Jointly Exploring Client Drift and Catastrophic Forgetting in Dynamic Learning

Federated and Continual Learning have emerged as potential paradigms for the robust and privacy-aware use of Deep Learning in dynamic environments. However, Client Drift and Catastrophic Forgetting are fundamental obstacles to guaranteeing consistent performance. Existing work only addresses these problems separately, which neglects the fact that the root cause behind both forms of performance deterioration is connected. We propose a unified analysis framework for building a controlled test environment for Client Drift -- by perturbing a defined ratio of clients -- and Catastrophic Forgetting -- by shifting all clients with a particular strength. Our framework further leverages this new combined analysis by generating a 3D landscape of the combined performance impact from both. We demonstrate that the performance drop through Client Drift, caused by a certain share of shifted clients, is correlated to the drop from Catastrophic Forgetting resulting from a corresponding shift strength. Correlation tests between both problems for Computer Vision (CelebA) and Medical Imaging (PESO) support this new perspective, with an average Pearson rank correlation coefficient of over 0.94. Our framework's novel ability of combined spatio-temporal shift analysis allows us to investigate how both forms of distribution shift behave in mixed scenarios, opening a new pathway for better generalization. We show that a combination of moderate Client Drift and Catastrophic Forgetting can even improve the performance of the resulting model (causing a "Generalization Bump") compared to when only one of the shifts occurs individually. We apply a simple and commonly used method from Continual Learning in the federated setting and observe this phenomenon to be reoccurring, leveraging the ability of our framework to analyze existing and novel methods for Federated and Continual Learning

Lymphologischer Kompressionsverband oder Standardbehandlung mit Kältepackung zur Schwellungsreduktion nach Knietotalprothesen-Operation

Background: After total knee arthroplasty (TKA) efficient control and reduction of postoperative edema is of great importance. Aim: The aim of this pilot study (EKNZ 2014 - 225 DRKS00006271) was to investigate the effectiveness of multi-layer compression therapy (MLCT) to reduce edema in the early period after surgery compared to the standard treatment with Cool Pack. Methods: In this randomized controlled pilot trial, sixteen patients after TKA were randomized into an intervention group (IG) or a control group (CG). Circumferential measurements were used to assess edema. Secondary outcomes were range of motion (ROM), pain (numeric rating scale, NRS) and function as measured with the fast Self Paced Walking Test (fSPWT). Results: Clinically relevant differences in edema reduction between the two groups were found in the early postoperative period and at the six weeks follow up. Six days postoperatively the group time interaction (IE) in favor of the IG were −3.8 cm (95 % CI: −5.1; −2.4) when measured 10 cm proximal to the joint space and −2.7 cm (CI: −4.1; −1.3) when measured 5 cm proximally. We further observed differences in secondary outcomes in favor of the CG. Six days postoperatively the IE for knee flexion was –8.3 ° (CI: −22.0; 5.4) and for the fSPWT it was 12.8 seconds (CI: −16.4; 41.3). Six weeks postoperatively these differences diminished. Conclusions: The findings suggest that MLCT could be an alternative treatment to reduce postoperative edema in patients after total knee arthroplasty. Eventually possible negative effects on early knee flexion and function must be considered

Empfehlung(en) "Verschleiß und Verklebung im Lockergestein" - ein erster Ausblick

Der Tagungsband "Vorträge der Fachsektionstage Geotechnik - Interdisziplinäres Forum 2023, Congress Centrum Würzburg, 12. - 13. September 2023" erscheint im Open Access und ist hier kostenfrei abrufbar: https://www.dggt.de/index.php?option=com_content&view=article&id=397%3Atagungsband-fstg&catid=45%3Apublikationen&Itemid=6

Origin of abundant moonmilk deposits in a subsurface granitic environment

22 páginas.-- 6 figuras.-- 115 referencias.-- Additional Supporting Information may be found in the online version of this article: http://dx.doi.org/10.1111/sed.12431Subsurface granitic environments are scarce and poorly investigated. A multi‐disciplinary approach was used to characterize the abundant moonmilk deposits and associated microbial communities coating the granite walls of the 16th Century Paranhos spring water tunnel in Porto city (north‐west Portugal). It is possible that this study is the first record of moonmilk in an urban subsurface granitic environment. The morphology and texture, mineralogical composition, stable isotope composition and microbial diversity of moonmilk deposits have been studied to infer the processes of moonmilk formation. These whitish secondary mineral deposits are composed of very fine needle‐fibre calcite crystals with different morphologies and density. Calcified filaments of fungal hyphae or bacteria were distinguished by field emission scanning electron microscopy. Stable isotope analysis revealed a meteoric origin of the needle‐fibre calcite, with an important contribution of atmospheric CO2, soil respiration and urn:x-wiley:00370746:media:sed12431:sed12431-math-0001 from weathering of Ca‐bearing minerals. The DNA‐based analyses revealed the presence of micro‐organisms related to urban contamination, including Actinobacteria, mainly represented by Pseudonocardia hispaniensis, Thaumarchaeota and Ascomycota, dominated by Cladosporium. This microbial composition is consistent with groundwater pollution and contamination sources of the overlying urban area, including garages, petrol stations and wastewater pipeline leakage, showing that the Paranhos tunnel is greatly perturbed by anthropogenic activities. Whether the identified micro‐organisms are involved in the formation of the needle‐fibre calcite or not is difficult to demonstrate, but this study evidenced both abiotic and biogenic genesis for the calcite moonmilk in this subsurface granitic environment.The authors acknowledge the Spanish Ministry of Economy, Industry and Competitiveness (MINEICO, project CGL2011-2569) and the Portuguese Foundation for Science and Technology, FCT (UID/GEO/04035/2013, UID/ECI/04028/2013, PEst-OE/CTE/UI0098/2011) and the LABCARGA| ISEP re-equipment program (IPP-ISEP|PAD’2007/ 08) for financial support. AZM thanks MINEICO for the ‘Juan de la Cierva – Incorporación’ postdoctoral contract (IJCI-2014-20443). PMMS thanks the Spanish Ministry of Science and Innovation for his contract associated with the ‘Research Programme in Technologies for the Assessment and Conservation of Cultural Heritage’ (TCP CSD2007-0005Peer reviewe