Journal articles on the topic 'Inline sorting'

Manipulation and sorting of particles utilizing microfluidic phenomena have been a hot spot in recent years. Here, we present numerical investigations on particle trapping techniques by using intrinsic hydrodynamic effects in an expansion-contraction microfluidic device. One emphasis is on the underlying fluid dynamical mechanisms causing cross-streamlines migration of the particles in shear and vortical flows. The results show us that the expansion-contraction geometric structure is beneficial to particle trapping according to its size. Particle Reynolds number and aspect ratio of the channel will influence the trapping efficiency greatly because the force balance between inertial lift and vortex drag forces is the intrinsic reason. Especially, obvious inline particles contribution presented when the particle Reynolds number being unit. In addition, we selected three particle sizes (2, 7, and 15 μm) to examine the trapping efficiency.

HighlightsIn the Emission Head (EH) configuration differences in apple bruise severity were well captured.A good representation of new samples variability, in calibration, ensured robust quantitative PLS-DA models.EH mode with PLS-DA is an attractive spectroscopic option for inline apple sorting based on bruise damage. Abstract. Bruise damage in apples is very common and undesirable because it hinders consumer satisfaction and greatly contributes to food loss. Fast detection of bruise damage in fruit using spectroscopic systems is still problematic, especially in terms of quantitative and objective assessments of mechanical damage and standardization of bruise measurement method, among other issues. Non-destructive techniques among which is near infrared (NIR) spectroscopy are under development as a potential solution carrier for such issues. A study of bruise damage was conducted on three apple cultivars using Fourier transform (FT) near infrared spectroscopy in two configurations (‘emission head’ of Bruker’s Matrix-F and ‘integrating sphere’ of Bruker’s multipurpose analyzer, MPA). The emission head (EH) allows for contactless large sample (100 mm) exposure that simulates on-line applications, while the MPA (sample size: 22 mm) is commonly used for in-laboratory analysis of inhomogeneous material such as fruit. Bruise damages were mechanically induced in apples, bruise sizes measured physically and destructively. Partial least squares discriminant analysis (PLS-DA) was used to determine the differences captured by the scanning spectrometers in apple fruit tissues. Discriminant analysis revealed that in both sample acquisition modes, distinction between bruised and non-bruised apple fruit tissue was achieved with high (from 78% to 93%) accuracy of classification (ACcl) based solely on spectral data. The classification accuracy improved when individual cultivars were considered and ranged from 94% to 96%. Classification models were tested for robustness and showed that both cultivar and bruise severity had influence on classification models’ performance. The results showed ability of the emission head configuration in detecting bruises and differentiating between severity of bruises in apple fruit, thus making it a good candidate for use in rapid detection and quantitative assessment of bruising in apple on sorting lines. Possibilities for improving the classification model performance and ensuring their robustness for the EH were suggested. Keywords: Apple bruise, Discriminant analysis, Model performance, Model threshold, NIR spectroscopy.

ABSTRACTDome dunes in four stabilized, inland dune fields in western Canada are predominantly composed of horizontal to low-angle cross-strata, indicating that slip face development was rare. Dip angles of lee side deposits decrease upward in the dome dunes. The spread of dip directions increases with elevation in the dunes, spanning 360° for topset deposits. Sedimentary structures indicative of moisture (adhesion laminae) and vegetation (scour surfaces) occur in the dunes and denivation features are also present. Sediment adhesion is responsible for the maintenance of the dome morphology. Sediment sorting within the dome dunes is poorer than in other local dune types in the vicinity, suggesting that less reworking/ineffective selective transport occurred and that the dome dunes are more efficient in retaining sediment. The rarity of slip face and grainfall deposits and the abundance of low angle deposits indicate that preferential accumulation of sediment at the top of the lee side did not occur. Development of domal morphology is a consequence of the inhibition of slip face development. In inland, relatively moist boreal environments, the primary factor limiting or precluding sediment accumulation at the crest of the dunes is a low rate of sedimentation.

AbstractLate Holocene sediment deposits in Pine Island Bay, West Antarctica, are hypothesized to be linked to intensive meltwater drainage during the retreat of the paleo-Pine Island Ice Stream after the Last Glacial Maximum. The uppermost sediment units show an abrupt transition from ice-proximal debris to a draped silt during the late Holocene, which is interpreted to coincide with rapid deglaciation. The small scale and fine sorting of the upper unit could be attributed to origins in subglacial meltwater; however the thickness and deposition rate for this unit imply punctuated- rather than continuous-deposition. This, combined with the deposit's location seaward of large, bedrock basins, has led to the interpretation of this unit as the result of subglacial lake outbursts in these basins. However, the fine-scale sorting of the silt unit is problematic for this energetic interpretation, which should mobilize and deposit a wider range of sediment sizes. To resolve this discrepancy, we present an alternative mechanism in which the silt was sorted by a distributed subglacial water system, stored in bedrock basins far inland of the grounding line, and subsequently eroded at higher flow speeds during retreat. We demonstrate that this mechanism is physically plausible given the subglacial conditions during the late Holocene. We hypothesize that similar silt units observed elsewhere in Antarctica downstream of bedrock basins could be the result of the same mechanism.

Bukit Keluang is one of the famous natural recreational sites in Besut, Terengganu due to their beautiful sandy beaches and beautiful landscapes. Bukit Keluang recreational forest consist coastal and lowland dipterocarp forest. The studies on the biodiversity are never been reported at this area and thus, we aimed to investigate the diversity and abundance of insects in the coastal and inland forest of Bukit Keluang recreational forest. We built two plots which are Plot A in the coastal area and Plot B in the inland forest at Bukit Keluang. For each plot, three types of insect traps were used; yellow pan traps, pitfall traps, and Malaise traps. The traps were left for seven days and all insect samples collected were brought to the laboratory for sorting, enumerating and identifying up to order level. A total of 455 individuals of insects consisted of 10 orders (i.e. Hymenoptera, Diptera, Lepidoptera, Coleoptera, Collembola, Homoptera, Orthoptera, Dermaptera, Blattodea and Isoptera) were successfully collected from the forest of Bukit Keluang. Among them, Hymenoptera order dominated the number of individuals collected at 67.25% followed by Diptera (11.21%) whilst Collembola and Dermaptera were the least abundance order collected at 0.22%, respectively. The coastal forest recorded a total of 271 individuals (nine orders) while inland forest recorded 184 individuals (eight orders). No significant difference (p>0.05) of insect abundance was recorded between both plots. However, the Shannon-Weiner Diversity Index (H’) showed that the diversity of insects in the inland forest was slightly higher (H’=1.52) than the coastal forest (H’=0.86). We conclude that the insects’ diversity in Bukit Keluang is relatively higher in inland forest but lower in coastal forest. As no other insect survey has been conducted in this study area in the past, this study delivers a basic evidence and dataset of diversity and abundance for insect which may beneficial for further conservation research at Bukit Keluang in the future.

AbstractThe North Pacific Ocean (NPO) has received abundant aeolian dust transported by westerlies from the Asian inland. The aeolian components preserved in NPO sediments record information on palaeoclimatic and palaeoenvironmental changes in Asian source areas at different timescales. Previous studies have systematically investigated the source–sink effect of aeolian dust using the sedimentology, geochemistry, isotope and magnetic methods. In this study, we focus more on recent developments of aeolian signals in NPO sediments obtained by magnetic approaches. Generally, aeolian components contain a mixture of magnetite, maghemite, hematite and goethite of different origins. Magnetic properties (mineral category, concentration and particle size) of these minerals are modulated primarily by climatic/environmental conditions in source areas and sorting effects during the transportation process. Compared with the other methods, magnetic measurements have the advantages of non-sample destruction, high sensitivity and high efficiency. Finally, future studies are also discussed to address the importance of magnetism for tracing the dynamic transportation processes of the aeolian dust.

ABSTRACT In October 2012, Hurricane Sandy caused severe erosion on beaches and dunes of Fire Island (New York, USA). Major shoreline changes occurred with erosional dominance in the upper shoreline and aggradation in the lowermost section of the beach due to the deposition of eroded upper-beach and dune sediment. Sand laminae with a high concentration of heavy minerals (“black sand laminae”) were observed in three excavated trenches located on a washover terrace and fan on the east side of Fire Island. The mineral composition of these laminae reveals the presence of high quantities of magnetite, ilmenite (as opaque minerals), and garnet (as the main translucent mineral). These heavy-mineral-enriched laminae were formed as waves eroded and transported sand from the primary dune and smaller relict dunes under specific hydrodynamic conditions that promoted grain sorting according to differences in size and specific gravity. Based on the concentrations of certain heavy minerals, the threshold for primarily density-driven sorting probably lies between the specific gravity of less dense opaque mineral (ilmenite, 4.7) and almandine (4.3), the most common transparent heavy mineral. The number of laminae and concentrations of heavy minerals vary between trenches on the overwash terrace and appear to be controlled by their distance from sediment sources. The trench with the greatest number of laminae and higher heavy-mineral concentrations is located farthest from the main dune but is just 10 m inland of a relict dune that acts as the primary source of sediment of the washover deposit in this trench. A conceptual model for deposition of heavy-mineral layers is presented based on geomorphological and sedimentological evidence allowing the definition of a density threshold.

AbstractThirty-five sand hills that form six scattered groups rise abruptly from the flat late Pleistocene coastal plain in southeastern Louisiana. New studies confirm their eolian origin. For the first time, several late Wisconsin to early Holocene episodes of arid climate conditions have been recognized and dated in this currently humid warm-temperate subtropical region. Periods of dune formation and reactivation (28,800 to 7900 yr B.P.) were determined by the thermoluminescence method. The onset of the current climate in this Gulf coastal region postdates early Holocene time. The textural and structural homogeneity of the ridge lithosomes, good sorting of their sand fraction, and the dominantly orange hues of the dune sediments contrast with the underlying yellowish–brown to light-brown sandy silts and the well-stratified, occasionally gravelly sands of the underlying alluvial Prairie Formation. Sharply defined, unconformable ridge bases; symmetrical, oval, occasionally parabolic mound shapes; and steep slopes confirm the dune origins. The dominant orientations of ridges and ridge chains clearly reflect paleowind directions. Age comparison with dunes of the lower Mississippi Valley, the northeastern–eastern Gulf of Mexico coast, and south Atlantic coastal areas confirms the existence of at least seasonally dry climate conditions from early Wisconsin to middle Holocene times. The onset of the modern humid-subtropical climate phase in this region thus dates back only to the middle Holocene.

Abstract The only representative of the extinct North American megafauna known from Québec is an American mastodon from Pointe de Chambord, Lac-Saint-Jean. Marine mammals have played a prominent part in our knowledge of the Quaternary vertebrates of Québec since Per Kalm was informed of a whale skeleton found inland from the St. Lawrence River about 1749. Five species of whales particularly adapted to inshore conditions have been reported from Late-glacial deposits of Champlain Sea age. The bones represent mainly white whales, but also narwhals, harbour porpoise, humpback, common finback and bowhead whales. Seals (ringed, harp, bearded and harbour) have also been discovered, and walrus remains are known from Sainte-Julienne-de-Montcalm and Saint-Nicolas. Sandpits at Saint-Nicolas (bottom-dwelling fishes, seabirds, ringed seal and white whale) and Saint-Césaire (fish, eider duck, ringed seal and white whale) have yielded important Champlain Sea vertebrate fossils, as well as paleoenvironmental information. Many well-preserved vertebrate remains have been found in calcareous nodules from Eardley and Breckenridge in the Gatineau area. Perhaps cave faunas will become increasingly important in sorting out the Quaternary vertebrate faunal sequence in Québec. The finds from caves near Saint-Elzéar and La Rédemption in Gaspésie, as well as Mine and Laflèche caves in the Gatineau region have already yielded fascinating insights. A list of radiocarbon dates on Quaternary vertebrates from Québec is provided.

Abstract Granite and/or gneiss inselbergs are excellent examples of geomorphologically stable island habitats, considered as old, climatically buffered, infertile landscapes (OCBILs). However, unlike oceanic islands, their underlying drivers of diversity patterns remain to be investigated. Here, we studied 24 inselbergs in south-eastern Brazil, aiming to understand the role of landscape variables and environmental conditions in the assembly of the characteristic extremophilic mat vegetation communities. We found that beta diversity was largely explained by climatic variables, whereas species richness did not vary among inselbergs. Classic determinants of the diversity of island communities do not generally seem to apply to these plant assemblages. Overall, these communities change along a coast-to-inland gradient that captures increased seasonality with a replacement of more hydrophilic taxa by more drought-tolerant taxa. Changes in species composition in space involved strong species replacement, with several widespread genera locally represented on distinct inselbergs by different narrowly distributed species. Despite the deterministic sorting of taxa based on climatic conditions, a substantial fraction of the beta diversity remained unexplained. This underlines the importance of historical processes, which are easier to notice in stable OCBIL regions, such as range expansion, local extinction, dispersal constraints and allopatric speciation.

"A 'community' is a set of persons involved in stable patterns of communication. Communities vary widely in the range of their interactions, the capacity of their networks, and the links between information and material exchange. A community is developed by actions which increase their range, capacity, or integration. -- S. J. Mandelbaum." "Critical to the rhetoric surrounding the information highway is the promise of a renewed sense of community and, in many instances, new types and formations of communities." -- Steven G. Jones. So what's new? Once upon a time, in 1680 to be exact, it was the postal system. In that year a merchant called Dockwra set up a 'penny post' in London, quickly establishing over four hundred receiving offices and seven sorting offices. In parts of central London this service provided up to twelve deliveries daily. Similar services were subsequently established in a variety of provincial towns throughout England. A century and a half later an insightful schoolmaster called Rowland Hill saw a huge potential for growth, arguing that the, by now well established, local penny posts be expanded to include all inland postal transit: his rationale being that the existence of such a cheap service would precipitate an upsurge in personal correspondence. This increased volume, sensibly handled of course, would so reduce the unit cost as to make it profitable to carry a letter all the way from Glasgow to London for the princely sum of one penny. In 1840 the penny post was indeed expanded to incorporate all such inland post; the benefits of providing such a cheap and efficient communication infrastructure lying in its potential to enhance society by facilitating stability and unity -- by making society into a community. Of course it shouldn't be forgotten that in order to avail oneself of this service it was necessary that one have 'access' to certain 'tools': literacy and a spare penny being not least among them. In nineteenth century England one demographic that most certainly had access to the tools which would allow them to make full use of the new communication network was the upper class. Many of those who could reasonably be said to have fitted this description lived within a couple of miles of Hyde Park Corner in London. The outstanding frequency of the postal service available to this relatively small group meant that it was theoretically possible for one of their number to mail a message, receive a reply, reply to the reply, and so on . . . all in the course of a single day. If we accept Mandelbaum's criterion for the development of communities, then, this availability of a cheap, regular, and easy to use mailing network must have gone some way towards the development of a sense of community amongst those who had access to the communications 'technology' of the day. In 1957 there was something new in the skies: a U.S.S.R.-launched satellite called Sputnik. One of the American responses to what they perceived as their sudden disadvantage in the space race was the setting up of the Advanced Research and Planning Association, ARPA. This was an intervention which ultimately led to the development of the global communications infrastructure that we know today as the Internet. Prior to this rush of ARPA-funded research into new forms of, and uses for computing technology, computers were unwieldy monsters; owning one meant needing an inconveniently large building to carry it around in (apologies to Douglas Adams). The new young programmers and engineers who developed such human-machine-interface facilitators as keyboards, screens, and graphics, quickly decided that what they wanted to do most of all with their newly networked machines was to communicate with each other -- computers, it seems, came to be conceived of as communication tools almost as soon as they stopped being card-punching, number-crunching megacephalic giants, amenable only to an esoteric bunch of Fortran-wielding lab-coats. So, within a few years the demystification of computers had gotten under way regardless. As Howard Rheingold puts it, "changes in the way computers were designed and used led to the expansion of the computer-using population from a priesthood in the 1950s, to an elite in the 1960s, to a subculture in the 1970s, and to a significant, still growing part of the population in the 1990s" (67-68). Electronic mail quickly became, and remains, one of the most common uses to which networked computers are put. Initially this "e-mail" followed the post office model, with single messages being sent from one individual to another within a group. But the opportunities that the medium afforded for the quick, easy, cheap and instantaneous dissemination of information to large numbers of individuals, were soon recognised. Out of this new mode of communication grew concepts and practices such as electronic bulletin boards, newsgroups and, ultimately, the burgeoning network-within-a-network known as Usenet. Today, then, what's new is that messages may be sent, replied to, the replies replied to . . . and so on, all in the course of a day; only the individuals engaged in this feverish activity don't have to be geographically proximate; indeed, they can be situated on opposite sides of the globe while it all takes place. The same message can be sent to many people without the need to undergo the strain of endlessly repeating your elegant copperplate (or, for that matter, spending a lot of pennies). Indeed the message can just be put into the public domain, read it who may. Of course, it shouldn't be forgotten that to engage in such untrammelled interaction with one's fellow travellers requires that one have 'access' to certain 'tools'. I have access; if you've read this far, then I guess you have too (one of those tools, by the way, is the time to spare). References "Post Office." Chamber's Encyclopaedia. Vol. 2. Rev. ed. 1966. Jones, Steven G., ed. Cybersociety: Computer-Mediated Communications and Community. Thousand Oaks, CA.: Sage, 1995. Mandelbaum, S. J. "Too Clever By Far: Communications and Community Development." Communication 7 (1983): 103-14. Rheingold, Howard. The Virtual Community: Finding Connection in a Computerised World. London: Minerva, 1994. Citation reference for this article MLA style: Paul Mc Cormack. "Communicating Community: Past and Present." M/C: A Journal of Media and Culture 1.1 (1998). [your date of access] <http://www.uq.edu.au/mc/9807/comp.php>. Chicago style: Paul Mc Cormack, "Communicating Community: Past and Present," M/C: A Journal of Media and Culture 1, no. 1 (1998), <http://www.uq.edu.au/mc/9807/comp.php> ([your date of access]). APA style: Paul Mc Cormack. (1998) Communicating community: past and present. M/C: A Journal of Media and Culture 1(1). <http://www.uq.edu.au/mc/9807/comp.php> ([your date of access]).

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Garde, A. A., Chadwick, B., McCaffrey, K., & Curtis, M. (1998). Reassessment of the north-western border zone of the Palaeoproterozoic Ketilidian orogen, South Greenland. Geology of Greenland Survey Bulletin, 180, 111-118. https://doi.org/10.34194/ggub.v180.5094 _______________ As part of ongoing research into the plate tectonic setting of the Palaeoproterozoic Ketilidian orogen led by the Geological Survey of Greenland and Denmark, four geologists from Denmark and the U.K. re-examined parts of the north-western border zone in July–August 1997. The field work was generously supported by the Danish Natural Science Research Council and the Carlsberg Foundation. One team studied the Proterozoic (Ketilidian) sedimentary and volcanic rocks and the regional structure, working from six inland camps along the variably deformed Archaean–Proterozoic unconformity between Midternæs and Qoornoq and on Arsuk Ø (Fig. 1). A second team investigated the plutonic and kinematic evolution of the Kobberminebugt area at the northwestern margin of the Julianehåb batholith (Fig. 1); the latter forms the central part of the Ketilidian orogen (Chadwick & Garde 1996). In addition, samples of volcanic and granitic rocks were collected for geochemical studies and dating of depositional and tectonic events. The first systematic study of the Ketilidian orogen took place in the 1960s and was largely concentrated in its western and southern parts (Allaart 1976). Essential new data from the central and eastern parts of the orogen were acquired during the Survey’s SUPRASYD project (1992–1996; e.g. Garde & Schønwandt 1994, 1995; Garde et al. 1997; Stendal et al. 1997), which was initiated with the aim of assessing the potential for mineral resources in supracrustal sequences (Nielsen et al. 1993). In the course of the SUPRASYD project a new plate-tectonic model for the entire orogen was also published (Chadwick & Garde 1996), in which the orogen is viewed as the result of oblique convergence between the Archaean craton of southern Greenland and a supposed oceanic plate located south of the present orogen, which was subducted towards the north. Chadwick & Garde (1996) also suggested a new division of the Ketilidian orogen into a ‘Border Zone’ adjacent to the Archaean craton, the ‘Julianehåb batholith’ (formerly the Julianehåb granite) in the central part of the orogen, and the ‘Psammite Zone’ and ‘Pelite Zone’ to the south-east, which largely consist of deformed and metamorphosed erosion products derived from the evolving batholith. The north-western border zone and the Ketilidian supracrustal sequences were mapped in the 1960s by Harry & Oen Ing Soen (1964), Watterson (1965), Bondesen (1970), Higgins (1970), Muller (1974), Berthelsen & Henriksen (1975) and Pulvertaft (1977). It was shown that an Archaean gneiss complex (part of the Archaean craton of southern West Greenland) and Palaeoproterozoic basic igneous rocks (the so-called ‘MD’ (metadolerite) dyke swarms and related intrusions), and the unconformably overlying Ketilidian supracrustal rocks are progressively affected by Ketilidian deformation and metamorphism towards the Julianehåb batholith in the south and south-east. Boundary relationships were reviewed by Henriksen (1969). Where the Ketilidian supracrustal rocks are best preserved at Midternæs and Grænseland, Bondesen (1970) and Higgins (1970) divided them into the Vallen Group, which largely consists of sedimentary rocks (Table 1), and the overlying Sortis Group, in which basic pillow lavas and related doleritic to gabbroic sills predominate. Supracrustal rocks of presumed Palaeoproterozoic age further south have previously been referred to as the Qipisarqo and Ilordleq Groups (Berthelsen & NoeNygaard 1965; Allaart et al. 1969). Based on data collected in the 1960s, the earliest plate-tectonic interpretation of the Ketilidian orogen included a prominent suture in Kobberminebugt (Windley 1991). However, other critical aspects of Windley’s model were not substantiated during the Survey’s studies in 1992–1996 (Chadwick et al. 1994; Chadwick & Garde 1996), and a re-evaluation of the north-west border zone was therefore a natural focus of subsequent investigations.