A Requirement-centric Approach to Web Service Modeling, Discovery, and Selection

Service-Oriented Computing (SOC) has gained considerable popularity for implementing Service-Based Applications (SBAs) in a flexible\ud and effective manner. The basic idea of SOC is to understand users'\ud requirements for SBAs first, and then discover and select relevant\ud services (i.e., that fit closely functional requirements) and offer\ud a high Quality of Service (QoS). Understanding users’ requirements\ud is already achieved by existing requirement engineering approaches\ud (e.g., TROPOS, KAOS, and MAP) which model SBAs in a requirement-driven\ud manner. However, discovering and selecting relevant and high QoS\ud services are still challenging tasks that require time and effort\ud due to the increasing number of available Web services. In this paper,\ud we propose a requirement-centric approach which allows: (i) modeling\ud users’ requirements for SBAs with the MAP formalism and specifying\ud required services using an Intentional Service Model (ISM); (ii)\ud discovering services by querying the Web service search engine Service-Finder\ud and using keywords extracted from the specifications provided by\ud the ISM; and(iii) selecting automatically relevant and high QoS services\ud by applying Formal Concept Analysis (FCA). We validate our approach\ud by performing experiments on an e-books application. The experimental\ud results show that our approach allows the selection of relevant and\ud high QoS services with a high accuracy (the average precision is\ud 89.41%) and efficiency (the average recall is 95.43%)

Numerical simulations of the convective dilution process in helium-rich white dwarfs

The 21st European Workshop on White Dwarfs was held in Austin, TX from July 23rd to 27th of 2018DB and DBA white dwarfs are generally believed to be the result of a process by which a thin radiative hydrogen atmosphere floating in diffusive equilibrium on top of a helium envelope is eventually completely diluted in the underlying more massive helium convection zone that develops with cooling. However, the observed hydrogen abundances in these objects exceed by several orders of magnitude the predictions obtained from such a scenario invoking diffusive equilibrium, thus currently leaving the very existence of DB and DBA white dwarfs unaccounted for in any satisfactory way. We present here the results of new numerical simulations aimed at improving the modeling of this convective dilution process. In particular, we show how DA white dwarfs can be transformed into DB stars below 20,000 K, and more importantly, we propose a model that predicts the correct amount of hydrogen observed in DBA stars without invoking any accretion mechanism, an alternative model that has been proposed over the years to account qualitatively for the presence of hydrogen in the atmospheres of DBA stars.Astronom

The experiences of women with polycystic ovary syndrome on a very low-calorie diet

The research was funded by an educational grant from LighterLife. Broom was the Medical Director for LighterLife at the time of the research. Johnson is the Head of Nutrition and Research at LighterLife. The authors report no other conflicts of interest in this work.Peer reviewedPublisher PD

PALAEONTOLOGICAL (RADIOLARIAN) LATE JURASSIC AGE CONSTRAINT FOR THE STEPANAVAN OPHIOLITE (LESSER CAUCASUS, ARMENIA)

Η χρονολόγηση με βάση μικροπαλαιοντολογικά δεδομένα, των ιζηματογενών καλυμμάτων των οφιολίθων είναι ιδιαίτερης σημασίας για την κατανόηση της παλαιογεωγραφικής και γεωδυναμικής εξέλιξης των περιοχών της Τηθύος. Η οφιολιθική ακολουθία του Stepanavan στη Βόρεια Αρμενία συνίσταται από περιδοτίτες, γάββρους, πλαγιογρανίτες και λάβες και ιζηματογενή καλύματα ραδιολαριτών. Θεωρείται ως η βόρεια επέκταση της οφιολιθικής ζώνης Sevan Akera και η ανατολική επέκταση της ζώνης Izmir-Ankara. Αντιπροσωπεύει κατάλοιπο μιας βραδέως εκτεινόμενης μεσο-ωκεάνιας ράχης, που ήταν ενεργή μεταξύ της Ευρασίας και του νότιου Αρμενικού τεμάχους γκοντβανικής προέλευσης. Τα ραδιολάρια που εξετάστηκαν από τους ραδιολαρίτες στην περιοχή της οφιολιθικής ακολουθίας του Stepanavan πιστοποιούν για πρώτη φορά ηλικία Ανώτερου Ιουρασικού (ανώτερο Κιμμερίδιο έως κατώτερο Τιθώνιο) προσδίδοντας ηλικία για αυτό το τμήμα του ωκεάνιου φλοιού της Τηθύος που παρατηρείται στο Lesser Caucasus.Micropalaeontological age evidence for the sedimentary cover of ophiolites is important to understand the palaeogeographic and geodynamic evolution of Tethyan realms. The Stepanavan ophiolitic suite of Northern Armenia consists of peridotites, gabbros, plagiogranite and lavas with a radiolarite sedimentary cover. It is regarded as the northern extension of the Sevan Akera ophiolitic zone and may be considered as the eastern extension of the Izmir-Ankara suture zone. It represents the relics of a slow-spreading mid oceanic ridge that was active between Eurasia and the South-Armenian Block of Gondwanian origin. Radiolaria extracted from radiolarites of the Stepanavan ophiolite provide for the first time a Late Jurassic (late Kimmeridgian to early Tithonian) age constraint for this part of Tethyan oceanic crust preserved in Lesser Caucasus