Barely Significant

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However, when we examined the average severity scores across ADI-R items for each ASD symptom category using a heatmap cluster plot (Supplementary Data 5), we found that the severity of symptoms in each ASD symptom category did not differ substantially among the transcriptome-based subgroups, although Microarray_sub3 showed a trend towards higher severity compared to the other groups.
The Likert 5-point scoring method is utilized, where 1 indicates “never,” 2 indicates “rarely,” 3 indicates “occasionally,” 4 indicates “often,” and 5 indicates “always.” compassion satisfaction represents a positive dimension reflecting a positive trend, while job burnout and secondary traumatic stress represent negative dimensions reflecting a negative trend.
Compared to μ a , the average reduced scattering coefficient ranges from 0.088 to 0.25 mm-1, and the μ′ s spectrum shows a valley at the wavelength corresponding to strong absorption in the μ a spectrum (980 nm), and only exhibits a decreasing trend with increasing wavelength from 550 to 1050 nm.When calculating optical properties using the IAD method, the light loss within the integrating sphere is not taken into account, which results in an overestimation of the absorption coefficient and underestimation of the reduced scattering coefficient.
In analyses stratified by age ( p = 0.07), sex ( p = 0.73), BMI ( p = 0.44) and hypertension ( p = 0.46) there were no significant interactions, although for age the p-value for interaction was approaching significance with a suggestive stronger association for current vs. never smokers (3.07, 2.14–4.41 vs. 1.77, 1.12–2.79) among participants aged ≥ 60 vs. those aged < 60 years (Supplemental Table 7).
From 2000 to 2010, the carbon storage distribution was relatively uniform, and in 2020, it was high in the middle of the region and low in the surrounding areas; water conservation services showed an increasing trend from north to south during the study period, which is consistent with the spatial pattern of high precipitation in the south and low precipitation in the north.
For the nonfrozen condition, the initial values of the exponential functions between the variation in the wind erosion rate and the wind speed of desert soil show an increasing trend, and the ratios of the functions decrease steadily; that is, with increasing moisture content, the degree of skewness of each function decreases, and the degree of influence of the wind speed on the wind erosion rate decreases.