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mean decrease » a decrease (Expand Search)
we decrease » _ decrease (Expand Search), a decrease (Expand Search), teer decrease (Expand Search)
ng decrease » _ decrease (Expand Search), a decrease (Expand Search), gy decreased (Expand Search)
nn decrease » _ decrease (Expand Search), a decrease (Expand Search), gy decreased (Expand Search)
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4421
Experimental Study on Water-in-Oil Emulsion Stability Induced by Asphaltene Colloids in Heavy Oil
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. …”
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4422
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4423
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4424
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4425
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4426
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4427
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4428
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4429
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4430
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4431
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4432
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4433
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4434
Proteomic and Targeted Metabolomic Studies on a Silkworm Model of Parkinson’s Disease
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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4435
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4436
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4437
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4438
Satellite-Based Monitoring of Methane Emissions from China’s Rice Hub
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.…”
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4439
Kinetics of Quartz Dissolution in Natural Silicate Melts and Dependence of SiO<sub>2</sub> Diffusivity on Melt Composition
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. …”
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4440
Kinetics of Quartz Dissolution in Natural Silicate Melts and Dependence of SiO<sub>2</sub> Diffusivity on Melt Composition
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. …”