Showing 4,421 - 4,440 results of 16,260 for search '(( 50 ((we decrease) OR (mean decrease)) ) OR ( 5 ((ng decrease) OR (nn decrease)) ))', query time: 0.62s Refine Results
  1. 4421

    Experimental Study on Water-in-Oil Emulsion Stability Induced by Asphaltene Colloids in Heavy Oil by Fatemeh Mahmoudi Alemi (10312321)

    Published 2025
    “…Under HPHT conditions, stability varied significantly, with the 75:25 oil−water ratio exhibiting temporary stability, while 50:50 and 25:75 ratios consistently produced unstable emulsions. …”
  2. 4422
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  7. 4427
  8. 4428
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  11. 4431
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  14. 4434

    Proteomic and Targeted Metabolomic Studies on a Silkworm Model of Parkinson’s Disease by Feifei Zhu (480283)

    Published 2022
    “…Proteomics analysis revealed a major downregulation of nearly 50 structural proteins constituting cuticles and microfilaments, indicating mechanical damage in the silkworm tissues. …”
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  18. 4438

    Satellite-Based Monitoring of Methane Emissions from China’s Rice Hub by Ruosi Liang (14018604)

    Published 2024
    “…Process-based modeling further suggests that this practice can lead to a reduction of methane emissions by more than 50% compared to continuous flooding of rice paddies and natural wetlands.…”
  19. 4439

    Kinetics of Quartz Dissolution in Natural Silicate Melts and Dependence of SiO<sub>2</sub> Diffusivity on Melt Composition by Yi Yu (28902)

    Published 2019
    “…An understanding of the kinetics of quartz dissolution and growth may provide insight into magma crystallization and constraints on magma dynamics and cooling rates. We have carried out quartz dissolution experiments in rhyolitic (0.1 wt % H<sub>2</sub>O, ∼73 wt % SiO<sub>2</sub>) and basaltic (∼0.35 wt % H<sub>2</sub>O, and ∼50 wt % SiO<sub>2</sub>) melts at 1300–1600 °C and 0.5 GPa using piston cylinder apparatus. …”
  20. 4440

    Kinetics of Quartz Dissolution in Natural Silicate Melts and Dependence of SiO<sub>2</sub> Diffusivity on Melt Composition by Yi Yu (28902)

    Published 2019
    “…An understanding of the kinetics of quartz dissolution and growth may provide insight into magma crystallization and constraints on magma dynamics and cooling rates. We have carried out quartz dissolution experiments in rhyolitic (0.1 wt % H<sub>2</sub>O, ∼73 wt % SiO<sub>2</sub>) and basaltic (∼0.35 wt % H<sub>2</sub>O, and ∼50 wt % SiO<sub>2</sub>) melts at 1300–1600 °C and 0.5 GPa using piston cylinder apparatus. …”