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With the acceleration of China's urbanization process, in order to meet the needs of new urban users' source-source interaction and multi-energy complementation, this paper proposes a new urban energy interconnection LAN design and construction ideas, from distributed photovoltaic systems, energy storage systems, phase change heat storage. The system and the AC-DC grid interconnection and intercommunication four specific aspects of the design and construction plan, given the electric vehicle charging and discharging interactive operation and phase change heat storage and ground source heat pump combined heating two typical application scenarios. [ABSTRACT FROM AUTHOR]

This study proposes a model for predicting tropical cyclone (TC) intensity evolution by utilizing the conditional Wasserstein generative adversarial network with gradient penalty (CWGAN-GP) for TC-related risk assessment. The TC intensity evolution is treated as a random variable, which is the output of a nonlinear system conditioned on a series of input random variables that characterize both the TC state (e.g., translation speed and potential intensity) and environment (e.g., vertical wind shear and ocean mixed layer depth). To represent the high-dimensional non-Gaussian probabilistic characteristics, the system is modeled by the CWGAN-GP and calibrated concerning the dataset of 1010 historical TCs from the western North Pacific basin. The over-ocean and overland branches of the model are calibrated separately and then merged. The suitability of the established model is validated by comparing the predicted TC intensity to the observations and the results of existing models such as those based on linear regression. Numerical results indicate that the proposed model successfully replicates the probabilistic properties such as the non-Gaussian marginal distribution of the intensity change and the input-output joint distribution and moments between the TC intensity and predictors, which the linear regression model cannot provide. Further application examples are also carried out by using the model to simulate the evolution of historical TC events and the extreme TC intensities in Southern China, demonstrating its potential role in the TC hazard assessment. • A deep-learning model for predicting tropical cyclone intensity evolution is proposed. • The CWGAN-GP is used to model TC intensity change every 6 h conditioned on environmental variables. • Numerical results demonstrate that the proposed model can replicate the probabilistic properties of TC intensity. [ABSTRACT FROM AUTHOR]

• A framework of TC wind hazard assessment based on the probability density evolution method integrated with the change-of-measure technique is proposed. • The high efficiency of the proposed framework in assessing the TC wind hazard at multiple locations is validated. • The sensitivity of the TC wind hazard to controlling random variables is analyzed. • The TC wind hazard on the southeast coast of China is assessed. The tropical cyclone (TC) wind hazard assessment formulates a change-of-random-variable problem, which maps the probability space of controlling parameters to that of the TC-induced wind. This study presents a framework for analyzing the TC wind hazard based on the probability density evolution method (PDEM) integrated with the change of probability measure (COM). It is advantageous in the problem of assessing the TC wind hazards at multiple locations over the traditional approach because a common set of representative deterministic solutions of physical equations can be re-used for all locations rather than solving a separate set of solutions at each location. The proposed method is applied to estimate the wind hazard on the Chinese southeast coastline. The common representative deterministic points are selected by the generalized-F-discrepancy-based method with the probability distributions of controlling parameters at Shantou. Based on the COM, the geographical dependence of probabilistic characteristics is represented by changing the assigned probability. The PDEM is incorporated to evaluate the propagation of randomness from the input-controlling parameters to the TC-induced surface wind. The comparison to the Monte Carlo simulation demonstrates the high efficiency and accuracy of the proposed method. [ABSTRACT FROM AUTHOR]

The Taihua metamorphic complex exposes in the southern Trans-North China Orogen (TNCO) and records at least three episodes of magmatism. The Shanxian TTG gneisses obtained at 2.54–2.48 Ga have high SiO 2 , variable Mg# with high (La/Yb) N and Sr/Y ratios (15.08–93.26 with average of 37.31 and 7.33–115.05 with average of 49.59, respectively). They show negative Nb and Ta but positive Zr and Hf anomalies with low Nb/Ta and Gd/Yb, and high Zr/Hf and Zr/Sm ratios (4.97–18.8, 1.92–6.37, 23.71–50.26, and 29.18–75.23, respectively), and have positive ε Hf (t) values (+1.7 to +7.9) and ε Nd (t) values (+0.72 to +2.55), indicating that they were possibly produced by partial melting of lower crust derived from metasomatized lithospheric mantle with the residue of minor garnet. The Sihe granitic gneisses recorded at 2.35–2.30 Ga are enriched in silica, Al 2 O 3 contents (13.59–15.33), K 2 O/Na 2 O ratios (1.13–1.7), defined as high-Al TTG. They exhibit high Sr/Y, Zr/Sm and Zr/Hf ratios and low Nb/Ta and Gd/Yb ratios (44.71–83.09, 47.79–62.58, 36.05–37.43, 12.04–16.36, and 2.95–3.68, respectively) with negative Eu anomaly. Combined with Hf and Nd isotopes (−2.5 to +4.7 and −0.74 to +0.36), the Sihe granitic gneiss was possibly generated from partial melting of lower crust with minor ancient material contributions, leaving residual amphibole and minor garnet in the source. The Muce monzonitic gneisses emplaced at 2.17–2.16 Ga have high Mg#, Ni and Cr contents, constant Sr/Y and (La/Yb) N (42.39–50.33, 19.8–41.4, 33.6–74.2, 31.32–34.14, and 15.32–16.7, respectively), with relatively low and constant Dy/Yb ratio (1.82–1.85). Together with Hf and Nd isotopes (−6.5 to −0.9 and −2.07 to −2.86), the Muce monzonitic gneisses might be derived from partial melting of Neoarchean pre-existing crustal materials, possibly in an arc setting. It is therefore found that four episodes of crustal growth and/or reworking in the southern segment of the TNCO have occurred at 2.85–2.72 Ga, 2.57–2.48 Ga, 2.35–2.30 Ga and 2.2–2.0 Ga, respectively, likely to connect with the subduction–collision between the Eastern and Western Blocks along the TNCO in the North China Craton. [ABSTRACT FROM AUTHOR]

[Display omitted] • VNS spectroscopy are used to investigate mineralogy and geochemistry of drill cores rapidly and non-destructively. • K-M values are negatively correlated with Fe 2 O 3 , Fe3+/Fe2+, TOC, and carbonates, and positively with clay and kaolinite. • Redox is found to be the key U enrichment factor, and kaolinite and organic matter may cause limited U enrichment. The Qianjiadian deposit is the first late Mesozoic–Cenozoic sandstone-type uranium deposit discovered in the Songliao Basin, northeast China. It remains uncertain whether high-temperature hydrothermal fluid or low-temperature groundwater dominated the mineralization process that led to uranium enrichment in this deposit. We investigated the gamma ray intensity and semi-quantitative mineralogical and geochemical characteristics of drill cores from the Qianjiadian deposit. A total of 60 gamma ray anomalies were identified; most of these anomalies are associated with negative Fe 2 O 3 and Fe3+/Fe2+ anomalies, four are associated with positive total organic carbon (TOC) anomalies, and none are associated with positive carbonate (calcite + dolomite) anomalies. The absence of positive carbonate anomalies, together with low kaolinite crystallinities, rules out the influence of high-temperature fluid on uranium enrichment. The dominant negative Fe 2 O 3 and Fe3+/Fe2+ anomalies and the occurrence of pyrite in thin section and gray-red sandstone and native sulfur in some U-rich drill cores indicate that redox reactions in low-temperature groundwater may have been the principal control on uranium enrichment. In addition, two gamma ray anomalies are associated with positive TOC, Fe 2 O 3 , and Fe3+/Fe2+ anomalies and another two are associated only with positive kaolinite anomalies, suggesting that carbonaceous debris and kaolinite could also cause limited uranium enrichment. [ABSTRACT FROM AUTHOR]

In this article, a new typhoon hazard analysis method is presented by introducing the probability density evolution theory. In the suggested method, the randomness in the typhoon occurrence is represented by the combination of a homogeneous Poisson process and a joint probability density function for both the typhoon genesis time and the genesis position. Then a set of physical models, including a typhoon intensity model, a typhoon track model and a boundary layer wind field model, is introduced to describe the typhoon process. The typhoon intensity model with high efficiency is used to simulate the evolution of typhoon intensity given the environmental variables. The typhoon motion is simulated by the beta-advection model where the steering flow is the linear combination of the large-scale flows at 850 hPa and 250 hPa, and the beta drift is solved from the non-divergent barotropic vorticity equation. At last, the typhoon induced surface wind at the interested engineering site is calculated with the help of a three-dimensional non-linear boundary layer wind field model. On the basis of the above physical models, the generalized density evolution equation is adopted to solve the probability distribution of the annual maximum typhoon surface wind speeds. The typhoon surface wind speeds associated with specified recurrence intervals are estimated consequently. As an example, the typhoon hazard at ten selected cities on the southeast coast of China is assessed. The surface wind records from the observation stations are collected to estimate the cumulative distribution function of the annual maximum wind and are compared to the analyzed results. The good comparison between the historical records and the analyzed results demonstrates the adequacy of the proposed method. • Physical models are used to generate the synthetic history of typhoon. • The probability density evolution theory is used to investigate the propagation of randomness. • The proposed method is used to assess the typhoon hazard of several cities on the southeast coast of China. [ABSTRACT FROM AUTHOR]

Typhoon track model plays an important role in typhoon wind hazard estimation. In this article, a beta-advection model is developed to simulate the typhoon track over the western North Pacific (WNP). The typhoon motion is driven by two effects, the steering flow and beta drift. The steering flow is modeled as the linear combination of the 850 ​hPa height large scale flow and 250 ​hPa height large scale flow. The spatially varying weights are estimated from the 20th Century Reanalysis dataset for each 5 ​° ​× ​5 ​° square in WNP. The large scale flows at both heights are simulated as multivariate random process based on the fact that the energy spectrum of the geostrophic turbulence follows a "-3" power law. As another driving force of typhoon motion, the beta drift is calculated by solving the non-divergent barotropical vorticity equation. The adequacy of the present model is validated by the comparison between the typhoon translation velocity inferred from the best-track dataset and that simulated by the model. Finally, integrated with an intensity model, the beta-advection model is used to analyze the statistics of typhoon key parameters and typhoon wind hazard along the southeast coast of mainland China. • The typhoon motion is modeled by combining the large scale steering flow and the beta drift effect. • The kinetic analysis is used to remove the typhoon structure in the reanalysis data. • The beta advection typhoon track model is used to assess the typhoon hazard along the southeast coast of China. [ABSTRACT FROM AUTHOR]

Tropical cyclone intensity model is one of the most important components in the tropical cyclone hazard assessment. In this study, the tropical cyclone fast intensity model, which uses features of the surrounding large-scale environment to predict the evolution of the tropical cyclone intensity, is used to estimate the typhoon wind hazard in the southeast coast of China. The fast tropical cyclone intensity model that consists of an intensity dynamic equation and a moisture dynamic equation is first validated for the western North Pacific basin. The coefficients in the moisture dynamic equation are calibrated by minimizing the error between the model and the observation from the best track dataset. The model is then integrated with a typhoon track model and a parametric radial wind profile to estimate the 50-year and 100-year recurrence-interval surface wind speeds at selected sites. Three different models for the radius of the maximum wind are considered in this analysis. Accordingly, surface wind records are utilized to estimate 50-year and 100-year recurrence-interval winds. The comparison shows a good agreement between the results of the model and that of the surface observations, which validates the adequacy of the model for engineering applications in the southeast coast of China. • The tropical cyclone fast intensity model is validated with the best track dataset. • The tropical cyclone fast intensity model is used for typhoon hazard analysis for southeast coast of China. • The influence of using different models for the radius of maximum wind on the estimated typhoon hazard is investigated. [ABSTRACT FROM AUTHOR]

• Metamorphic time was determined by SIMS U–Th–Pb dating of metapelitic monazite. • The peak metamorphism occurred at ~1.95–1.83 Ga. • Subduction and collision of the TNCO occurred between 1.97 Ga and 1.80 Ga. As a key accessory mineral in metapelite, monazite forms in the metamorphic event and therefore, places important direct constraint on the timing of the tectono-metamorphic event. In this study, we investigate four representative metapelites from different metamorphic terranes in the central-south Trans-North China Orogen (TNCO), applying secondary ion mass spectrometry (SIMS) U–Th–Pb dating on monazite. The dating results reveal that monazite collected from the Huashan, Luoning, Zanhuang and Wutai metamorphic complexes record the metamorphic ages of ~ 1.83 Ga, ~ 1.95 Ga, ~ 1.85 Ga and ~ 1.91 to 1.83 Ga, respectively. Combined with the literature data of metamorphic geochronology on the discrete terranes within the TNCO, it is suggested that the amalgamation between the Western and Eastern Blocks of the North China Craton along the nearly NS-trending TNCO stared as earlier as ~ 1.97 Ga and continued to as late as ~ 1.80 Ga, which was in fact a long-lived tectono-metamorphic event. [ABSTRACT FROM AUTHOR]

Metamorphic evolution and geochronology of pelitic granulites were reported for the first time in the Taihua metamorphic complex, Mts. Huashan area, southern segment of the trans-North China Orogen (TNCO). Three generations of metamorphic mineral assemblages are recognized: (1) the prograde metamorphic mineral assemblages (M 1 ) are represented by mineral inclusions within the garnet porphyroblasts; (2) the metamorphic peak assemblage (M 2 ) are the garnet porphyroblasts and minerals in the matrix (biotite + orthopyroxene + plagioclase + quartz + K-feldspar + ilmenite + zircon + magnetite); and (3) the retrograde metamorphic mineral assemblages (M 3 ) are represented by the symplectic assemblages around the garnet porphyroblasts, resulted from decomposition reactions between garnet rims and neighboring minerals in the matrix. Calculated by both conventional thermobarometry and pseudosection modeling in the NCKFMASHT system using the Perple_X technique, the P–T conditions of these three metamorphic stages are constrained to be of 4–5 kbar/520–530 °C for the M 1 stage, 6.8–8.6 kbar/730–810 °C for the M 2 stage and 4.1–6.4 kbar/570–740 °C for the M 3 stage, respectively. The derived clockwise P–T paths imply that the Mts. Huashan terrane involved in the subduction and subsequent collision between the Eastern and Western Blocks of the North China Craton (NCC) along the Palaeoproterozoic Trans-North China Orogen (TNCO). High resolution SIMS U–Pb dating of metamorphic zircons reveals the metamorphic ages of 1.85–1.82 Ga. Combined with geochronological data from the literature, it is concluded that the tectonothermal evolution between the Eastern and Western Blocks started as early as ∼1.97 Ga and lasted as late as 1.80 Ga. Furthermore, the eastern Taihua complex records older metamorphic ages and higher peak metamorphic pressures than those of the western Taihua complex, possibly suggesting an eastward subduction model for the TNCO. [ABSTRACT FROM AUTHOR]

Highlights: [•] Clockwise ITD P–T paths were retrieved from the Mts. Huashan amphibolites. [•] U–Pb geochronology of metamorphic zircons demonstrates the metamorphism occurred during ca. 1.96–1.80Ga. [•] Metamorphism of the southernmost Trans-North China Orogen started earlier and lasted longer than other terranes in the TNCO. [ABSTRACT FROM AUTHOR]

• Garnet-bearing mafic granulites occur as lenses within TTG gneiss. • These mafic granulites contain three to four generations of mineral assemblages. • They record clockwise P-T paths with ITD and subsequent near IBC segments. • The metamorphic peak occurred at ∼1.85 Ga. Garnet-bearing mafic granulites occur as lenses within TTG gneiss or metapelite in the Fuping Complex, middle Palaeoproterozoic Trans-North China Orogen. They are composed mainly of garnet, clinopyroxene, orthopyroxene, hornblende, plagioclase, quartz and accessary zircon and titanite. Four stages of metamorphic mineral assemblages have been found in these mafic granulites: (a) the prograde assemblages (M1) are inclusions preserved in the garnet porphyroblasts, including clinopyroxene, hornblende, plagioclase and quartz; (b) the metamorphic peak assemblages (M2) consist of garnet porphyroblasts plus matrix minerals clinopyroxene + orthopyroxene + hornblende + plagioclase + quartz + zircon + titanite; (c) the first retrograde assemblages (M3) are represented by clinopyroxene + orthopyroxene + plagioclase + quartz symplectites rimming the garnets; and (4) the final retrograde assemblages (M4) are hornblende + plagioclase + quartz symplectites rimming or adjacent to the garnets. The retrieved metamorphic P-T paths pass from 530–600 °C/6.5–7.0 kbar (M1) through 680–820 °C/7.2–11.7 kbar (M2) to 730–760 °C/3.2–3.9 kbar (M3) and finally to 600–640 °C/3.2–3.7 kbar (M4). All the P-T paths of the mafic granulites are clockwise, two of these even contain near isothermal decompression (ITD) and subsequent near isobaric cooling (IBC) segments. SHRIMP U-Pb dating of metamorphic zircons of the mafic granulites yields a mean weighted age of ∼1849 ± 9Ma, which is consistent with the metamorphic time of surrounding TTG gneisses. Therefore, the Fuping Complex records the collision event between the Eastern and Western Blocks of the North China Craton that led to the final assembly of this craton during the late Paleoproterozoic. [ABSTRACT FROM AUTHOR]

[Display omitted] • ZIF-90 nanoparticles with different particle sizes were synthesized. • pH- and α-amylase-responsive nanocarriers were successfully prepared. • β-CD-NH 2 surface coating reduced the photodegradation of indoxacarb. • IDC@ZIF-90-CD was able to disrupt the intestinal cells of red imported fire ants. • IDC@ZIF-90-CD affected amino acid metabolic pathways in red imported fire ants. The invasion area of red imported fire ants (RIFAs) in China continues to expand due to factors such as ecological changes and human activities, and the resulting damage is becoming increasingly severe. The development of smart nanopesticides that respond to environmental stimuli response with precisely controlled release has great potential in improving insecticidal effects. In this work, a smart pH and α-amylase dual stimuli-responsive pesticide delivery system was constructed by combining mono-(6-amino-6-deoxy)-β-cyclodextrin (β-CD-NH 2) with zeolitic imidazole skeleton-90 (ZIF-90) nanoparticles (IDC@ZIF-90-CD) loaded with indoxacarb. The average particle size of the prepared IDC@ZIF-90-CD was 249 nm, and the loading efficiency was 18.43%. The β-CD-NH 2 coating on the surface of nanoparticles reduced the photodegradation of indoxacarb and prevented the premature release of the active ingredient. In vitro release kinetics showed that IDC@ZIF-90-CD rapidly released IDC under acidic and amylase conditions, consistent with the oral and intestinal environment of RIFAs. The results of bioactivity tests showed that IDC@ZIF-90-CD enhanced the toxicity of IDC toward RIFAs by increasing feeding and damaging intestinal cells. The mortality rate of the IDC@ZIF-90-CD-treated group was significantly higher than that of the IDC EC-treated group at 72 h. The nontargeted metabolomic results showed that IDC@ZIF-90-CD affected the metabolism of RIFAs by interfering with the metabolic pathways of six amino acids and one amino acid transport carrier, whereas IDC EC interfered with only two of these amino acid metabolic pathways. Overall, this work provides insight into the effective control of RIFA damage for sustainable pest management. [ABSTRACT FROM AUTHOR]