Saint Mary's University

About: Saint Mary's University is a education organization based out in Halifax, Nova Scotia, Canada. It is known for research contribution in the topics: Population & Stars. The organization has 1931 authors who have published 4993 publications receiving 143226 citations.

On dominating the Cartesian product of a graph and K

Abstract: In this paper we consider the Cartesian product of an arbitrary graph and a complete graph of order two. Although an upper and lower bound for the domination number of this product follow easily from known results, we are interested in the graphs that actually attain these bounds. In each case, we provide an infinite class of graphs to show that the bound is sharp. The graphs that achieve the lower bound are of particular interest given the special nature of their dominating sets and are investigated further.

Atomic data and spectral modeling constraints from high-resolution X-ray observations of the Perseus cluster with Hitomi

Abstract: The Hitomi Soft X-ray Spectrometer spectrum of the Perseus cluster, with similar to 5 eV resolution in the 2-9 keV band, offers an unprecedented benchmark of the atomic modeling and database for hot collisional plasmas. It reveals both successes and challenges of the current atomic data and models. The latest versions of AtomDB/APEC (3.0.8), SPEX (3.03.00), and CHIANTI (8.0) all provide reasonable fits to the broad-band spectrum, and are in close agreement on best-fit temperature, emission measure, and abundances of a few elements such as Ni. For the Fe abundance, the APEC and SPEX measurements differ by 16%, which is 17 times higher than the statistical uncertainty. This is mostly attributed to the differences in adopted collisional excitation and dielectronic recombination rates of the strongest emission lines. We further investigate and compare the sensitivity of the derived physical parameters to the astrophysical source modeling and instrumental effects. The Hitomi results show that accurate atomic data and models are as important as the astrophysical modeling and instrumental calibration aspects. Substantial updates of atomic databases and targeted laboratory measurements are needed to get the current data and models ready for the data from the next Hitomi-level mission.

Selection of appropriate host plants used in trap culture of arbuscular mycorrhizal fungi.

Abstract: Arbuscular mycorrhizal (AM) fungi in coalmine spoil, island forest and saline soils were enriched in pot culture with maize (Zea mays L.), tobacco (Nicotiana tabacum L.), white clover (Trifolium repens Linn.) and silverweed cinquefoil (Potentilla anserina L.). Based on spores, there were more species of AM fungi in the coalmine spoil (15 species, 3 genera), than in the forest soil (11 species, 4 genera) and the saline soil (5 species, 2 genera). In the trap cultures, the total of 28 species in Acaulospora, Gigaspora, Glomus, and Sclerocystis detected in the original soils were all recovered with at least one of the four trap plants. The highest spore and species numbers were recovered in trap cultures of T. repens inoculated with coalmine spoil. Glomus constrictum and Glomus multicaule were the dominant species associated with N. tabacum grown in saline soil and forest soil. The dominant species of AM fungi on the four hosts was Acaulospora mellea, which had over 90% of the spore incidence in pot trap culture in coalmine spoil. It is suggested that there be selectivity between host plants and AM fungi. The number of species of AM fungi detected was influenced by host plants under certain conditions and white clover was generally the optimal host plant to detect diversity of AM fungi.

Evolution of boninites and island-arc tholeiites in the Pindos Ophiolite, Greece

Abstract: Whole-rock geochemical and Sm/Nd isotope data are presented for a representative suite of crustal rocks from the Pindos Ophiolite in order to resolve the origin of the geochemical signature of the boninites. Comparison is made with Triassic MORB from the Avdella melange and with other ophiolitic rocks of northwestern Greece. Hydrothermal alteration results in large scatter in Sr and K and some variability in Ba, Th and U. The Pindos boninites contain high Zr and Hf with respect to REE, characteristic of many boninites. Pb, La/Sm and Nb decrease with decreasing TiO2 from MORB to IAT, but then increase in the boninites. Nd isotopic values expressed as eNd decrease systematically with decreasing TiO2, from 7–8 in IAT to 0.6–3.0 in boninites. As mantle wedge harzburgite became increasingly depleted, another magma source contributed significant amounts of Pb, REE and probably Nb. The Pb and other large-ion lithophile elements may have been transported in aqueous solutions from the subducting slab, but the REE and Nb imply an ocean-island basalt (OIB)-type source within the mantle wedge. This OIB source is a consequence of mantle plume activity during late Triassic rifting.