105 research outputs found
Deal or No Deal? Evaluating Big Deals and Their Journals
This paper presents methods to develop metrics that compare Big Deal
journal packages and the journals within those packages. Deal-level
metrics guide selection of a Big Deal for termination. Journal-level metrics
guide selection of individual subscriptions from journals previously
provided by a terminated deal. The paper argues that, while the proposed
metrics provide helpful quantitative data for comparative analysis, selection
of individual subscriptions must also involve informed judgment about
a library’s subject coverage needs and alternative sources of access. The
paper also discusses how replacing a Big Deal with a reduced number
of individual subscriptions may affect the collections budget, use of other
resources, and interlibrary loan.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/96846/1/178.full.pd
Modeling the Sources and Chemistry of Polar Tropospheric Halogens (Cl, Br, and I) Using the CAM-Chem Global Chemistry-Climate Model
31 pags., 12 figs., 6 tabs. -- Open Access funded by Creative Commons Atribution Licence 4.0. -- jame20925-sup-0001_Supporting_Information.pdfCurrent chemistry climate models do not include polar emissions and chemistry of halogens. This work presents the first implementation of an interactive polar module into the very short-lived (VSL) halogen version of the Community Atmosphere Model with Chemistry (CAM-Chem) model. The polar module includes photochemical release of molecular bromine, chlorine, and interhalogens from the sea-ice surface, and brine diffusion of iodine biologically produced underneath and within porous sea-ice. It also includes heterogeneous recycling of inorganic halogen reservoirs deposited over fresh sea-ice surfaces and snow-covered regions. The polar emission of chlorine, bromine, and iodine reach approximately 32, 250, and 39 Gg/year for Antarctica and 33, 271, and 4 Gg/year for the Arctic, respectively, with a marked seasonal cycle mainly driven by sunlight and sea-ice coverage. Model results are validated against polar boundary layer measurements of ClO, BrO, and IO, and satellite BrO and IO columns. This validation includes satellite observations of IO over inner Antarctica for which an iodine “leapfrog” mechanism is proposed to transport active iodine from coastal source regions to the interior of the continent. The modeled chlorine and bromine polar sources represent up to 45% and 80% of the global biogenic VSL and VSL emissions, respectively, while the Antarctic sea-ice iodine flux is ~10 times larger than that from the Southern Ocean. We present the first estimate of the contribution of polar halogen emissions to the global tropospheric halogen budget. CAM-Chem includes now a complete representation of halogen sources and chemistry from pole-to-pole and from the Earth's surface up to the stratopause.This study has been funded by the European Research Council Executive Agency under the European Union′s Horizon 2020 Research and Innovation
program (Project “ERC‐2016‐COG 726349 CLIMAHAL”) and supported by the Consejo Superior de Investigaciones Científicas (CSIC) of Spain. Computing
resources, support, and data storage are provided and maintained by the Computational and Information System Laboratory from the National
Center of Atmospheric Research (CISL,2017). R. P. F. would like to thank CONICET, ANPCyT (PICT 2015‐0714), UNCuyo (SeCTyP M032/3853), and
UTN (PID 4920‐194/2018) for the financial support. Partial funding for this work was provided by the Korea Polar Research Institute (KOPRI) project (PE18200). The contributions of the University of Bremen have been supported by the State of Bremen, the German Research Foundation (DFG),
the German Aerospace (DLR), and the European Space Agency (ESA). We gratefully acknowledge the funding by the Deutsche Forschungsgemeinschaft
(DFG, German Research Foundation) —Projektnummer 268020496—TRR 172, within the Transregional Collaborative Research Center “ArctiC
Amplification: Climate Relevant Atmospheric and SurfaCe Processes,and Feedback Mechanisms (AC)3 ” in subproject C03 as well as the support by
the University of Bremen Institutional Strategy Measure M8 in the framework of the DFG Excellence Initiative
Light and flow regimes regulate the metabolism of rivers
Mean annual temperature and mean annual precipitation drive much of the variation in productivity across Earth's terrestrial ecosystems but do not explain variation in gross primary productivity (GPP) or ecosystem respiration (ER) in flowing waters. We document substantial variation in the magnitude and seasonality of GPP and ER across 222 US rivers. In contrast to their terrestrial counterparts, most river ecosystems respire far more carbon than they fix and have less pronounced and consistent seasonality in their metabolic rates. We find that variation in annual solar energy inputs and stability of flows are the primary drivers of GPP and ER across rivers. A classification schema based on these drivers advances river science and informs management.We thank Ted Stets, Jordan Read, Tom Battin, Sophia
Bonjour, Marina Palta, and members of the Duke River Center for their help in
developing these ideas. This work was supported by grants from the NSF
1442439 (to E.S.B. and J.W.H.), 1834679 (to R.O.H.), 1442451 (to R.O.H.),
2019528 (to R.O.H. and J.R.B.), 1442140 (to M.C.), 1442451 (to A.M.H.),
1442467 (to E.H.S.), 1442522 (to N.B.G.), 1624807 (to N.B.G.), and US Geological
Survey funding for the working group was supported by the John Wesley
Power Center for Analysis and Synthesis. Phil Savoy contributed as a postdoc-
toral associate at Duke University and as a postdoctoral associate (contractor)
at the US Geological Survey
Oral hygiene in children suffering from acute lymphoblastic leukemia living in rural and urban regions
Introduction and objective. During acute lymphoblastic leukemia treatment, oral mucositis is a hugely important dental
problem. In order to lower the risk of such complications, patients should take special care of their oral hygiene. The aim of
this study was to assess the oral hygiene status in children with ALL during anti-cancer treatment protocols.
Materials and methods. 78 children with ALL who were examined in 3 stages, and 78 generally healthy children, who
constituted the control group, participated in the study. In the group of patients were 55 children from the rural environment
and 23 children living in towns. Oral hygiene status was assessed with the use of the Oral Hygiene Simplified Index, Plaque
Index, and Gingival Index.
Results. The average value of OHI-S index in children with ALL before the chemotherapy was 0.64 ± 0.85, the value of the
Pl.I index was 0.59 ± 0.74, GI index value was 0.08 ± 0.34. In the period from 0.5 – 1.5 years, the anti-cancer therapy value
indicators of oral hygiene in children with ALL developed as follows: OHI-S – 0.49 ± 0.69, Pl.I – 0.49 ± 0.67, GI – 0.02 ± 0.13.
Conclusions. Oral hygiene was significantly better in children with ALL than in children in the control group. The better
condition of oral hygiene in children with ALL than children in the control group is the result of the oral hygiene regime
that the children were following during cancer treatment protocols. Significantly higher GI in children with ALL, compared
to children from the control group, was observed despite the better oral hygiene
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