Generalised time functions and finiteness of the Lorentzian distance

We show that finiteness of the Lorentzian distance is equivalent to the existence of generalised time functions with gradient uniformly bounded away from light cones. To derive this result we introduce new techniques to construct and manipulate achronal sets. As a consequence of these techniques we obtain a functional description of the Lorentzian distance extending the work of Franco and Moretti.Comment: 22 pages. Some imprecisions clarified compared to first versio

Effect of rhizobial strain on lentil N2-fixation and yield

Non-Peer Reviewe

An exploration into the client at the heart of therapy : a qualitative perspective

Over 50 years ago Eysenck challenged the existing base of research into psychotherapy. Since that time, a large number of investigations have been conducted to verify the efficacy of therapy. Recently however, an increasing number of studies have cast new doubts on this research base. Instead of therapy being a function of the therapist, it is now becoming ever more apparent that the client plays a prime role in the therapeutic process. The qualitative studies presented in this paper provide some examples of research that demonstrates that clients are actively involved in their therapy, even making counselling work despite their counsellor. These studies suggest that clients may not experience therapy as beneficially as traditional outcome studies indicate. This raises a new challenge to researchers to more fully explore the client's experience of therapy, a challenge to which qualitative methods of inquiry would appear well suited

Nitrogen fixation of several grain legumes in Saskatchewan

Non-Peer Reviewe

Wind interaction with buoyant plumes on the inner continental shelf

The characteristics and effects of intrusions of estuarine outflow over the inner shelf were examined, based on hydrographic and meteorological observations obtained during the Coastal Ocean Processes (CoOP\u2794) field experiment located off the Outer Banks at Duck, North Carolina. The episodic presence of distinct low salinity water masses issuing from the Chesapeake Bay created an intermittent baroclinic coastal current along the North Carolina coast. Under low wind conditions, this current occupied the upper half of the water column within 9 km of the coast. The plume was bounded by a distinct southward-propagating front, a region offshore of high horizontal salinity and velocity gradients, and a strong pycnocline underneath. The intrusion traveled along the coast at a speed comparable to the linear internal wave speed of a two-layer system. Intrusions were generally associated with southward winds (downwelling conditions); however, several observed events opposed northward wind-driven flow. The geometry and dynamics of the low salinity plume were strongly controlled by the local winds. Northward (upwelling) winds caused the plumes to widen offshore and thin vertically. Southward (downwelling) winds acted initially to speed the intrusions\u27 alongcoast movement and cause them to narrow and deepen. Under strong downwelling winds, however, the intrusions contacted the bottom. This greatly decreased their speeds and caused diffusive widening. Propagation speeds of all plumes were seen to slow steadily through the study region. This was attributed to the observed mixing with ambient water along the path of the intrusion which increased its salinity, thereby reducing the buoyancy forcing. Under the continued influence of upwelling winds, the low salinity intrusions moved rapidly away from the coast and formed shallow lenses floating over the ambient shelf water. These generally dissipated in 1 to 2 days. The theoretical offshore transport response to wind forcing was investigated, illustrating two dynamical behaviors of the plumes, depending on whether they occupied the entire water column or were vertically segregated by stratification. The meteorological control of Bay/shelf exchange was examined to better comprehend the pulsed timing of the low salinity intrusions, which occurred every 2 to 8 days. Estimates of volume flux were derived from temporal variations of waterlevel measurements within the Chesapeake Bay. The volume flux time series exhibited strong peaks of outflow, which preceded the low salinity events off Duck, N.C. by an average of 1.1 days, a time lag consistent with the observed alongcoast propagation speeds

Associations between dietary added sugar intake and micronutrient intake: a systematic review

Original article can be found at: http://journals.cambridge.org/ Copyright The Authors. DOI: 10.1017/S0007114507617206There is increasing concern that high intakes of added sugars might compromise intakes of micronutrients. The objectives of this systematic review were (1) to determine whether dietary added sugar intake was associated with micronutrient intakes, and if so, whether there was evidence of micronutrient dilution as a result of higher dietary added sugar intake and (2) if micronutrient dilution was present, to determine whether there was sufficiently robust evidence to support a threshold effect above which there was a significant decline in micronutrient intake or status relative to the recommended intakes. A systematic computerised literature search was undertaken, limited to studies written in English published from 1980 onwards and further studies identified through hand searching papers. Fifteen studies that assessed associations between intakes of added sugars or non-milk extrinsic sugars and micronutrients were included. Overall, there are insufficient data and inconsistency between studies in relationships between added sugars and micronutrient intakes, with no clear evidence of micronutrient dilution or a threshold for a quantitative amount of added sugar intake for any of the micronutrients investigated. The current evidence base is considerably constrained by methodological issues. Further research is required to determine which food products high in added sugars might adversely affect micronutrient intakes by displacing other food items from the diet. Analyses should take into account the magnitude of any observed associations to determine their true biological significance.Peer reviewe

Temporal and Spatial Variations in Chesapeake Bay Water Quality: A Video Data Report

Over the past two years we have been developing computer programs to investigate various scientific visualization techniques as applied to estuarine data. The original impetus was to be able to visualize the results of the three-dimensional hydrodynamic model under development at the Virginia Institute of Marine Science, College of William and Mary (VIMS). We quickly recognized the superior ability of certain graphic approaches, especially pseudocolor animation, to efficiently transmit a tremendous amount of information to the viewer, allowing the scientist to gain an insight into the dynamics of the data not otherwise available. We decided to apply this technique to the U.S. Environmental Protection Agency (EPA) Bay Monitoring data set, a field collection effort so large that it sometimes overwhelms our traditional information presentations. What we present here is an alternative way of presenting and archiving large amounts of field measurements. The Chesapeake Bay Program began its water quality monitoring in the summer of 1984. Data collection in the mainstem of the Bay was done by University of Maryland (UMD), VIMS, and Old Dominion University (ODU), supported by EPA, while state regulatory agencies have been responsible for water quality data from the Maryland and Virginia tributaries. More than 130 stations ( 49 in the Bay proper) were occupied over 120 times each during the water years 1985 through 1990 (Figure 1). This information has been brought together to create color contoured images of the 10 different physical and water quality parameters that were measured. Each parameter for each month is summarized in a color image that shows the map-view surface and bottom distributions plus a vertical North-South section running down the natural channel from the Susquehanna to the mouth of the Bay, Each pixel in the map-view represents a lkm X lkm area. Although a certain amount of data manipulation must occur between the original logged measurements and these images, the distributions shown should best be understood as raw snapshots of what was present in the Chesapeake during that month. No data analysis or interpretation is attempted in this report

Automated clinical system for chromosome analysis

An automatic chromosome analysis system is provided wherein a suitably prepared slide with chromosome spreads thereon is placed on the stage of an automated microscope. The automated microscope stage is computer operated to move the slide to enable detection of chromosome spreads on the slide. The X and Y location of each chromosome spread that is detected is stored. The computer measures the chromosomes in a spread, classifies them by group or by type and also prepares a digital karyotype image. The computer system can also prepare a patient report summarizing the result of the analysis and listing suspected abnormalities