Search alternatives:
significant progressive » significant progress (Expand Search), significant protective (Expand Search), significant processes (Expand Search)
progressive decrease » progressive decline (Expand Search)
changes decrease » largest decrease (Expand Search), change increases (Expand Search)
larger decrease » marked decrease (Expand Search)
significant progressive » significant progress (Expand Search), significant protective (Expand Search), significant processes (Expand Search)
progressive decrease » progressive decline (Expand Search)
changes decrease » largest decrease (Expand Search), change increases (Expand Search)
larger decrease » marked decrease (Expand Search)
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341
Box plot displaying the distributions of the deconvolution derived proportions of cell types.
Published 2024Subjects: -
342
Spearman correlation of age with proportions of cell types in men, for each brain region.
Published 2024Subjects: -
343
Analysis of the significantly different metabolomic features.
Published 2025“…<b>(B)</b> Volcano plot highlighting the significantly different metabolomic features. The red dots represent the features with significantly increased intensity, and the purple dots represent the features with significantly decreased intensity. …”
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344
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Lipidomic analysis of epidermis using LC-IMS-CID-MS reveals major changes in CKO// epidermis.
Published 2025“…(D) Proportion of significantly changed lipids by lipid class in CKO vs K5Cre epidermis. …”
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Changes in the hemoglobin.
Published 2025“…The leukocyte and neutrophil counts of the patients in the bone pain group were significantly higher than those of the patients in the no bone pain group, P(WBC) = 0.001, P(ANC) = 0.002.…”
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eQTL analysis of significant SNPs.
Published 2025“…These significant associations could be explained by the change in downstream NO signaling, supporting the relationship between the investigated traits and vascular function. …”
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Graded loading creep stress loading level.
Published 2025“…The results reveal that (1) freeze-thaw cycles exert a significant influence on the rock’s creep behavior, with axial strain, instantaneous strain, and creep strain increasing progressively with the number of freeze-thaw cycles; (2) dual-fractured rock samples with varying fracture angles exhibit distinct differences in creep phenomena, where increased fracture angles result in pronounced increases in instantaneous and creep strains, and higher horizontal stress levels lead to greater strain generation; (3) all rock samples with different pre-existing fractures exhibit rock bridge breakthrough during creep failure, and the variation in fracture angle affects the failure mode; (4) and the long-term strength of the rock varies with changes in fracture angle and freeze-thaw cycle frequency, showing an increasing trend with greater fracture angles but a rapid decrease with increasing freeze-thaw cycles. …”
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357
Schematic diagram of rock samples.
Published 2025“…The results reveal that (1) freeze-thaw cycles exert a significant influence on the rock’s creep behavior, with axial strain, instantaneous strain, and creep strain increasing progressively with the number of freeze-thaw cycles; (2) dual-fractured rock samples with varying fracture angles exhibit distinct differences in creep phenomena, where increased fracture angles result in pronounced increases in instantaneous and creep strains, and higher horizontal stress levels lead to greater strain generation; (3) all rock samples with different pre-existing fractures exhibit rock bridge breakthrough during creep failure, and the variation in fracture angle affects the failure mode; (4) and the long-term strength of the rock varies with changes in fracture angle and freeze-thaw cycle frequency, showing an increasing trend with greater fracture angles but a rapid decrease with increasing freeze-thaw cycles. …”
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358
Rock mechanics testing machine.
Published 2025“…The results reveal that (1) freeze-thaw cycles exert a significant influence on the rock’s creep behavior, with axial strain, instantaneous strain, and creep strain increasing progressively with the number of freeze-thaw cycles; (2) dual-fractured rock samples with varying fracture angles exhibit distinct differences in creep phenomena, where increased fracture angles result in pronounced increases in instantaneous and creep strains, and higher horizontal stress levels lead to greater strain generation; (3) all rock samples with different pre-existing fractures exhibit rock bridge breakthrough during creep failure, and the variation in fracture angle affects the failure mode; (4) and the long-term strength of the rock varies with changes in fracture angle and freeze-thaw cycle frequency, showing an increasing trend with greater fracture angles but a rapid decrease with increasing freeze-thaw cycles. …”
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