Alterations of Ceramides, Acylcarnitines, GlyceroLPLs, and Amines in NSCLC Tissues by Jie Zhang (64655)

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Demographic information of participants. by Zixia Bu (21475019)

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Difference in various variables with different PA level. by Zixia Bu (21475019)

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Characterization and difference in various variables with different PA level. by Zixia Bu (21475019)

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Correlation results between PA and different table variables. by Zixia Bu (21475019)

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Correlation heatmap between physical activity and individual variables. by Zixia Bu (21475019)

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Cross-lagged panel model based on physical activity, aggressive behavior and Chinese language learning. by Zixia Bu (21475019)

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Cross-lagged panel model consistency test based on physical activity, aggressive behavior and Chinese language learning. by Zixia Bu (21475019)

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Comparison of the fit of multiple cluster analyses of the cross-lagged panel model. by Zixia Bu (21475019)

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Statistical association (P < 0.10) between background factors and dog owners’ attitude (AT), subjective norms (SN) and perceived behavioral control (PBC) that were significantly as... by Fentahun Mengie (20862454)

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Basic features of microtopography. by Qingping Gou (22641045)

“…The results showed that: the difference of shallow soil moisture in different microtopographies on a slope surface was not significant, the difference of deep soil moisture was significant, and the soil moisture overuse was the largest in the gully (GU), amounting to 386.36 mm, and the smallest in the ephemeral gully (EG) (131.02 mm); the GU, the sink hole (SH), and the scarp (SC) showed a trend of decreasing and then increasing with the increase of soil depth, and the platform (PL) has little overall trend of change in soil moisture with the increase of soil depth, and the soil moisture of US and EG shows the trend of “decreasing-then increasing-then decreasing” with the increase of soil depth. …”

Soil bulk density of different microtopographies. by Qingping Gou (22641045)

“…The results showed that: the difference of shallow soil moisture in different microtopographies on a slope surface was not significant, the difference of deep soil moisture was significant, and the soil moisture overuse was the largest in the gully (GU), amounting to 386.36 mm, and the smallest in the ephemeral gully (EG) (131.02 mm); the GU, the sink hole (SH), and the scarp (SC) showed a trend of decreasing and then increasing with the increase of soil depth, and the platform (PL) has little overall trend of change in soil moisture with the increase of soil depth, and the soil moisture of US and EG shows the trend of “decreasing-then increasing-then decreasing” with the increase of soil depth. …”

Effects of LTS on G_s. by Lifeng Guo (17320116)

Effects of LTS on T_r. by Lifeng Guo (17320116)

Effects of LTS on pollen viability. by Lifeng Guo (17320116)

Effects of LTS on MDA. by Lifeng Guo (17320116)

Effects of LTS on proline. by Lifeng Guo (17320116)

Effects of LTS on EL. by Lifeng Guo (17320116)

Effects of LTS on SOD. by Lifeng Guo (17320116)

Effects of LTS on CAT. by Lifeng Guo (17320116)