Background: To demonstrate the real-word situation of burdens that are attributed to the risk factor of high low-density lipoprotein cholesterol (LDL-C) at the global, regional, national levels, among different age groups and between genders.Methods: We analyzed data from the Global Burden of Disease study 2019 related to global deaths, disability-adjusted life years (DALYs), summary exposure value (SEV), average annual percentage change (AAPC), and observed to expected ratios (O/E ratios) attributable to high LDL-C from 1990 to 2019.Results: Globally, in 2019, the total numbers of deaths and DALYs attributed to high LDL cholesterol were 1.47 and 1.41 times higher than that in 1990. The age-standardized deaths and DALYs rate was 1.45 and 1.70 times in males compared to females, while the age-standardized SEVs rate was 1.10 times in females compared to males. The deaths, DALYs, and SEV rates increased with age. In 2019, the highest age-standardized rates of both deaths and DALYs occurred in Eastern Europe while the lowest occurred in high-income Asia Pacific. High-income North America experienced a dramatic reduction of risk related to high LDL-C. Correlation analysis identified that the age-standardized SEV rate was positively correlated with Socio-demographic Index (SDI; r = 0.7753, P < 0.001). The average annual percentage change (AAPC) of age-standardized SEV rate decreased in the high SDI and high-middle SDI regions but increased in the middle SDI, low-middle SDI, and low SDI regions. High LDL-C mainly contributed to ischemic heart diseases.Conclusion: High LDL-C contributed considerably to health burden worldwide. Males suffered worse health outcomes attributed to high LDL-C when compared to females. The burden attributed to high LDL-C increased with age. Lower SDI regions and countries experienced more health problem challenges attributed to high LDL-C as the result of social development and this should be reflected in policymaking.

In this paper, we present the recent progress in the experimental studies of the electrical conductivity of dominant nominally anhydrous minerals in the upper mantle and mantle transition zone of Earth, namely, olivine, pyroxene, garnet, wadsleyite and ringwoodite. The main influence factors, such as temperature, pressure, water content, oxygen fugacity, and anisotropy are discussed in detail. The dominant conduction mechanisms of Fe-bearing silicate minerals involve the iron-related small polaron with a relatively large activation enthalpy and the hydrogen-related defect with lower activation enthalpy. Specifically, we mainly focus on the variation of oxygen fugacity on the electrical conductivity of anhydrous and hydrous mantle minerals, which exhibit clearly different charge transport processes. In representative temperature and pressure environments, the hydrogen of nominally anhydrous minerals can tremendously enhance the electrical conductivity of the upper mantle and transition zone, and the influence of trace structural water (or hydrogen) is substantial. In combination with the geophysical data of magnetotelluric surveys, the laboratory-based electrical conductivity measurements can provide significant constraints to the water distribution in Earth’s interior.

The vibrational, electrical and structural properties of Ga₂S₃ were explored by Raman spectroscopy, EC measurements, HRTEM and First-principles theoretical calculations under different pressure environments up to 36.4 GPa.

A series of structural, vibrational and electrical transport behaviors for HfS₂ were systematically investigated upon compression and decompression under different hydrostatic environments. High-pressure structure and stability were deeply explored.

A systematic and detailed investigation on the high-pressure structural, electrical transport and magnetic properties was conducted for CrBr₃.