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We present a study characterizing aerosol particles resulting from a skyscraper blasting. High mass concentrations with a maximum of 844.9 μg m-3 were present for a short time period of approximately 15 minutes. They result in a day mean of 32.6 μg m-3 compared to a 27.6 μg m-3 background not exceeding the 50 μg m-3 EU maximum permissive value. The increase in particle number concentration was less pronounced with a maximum concentration of 6.9 ⋅ 104 cm-3 compared to the local background value of 1.8 ⋅ 104 cm-3. The size-resolved number concentration shows a single mode of ultrafine particles at approximately 93 nm. The spatial distribution of deposited dust was investigated with Bergerhoff glass collection vessels, showing a decrease with distance. In the deposited dust samples the concentrations of twelve metals was determined, non of them exceeded the regional background concentrations significantly. The chemical composition of individual particles emitted by the demolition was studied by Scanning Electron Microscopy. They were mainly concrete and steel particles, with 60% calcium carbonates, 19% calcium sulfates, 19% silicates and 2% steel. In energy-dispersive X-Ray Spectroscopy, no fibers like asbestos were observed. Using a broad spectrum of instruments and methods, we obtain comprehensive characterization of the particles emitted by the demolition.
Recently significant advances have been made in the collection, detection, and characterization of ice nucleating particles (INP). Ice nuclei are particles that facilitate the heterogeneous formation of ice within the atmospheric aerosol by lowering the free energy barrier to spontaneous nucleation and growth of ice from atmospheric water and/or vapor. The Frankfurt isostatic diiffusion chamber (FRIDGE) is an INP collection and offline detection system that has become widely deployed and shows additional potential for ambient measurements. Since its initial development FRIDGE has gone through several iterations and improvements. Here we describe improvements that have been made in the collection and analysis techniques. We detail the uncertainties inherent in the measurement method, and suggest a systematic method of error analysis for FRIDGE measurements. Thus what is presented herein should serve as a foundation for the dissemination of all current and future measurements using FRIDGE instrumentation.
Ice nucleating particles over the eastern mediterranean measured by unmanned aircraft systems
(2017)
During an intensive field campaign on aerosol, clouds, and ice nucleation in the Eastern Mediterranean in April 2016, we measured the abundance of ice nucleating particles (INPs) in the lower troposphere from unmanned aircraft systems (UASs). Aerosol samples were collected by miniaturized electrostatic precipitators onboard the UASs at altitudes up to 2.5 km. The number of INPs in these samples, which are active in the deposition and condensation modes at temperatures from −20 to −30 °C, were analyzed immediately after collection on site using the ice nucleus counter FRIDGE (FRankfurt Ice nucleation Deposition freezinG Experiment). During the 1-month campaign, we encountered a series of Saharan dust plumes that traveled at several kilometers' altitude. Here we present INP data from 42 individual flights, together with aerosol number concentrations, observations of lidar backscattering, dust concentrations derived by the dust transport model DREAM (Dust Regional Atmospheric Model), and results from scanning electron microscopy. The effect of the dust plumes is reflected by the coincidence of INPs with the particulate matter (PM), the lidar signal, and the predicted dust mass of the model. This suggests that mineral dust or a constituent related to dust was a major contributor to the ice nucleating properties of the aerosol. Peak concentrations of above 100 INPs std L−1 were measured at −30 °C. The INP concentration in elevated plumes was on average a factor of 10 higher than at ground level. Since desert dust is transported for long distances over wide areas of the globe predominantly at several kilometers' altitude, we conclude that INP measurements at ground level may be of limited significance for the situation at the level of cloud formation.
Ice nucleating particles over the Eastern Mediterranean measured by unmanned aircraft systems
(2016)
During an intensive field campaign on aerosol, clouds and ice nucleation in the Eastern Mediterranean in April 2016, we have measured the abundance of ice nucleating particles (INP) in the lower troposphere from unmanned aircraft systems (UAS). Aerosol samples were collected by miniaturized electrostatic precipitators onboard the UAS at altitudes up to 2.5 km. The number of INP in these samples, which are active in the deposition and condensation modes at temperatures from −20 to −30 ◦C, were analyzed immediately after collection on site using the ice nucleus counter FRIDGE. During the one month campaign we encountered a series of Saharan dust plumes that traveled at several kilometers altitude. Here we present INP data from 42 individual flights, together with aerosol number concentrations, observations of lidar backscattering, dust concentrations derived by the dust transport model DREAM (Dust Regional Atmospheric Model), and results from scanning electron microscopy. The effect of the dust plumes is reflected by the coincidence of INP with the particulate mass (PM), the lidar signal and with the predicted dust mass of the model. This suggests that mineral dust or a constituent related to dust was a major contributor to the ice nucleating properties of the aerosol. Peak concentrations of above 100 INP std.l -1 were measured at −30 ◦C. The INP concentration in elevated plumes was on average a factor of 10 higher than at ground level. Since desert dust is transported for long distances over wide areas of the globe predominantly at several km altitude we conclude that INP measurements at ground level may be of limited significance for the situation at the level of cloud formation.
Das Wissen über die Wolkenmikrophysik und die Wechselwirkung zwischen Niederschlag und Aerosol ist ein wichtiger Baustein zur Optimierung von Klima- und Wettermodellen. Ein Großteil des Niederschlags in den mittleren Breiten fällt aus Mischphasenwolken, die aus unterkühlten Tröpfchen und Eispartikeln bestehen. Die Eispartikel bilden sich an speziellen Aerosolpartikeln, die als Eiskeime (INP) wirken können. Die Wahrscheinlichkeit eines Aerosols als Eiskeim zu wirken, nimmt mit abnehmender Temperatur und steigender Wassersättigung zu. Mineralstaubpartikel sind die häufigsten Eiskeime, die ab Temperaturen ≤−15°C aktiv sind, biologische Partikel wirken schon bei wärmeren Bedingungen. Große Wissenslücken bestehen noch bei der globalen Konzentration von Eiskeimen, inklusive deren geographischer und jahreszeitlicher Variabilität.
Im Zentrum der Experimente, die für diese Arbeit durchgeführt wurden, steht der Eiskeimzähler FRIDGE (Frankfurt Ice Deposition Freezing Experiment). Je nach Aufbau und Anwendung des Instruments werden zwei verschiedene Ansätze zur Aktivierung von Eiskeimen verfolgt. Die ursprüngliche und namensgebende Methode in Form einer Vakuum-Diffusionskammer wurde zur Untersuchung von Eisnukleation via Depositionsgefrieren (an INP_D) entwickelt (Klein et al., 2010). Danielczok (2015) nutzte einige Bestandteile des Analysegeräts, um auch Immersionsgefrieren (an INP_I) in Form von Tröpfchengefrieren à la Vali (1971) zu studieren. In der vorliegenden Arbeit wurde diese Anwendungsmöglichkeit von FRIDGE weiterentwickelt. Ein zentraler Schritt war dabei die präzise Charakterisierung des Gefrierverhaltens von Tröpfchen aus Reinstwasser ohne zusätzliches Aerosol. Die Einbeziehung dieses sogenannten Hintergrundgefrierens, das für jedes Instrument und Messverfahren spezifisch ist, ermöglichte es, die Minimaltemperatur, für die zuverlässige Ergebnisse produziert werden können, von −22°C auf −29°C herabzusetzen. Der dadurch hinzugewonnene Temperaturbereich ist für Eisnukleation in Mischphasenwolken äußerst relevant.
Beide Anwendungsmethoden wurden im Rahmen des Fifth International Workshop on Ice Nucleation – Phase 2 (FIN-02) sowie bei einer weiteren Kampagne zur Messung von Eisnukleation an Cellulosepartikeln mit über zwanzig anderen Eiskeimzählern verglichen. Mit FRIDGE als Diffusionskammer wurde für die Mehrheit der untersuchten Aerosoltypen eine zufriedenstellende Übereinstimmung mit den anderen Instrumenten beobachtet. Die Experimente mit gefrierenden Tröpfchen in FRIDGE erzielten ausnahmslos Ergebnisse, die inmitten der Werte der anderen Instrumente lagen. Die erfolgreiche Validierung – besonders der neuen Anwendungsmethode – war das erste Ziel dieser Arbeit und die notwendige Voraussetzung für die anschließenden Feldmessungen.
Atmosphärische Eiskeimkonzentrationen wurden in mehrwöchigen Feldmesskampagnen an drei sehr unterschiedlichen Orten und atmosphärischen Bedingungen untersucht: an der Hochalpinen Forschungsstation Jungfraujoch (JFJ), am Storm Peak Laboratory (SPL) in den Rocky Mountains und am Cyprus Atmospheric Observatory (CAO) in Zypern. Am JFJ wurde eine INP-Konzentration beobachtet, die um den Faktor 20 niedriger als an den anderen beiden Stationen war. Der Grund dafür war, dass sich das Jungfraujoch die meiste Zeit der Messungen in der freien Troposphäre befand. Dementsprechend waren die Bedingungen an der Station von aerosolpartikelarmer Luft mit wenigen Eiskeimen geprägt. An zwei Standorten wurde Mineralstaub als ein Parameter, der die lokale INP-Konzentration positiv beeinflusst, identifiziert. Sowohl am JFJ als auch am CAO erhöhte ferntransportierter Saharastaub die INP-Konzentration.
Die Kombination der zwei Analysemethoden, die Aerosolproben aus derselben Luft entweder in trockenem Ausgangszustand oder in Tröpfchen suspendiert untersuchen, offenbarte eine interessante Eigenschaft der INP. Es herrschte eine offensichtliche Parallelität von INP_D- und INP_I- Konzentrationen. Bei fast allen Messungen waren INP_I etwa 10-mal häufiger als INP_D. Die Aussage trifft gleichermaßen auf sehr niedrige Konzentrationen am JFJ wie auch auf hohe Konzentrationen am SPL und CAO zu. Die einzige Ausnahme bilden Cellulosepartikel. Daraus lässt sich schließen, dass INP_D und INP_I dieselben Partikel sind, die je nach Aktivierungskonditionen Eisnukleation unterschiedlich effektiv hervorrufen.
Recently significant advances have been made in the collection, detection and characterization of ice nucleating particles (INPs). Ice nuclei are particles that facilitate the heterogeneous formation of ice within the atmospheric aerosol by lowering the free energy barrier to spontaneous nucleation and growth of ice from atmospheric water and/or vapor. The Frankfurt isostatic diffusion chamber (FRankfurt Ice nucleation Deposition freezinG Experiment: FRIDGE) is an INP collection and offline detection system that has become widely deployed and shows additional potential for ambient measurements. Since its initial development FRIDGE has gone through several iterations and improvements. Here we describe improvements that have been made in the collection and analysis techniques. We detail the uncertainties inherent in the measurement method and suggest a systematic method of error analysis for FRIDGE measurements. Thus what is presented herein should serve as a foundation for the dissemination of all current and future measurements using FRIDGE instrumentation.
The antibody-drug conjugate polatuzumab vedotin (pola) has recently been approved in combination with bendamustine and rituximab (pola-BR) for patients with refractory or relapsed (r/r) large B-cell lymphoma (LBCL). To investigate the efficacy of pola-BR in a real-world setting, we retrospectively analyzed 105 patients with LBCL who were treated in 26 German centers under the national compassionate use program. Fifty-four patients received pola as a salvage treatment and 51 patients were treated with pola with the intention to bridge to chimeric antigen receptor (CAR) T-cell therapy (n = 41) or allogeneic hematopoietic cell transplantation (n = 10). Notably, patients in the salvage and bridging cohort had received a median of 3 prior treatment lines. In the salvage cohort, the best overall response rate was 48.1%. The 6-month progression-free survival and overall survival (OS) was 27.7% and 49.6%, respectively. In the bridging cohort, 51.2% of patients could be successfully bridged with pola to the intended CAR T-cell therapy. The combination of pola bridging and successful CAR T-cell therapy resulted in a 6-month OS of 77.9% calculated from pola initiation. Pola vedotin-rituximab without a chemotherapy backbone demonstrated encouraging overall response rates up to 40%, highlighting both an appropriate alternative for patients unsuitable for chemotherapy and a new treatment option for bridging before leukapheresis in patients intended for CAR T-cell therapy. Furthermore, 7 of 12 patients with previous failure of CAR T-cell therapy responded to a pola-containing regimen. These findings suggest that pola may serve as effective salvage and bridging treatment of r/r LBCL patients.
Wastewater-based SARS-CoV-2 epidemiology (WBE) has been established as an important tool to support individual testing strategies. Omicron sub-variants BA.4/5 have spread globally displacing the predeceasing variants. Due to the severe transmissibility and immune escape potential of BA.4/5, early monitoring was required to asses and implement countermeasures in time.
In this study, we monitored the prevalence of SARS-CoV-2 BA.4/5 at six municipal wastewater treatment plants (WWTPs) in the Federal State of North-Rhine-Westphalia (NRW, Germany) in May and June 2022. Initially, L452R-specific primers/probes originally designed for SARS-CoV-2 Delta detection were validated using inactivated authentic viruses and evaluated for their suitability to detect BA.4/5. Subsequently, the assay was used for RT-qPCR analysis of RNA purified from wastewater obtained twice a week at six WWTPs. The occurrence of L452R carrying RNA was detected in early May 2022 and the presence of BA.4/5 was confirmed by variant-specific single nucleotide polymorphism PCR (SNP-PCR) targeting E484A/F486V. Finally, the mutant fractions were quantitatively monitored by digital PCR confirming BA.4/5 as the majority variant by 5th June 2022.
In conclusions, the successive workflow using RT-qPCR, variant-specific SNP-PCR, and RT-dPCR demonstrates the strength of WBE as a versatile tool to rapidly monitor variant spreading independent of individual test capacities.
Epigenetic neural glioblastoma enhances synaptic integration and predicts therapeutic vulnerability
(2023)
Neural-tumor interactions drive glioma growth as evidenced in preclinical models, but clinical validation is nascent. We present an epigenetically defined neural signature of glioblastoma that independently affects patients survival. We use reference signatures of neural cells to deconvolve tumor DNA and classify samples into low- or high-neural tumors. High-neural glioblastomas exhibit hypomethylated CpG sites and upregulation of genes associated with synaptic integration. Single-cell transcriptomic analysis reveals high abundance of stem cell-like malignant cells classified as oligodendrocyte precursor and neural precursor cell-like in high-neural glioblastoma. High-neural glioblastoma cells engender neuron-to-glioma synapse formation in vitro and in vivo and show an unfavorable survival after xenografting. In patients, a high-neural signature associates with decreased survival as well as increased functional connectivity and can be detected via DNA analytes and brain-derived neurotrophic factor in plasma. Our study presents an epigenetically defined malignant neural signature in high-grade gliomas that is prognostically relevant.
Background: Microdeletions are known to confer risk to epilepsy, particularly at genomic rearrangement ‘hotspot’ loci. However, microdeletion burden not overlapping these regions or within different epilepsy subtypes has not been ascertained.
Objective: To decipher the role of microdeletions outside hotspots loci and risk assessment by epilepsy subtype.
Methods: We assessed the burden, frequency and genomic content of rare, large microdeletions found in a previously published cohort of 1366 patients with genetic generalised epilepsy (GGE) in addition to two sets of additional unpublished genome-wide microdeletions found in 281 patients with rolandic epilepsy (RE) and 807 patients with adult focal epilepsy (AFE), totalling 2454 cases. Microdeletions were assessed in a combined and subtype-specific approaches against 6746 controls.
Results: When hotspots are considered, we detected an enrichment of microdeletions in the combined epilepsy analysis (adjusted p=1.06×10−6,OR 1.89, 95% CI 1.51 to 2.35). Epilepsy subtype-specific analyses showed that hotspot microdeletions in the GGE subgroup contribute most of the overall signal (adjusted p=9.79×10−12, OR 7.45, 95% CI 4.20–13.5). Outside hotspots , microdeletions were enriched in the GGE cohort for neurodevelopmental genes (adjusted p=9.13×10−3,OR 2.85, 95% CI 1.62–4.94). No additional signal was observed for RE and AFE. Still, gene-content analysis identified known (NRXN1, RBFOX1 and PCDH7) and novel (LOC102723362) candidate genes across epilepsy subtypes that were not deleted in controls.
Conclusions: Our results show a heterogeneous effect of recurrent and non-recurrent microdeletions as part of the genetic architecture of GGE and a minor contribution in the aetiology of RE and AFE.