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To analyze the influence of professional identity and academic efficacy on the professional attitude of higher vocational nursing students.

The Wangjiadashan Cu–Au deposit is a vein‐type deposit controlled by the secondary faults of the Wushan Fault zone in the Suizao area of Hubei Province. Three hydrothermal stages are identified, namely, (I) barren quartz stage, (II) the quartz‐sulphide stage, and (III) quartz‐carbonate stage. Six types of fluid inclusions occur in quartz: (a) liquid‐rich aqueous fluid inclusions (L + V), (b) vapour‐rich aqueous‐carbonic fluid inclusions (V + L), (c) water‐rich aqueous‐carbonic fluid inclusions (L + V + CO2), (d) CO2‐rich aqueous‐carbonic fluid inclusions (V + L + CO2), (e) pure carbonic fluid inclusions (pure CO2), and (f) daughter mineral‐bearing multiphase inclusions (S‐type) with three subclasses (S1, S2, and S3 subtype). Two types of fluid inclusions occur in calcite: (a) liquid‐rich aqueous fluid inclusions (L + V) and (b) pure carbonic fluid inclusions (pure CO2). The S‐type fluid inclusions include halite (NaCl), calcite (CaCO3), and chalcopyrite (CuFeS2). The fluid system is composed of CO2–NaCl–H2O. The homogenization temperatures of the three stages are 295°C to 390°C, 245°C to 280°C, and 200°C to 241°C, with salinities of 7.3–19.8 wt% NaCl equiv. (except for several high values of 33.8 to 44.3 wt% NaCl equiv.), 7.7–13.7 wt% NaCl equiv., and 5.6–10.1 wt% NaCl equiv., respectively. Fluid immiscibility occurred in stage I that accounts for the high‐salinity fluids, but the dominant ore precipitation occurred afterward during temperature drop. In situ sulphur isotope analysis indicates a δ34S value around 0 (+1.1% to +2.2%) for the chalcopyrite, suggesting that the sulphur likely derived from the deep‐seated magma. Pyrites show δ34S values from −0.5‰ to +6.5‰ in stage II, from +0.7‰ to +6.6‰ in country rock of marble, but significantly higher from +12.8‰ to +21.7‰ in country rock of greenschist. These results indicate the sulphur for pyrite in stage II likely derived from the mixing of deep‐seated magma and country rocks. From stages I to II, a slightly increase of δD (from −86‰ and −73‰ to −59‰ and −56‰) and a decrease of δ18O (from 8.9‰ and 7.1‰ to 1.3‰ and 3.4‰) indicate that an increasing involvement of meteoric water. The carbon isotopes of fluid inclusions CO2 in quartz of stage I (−11.0‰ to −13.0‰) indicate a major magmatic or metamorphic carbon source mixed with minor sedimentary sourced carbon, but a major organic carbon source (−32.0‰ to −35.0‰) for stage II fluids. In conclusion, the Wangjiadashan Cu–Au deposit belongs to the orogenic type. [ABSTRACT FROM AUTHOR]

It has been supposed that the interplay of elasticity and activity plays a key role in triggering the non-equilibrium behaviors in biological systems. However, the experimental model system is missing to investigate the spatiotemporally dynamical phenomena. Here, a model system of an active chain, where active eccentric-disks are linked by a spring, is designed to study the interplay of activity, elasticity, and friction. Individual active chain exhibits longitudinal and transverse motions; however, it starts to self-rotate when pinning one end and self-beat when clamping one end. In addition, our eccentric-disk model can qualitatively reproduce such behaviors and explain the unusual self-rotation of the first disk around its geometric center. Furthermore, the structure and dynamics of long chains were studied via simulations without steric interactions. It was found that a hairpin conformation emerges in free motion, while in the constrained motions, the rotational and beating frequencies scale with the flexure number (the ratio of self-propelling force to bending rigidity), χ, as ∼(χ)4/3. Scaling analysis suggests that it results from the balance between activity and energy dissipation. Our findings show that topological constraints play a vital role in non-equilibrium synergy behaviors., (© 2024 Author(s). Published under an exclusive license by AIP Publishing.)

Objective: To evaluate the efficacy of cognitive behavioral therapy for depression in advanced schistosomiasis patients., Methods: A total of 60 advanced schistosomiasis patients with major depressive disorder were divided into a combination therapy group (30 cases) who received sertraline plus cognitive behavior therapy and a monotherapy group (30 cases) who received sertraline only. Before the treatment and at the 1st, 2nd, 4th, 8th week after the treatment, the efficacy and safety were assessed with the HAMD17 item score and the related factor points and TESS. The effective rate, side effect rate and relapse rate in six months were calculated and compared between the two groups., Results: At the end of 8th week after the treatment, the total scores of HAMD, factor scores of cognitive impairment, retardation factor scores and sleep disturbance factor scores in the 2 groups were statistically decreased compared with those before the treatment (P < 0.05 or P < 0.01). The factor scores in the combined therapy group were lower than those in the monotherapy group. The effective rate in the combination therapy group was 86.7% (26/30), and it was significantly higher than that in the monotherapy group (56.7%, 17/30), (chi2 = 6.65, P < 0.05). The doses of the drug were lower in the combination therapy group than those in the monotherapy group (t = 2.25, P < 0.05). Within six months, the relapse rate was 13.3% in the combination therapy group, and it was significantly lower than that in the monotherapy group (46.7%) (chi2 = 7.937, P < 0.025). The side effect rate was 23.3% in the combination therapy group and that was 26.7% in the monotherapy group, and there was no statistically significant difference between the two groups (P > 0.05)., Conclusion: The combination therapy (drug combined with cognitive behavioral therapy) is effective in advanced schistosomiasis patients with depression, and it also can reduce the amount of medication and the relapse.