Benign Orbital Tumors with Bone Destruction in Children

Purpose: To present rare benign orbital tumors with bone destruction in children who could not be diagnosed presurgically and may simulate malignant ones. Methods: A retrospective review of cases. Clinical, operative and pathological records in all children with a diagnosis of benign orbital tumors who showed remarkable bone destruction at a tertiary Ophthalmic Center in China between Jan 1, 2000 and Dec 31, 2009 were reviewed. All patients had definitive histopathologic diagnosis. Results: Eight patients with benign orbital tumors showed obvious bone destruction, including six cases of eosinophilic granuloma, one case of leiomyoma and one case of primary orbital intraosseous hemangioma. Among them, three patients were females and five patients were males. Tumors were unilateral in all cases, with both the right and left side affected equally. Age ranged from 3 to 7 years (mean 4.1 years). Symptom duration ranged from 1 to 5 weeks (mean 4.8 weeks). Eyelid swelling and palpable mass were the most common complaint. There was no evidence for multifocal involvement in cases with eosinophilic granuloma. Among six patients with eosinophilic granuloma, two were treated with low dose radiation (10 Gy), three received systemic corticosteroid and one was periodically observed only after incisional biopsy or subtotal curettage. There was no postoperative therapeutic intervention in the two patients with leiomyoma and intraosseous hemangioma. All eight patients regained normal vision without local recurrence after a mean follow-up time o

Three-dimensional culture of human meniscal cells: Extracellular matrix and proteoglycan production

<p>Abstract</p> <p>Background</p> <p>The meniscus is a complex tissue whose cell biology has only recently begun to be explored. Published models rely upon initial culture in the presence of added growth factors. The aim of this study was to test a three-dimensional (3D) collagen sponge microenvironment (without added growth factors) for its ability to provide a microenvironment supportive for meniscal cell extracellular matrix (ECM) production, and to test the responsiveness of cells cultured in this manner to transforming growth factor-β (TGF-β).</p> <p>Methods</p> <p>Experimental studies were approved prospectively by the authors' Human Subjects Institutional Review Board. Human meniscal cells were isolated from surgical specimens, established in monolayer culture, seeded into a 3D scaffold, and cell morphology and extracellular matrix components (ECM) evaluated either under control condition or with addition of TGF-β. Outcome variables were evaluation of cultured cell morphology, quantitative measurement of total sulfated proteoglycan production, and immunohistochemical study of the ECM components chondroitin sulfate, keratan sulfate, and types I and II collagen.</p> <p>Result and Conclusion</p> <p>Meniscal cells attached well within the 3D microenvironment and expanded with culture time. The 3D microenvironment was permissive for production of chondroitin sulfate, types I and II collagen, and to a lesser degree keratan sulfate. This microenvironment was also permissive for growth factor responsiveness, as indicated by a significant increase in proteoglycan production when cells were exposed to TGF-β (2.48 μg/ml ± 1.00, mean ± S.D., vs control levels of 1.58 ± 0.79, p < 0.0001). Knowledge of how culture microenvironments influence meniscal cell ECM production is important; the collagen sponge culture methodology provides a useful in vitro tool for study of meniscal cell biology.</p

Extracellular NAD and ATP: Partners in immune cell modulation

Extracellular NAD and ATP exert multiple, partially overlapping effects on immune cells. Catabolism of both nucleotides by extracellular enzymes keeps extracellular concentrations low under steady-state conditions and generates metabolites that are themselves signal transducers. ATP and its metabolites signal through purinergic P2 and P1 receptors, whereas extracellular NAD exerts its effects by serving as a substrate for ADP-ribosyltransferases (ARTs) and NAD glycohydrolases/ADPR cyclases like CD38 and CD157. Both nucleotides activate the P2X7 purinoceptor, although by different mechanisms and with different characteristics. While ATP activates P2X7 directly as a soluble ligand, activation via NAD occurs by ART-dependent ADP-ribosylation of cell surface proteins, providing an immobilised ligand. P2X7 activation by either route leads to phosphatidylserine exposure, shedding of CD62L, and ultimately to cell death. Activation by ATP requires high micromolar concentrations of nucleotide and is readily reversible, whereas NAD-dependent stimulation begins at low micromolar concentrations and is more stable. Under conditions of cell stress or inflammation, ATP and NAD are released into the extracellular space from intracellular stores by lytic and non-lytic mechanisms, and may serve as ‘danger signals–to alert the immune response to tissue damage. Since ART expression is limited to naïve/resting T cells, P2X7-mediated NAD-induced cell death (NICD) specifically targets this cell population. In inflamed tissue, NICD may inhibit bystander activation of unprimed T cells, reducing the risk of autoimmunity. In draining lymph nodes, NICD may eliminate regulatory T cells or provide space for the preferential expansion of primed cells, and thus help to augment an immune response

Caratterizzazione di alcuni siti della rete accelerometrica nazionale al fine di individuare la risposta sismica locale

Le indagini geotecniche finalizzate alla stima della risposta sismica locale si limitano molto spesso ai primi 30 m di profondità, valore che è diventato uno standard per la classificazione delle caratteristiche di un sito. Negli anni ’90 Borcherdt (1994) e Martin e Dobry (1994) suggerirono 30 m come la profondità standard di indagine per la verifica delle strutture. Boore et al. (1993, 1994, 1997) e Boore e Joyner (1997) basarono le regressioni per il calcolo delle leggi predittive del moto del suolo sullo stesso parametro. Nel 1997 negli Stati Uniti il National Earthquake Hazards Reduction Program (NEHRP) nella stesura delle norme tecniche per le costruzioni in zona sismica (FEMA, 1997) utilizza per la prima volta il parametro Vs30 come indice per la classificazione dei suoli, con lo scopo di definirne l’amplificazione. Le norme tecniche per le costruzioni in zona sismica della comunità Europea, EC8 (ENV, 1998) ente da dati provenienti dagli Stati Uniti occidentali e, utilizzando dati provenienti dalla stessa regione, Wald & Mori (2000) segnalano che le VS,30 non sono molto ben correlate con l’entità dell’amplificazione, in quanto esiste una forte dispersione dei dati. La figura 1.1 mostra il rapporto tra le amplificazioni, mediate sull’intervallo di frequenza compreso tra 3-5 Hz. raccomandano lo stesso parametro per suddividere i terreni, anche se le classi differiscono in parte dalla classificazione NEHRP. Infine, anche in Italia, le Norme Tecniche per le Costruzioni (Normative Tecniche per le Costruzioni, Gazzetta Ufficiale del 14/01/2008) adottano la stessa suddivisione dei terreni adottata dall’EC8.L’attendibilità della velocità delle onde di taglio nei primi 30 m (VS,30) come estimatore della risposta sismica di un sito, in termini di frequenza e amplificazione, è tuttavia molto discussa.Innanzitutto il parametro è stato ricavato unicamente da dati provenienti dagli Stati Uniti occidentali e, utilizzando dati provenienti dalla stessa regione, Wald & Mori (2000) segnalano che le Vs30 non sono molto ben correlate con l’entità dell’amplificazione, in quanto esiste una forte dispersione dei dati. La figura 1.1 mostra il rapporto tra le amplificazioni, mediate sull’intervallo di frequenza compreso tra 3-5 Hz. I valori risultano effettivamente molto dispersi, ma questo risultato può essere spiegato col fatto che non tutte le classi di sito hanno frequenza di risonanza compreso in questo intervallo di frequenza. Perciò per alcuni siti la media è stata calcolata nell’intorno della frequenza di risonanza (sulle amplificazioni massime), mentre per altri è stata calcolata sulle armoniche superiori, che hanno ampiezze minori. Lavori eseguiti con dati provenienti da altre regioni sottolineano come le Vs30 non siano buoni estimatori per la predizione di amplificazioni in bacini profondi (Park & Hashash, 2004), per la stima delle amplificazioni in altre regioni (Stewart et al., 2003) o in presenza di inversioni di velocità (Di Giacomo et al., 2005). Uno studio recente, eseguito su dati giapponesi (Zhao et al., 2006) si è evitato l’uso della Vs30 perché strati spessi di terreno rigido posti sopra il substrato roccioso amplificano il moto di lungo periodo, mentre gli strati sottili e soffici tendono ad amplificare il moto di corto periodo: ciò significa che la VS,30 non può rappresentare il periodo predominante del sito, dato che si basa solo sugli strati superficiali. Secondo Mucciarelli e Gallipoli (2006) il confronto tra l’amplificazione sismica al sito e la Vs30 mostra che quest’ultimo parametro non è adeguato per spiegare gli effetti di sito osservati in Italia a causa delle situazioni geologiche particolari che sono diffuse nel nostro paese. La figura 1.2 mostra la distribuzione dell’ampiezza rispetto alla classe di sito, in cui si vede che le classi sono mal discriminate e le mediane delle classi A e B (indicate dalla linea nera) sono uguali. È però necessario notare che questo grafico è stato costruito utilizzando le ampiezze ricavate col metodo dei rapporti spettrali H/V, ma in letteratura (Bard, 1999) è dimostrato che tali rapporti spettrali permettono di stimare la frequenza di risonanza, ma falliscono nella stima del valore di amplificazione. In particolare la Vs30 sottostima gli effetti locali ai siti con inversione di velocità e li sovrastima in siti con bacini profondi. La Vs30 sembra fornire dei buoni risultati solo in siti che abbiano un profilo di velocità monotono, crescente con la profondità e un forte contrasto di impedenza nella prima decina di metri. Questo studio si propone di verificare l’attendibilità della velocità delle onde di taglio valutate nei primi 30 m come estimatore della risposta sismica di un sito. Per questo scopo sono state selezionate 45 stazioni della Rete Accelerometrica Nazionale, di cui si conoscono i profili stratigrafici e i profili di velocità delle onde di taglio e di compressione. Inoltre sono state raccolte le registrazioni strong motion relative ai terremoti registrati da queste stazioni. Gli effetti di sito sono stati valutati in due modi: · Le registrazioni sono state utilizzate per calcolare i rapporti spettrali H/V per ricavare la frequenza fondamentale propria di ciascun sito (f0) e il relativo valore di amplificazione; · I profili di velocità delle onde di taglio sono serviti per ricavare il modello teorico monodimensionale per il calcolo della funzione di trasferimento del sito, eseguito per mezzo del modello proposto da Haskell e Thomson (Haskell, 1953, Thomson 1950), da cui ricavare la f0 e l’amplificazione. I valori ottenuti con i due metodi sono stati poi confrontati per verificare la congruenza dei risultati. I profili di velocità hanno permesso di classificare le stazioni utilizzando la velocità media delle onde di taglio nei primi 30 m (Vs30), secondo la normativa italiana. I risultati ottenuti dalla valutazione della risposta di ciascun sito, espressi in termini di frequenza fondamentale e amplificazione, sono stati correlati con la rispettiva classe di sito per verificare l’attendibilità del parametro delle Vs30 come estimatore degli effetti di sito

Evidence for tWZ production in proton-proton collisions at √s=13 TeV in multilepton final states

Data availability - https://www.sciencedirect.com/science/article/pii/S0370269324003733?via%3Dihub#dav0001 [Release and preservation of data used by the CMS Collaboration as the basis for publications is guided by the CMS data preservation, re-use and open access policy (https://cms-docdb.cern.ch/cgi-bin/PublicDocDB/RetrieveFile?docid=6032&filename=CMSDataPolicyV1.2.pdf&version=2)]The first evidence for the standard model production of a top quark in association with a W boson and a Z boson is reported. The measurement is performed in multilepton final states, where the Z boson is reconstructed via its decays to electron or muon pairs. At least one W boson, associated or from top quark decay, decays leptonically, too. The analysed data were recorded by the CMS experiment at the CERN LHC in 2016–2018 in proton-proton collisions at √s=13 TeV, and correspond to an integrated luminosity of 138 fb−1. The measured cross section is 354±54(stat)±95(syst) fb, and corresponds to a statistical significance of 3.4 standard deviations.SCOAP

Search for new heavy resonances decaying to WW, WZ, ZZ, WH, or ZH boson pairs in the all-jets final state in proton-proton collisions at s\sqrt{s} = 13 TeV

A preprint version of this article is available at arXiv:2210.00043v2 [hep-ex], https://arxiv.org/abs/2210.00043v2 . Comments: Replaced with the published version. Added the journal reference and the DOI. All the figures and tables, including additional supplementary figures, can be found at https://cms-results.web.cern.ch/cms-results/public-results/publications/B2G-20-009 (CMS Public Pages). Report number: CMS-B2G-20-009, CERN-EP-2022-152.Data availability: see: https://cms-results.web.cern.ch/cms-results/public-results/publications/B2G-20-009 .A search for new heavy resonances decaying to WW, WZ, ZZ, WH, or ZH boson pairs in the all-jets final state is presented. The analysis is based on proton-proton collision data recorded by the CMS detector in 2016-2018 at a centre-of-mass energy of 13 TeV at the CERN LHC, corresponding to an integrated luminosity of 138 fb^{-1}. The search is sensitive to resonances with masses between 1.3 and 6 TeV, decaying to bosons that are highly Lorentz-boosted such that each of the bosons forms a single large-radius jet. Machine learning techniques are employed to identify such jets. No significant excess over the estimated standard model background is observed. A maximum local significance of 3.6 standard deviations, corresponding to a global significance of 2.3 standard deviations, is observed at masses of 2.1 and 2.9 TeV. In a heavy vector triplet model, spin-1 Z' and W' resonances with masses below 4.8 TeV are excluded at the 95% confidence level (CL). These limits are the most stringent to date. In a bulk graviton model, spin-2 gravitons and spin-0 radions with masses below 1.4 and 2.7 TeV, respectively, are excluded at 95% CL. Production of heavy resonances through vector boson fusion is constrained with upper cross section limits at 95% CL as low as 0.1 fb.SCOAP3

Measurement of the Higgs boson production via vector boson fusion and its decay into bottom quarks in proton-proton collisions at s \sqrt{s} = 13 TeV

A preprint version of the article is available at arXiv:2308.01253v2 [hep-ex], https://arxiv.org/abs/2308.01253v2 . Comments: Replaced with the published version. Added the journal reference and the DOI. All the figures and tables can be found at https://cms-results.web.cern.ch/cms-results/public-results/publications/HIG-22-009 (CMS Public Pages). Report number: CMS-HIG-22-009, CERN-EP-2023-110.A measurement of the Higgs boson (H) production via vector boson fusion (VBF) and its decay into a bottom quark-antiquark pair (bb¯) is presented using proton-proton collision data recorded by the CMS experiment at s√ = 13 TeV and corresponding to an integrated luminosity of 90.8 fb−1. Treating the gluon-gluon fusion process as a background and constraining its rate to the value expected in the standard model (SM) within uncertainties, the signal strength of the VBF process, defined as the ratio of the observed signal rate to that predicted by the SM, is measured to be μqqHHbb¯ = 1.01 +0.55−0.46. The VBF signal is observed with a significance of 2.4 standard deviations relative to the background prediction, while the expected significance is 2.7 standard deviations. Considering inclusive Higgs boson production and decay into bottom quarks, the signal strength is measured to be μincl.Hbb¯ = 0.99 +0.48−0.41, corresponding to an observed (expected) significance of 2.6 (2.9) standard deviations.SCOAP3, STFC; Marie-Curie program and the European Research Council and Horizon 2020 Gran

Search for new Higgs bosons via same-sign top quark pair production in association with a jet in proton-proton collisions at √s = 13 TeV

Data availability: Release and preservation of data used by the CMS Collaboration as the basis for publications is guided by the CMS policy as stated in “CMS data preservation, re-use and open access policy” available online at: https://cms-docdb.cern.ch/cgi-bin/PublicDocDB/RetrieveFile?docid=6032&filename=CMSDataPolicyV1.2.pdf&version=2 .A preprint of this article is available online at arXiv:2311.03261v2 [hep-ex] https://arxiv.org/abs/2311.03261v2 . Comments: Replaced with the published version. Added the journal reference and the DOI. All the figures and tables can be found at https://cms-results.web.cern.ch/cms-results/public-results/publications/TOP-22-010 (CMS Public Pages)A search is presented for new Higgs bosons in proton-proton (pp) collision events in which a same-sign top quark pair is produced in association with a jet, via the pp → tH/A → tt¯c and pp → tH/A → tt¯u processes. Here, H and A represent the extra scalar and pseudoscalar boson, respectively, of the second Higgs doublet in the generalized two-Higgs-doublet model (g2HDM). The search is based on pp collision data collected at a center-of-mass energy of 13 TeV with the CMS detector at the LHC, corresponding to an integrated luminosity of 138 fb−1. Final states with a same-sign lepton pair in association with jets and missing transverse momentum are considered. New Higgs bosons in the 200-1000 GeV mass range and new Yukawa couplings between 0.1 and 1.0 are targeted in the search, for scenarios in which either H or A appear alone, or in which they coexist and interfere. No significant excess above the standard model prediction is observed. Exclusion limits are derived in the context of the g2HDM.SCOAP3

Search for Higgs boson decays to a Z boson and a photon in proton-proton collisions at s \sqrt{s} = 13 TeV

A preprint version of the article is available at arXiv:2204.12945v2 [hep-ex], https://arxiv.org/abs/2204.12945v2 . Comments: Replaced with the published version. Added the journal reference and the DOI. All the figures and tables can be found at https://cms-results.web.cern.ch/cms-results/public-results/publications/HIG-19-014 (CMS Public Pages). Report number: CMS-HIG-19-014, CERN-EP-2022-019.Results are presented from a search for the Higgs boson decay H → Zγ, where Z → ℓ+ℓ− with ℓ = e or μ. The search is performed using a sample of proton-proton (pp) collision data at a center-of-mass energy of 13 TeV, recorded by the CMS experiment at the LHC, corresponding to an integrated luminosity of 138 fb^{−1}. Events are assigned to mutually exclusive categories, which exploit differences in both event topology and kinematics of distinct Higgs production mechanisms to enhance signal sensitivity. The signal strength μ, defined as the product of the cross section and the branching fraction [σ(pp → H)B(H → Zγ)] relative to the standard model prediction, is extracted from a simultaneous fit to the ℓ+ℓ−γ invariant mass distributions in all categories and is found to be μ = 2.4 ± 0.9 for a Higgs boson mass of 125.38 GeV. The statistical significance of the observed excess of events is 2.7 standard deviations. This measurement corresponds to σ(pp → H)B(H → Zγ) = 0.21 ± 0.08 pb. The observed (expected) upper limit at 95% confidence level on μ is 4.1 (1.8). The ratio of branching fractions B(H → Zγ)/B(H → γγ) is measured to be 1.5 +0.7−0.6, which agrees with the standard model prediction of 0.69 ± 0.04 at the 1.5 standard deviation level.SCOAP3

Measurements of the Higgs boson production cross section and couplings in the W boson pair decay channel in proton-proton collisions at s\sqrt{s} = 13 TeV

A preprint version of the article is available at arXiv:2206.09466v2 [hep-ex], https://arxiv.org/abs/2206.09466v2 . Comments: Replaced with the published version. Added the journal reference and the DOI. All the figures and tables can be found at httpS://cms-results.web.cern.ch/cms-results/public-results/publications/HIG-20-013 (CMS Public Pages). Report number: CMS-HIG-20-013, CERN-EP-2022-120.Production cross sections of the standard model Higgs boson decaying to a pair of W bosons are measured in proton-proton collisions at a center-of-mass energy of 13 TeV. The analysis targets Higgs bosons produced via gluon fusion, vector boson fusion, and in association with a W or Z boson. Candidate events are required to have at least two charged leptons and moderate missing transverse momentum, targeting events with at least one leptonically decaying W boson originating from the Higgs boson. Results are presented in the form of inclusive and differential cross sections in the simplified template cross section framework, as well as couplings of the Higgs boson to vector bosons and fermions. The data set collected by the CMS detector during 2016-2018 is used, corresponding to an integrated luminosity of 138 fb^−1. The signal strength modifier μ, defined as the ratio of the observed production rate in a given decay channel to the standard model expectation, is measured to be μ = 0.95 +0.10−0.09. All results are found to be compatible with the standard model within the uncertainties.SCOAP3