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Climate prediction is of great significance to the prevention of drought and flood. "Ground-synoptic" map is a method for short-term climate prediction. The main content of this method is "Geothermal Vortex"(GV). Therefore, some characteristics of 3.2 m soil temperature anomaly (hereinafter abbreviated as T′ 3.2 m) and GV are analyzed by using the data of monthly soil temperature at the depth of 3.2 m from 1980 to 2017 in China. Results show that there are regional differences in the frequency of positive anomaly. Overall, there are more positive anomalies in southern China and fewer in Western China. Soil temperature anomaly has good memory, the shortest being 5 months and the longest being nearly 2 years. Moreover, results show the nonuniform distribution of memory duration and decreases from northwest to southeast as a whole. Statistical analysis of GV shows that the average life cycle of each GV is 9.7 months, with an average horizontal scale of 604 km and a characteristic scale of 2.4 cm/s. Spatially, the GV scale is largest in Northwest, with a horizontal scale of 1087 km, and the GV appear most frequently in North China. The central location of GV is uneven, mainly in the central area with strong crustal activity and large absolute vertical deformation rate or in the high value area of soil heat flow. [ABSTRACT FROM AUTHOR]

Purpose: Microvascular invasion (MVI) is a critical factor in predicting the recurrence and prognosis of hepatocellular carcinoma (HCC) after liver transplantation (LT). However, there is a lack of reliable preoperative predictors for MVI. The purpose of this study is to evaluate the potential of an 18F-FDG PET/CT-based nomogram in predicting MVI before LT for HCC. Methods: 83 HCC patients who obtained 18F-FDG PET/CT before LT were included in this retrospective research. To determine the parameters connected to MVI and to create a nomogram for MVI prediction, respectively, Logistic and Cox regression models were applied. Analyses of the calibration curve and receiver operating characteristic (ROC) curves were used to assess the model's capability to differentiate between clinical factors and metabolic data from PET/CT images. Results: Among the 83 patients analyzed, 41% were diagnosed with histologic MVI. Multivariate logistic regression analysis revealed that Child–Pugh stage, alpha-fetoprotein, number of tumors, CT Dmax, and Tumor-to-normal liver uptake ratio (TLR) were significant predictors of MVI. A nomogram was constructed using these predictors, which demonstrated strong calibration with a close agreement between predicted and actual MVI probabilities. The nomogram also showed excellent differentiation with an AUC of 0.965 (95% CI 0.925–1.000). Conclusion: The nomogram based on 18F-FDG PET/CT metabolic characteristics is a reliable preoperative imaging biomarker for predicting MVI in HCC patients before undergoing LT. It has demonstrated excellent efficacy and high clinical applicability. [ABSTRACT FROM AUTHOR]

There are many types of atmospheric heat engines in land-air systems. The accurate definition, calculation and interpretation of the efficiency of atmospheric heat engines are key to understanding energy transfer and transformation of land-air systems. The atmosphere over the Qinghai-Tibet Plateau (QTP) in summer can be regarded as a positive heat engine. The study of the heat engine efficiency is helpful to better understand land-air interaction and thermal-dynamic processes on the QTP. It also provides a new perspective to explain the impact of the QTP on the climate of China, East Asia and even the world. In this paper, we used MOD08 and ERA5 reanalysis data to calculate the atmospheric heat engine efficiency, surface heat source and atmospheric heat source on the QTP in summer (May to September) from 2000 to 2020. The average atmospheric heat engine efficiency on the QTP in summer from 2000 to 2020 varies between 1.2% and 1.5%, which is less than 1.6%; the heat engine efficiency in summer is higher than that in June, July and August; the Qaidam Basin is the region with the highest atmospheric heat engine efficiency, followed by the western QTP. The mean surface heat source on the QTP in summer from 2000 to 2020 is 96.0 W m−2, the atmospheric heat source is 90.7 W m−2, and the release of precipitation condensation latent heat is the most important component of the atmospheric heat source on the QTP in summer. There is a strong and significant positive correlation between the atmospheric heat engine efficiency and the surface heat source on the QTP in summer. The precipitation con densation latent heat is the most important component of the atmospheric heat source in summer and can reflect the precipitation process. There is a strong and significant negative correlation between the atmospheric heat engine efficiency and the atmo spheric heat source on the QTP in summer. [ABSTRACT FROM AUTHOR]

There has been much debate on whether color categories affect how we perceive color. Recent theories have put emphasis on the role of top-down influence on color perception that the original continuous color space in the visual cortex may be transformed into categorical encoding due to top-down modulation. To test the influence of color categories on color perception, we adopted an RSVP paradigm, where color stimuli were presented at a fast speed of 100 ms per stimulus and were forward and backward masked by the preceding and following stimuli. Moreover, no explicit color naming or categorization was required. In theory, backward masking with such a short interval in a passive viewing task should constrain top-down influence from higher-level brain areas. To measure any potentially subtle differences in brain response elicited by different color categories, we embedded a sensitive frequency-tagging-based EEG paradigm within the RSVP stimuli stream where the oddball color stimuli were encoded with a different frequency from the base color stimuli. We showed that EEG responses to cross-category oddball colors at the frequency where the oddball stimuli were presented was significantly larger than the responses to within-category oddball colors. Our study suggested that the visual cortex can automatically and implicitly encode color categories when color stimuli are presented rapidly. [ABSTRACT FROM AUTHOR]

[Display omitted] • ZIF-8 derived ZnO@NC can anchor Ru nanoparticles to create Ru-O-Zn interface. • Ru/ZnO@NC achieved complete conversion and 99.2% GVL yield in LA hydrogenation. • Ru/ZnO@NC achieved excellent reaction activity with a TOF of 6032 h−1 at 40 °C. • Reaction mechanism of LA hydrogenation to GVL has been revealed by DFT calculation. • Ru-O-Zn interface can remarkably decline activation energy of rate-determining step. Highly efficient synthesis of valuable γ-valerolactone (GVL) by levulinic acid (LA) hydrogenation is of interest for biomass refinery, but it suffers from great challenge to design highly active Ru-based catalyst at low temperature. ZIF-8 derived ZnO@NC nanocomposite can firmly anchor Ru nanoparticles to create strong Ru-ZnO interfacial structure, as revealed by characterization techniques and DFT calculations. By optimizing Ru content and ZnO particle size, Ru/ZnO@NC achieved excellent reaction activity with a turnover frequency (TOF) of 6032 h−1 at low temperature of 40 °C, which is never reported before. After etching the accessible ZnO, the TOF value was significantly declined to 125 h−1 on Ru/ZnO@NC-HF owing to the lack of effective Ru-ZnO interface. DFT calculation results demonstrate that the Ru-ZnO interfacial structure can facilitate the activation of intermediate CH 3 CHOCH 2 CH 2 COOH* and remarkably decline the activation energy barrier of rate-determining step (CH 3 CHOCH 2 CH 2 COOH + H = HPA) from 1.28 eV to 0.82 eV, thus leading to excellent activity of LA hydrogenation at low temperature. [ABSTRACT FROM AUTHOR]

It is well accepted that tidal wetland vegetation performs a significant amount of water filtration for wetlands. However, there is currently little information on how various wetland plants remove nitrogen (N) and phosphorus (P) and how they differ in their denitrification processes. This study compared and investigated the denitrification and phosphorus removal effects of three typical wetland plants in the Yangtze River estuary wetland (Phragmites australis , Spartina alterniflora , and Scirpus mariqueter), as well as their relevant mechanisms, using an experimental laboratory-scale horizontal subsurface flow constructed wetland (CW). The results showed that all treatment groups with plants significantly reduced N pollutants as compared to the control group without plants. In comparison to S. mariqueter (77.2–83.2%), S. alterniflora and P. australis had a similar total nitrogen (TN)removal effectiveness of nearly 95%. With a removal effectiveness of over 99% for ammonium nitrogen (NH 4 +-N), P. australis outperformed S. alterniflora (95.6–96.8%) and S. mariqueter (94.6–96.5%). The removal of nitrite nitrogen (NO 2 −-N)and nitrate nitrogen (NO 3 −-N)from wastewater was significantly enhanced by S. alterniflora compared to the other treatment groups. Across all treatment groups, the removal rate of PO 4 3--P was greater than 95%. P. australis and S. alterniflora considerably enriched more 15N than S. mariqueter , according to the results of the 15N isotope labeling experiment. While the rhizosphere and bulk sediments of S. alterniflora were enriched with more simultaneous desulfurization-denitrification bacterial genera (such as Paracoccus , Sulfurovum , and Sulfurimonas), which have denitrification functions, the rhizosphere and bulk sediments of P. australis were enriched with more ammonia-oxidizing archaea and ammonia-oxidizing bacteria. As a result, compared to the other plants, P. australis and S. alterniflora demonstrate substantially more significant ability to remove NH 4 +-N and NO 2 −-N/NO 3 −-N from simulated domestic wastewater. [Display omitted] • CWs with plants removed substantially more N than controls. • Plant groups enriched more denitrifying bacteria in plant rhizospheres than controls. • The Spartina and Phragmites groups removed much more N than the Scirpus group. • Phragmites have the highest NH 4 +_N removal rate due to enrichment of AOA and AOB. • CWs with Spartina had the highest removal rate for NO 3 −_N and NO 2 −_N. [ABSTRACT FROM AUTHOR]

Highlights Although 3D printing technology has been widely applied in fabrication of polymer composite, yet, it still exhibits low mechanical performance, restricting its application in structural materials. Herein, a new 3D printing polymer composite composed of carbon fiber and polyamide12 (PA12) is fabricated and subsequently treated by microwave treatment. It is found that the tensile strength and modulus of 3D printing CF/PA12 composite with microwave treatment are improved by 23.8% and 10.2% compared with the original specimen, respectively. Moreover, a new mechanism of mechanical reinforcement is investigated and proposed by nanoindentation and 3D X‐ray computed tomography. The work does not only confirm formation of 3D printing CF/PA12 composite with good mechanical properties, but also proposes a new mechanism of microwave treatment effect on 3D printing polymer composite based on carbon fiber. A new 3D printing CF/PA12 composite based on microwave treatment is developed. The 3D printing composite exhibits good mechanical properties. A new mechanism of mechanical reinforcement is proposed. [ABSTRACT FROM AUTHOR]

Owing to their attractive optical and chiroptical properties, chiral metal halide perovskites have received increasing attention, with potential applications ranging from photonics and optoelectronics to spintronics. Metal halide perovskite nanocrystals with either intrinsic or extrinsic (e.g., chiral ligand‐induced) chirality have been reported recently, and the interplay between these two types of chirality has yet to be addressed. Herein, the inversion and tuning of excitonic optical activity is reported in intrinsically chiral perovskite nanoplatelets, originating from interactions between their structural chirality (due to the spontaneously formed screw dislocations in the crystalline lattice) and the surface enantiomeric (R/S) chiral ligands R/S‐phenylethylammonium bromide. Through post‐preparative exposure of the perovskite nanoplatelets to these R/S ligands of varied contents, either chiral ligand‐induced intrinsic chirality inversion or negative and positive Cotton effects induced by the ligands via electronic coupling between the ligand and the nanoplatelets are identified. These findings deepen understanding of the modulation of excitonic optical activity in chiral perovskites and can guide the rational design and synthesis of novel chiral materials. [ABSTRACT FROM AUTHOR]

Aims: The objective of this study was to investigate the response of the iron (Fe) (hydr-) oxides-bounded organic carbon (Fe-OC) process, characterized by the interaction of Fe (hydr-) oxides with soil organic carbon (SOC) in coastal wetlands, to different flooding and soil salinity conditions.The study concentrated on Scirpus mariqueter in the Yangtze River Estuary, analyzing variations in various forms of Fe (hydr-) oxides, Fe-OC, and Fe redox cycling bacteria in the rhizosphere and bulk soils under diverse flooding and soil salinity conditions.The study found that during the growing season, the levels of crystalline (FeDH) and amorphous (FeHH) Fe (hydr-) oxides were elevated compared to the non-growing season. In the rhizosphere, around 80% of SOC was associated with Fe (hydr-) oxides, significantly higher than the 50% in bulk soil. Elevated areas in the tidal flat exhibited increased FeDH, FeHH, and total Fe content in rhizosphere soils. Soils with higher salinity had more Fe (hydr-) oxides compared to low salinity soils. Furthermore, salinity reduced the prevalence of Gallionella and Geobacter, which are conducive to the preservation of FeHH, leading to a greater FeHH-OC ratio in the total SOC.The bond between Fe (hydr-) oxides and SOC in soils becomes stronger during the growth season of S. mariqueter. The Fe-OC process’s reaction to environmental factors like salinity and flooding profoundly affects the dynamics of SOC in wetland ecosystems. These findings are essential for wetland management, emphasizing the need to preserve these ecosystems for their role in SOC sequestration.Methods: The objective of this study was to investigate the response of the iron (Fe) (hydr-) oxides-bounded organic carbon (Fe-OC) process, characterized by the interaction of Fe (hydr-) oxides with soil organic carbon (SOC) in coastal wetlands, to different flooding and soil salinity conditions.The study concentrated on Scirpus mariqueter in the Yangtze River Estuary, analyzing variations in various forms of Fe (hydr-) oxides, Fe-OC, and Fe redox cycling bacteria in the rhizosphere and bulk soils under diverse flooding and soil salinity conditions.The study found that during the growing season, the levels of crystalline (FeDH) and amorphous (FeHH) Fe (hydr-) oxides were elevated compared to the non-growing season. In the rhizosphere, around 80% of SOC was associated with Fe (hydr-) oxides, significantly higher than the 50% in bulk soil. Elevated areas in the tidal flat exhibited increased FeDH, FeHH, and total Fe content in rhizosphere soils. Soils with higher salinity had more Fe (hydr-) oxides compared to low salinity soils. Furthermore, salinity reduced the prevalence of Gallionella and Geobacter, which are conducive to the preservation of FeHH, leading to a greater FeHH-OC ratio in the total SOC.The bond between Fe (hydr-) oxides and SOC in soils becomes stronger during the growth season of S. mariqueter. The Fe-OC process’s reaction to environmental factors like salinity and flooding profoundly affects the dynamics of SOC in wetland ecosystems. These findings are essential for wetland management, emphasizing the need to preserve these ecosystems for their role in SOC sequestration.Results: The objective of this study was to investigate the response of the iron (Fe) (hydr-) oxides-bounded organic carbon (Fe-OC) process, characterized by the interaction of Fe (hydr-) oxides with soil organic carbon (SOC) in coastal wetlands, to different flooding and soil salinity conditions.The study concentrated on Scirpus mariqueter in the Yangtze River Estuary, analyzing variations in various forms of Fe (hydr-) oxides, Fe-OC, and Fe redox cycling bacteria in the rhizosphere and bulk soils under diverse flooding and soil salinity conditions.The study found that during the growing season, the levels of crystalline (FeDH) and amorphous (FeHH) Fe (hydr-) oxides were elevated compared to the non-growing season. In the rhizosphere, around 80% of SOC was associated with Fe (hydr-) oxides, significantly higher than the 50% in bulk soil. Elevated areas in the tidal flat exhibited increased FeDH, FeHH, and total Fe content in rhizosphere soils. Soils with higher salinity had more Fe (hydr-) oxides compared to low salinity soils. Furthermore, salinity reduced the prevalence of Gallionella and Geobacter, which are conducive to the preservation of FeHH, leading to a greater FeHH-OC ratio in the total SOC.The bond between Fe (hydr-) oxides and SOC in soils becomes stronger during the growth season of S. mariqueter. The Fe-OC process’s reaction to environmental factors like salinity and flooding profoundly affects the dynamics of SOC in wetland ecosystems. These findings are essential for wetland management, emphasizing the need to preserve these ecosystems for their role in SOC sequestration.Conclusions: The objective of this study was to investigate the response of the iron (Fe) (hydr-) oxides-bounded organic carbon (Fe-OC) process, characterized by the interaction of Fe (hydr-) oxides with soil organic carbon (SOC) in coastal wetlands, to different flooding and soil salinity conditions.The study concentrated on Scirpus mariqueter in the Yangtze River Estuary, analyzing variations in various forms of Fe (hydr-) oxides, Fe-OC, and Fe redox cycling bacteria in the rhizosphere and bulk soils under diverse flooding and soil salinity conditions.The study found that during the growing season, the levels of crystalline (FeDH) and amorphous (FeHH) Fe (hydr-) oxides were elevated compared to the non-growing season. In the rhizosphere, around 80% of SOC was associated with Fe (hydr-) oxides, significantly higher than the 50% in bulk soil. Elevated areas in the tidal flat exhibited increased FeDH, FeHH, and total Fe content in rhizosphere soils. Soils with higher salinity had more Fe (hydr-) oxides compared to low salinity soils. Furthermore, salinity reduced the prevalence of Gallionella and Geobacter, which are conducive to the preservation of FeHH, leading to a greater FeHH-OC ratio in the total SOC.The bond between Fe (hydr-) oxides and SOC in soils becomes stronger during the growth season of S. mariqueter. The Fe-OC process’s reaction to environmental factors like salinity and flooding profoundly affects the dynamics of SOC in wetland ecosystems. These findings are essential for wetland management, emphasizing the need to preserve these ecosystems for their role in SOC sequestration. [ABSTRACT FROM AUTHOR]

• Roots of P. australis enhance Fe-OC coupling, especially in low-tide areas. • Rhizosphere Fe-OC fluctuates seasonally, higher in low-tide flats in the growing season. • Plant growth stages significantly influence Fe-OC dynamics in tidal flat wetlands. • Significant rise in FeRB abundance in low-tide flat during non-growing season. • Seasonal shifts in microbial communities affect Fe-OC content in tidal sediments. As sea levels rise, coastal tidal wetlands are increasingly threatened by flooding and salt stress, highlighting the importance of iron (Fe) (hydr-) oxides in soil for stabilizing organic carbon (OC). This study focuses on Phragmites australis , common in the Yangtze River Estuary, exploring the interplay between OC and Fe (hydr-) oxides in the rhizosphere of P. australis across various seasons and elevations. It also examines microbial community shifts in the Fe oxidation–reduction cycle. Results show that in the non-growing season (January), Fe (hydr-) oxides and total organic carbon (TOC) levels in the rhizosphere soil of high-tide P. australis are significantly higher than during the growing season (August), with a notable increase in Fe oxide-bound OC (Fe-OC). The content of Fe-OC in tidal wetland soil fluctuates with plant growth stages and elevation. Notably, during the growing season, the Fe-OC content in the rhizosphere of low-tide P. australis is markedly higher than in high-tide areas, reversing in the non-growing season. The presence of P. australis roots is found to significantly enhance the accumulation and coupling of Fe (hydr-) oxides and OC, especially in low-tide areas compared to bare flats. This coupling is affected by the organic matter contributed by roots, microbial metabolism, and redox conditions of the soil. The study also highlights how plant and microbial metabolism regulate the response of rhizosphere Fe-OC across different tidal flat elevations. In low-tide environments during the non-growing season, the prevalence of Fe-reducing bacteria results in decreased Fe-OC content, while in high-tide areas, increased organic matter input boosts complexed Fe-OC formation. Overall, this study emphasizes the significance of plant metabolism in understanding the impact of sea level rise on Fe-OC stores in tidal wetlands, a vital factor for comprehending C cycling mechanisms and assessing C sequestration potential under future climate change scenarios. [ABSTRACT FROM AUTHOR]

[Display omitted] • A novel extractant resin DtBuCH18C6@CG-71 was successfully prepared with simple and low-cost method. • DtBuCH18C6@CG-71 exhibited remarkable separation ability of Sr(II) even in high concentration HNO 3 (3–12 mol/L). • DtBuCH18C6@CG-71 possessed great acid, irradiation and thermal resistance stability. • DtBuCH18C6@CG-71 can adeptly sequesters and recovers Sr(II) from wastewater via an automated separation system. Effective removal of radioactive 90Sr is crucial for both management of spent nuclear fuel and recovery of radioactive strontium resources, while it's still a great challenge due to the presence of high acid levels and intense radiation. Herein, a novel porous resin (DtBuCH18C6@CG-71) were synthesized by introducing 4′,4″(5″)-di- tert -butyldicyclohexano-18-crown-6 onto CG-71 resin using vacuum impregnation. The DtBuCH18C6@CG-71 resin maintains superior adsorption abilities in extreme conditions, including high acid resistance (3–12 mol/L HNO 3), substantial γ-irradiation (200 kGy 60Co), and elevated temperatures (50–100 ℃). Impressively, even when exposed to a high concentration of matrix ions (59 elemental ions), the Sr(II) adsorption ratio onto DtBuCH18C6@CG-71 resin remains near 100 % even in highly acidic condition, which performance outpaces most of commercial resins. Dynamic column tests using an automated separation system further confirmed the superior ability of DtBuCH18C6@CG-71 in term of extracting Sr(II) from wastewater. Given its impressive features, cost-effectiveness, and scalability, DtBuCH18C6@CG-71 resin holds promising potential for 90Sr disposal in nuclear wastewater. [ABSTRACT FROM AUTHOR]