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In the present work, a carbon/cobalt composite was prepared and evaluated for adsorption of ecologically harmful tannic acid (TA). The composite was prepared by simply mixing phenolic resin with ZIF-67 and following by carbonization. TEM and SEM images showed that ZIF-67 was etched by phenolic resin and cobalt nanoparticles were formed and evenly distributed in carbon. Macroporous structure was generated between the carbonized phenolic resin and ZIF-67. N2 adsorption-desorption isotherms results exhibited that the composite also had both micro- and meso-pores (average pore size of 5 nm) with a high surface area of 393 m2 g−1. Porous structure and evenly distributed cobalt nanoparticles facilitated the diffusion and adsorption of TA due to the formation of the complex between TA macromolecules and cobalt. The highest observed adsorption amount was as high as 2778 mg g−1, significantly higher than that of the carbon prepared from carbonization of phenolic resin (205 mg g−1) and ZIF-67 (1375 mg g−1). The carbon composite material is easy to recover and reuse due to the magnetic property. The reuse experiment also showed high stability of the composite. All of the results indicated a great potential of the developed carbon composite material in wastewater treatment in the industry.

Purpose Stereotactic ablative body radiotherapy (SABR) represents an exciting, tolerable, and highly effective form of radiotherapy. Ongoing investigations into the interactions between radiotherapy and the immune system have uncovered new mechanisms that can be exploited to improve efficacy. We determined whether baseline or posttreatment immune parameters could predict disease control and toxicity in stage I non–small-cell lung cancer (NSCLC) patients treated with SABR. Patients and Methods Peripheral blood samples were collected from 62 patients 24 hours before treatment and within 4 weeks after treatment for lymphocyte subset count analysis. All peripheral blood samples were analyzed by flow cytometry. Associated parameters were evaluated to determine their association with progression-free survival (PFS) and symptomatic radiation pneumonitis (grade 2 or higher). The survival rates were estimated with Kaplan-Meier and multivariable analyses using binary logistic regression analysis or a Cox proportional hazards model. Results At a median follow-up time of 36.0 months, the PFS rates for years 1, 2, and 3 were 91.0%, 82.5%, and 48.9%, respectively. The multivariable logistic regression analysis showed that only proportion of lung receiving 20 Gy of radiotherapy (odds ratio = 1.41; 95% confidence interval, 1.05-1.87; P = .023) and mean lung dose (odds ratio = 2.02; 95% confidence interval, 1.16-3.53; P = .016) were associated with symptomatic radiation pneumonitis (grade 2 or higher). Moreover, the immune parameters had no predictive value. In the multivariable Cox regression analysis, an elevated posttreatment cytotoxic CD8+ T-cell level was an independent prognostic factor for longer PFS in stage I NSCLC (hazard ratio, 1.16; 95% confidence interval, 1.01-1.28; P = .01). Conclusion A higher posttreatment cytotoxic CD8+ T-cell level was predictive of better PFS in stage I NSCLC patients receiving SABR. Thus, enhancing tumor antigen-specific cellular immunity by combining radiotherapy and immunotherapy might be a crucial strategy for improving survival in these patients.

Few reconstructions of sea-surface temperature (SST) have focused on seasonal and interannual variability, two major components of the global climate system, due to the limited temporal resolution of proxies. This study presents a combined 228-year-long, monthly resolved strontium to calcium ratios (Sr/Ca) record covering the period of 2070–1740 a BP (years before 1950 CE (Common Era)) extracted from three U-series-based sub-fossil Porites corals located on the Xisha Islands, northern South China Sea (SCS). The composite time series allowed for accurate assessment of the natural range of SST variations during snapshots of the Roman Warm Period (RWP). Reconstructed SST revealed that the RWP was characterized by cooler conditions compared with the 20th century, consistent with climatic variations in the western Pacific and East Asia. The amplitude of SST seasonality was within the modern range, except for a lower value at 1980–1928 a BP. Interannual variability associated with El Nino–Southern Oscillation (ENSO) activity was enhanced by 39% relative to 1980–2014 CE. The results of the sliding window demonstrate that ENSO variability persistently strengthened during 2070–2010 a BP, followed by an overall fluctuating attenuation during 1980–1928 a BP. Then, the trends of rising first before descending twice during 1852–1800 a BP appeared. Furthermore, ENSO activity played a leading role in steering short-term changes in SST seasonality in the northern SCS, manifested as stronger ENSO activity with more frequent El Nino events and decreased SST seasonality. Considering that the frequency of extreme ENSO events may strengthen in the future under global warming, the climate in the northern SCS might become more variable and complex.