Showing 3,961 - 3,980 results of 21,342 for search '(( significant decrease decrease ) OR ( significant ((anti decrease) OR (a decrease)) ))', query time: 0.67s Refine Results
  1. 3961

    Dynamic Covalent Chemistry Enabled Closed-Loop Recycling of Thermally Modified Polymer Membrane by Ching Yoong Loh (17863097)

    Published 2025
    “…Thermal and mechanical characterizations confirmed the great stability of the membranes, with the Diels–Alder reaction enabling depolymerization and reformation of the network without causing significant degradation. Additionally, the RFMs were recycled the third time, maintaining the fluxes (752 to 823 LMH) from the previous generation with a slight decrease in separation efficiency in dichloromethane-water emulsion separation (98.3 to 97%). …”
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  3. 3963

    Regression situation of each cross-section. by Puzhen An (21169189)

    Published 2025
    “…Furthermore, as the coarse particle content rises, the strata loss rate tends to decrease gradually. The final settlement curve, calculated using the method that considers changes in coarse particle content, is closer to the measured values. …”
  4. 3964

    Statistical Table of Formation Loss Rate <i>V1.</i> by Puzhen An (21169189)

    Published 2025
    “…Furthermore, as the coarse particle content rises, the strata loss rate tends to decrease gradually. The final settlement curve, calculated using the method that considers changes in coarse particle content, is closer to the measured values. …”
  5. 3965

    Fitting Results for Each Operating Condition. by Puzhen An (21169189)

    Published 2025
    “…Furthermore, as the coarse particle content rises, the strata loss rate tends to decrease gradually. The final settlement curve, calculated using the method that considers changes in coarse particle content, is closer to the measured values. …”
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  7. 3967

    Upper-crust thermal evolution of the Patagonian Precordillera basement (Argentina): insights from fission track, (U-Th)/He thermochronology and geodynamic significance by Paulo Marcos (7459064)

    Published 2025
    “…This first stage might have resulted from coupled tectonothermal processes consisting of extensional faulting and high-temperature gradient. Subsequently, a relatively fast temperature decrease (2.75–5°C/My) for the late Early Cretaceous to Paleocene is likely related to a compressive stage associated with the growth of the early Andean Orogen. …”
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