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Discrete Zones (discrete + zone)

Distribution by Scientific Domains

Medical Sciences	50%

Selected Abstracts

P-P Cycle Alternans During Atrial Tachycardia:

ANNALS OF NONINVASIVE ELECTROCARDIOLOGY, Issue 2 2000
A Manifestation of Longitudinal Dissociation Within the Atrial Reentry Circuit
Background: A-63 year-old man complaining of palpitations underwent a 24-hour ambulatory ECG monitoring that revealed the presence of recurrent episodes of nonsustained supraventricular tachycardia. Analysis of the tracings suggests an atrial origin of the arrhythmia. Tachycardias, quite regular at the beginning, suddenly showed a P-P cycle alternans, namely, P-P intervals alternately short and long. The evidence of two separate cycle ranges can be explained by the presence of a longitudinal dissociation within a discrete zone of the atrial circuit. [source]

An exhumed palaeo-hydrocarbon migration fairway in a faulted carrier system, Entrada Sandstone of SE Utah, USA

GEOFLUIDS (ELECTRONIC), Issue 3 2001
I. R. Garden
Abstract The Moab Anticline, east-central Utah, is an exhumed hydrocarbon palaeo-reservoir which was supplied by hydrocarbons that migrated from the Moab Fault up-dip towards the crest of the structure beneath the regional seal of the Tidwell mudstone. Iron oxide reduction in porous, high permeability aeolian sandstones records the secondary migration of hydrocarbons, filling of traps against small sealing faults and spill pathways through the Middle Jurassic Entrada Sandstone. Hydrocarbons entered the Entrada Sandstone carrier system from bends and other leak points on the Moab Fault producing discrete zones of reduction that extend for up to 400 m from these leak points. They then migrated in focused stringers, 2,5 m in height, to produce accumulations on the crest of the anticline. Normal faults on the anticline were transient permeability barriers to hydrocarbon migration producing a series of small compartmentalized accumulations. Exsolution of CO2 as local fault seals were breached resulted in calcite cementation on the up-dip side of faults. Field observations on the distribution of iron oxide reduction and calcite cements within the anticline indicate that the advancing reduction fronts were affected neither by individual slip bands in damage zones around faults nor by small faults with sand: sand juxtapositions. Faults with larger throws produced either sand: mudstone juxtapositions or sand: sand contacts and fault zones with shale smears. Shale-smeared fault zones provided seals to the reducing fluid which filled the structural traps to spill points. [source]

A New Multilevel Ground Water Monitoring System Using Multichannel Tubing

GROUND WATER MONITORING & REMEDIATION, Issue 4 2002
Murray D. Einarson
A new multilevel ground water monitoring system has been developed that uses custom-extruded flexible 1.6-inch (4.1 cm) outside-diameter (O.D.) multichannel HOPE tubing (referred to as Continuous Multichannel Tubing or CMT) to monitor as many as seven discrete zones within a single borehole in either unconsolidated sediments or bedrock. Prior to inserting the tubing in the borehole, ports are created that allow ground water to enter six outer pie-shaped channels (nominal diameter = 0.5 inch [1.3 cm]) and a central hexagonal center channel (nominal diameter = 0.4 inch [1 cm]) at different depths, facilitating the measurement of depth-discrete piezometric heads and the collection of depth-discrete ground water samples. Sand packs and annular seals between the various monitored zones can be installed using conventional tremie methods. Alternatively, bentonite packers and prepacked sand packs have been developed that are attached to the tubing at the ground surface, facilitating precise positioning of annular seals and sand packs. Inflatable rubber packers for permanent or temporary installations in bedrock aquifers are currently undergoing site trials. Hydraulic heads are measured with conventional water-level meters or electronic pressure transducers to generate vertical profiles of hydraulic head. Ground water samples are collected using peristaltic pumps, small-diameter bailers, inertial lift pumps, or small-diameter canister samplers. For monitoring hydrophobic organic compounds, the CMT tubing is susceptible to both positive and negative biases caused by sorption, desorption, and diffusion. These biases can be minimized by: (1) purging the channels prior to sampling, (2) collecting samples from separate 0.25-inch (0.64 cm) O.D. Teflon sampling tubing inserted to the bottom of each sampling channel, or (3) collecting the samples downhole using sampling devices positioned next to the intake ports. More than 1000 CMT multilevel wells have been installed in North America and Europe to depths up to 260 feet (79 m) below ground surface. These wells have been installed in boreholes created in unconsolidated sediments and bedrock using a wide range of drilling equipment, including sonic, air rotary, diamond-bit coring, hollow-stem auger, and direct push. This paper presents a discussion of three field trials of the system, demonstrating its versatility and illustrating the type of depth-discrete data that can be collected with the system. [source]

A histopathological study of lymphoepithelial island formation in labial salivary glands in patients with primary Sjögren's syndrome

JOURNAL OF ORAL PATHOLOGY & MEDICINE, Issue 3 2000
Yukiko Yamamura
Abstract: The proliferative status of lymphoepithelial islands in the labial salivary glands of primary Sjögren's syndrome (pSS) patients was investigated by counting the number of argyrophilic nucleolar organizer regions (AgNORs) in epithelial cells constituting the islands. The islands were classified into four groups and evaluated in terms of total area and three discrete zones of the islands. In each pSS group, the mean AgNOR number per total island epithelial cell nucleus was significantly higher than in control ductal epithelial cells. The zonal AgNOR number fluctuated during the process of island formation but became more uniform as the islands developed. Furthermore, statistically significant trends among the four pSS groups were observed in the ratio of T lymphocytes, B lymphocytes and plasma cells surrounding the islands. The results indicated that the islands are highly proliferative once island formation begins and that zonal island cell proliferation may be associated with the inflammatory cells. [source]