Simulations of the model showing different motility types. by Leonie van Steijn (10142786)

Video 1_v1_Clinical application of endoscopic surgery using a gasless unilateral transaxillary approach in the treatment of primary hyperparathyroidism.mp4 by Wan-Chen Zhang (13841521)

“…During a follow-up period of 3 to 36 months, a total of 1 patient in the open group experienced recurrence at 10 months after surgery and was treated non-surgically.…”

Dataset for WATP study: Willingness and ability to pay for breast cancer treatment among patients from Addis Ababa, Ethiopia: a cross-sectional study by Pablo Santos (7025705)

“…In contrast, a monthly income increase by 100 USD corresponds to a 17 % decrease of WATP (OR 0.83; 95% CI 0.70 to 0.99).…”

Table_1_Type 2 diabetes attributable to ambient particulate matter pollution: a global burden study from 1990 to 2019.DOCX by Yuyi Sha (18581944)

“…Conversely, regions with high SDI levels like High-income North America demonstrated decreasing trends.</p>Conclusion<p>This study reveals a significant increase in T2D worldwide as a result of APMP from 1990 to 2019, with a particular emphasis on its impact on men, the older adult, and regions with low to middle SDI levels. …”

Table 1_A national population-based study of mortality and risk factors in COVID-19-hospitalized patients in Spain (2020–2021).docx by José-Manuel Ramos-Rincón (10428656)

“…Hospitalization rates dropped from 697/100,000 people to 411/100,000, and in-hospital mortality (IHM) decreased from 16.2 to 11.5% (adjusted odds ratio [AOR]: 0.71, 95% CI: 0.70–0.73, p < 0.001). …”

Table_1_Identification and physiological activity of (methoxymethyl)triphenylphosphonium chloride as a new phytotoxin isolated from Rhizoctonia solani AG-3 TB.docx by Xinchun Li (551742)

“…The pure compound MMC treated at 20 μg/mL, 50 μg/mL, and 100 μg/mL can cause obvious necrosis on leaves, increase active oxygen species (AOS), decrease chlorophyll content, and damage cellular structure. …”

Fürth with translational diffusion fits MSD of model better than Fürth without translational diffusion. by Leonie van Steijn (10142786)

DataSheet_2_Radiotherapy Response Assessment of Multiple Myeloma: A Dual-Energy CT Approach With Virtual Non-Calcium Images.docx by Philipp Fervers (5616980)

“…</p>Results<p>Attenuation of LBLs decreased after RT depending on the time that had passed after irradiation [absolute thresholds for identification of irradiated LBLs 30.5–70.0 HU [best area under the curve [AUC] 0.75 (0.59–0.91)] and -77.0 to -22.5 HU [best AUC 0.85 (0.65–1.00)]/-50% and -117% to -167% proportional change of attenuation on conventional and VNCa images, respectively]. …”

DataSheet_2_Radiotherapy Response Assessment of Multiple Myeloma: A Dual-Energy CT Approach With Virtual Non-Calcium Images.docx by Philipp Fervers (5616980)

“…</p>Results<p>Attenuation of LBLs decreased after RT depending on the time that had passed after irradiation [absolute thresholds for identification of irradiated LBLs 30.5–70.0 HU [best area under the curve [AUC] 0.75 (0.59–0.91)] and -77.0 to -22.5 HU [best AUC 0.85 (0.65–1.00)]/-50% and -117% to -167% proportional change of attenuation on conventional and VNCa images, respectively]. …”

DataSheet_1_Radiotherapy Response Assessment of Multiple Myeloma: A Dual-Energy CT Approach With Virtual Non-Calcium Images.docx by Philipp Fervers (5616980)

“…</p>Results<p>Attenuation of LBLs decreased after RT depending on the time that had passed after irradiation [absolute thresholds for identification of irradiated LBLs 30.5–70.0 HU [best area under the curve [AUC] 0.75 (0.59–0.91)] and -77.0 to -22.5 HU [best AUC 0.85 (0.65–1.00)]/-50% and -117% to -167% proportional change of attenuation on conventional and VNCa images, respectively]. …”

DataSheet_1_Radiotherapy Response Assessment of Multiple Myeloma: A Dual-Energy CT Approach With Virtual Non-Calcium Images.docx by Philipp Fervers (5616980)

“…</p>Results<p>Attenuation of LBLs decreased after RT depending on the time that had passed after irradiation [absolute thresholds for identification of irradiated LBLs 30.5–70.0 HU [best area under the curve [AUC] 0.75 (0.59–0.91)] and -77.0 to -22.5 HU [best AUC 0.85 (0.65–1.00)]/-50% and -117% to -167% proportional change of attenuation on conventional and VNCa images, respectively]. …”

Acceptability, feasibility, and individual preferences of blood-based HIV self-testing in a population-based sample of adolescents in Kisangani, Democratic Republic of the Congo by Serge Tonen-Wolyec (4752156)

“…The correct interpretation decreased significantly when adolescents had no formal education or attended primary school as compared to those currently attending university (37.0% <i>versus</i> 100%; adjusted OR: 0.01 [95% CI: 0.004–0.03]). …”

Evidence for <em>STAT4</em> as a Common Autoimmune Gene: rs7574865 Is Associated with Colonic Crohn's Disease and Early Disease Onset by Jürgen Glas (107816)

“…For two other <em>STAT4</em> variants, there was a trend towards protection against CD susceptibility (rs7568275, p = 0.058, OR 0.86 [95% CI 0.74–1.00]; rs10174238, p = 0.057, OR 0.86 [95% CI 0.75–1.00]). …”

Pathogen load in control and rough box migratory colonies. by Maggie Shanahan (17879479)

Image4_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image5_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image9_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image12_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image2_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”

Image6_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO₂ and fS₂) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”