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Background: The elderly population deals with multimorbidity (three chronic conditions) and increasinged drug use with age. A comprehensive characterisation of the medication – including prescription and over-the-counter (OTC) drugs – of elderly patients in primary care is still insufficient.
Objectives: This study aims to characterise the medication (prescription and OTC) of multimorbid elderly patients in primary care and living at home by identifying drug patterns to evaluate the relationship between drugs and drug groups and reveal associations with recently published multimorbidity clusters of the same cohort.
Methods: MultiCare was a multicentre, prospective, observational cohort study of 3189 multimorbid patients aged 65 to 85 years in primary care in Germany. Patients and general practitioners were interviewed between 2008 and 2009. Drug patterns were identified using exploratory factor analysis. The relations between the drug patterns with the three multimorbidity clusters were analysed with Spearman-Rank-Correlation.
Results: Patients (59.3% female) used in mean 7.7 drugs; in total 24,535 drugs (23.7% OTC) were detected. Five drug patterns for men (drugs for obstructive pulmonary diseases (D-OPD), drugs for coronary heart diseases and hypertension (D-CHD), drugs for osteoporosis (D-Osteo), drugs for heart failure and drugs for pain) and four drug patterns for women (D-Osteo, D-CHD, D-OPD and drugs for diuretics and gout) were detected. Significant associations between multimorbidity clusters and drug patterns were detectable (D-CHD and CMD: male: ρ = 0.376, CI 0.322–0.430; female: ρ = 0.301, CI 0.624–0.340).
Conclusion: The drug patterns demonstrate non-random relations in drug use in multimorbid elderly patients and systematic associations between drug patterns and multimorbidity clusters were found in primary care.
The formation of secondary particles in the atmosphere accounts for more than half of global cloud condensation nuclei. Experiments at the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber have underlined the importance of ions for new particle formation, but quantifying their effect in the atmosphere remains challenging. By using a novel instrument setup consisting of two nano-particle counters, one of them equipped with an ion filter, we were able to further investigate the ion-related mechanisms of new particle formation. In autumn 2015, we carried out experiments at CLOUD on four systems of different chemical compositions involving monoterpenes, sulfuric acid, nitrogen oxides, and ammonia. We measured the influence of ions on the nucleation rates under precisely controlled and atmospherically relevant conditions. Our results indicate that ions enhance the nucleation process when the charge is necessary to stabilize newly formed clusters, i.e. in conditions where neutral clusters are unstable. For charged clusters that were formed by ion-induced nucleation, we were able to measure, for the first time, their progressive neutralization due to recombination with oppositely charged ions. A large fraction of the clusters carried a charge at 1.2 nm diameter. However, depending on particle growth rates and ion concentrations, charged clusters were largely neutralized by ion–ion recombination before they grew to 2.2 nm. At this size, more than 90 % of particles were neutral. In other words, particles may originate from ion-induced nucleation, although they are neutral upon detection at diameters larger than 2.2 nm. Observations at Hyytiälä, Finland, showed lower ion concentrations and a lower contribution of ion-induced nucleation than measured at CLOUD under similar conditions. Although this can be partly explained by the observation that ion-induced fractions decrease towards lower ion concentrations, further investigations are needed to resolve the origin of the discrepancy.
A new method for size-resolved chemical analysis of nucleation mode aerosol particles (size range from ∼10 to ∼30 nm) is presented. The Thermal Desorption Differential Mobility Analyzer (TD-DMA) uses an online, discontinuous principle. The particles are charged, a specific size is selected by differential mobility analysis and they are collected on a filament by electrostatic precipitation. Subsequently, the sampled mass is evaporated in a clean carrier gas and analyzed by a chemical ionization mass spectrometer. Gas-phase measurements are performed with the same mass spectrometer during the sampling of particles. The characterization shows reproducible results, with a particle size resolution of 1.19 and the transmission efficiency for 15 nm particles being slightly above 50 %. The signal from the evaporation of a test substance can be detected starting from 0.01 ng and shows a linear response in the mass spectrometer. Instrument operation in the range of pg m−3 is demonstrated by an example measurement of 15 nm particles produced by nucleation from dimethylamine, sulfuric acid and water.
Nucleation and growth of aerosol particles from atmospheric vapors constitutes a major source of global cloud condensation nuclei (CCN). The fraction of newly formed particles that reaches CCN sizes is highly sensitive to particle growth rates, especially for particle sizes <10 nm, where coagulation losses to larger aerosol particles are greatest. Recent results show that some oxidation products from biogenic volatile organic compounds are major contributors to particle formation and initial growth. However, whether oxidized organics contribute to particle growth over the broad span of tropospheric temperatures remains an open question, and quantitative mass balance for organic growth has yet to be demonstrated at any temperature. Here, in experiments performed under atmospheric conditions in the Cosmics Leaving Outdoor Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN), we show that rapid growth of organic particles occurs over the range from −25 ∘C to 25 ∘C. The lower extent of autoxidation at reduced temperatures is compensated by the decreased volatility of all oxidized molecules. This is confirmed by particle-phase composition measurements, showing enhanced uptake of relatively less oxygenated products at cold temperatures. We can reproduce the measured growth rates using an aerosol growth model based entirely on the experimentally measured gas-phase spectra of oxidized organic molecules obtained from two complementary mass spectrometers. We show that the growth rates are sensitive to particle curvature, explaining widespread atmospheric observations that particle growth rates increase in the single-digit-nanometer size range. Our results demonstrate that organic vapors can contribute to particle growth over a wide range of tropospheric temperatures from molecular cluster sizes onward.
A new method for size resolved chemical analysis of nucleation mode aerosol particles (size range from ~10 to ~30 nm) is presented. The Thermal Desorption Differential Mobility Analyzer (TD-DMA) uses an online, discontinuous principle. The particles are charged, a specific size is selected by differential mobility analysis and they are collected on a filament by electrostatic precipitation. Subsequently, the sampled mass is evaporated in a clean carrier gas and analyzed by a chemical ionization mass spectrometer. Gas phase measurements are performed with the same mass spectrometer during the sampling of particles. The characterization shows reproducible results, with a particle size resolution of 1.19 and the transmission efficiency for 15 nm particles being slightly above 50 %. The signal from the evaporation of a test substance can be detected starting from 0.01 ng and shows a linear response in the mass spectrometer. Instrument operation in the range of pg/m3 is demonstrated by an example measurement of 15 nm particles produced by nucleation from dimethylamine, sulfuric acid and water.
Rezensionen [2017]
(2017)
156 Ansari, Christine (Hrsg.): Adoleszenz in Medienkontexten. Literaturrezeption, Medienwirkung und Jugendmedienschutz (judith mathez)
158 Bachmann, Christian A. / Emans, Laura / Schmitz-Emans, Monika (Hrsg.): Bewegungsbücher. Spielformen, Poetiken, Konstellationen (gundel mattenklott)
160 Ballis, Anja /Schlachter, Birgit (Hrsg.): Schätze der Kinder- und Jugendliteratur wiederentdeckt. Frühe Lektüreerfahrung und Kanonbildung im akademischen Kontext (ernst seibert)
162 Benner, Julia: Federkrieg. Kinder- und Jugendliteratur gegen den Nationalsozialismus 1933 – 1945 (linde storm)
164 Born, Stefan: Allgemeinliterarische Adoleszenzromane. Untersuchungen zu Herrndorf, Regener, Strunk, Kehlmann und anderen (lena hoffmann)
166 Börnchen, Stefan: Poetik der Linie. Wilhelm Busch, Max und Moritz und die Tradition (lukas sarvari)
168 Burwitz-Melzer, Eva /O’Sullivan, Emer (Hrsg.): Einfachheit in der Kinder- und Jugendliteratur. Ein Gewinn für den Fremdsprachenunterricht (roland alexander issler)
169 Emde, Oliver /Möller, Lukas /Wicke, Andreas (Hrsg.): Von »Bibi Blocksberg« bis »TKKG«. Kinderhörspiele aus gesellschafts- und kulturwissenschaftlicher Perspektive (anika ullmann)
171 Ferstl, Paul /Walach, Thomas / Zahlmann, Stefan (Hrsg.): Fantasy Studies (maren bonacker)
173 Giesa, Felix: Graphisches Erzählen von Adoleszenz. Deutschsprachige Autorencomics nach 2000 (michael staiger)
175 Hahn, Heidi / Laudenberg, Beate / Rösch, Heidi (Hrsg.): »Wörter raus!?« Zur Debatte um eine diskriminierungsfreie Sprache im Kinderbuch (julia benner)
177 Haug, Christine / Frimmel, Johannes (Hrsg.): Schulbücher um 1800. Ein Spezialmarkt zwischen staatlichem, volksaufklärerischem und konfessionellem Auftrag (ortwin beisbart)
179 Hollerweger, Elisabeth /Stemmann, Anna (Hrsg.): Narrative Delikatessen. Kulturelle Dimensionen von Ernährung (sonja loidl)
180 Hopp, Margarete: Sterben, Tod und Trauer im Bilderbuch seit 1945 (iris schäfer)
182 Huemer, Georg: Mira Lobe. Doyenne der österreichischen Kinder- und Jugendliteratur (andreas schumann)
183 Josting, Petra (Hrsg.): Andreas Steinhöfel, Bielefelder Poet in Residence 2014 (heinke kilian)
185 Josting, Petra /Roeder, Caroline /Dettmar, Ute (Hrsg.): Immer Trouble mit Gender. Genderperspektiven in Kinder- und Jugendliteraturforschung und -medien (jana mikota)
187 Kurwinkel, Tobias /Schmerheim, Philipp /Sevi, Annika (Hrsg.): Michael Ende intermedial. Von Lokomotivführern, Glücksdrachen und dem (phantastischen) Spiel mit Mediengrenzen (michael stierstorfer)
188 Mikota, Jana / Pecher, Claudia Maria / von Glasenapp, Gabriele (Hrsg.): Literarisch-kulturelle Begegnungen mit dem Judentum. Beiträge zur kinderliterarischen Fachöffentlichkeit (susanne blumesberger)
190 Müller, Karla / Decker, Jan-Oliver / Krah, Hans / Schilcher, Anita (Hrsg.): Genderkompetenz mit Kinder- und Jugendliteratur entwickeln: Grundlagen – Analysen – Modelle (annette kliewer)
192 Nikolajeva, Maria: Reading for Learning. Cognitive Approaches to Children’s Literature (sabine fuchs)
194 Paul, Lissa / Johnston, Rosemary R. / Short, Emma (Hrsg.):Children’s Literature and Culture of the First World War.(julia benner)
195 Payrhuber, Franz-Josef / Meier, Bernhard(Hrsg.): Franz, Kurt: Kinderlyrik. Geschichte, Formen, Rezeption(ludger scherer)
197 Payrhuber, Franz-Josef:Gedichte entdecken. Wege zu Gedichten in der ersten bis sechsten Klasse (andreas schumann)
198 Pohlmann, Carola (Hrsg): Kinder- und Jugendliteratur. Sammeln und Erwerben (wolfgang wangerin)
200 Pompe, Anja (Hrsg): Kind und Gedicht. Wie wir lesen lernen (heinz-jürgen kliewer)
202 Preindl, Nadia:Russische Kinderliteratur im europäischen Exil der Zwischenkriegszeit (verena rutschmann)
204 Richter, Karin: Die Kinder- und Jugend-literatur der DDR. Entwicklungslinien – Themen und Genres. Autorenporträts und Textanalysen (maria becker)
206 Riemhofer, Andra:Interkulturelle Kinder- und Jugendliteratur in Deutschland. Lesen auf eigene Gefahr (roger meyer)
208Roeder, Caroline (Hrsg.): Himmel und Hölle. Raumerkundungen – interdisziplinär & in schulischer Praxis (claudia blei-hoch)
210 Ruzicka Kenfel, Vejka (Hrsg.): New Trends in Children’s Literature Research. Twenty-first Century Approaches (2000–2012) from the University of Vigo (Spain) (susanne blumesberger)
212 Schäfer, Iris:Von der Hysterie zur Magersucht. Adoleszenz und Krankheit in Romanen und Erzählungen der Jahrhundert- und der Jahrtausendwende (philipp schmerheim)
214 Scherer, Gabriela / Volz, Steffen (Hrsg.): Im Bildungsfokus: Bilderbuchrezeptions-forschung (margarete hopp)
216 Schmitt, Susann Sophie:Nachwuchs für die Literatur. Kinder- und Jugendprogramme ausgewählter Literaturhäuser Deutschlands, Österreichs und der Schweiz (renate grubert)
217 Seelinger Trites, Roberta:Literary Conceptu-alizations of Growth. Metaphors and Cogni-tion in Adolescent Literature (iris schäfer)
219 Seifert, Martina:Die Bilderfalle. Kanada in der deutschsprachigen Kinder- und Jugend-literatur: Produktion und Rezeption (sabine planka)
222 Stein, Daniel / Thon, Jan-Noël (Hrsg.): From Comic Strips to Graphic Novels. Contributions to the Theory and History of Graphic Narrative (anna stemmann)
223 Tomberg, Markus (Hrsg.): Alle wichtigen Bücher handeln von Gott. Religiöse Spuren in aktueller Kinder- und Jugendliteratur (martin anker)
Cloud microphysical processes involving the ice phase in tropospheric clouds are among the major uncertainties in cloud formation, weather and General Circulation Models (GCMs). The simultaneous detection of aerosol particles, liquid droplets, and ice crystals, especially in the small cloud-particle size range below 50 µm, remains challenging in mixed phase, often unstable ice-water phase environments. The Cloud Aerosol Spectrometer with Polarisation (CASPOL) is an airborne instrument that has the ability to detect such small cloud particles and measure their effects on the backscatter polarisation state. Here we operate the versatile Cosmics-Leaving- OUtdoor-Droplets (CLOUD) chamber facility at the European Organisation for Nuclear Research (CERN) to produce controlled mixed phase and other clouds by adiabatic expansions in an ultraclean environment, and use the CASPOL to discriminate between different aerosols, water and ice particles. In this paper, optical property measurements of mixed phase clouds and viscous Secondary Organic Aerosol (SOA) are presented. We report observations of significant liquid – viscous SOA particle polarisation transitions under dry conditions using CASPOL. Cluster analysis techniques were subsequently used to classify different types of particles according to their polarisation ratios during phase transition. A classification map is presented for water droplets, organic aerosol (e.g., SOA and oxalic acid), crystalline substances such as ammonium sulphate, and volcanic ash. Finally, we discuss the benefits and limitations of this classi- fication approach for atmospherically relevant concentration and mixtures with respect to the CLOUD 8–9 campaigns and its potential contribution to Tropical Troposphere Layer (TTL) analysis.
The growth of aerosol due to the aqueous phase oxidation of sulfur dioxide by ozone was measured in laboratory-generated clouds created in the Cosmics Leaving OUtdoor Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN). Experiments were performed at 10 and −10 °C, on acidic (sulfuric acid) and on partially to fully neutralised (ammonium sulfate) seed aerosol. Clouds were generated by performing an adiabatic expansion – pressurising the chamber to 220 hPa above atmospheric pressure, and then rapidly releasing the excess pressure, resulting in a cooling, condensation of water on the aerosol and a cloud lifetime of approximately 6 min. A model was developed to compare the observed aerosol growth with that predicted using oxidation rate constants previously measured in bulk solutions. The model captured the measured aerosol growth very well for experiments performed at 10 and −10 °C, indicating that, in contrast to some previous studies, the oxidation rates of SO2 in a dispersed aqueous system can be well represented by using accepted rate constants, based on bulk measurements. To the best of our knowledge, these are the first laboratory-based measurements of aqueous phase oxidation in a dispersed, super-cooled population of droplets. The measurements are therefore important in confirming that the extrapolation of currently accepted reaction rate constants to temperatures below 0 °C is correct.
The growth of aerosol due to the aqueous phase oxidation of sulfur dioxide by ozone was measured in laboratory-generated clouds created in the Cosmics Leaving OUtdoor Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN). Experiments were performed at 10 and −10 °C, on acidic (sulfuric acid) and on partially to fully neutralised (ammonium sulfate) seed aerosol. Clouds were generated by performing an adiabatic expansion – pressurising the chamber to 220 hPa above atmospheric pressure, and then rapidly releasing the excess pressure, resulting in a cooling, condensation of water on the aerosol and a cloud lifetime of approximately 6 min. A model was developed to compare the observed aerosol growth with that predicted using oxidation rate constants previously measured in bulk solutions. The model captured the measured aerosol growth very well for experiments performed at 10 and −10 °C, indicating that, in contrast to some previous studies, the oxidation rates of SO2 in a dispersed aqueous system can be well represented by using accepted rate constants, based on bulk measurements. To the best of our knowledge, these are the first laboratory-based measurements of aqueous phase oxidation in a dispersed, super-cooled population of droplets. The measurements are therefore important in confirming that the extrapolation of currently accepted reaction rate constants to temperatures below 0 °C is correct.
Cloud microphysical processes involving the ice phase in tropospheric clouds are among the major uncertainties in cloud formation, weather, and general circulation models. The detection of aerosol particles, liquid droplets, and ice crystals, especially in the small cloud particle-size range below 50 μm, remains challenging in mixed phase, often unstable environments. The Cloud Aerosol Spectrometer with Polarization (CASPOL) is an airborne instrument that has the ability to detect such small cloud particles and measure the variability in polarization state of their backscattered light. Here we operate the versatile Cosmics Leaving OUtdoor Droplets (CLOUD) chamber facility at the European Organization for Nuclear Research (CERN) to produce controlled mixed phase and other clouds by adiabatic expansions in an ultraclean environment, and use the CASPOL to discriminate between different aerosols, water, and ice particles. In this paper, optical property measurements of mixed-phase clouds and viscous secondary organic aerosol (SOA) are presented. We report observations of significant liquid–viscous SOA particle polarization transitions under dry conditions using CASPOL. Cluster analysis techniques were subsequently used to classify different types of particles according to their polarization ratios during phase transition. A classification map is presented for water droplets, organic aerosol (e.g., SOA and oxalic acid), crystalline substances such as ammonium sulfate, and volcanic ash. Finally, we discuss the benefits and limitations of this classification approach for atmospherically relevant concentrations and mixtures with respect to the CLOUD 8–9 campaigns and its potential contribution to tropical troposphere layer analysis.