide gingival (GCF) des patients atteints de parodontite chronique. Méthodes: Des échantillons de GCF furent prélevés pendant 30 secondes chacun de 3 dents avec des profondeurs de poches de plus de 3 mm (sites DD), chez 14 patients atteints de parodontites chroniques. Des échantillons contrôles furent prélevés sur des sites sains (sites DH) chez les mêmes patients, et aussi chez 7 sujets au parodonte sain (sites HH). Les volumes de fluide furent déterminés et les bandelettes ont été mises dans 0.5 N d'acide perchlorique. Puis, les échantillons furent transformés à l'aide de o-phenylenediamine et la méthylquinoxaline ainsi créée fut analysé par chromatographie liquide à haute performance sur une Lichrospher®-100 RP-18, avec détection aux UV. Résultats: Les profondeurs de poche moyenne étaient de 5.7 ± 0.7, 2.7 ± 0.6 et 2.7±0.5 mm (moyenne ± SD) pour les sites DD, DH et HH, respectivement. Les niveaux moyen de MG étaient de 208.7±241.7 et 142.9±235.7 pmol/site dans le fluide des sites in DD et DH, respectivement (p=0.0023), mais seulement de 11.5±4.4 pmol/site pour les sites HH. On a trouvé que Bacteroides forsythus accumulait de hauts niveaux de MG en culture (données non publiées) et les sites malades échantillonnés contenait effectivement de plus hauts niveaux de B. forsythus que les sites sains correspondants (2.7±4.2×105 contre 0.7±1.1×105, respectivement; p=0.022). Les microorganismes du complexe rouge étaient significativement en nombre élevé dans les sites DD. Conclusions: Au vu des effets connus de MG pour modifier les protéines et l'AND, la découverte de niveaux élevés de MG dans le fluide gingival de patients atteints de maladie parodontale chronique supporte l'hypothèse selon laquelle MG pourrait contribuer aux dommages tissulaires destructifs rencontrés au cours de cette maladie. [source] Silica precipitates in omphacite from eclogite at Alpe Arami, Switzerland: evidence of deep subductionJOURNAL OF METAMORPHIC GEOLOGY, Issue 5 2002L. F. Dobrzhinetskaya Abstract Observations of oriented SiO2 precipitates in omphacite from eclogite with tholeiitic basalt protolith bordering the Alpe Arami garnet peridotite massif, Ticino, Switzerland, and petrological studies of the eclogitic mineral assemblages, suggest that this rock was subjected to higher-pressure metamorphism than previously realized. We employed various calibrations of the Fe2+ , Mg exchange thermometer and calculations of equilibria with thermodynamic data, considering the calcium,Tschermak's component (CaAl2SiO6), of garnet-pyroxene pairs. From these calculations, it is concluded that the eclogitic lenses have recorded at least four stages of mineral growth corresponding to the following: Stage I (prograde) c. 2.4 GPa; 700 °C; Stage IIa (maximum recorded grade) c. 7.0 GPa; 1100 °C; Stage IIb (retrograde) c. 3.7 GPa; 900 °C; Stage III (retrograde) c. 2.1 GPa; 750 °C. Because of the preservation of Stage I, a relatively rapid subduction and exhumation of Alpe Arami eclogite is suggested. The exhumation path of the eclogitic rock is in good agreement with most exhumation paths inferred for the Alpe Arami garnet lherzolite proposed previously by several authors based upon a variety of different observations, although the eclogite and peridotite exhumation paths may diverge at depths greater than 120 km. [source] Community structure of bathyal decapod crustaceans off South-Eastern Sardinian deep-waters (Central-Western Mediterranean)MARINE ECOLOGY, Issue 2009Maria Cristina Follesa Abstract Community structure and faunal composition of bathyal decapod crustaceans off South-Eastern Sardinian deep-waters (Central-Western Mediterranean) were investigated. Samples were collected during 32 hauls between 793 and 1598 m in depth over the 2003,2007 period. A total of 1900 decapod specimens belonging to 23 species were collected. Multivariate analysis revealed the occurrence of three faunistic assemblages related to depth: (i) an upper slope community at depths of 793,1002 m; (ii) a middle slope community at depths of 1007,1212 m and (iii) a lower slope community at depths greater 1420 m. In the upper and middle slopes the benthic (Polycheles typhlops) and epibenthic,endobenthic feeders (mainly Aristeus antennatus and Geryon longipes), which eat infaunal prey, were dominant, followed by the macroplankton,epibenthic feeders such as Acanthephyra eximia and Plesionika acanthonotus. In the deepest stratum, the most remarkable feature was the prevalence of macroplankton,epibenthic feeders (A. eximia and P. acanthonotus). A small percentage of the benthic deep-sea lobster Polycheles sculptus was also present. The biomass presented higher values in the middle slope and declined strongly in the lower slope. There was no general pattern of mean individual weight/size versus depth among decapods, and the changes seemed to be species-specific with different trends. [source] Initial investigation on the use of waterjets to place amendments in the subsurfaceREMEDIATION, Issue 1 2005John W. Cable Quasi-passive in situ remediation technologies, such as the use of permeable reactive barriers to treat contaminated groundwater or applications of granular activated carbon to treat polychlorinated biphenyl (PCB)-contaminated, near-surface sediments, are proven or promising technologies that may be limited in application due to the traditional construction techniques normally used for placement in the environment. High-pressure waterjets have traditionally been used to excavate material during mining operations or to cut rock or other durable material. Waterjets have the potential to place amendments in the subsurface at depths greater than those that can be obtained using traditional construction techniques. Likewise, waterjets may have less negative impact on near-surface utilities and/or sensitive ecological systems. Laboratory experiments were performed to characterize the placement of two solid amendments in a simulated saturated aquifer. A second set of experiments was performed to characterize the effectiveness of waterjets for placing a third amendment in simulated intertidal sediments. The laboratory work focused on characterizing the nature of the waterjet penetration of the aquifer matrix and the saturated sediments, as well as the corresponding waterjet parameters of pressure, nozzle size, and injection time. The laboratory results suggest that field trials may be appropriate for future investigations. © 2005 Wiley Periodicals, Inc. [source] Resolving the differences in plant burial responsesAUSTRAL ECOLOGY, Issue 1 2010MATTHEW E. GILBERT Abstract Burial is one of the major factors influencing plant ecology in deserts and coastal areas. Consequently, many studies have measured the responses of dune plants to sand burial. However, there remains little agreement about the mechanisms and characteristics constituting the burial response of plants. In particular, stimulation of growth has been reported as the most common plant burial response; however, stimulation has not been reported consistently among studies. Here, a literature survey showed that the depth of burial relative to the height of the plant determined whether the growth of a species was stimulated by burial. Growth stimulation was limited to shallow burial depths, while burial depths greater than the height of the plant consistently resulted in reduced growth. As studies used widely differing burial depths or units of growth measurement, the variation in reported stimulation of plant growth can be partly attributed to differences in experimental procedure. The stimulation of growth in many species was accompanied by an increase in photosynthesis over a limited period and by a shift in biomass allocation from root to shoot. Most plants demonstrated stimulated growth (up to 200%) in response to shallow burial indicating that some burial response mechanisms are general to many species. However, a few specialist dune species displayed a much greater ability to respond to burial (up to 700% stimulation of plant mass). Although allocation shifts and increased photosynthesis have been shown to be associated with dune plant burial response, there remains a need for field measurements that focus on the diversity of mechanisms underlying plant response to burial. [source] A Preliminary Study of the Gas Hydrate Stability Zone in the South China SeaACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 4 2002JIN Chunshuang Abstract, Based on the analysis of sea-bottom temperature and geothermal gradient, and by means of the phase boundary curve of gas hydrate and the sea-bottom temperature versus water depth curve in the South China Sea, this paper studies the temperature and pressure conditions for gas hydrate to keep stable. In a marine environment, methane hydrate keeps stable at water depths greater than 550 m in the South China Sea. Further, the thickness of the gas hydrate stability zone in the South China Sea was calculated by using the phase boundary curve and temperature-depth equations. The result shows that gas hydrate have a better perspective in the southeast of the Dongsha Islands, the northeast of the Xisha Islands and the north of the Nansha Islands for thicker stability zones. [source] | |||||||||||||||||||