Xinfeng Zhao

Xinfeng Zhao

orcid

Research Focus & Metrics

Academic Career Length

9Years (2018-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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16 August 2018 in Environmental Geochemistry and Health
Verified
Journal Article
Closed access
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ZLZuobing Liang
Zuobing Liang
XZXinfeng Zhao
Xinfeng Zhao
JCJianyao Chen
Jianyao Chen
LGLei Gao
Lei Gao
AZAiping Zhu
Aiping Zhu
KZKai Zhang
Kai Zhang

28 January 2026 in Marine Pollution Bulletin
Verified
Journal Article
Closed access
HZHeng Zhang
Heng Zhang
ZZZijian Zhang
Zijian Zhang
XZXinfeng Zhao
Xinfeng Zhao
HYHong Yang
Hong Yang
TLTong Li
Tong Li
GZGuang Zhang
Guang Zhang

9 May 2025 in Water
Verified
Journal Article
Open access
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TLTianyu Li
Tianyu Li
JZJiayu Zhang
Jiayu Zhang
XZXinfeng Zhao
Xinfeng Zhao
Zihao WuZihao Wu
Zihao Wu
This study elucidates soil–climate regulatory mechanisms on regional health baselines in China and hydrogeochemical roles in cardiovascular biomarker differentiation. Utilizing data from 26,759 healthy adult samples across 286 Chinese cities/counties, seven core factors were identified via Pearson correlation analysis from 25 indicators, including longitude (X1, r = −0.192, p = 0.009), elevation (X3, r = 0.377, p = 0.001), and precipitation (X7, r = −0.200, p = 0.006). Ridge regression analysis (R2 = 0.714) was subsequently applied to simulate predicted values for 2232 cities/counties. The synergistic effects of soil calcium sulfate content and salinity (X25) on serum cardiac troponin I (cTnI) reference values were rigorously validated, explaining 25.5% of regional cTnI elevation (ΔR2 = 0.183). The findings demonstrate that precipitation leaching and groundwater recharge processes collectively drive a 25.5% elevation in cTnI levels in northwestern regions (e.g., Nagqu, Tibet: altitude > 4500 m, annual sunshine > 3000 h) compared to southeastern areas. To mitigate salinity transport dynamics, optimization strategies targeting soil cation exchange capacity (X18/X19) were proposed, providing a theoretical foundation for designing gradient water treatment schemes in high-calcium-sulfate zones (CaSO4 > 150 mg/L). Crucially, regression equations derived from the predictive model enable the construction of a geographically stratified reference framework for cTnI in Chinese adults, with spatial analysis delineating its latitudinal (R2 = 0.83) and longitudinal (R2 = 0.88) distribution patterns. We propose targeted strategies optimizing soil cation exchange capacity to mitigate sulfate transport in groundwater, informing geographically tailored water treatment and cardiovascular disease prevention efforts. Our findings provide localized empirical evidence critical for refining WHO drinking water sulfate guidelines, demonstrating direct integration of hydrogeochemistry, water quality management, and public health.

17 July 2026 in Remote Sensing
Verified
Journal Article
Open access
PDF file
NWNa Wang
Na Wang
Le LiLe Li
Le Li
XZXinfeng Zhao
Xinfeng Zhao
YXYingxue Xuan
Yingxue Xuan
泽张泽彬 张
泽彬 张
LZLingling Zhao
Lingling Zhao
Rapid urbanization exacerbates atmospheric pollutant emissions, markedly altering precipitation chemistry. However, a comprehensive understanding of the equilibrium between multicomponent precipitation chemistry and urbanization remains unclear. This study characterizes the spatiotemporal urbanization dynamics of the Pearl River Delta (PRD) urban agglomeration from 2000 to 2020 by integrating multi-source datasets, including nighttime light (NTL) observations, Landsat-derived land cover, and gridded population products. The interplay between precipitation chemistry and urbanization was evaluated through a multidimensional equilibrium assessment framework integrating spatial heterogeneity, trade-off and synergy analysis, and decoupling diagnosis. The results indicated that interannual variation in precipitation ion concentrations initially increased and then decreased from 2000 to 2020. Spatially, major ion concentrations (SO42−, NO3−, Ca2+, and NH4+) generally declined across the region after 2009, with the most pronounced declines in peripheral PRD areas. Conversely, urbanization intensified, spreading from the central core to the periphery. NTL intensity exhibited the strongest explanatory power for major ion concentrations, suggesting that economic urbanization is more closely associated with spatial variability in precipitation chemistry. Over time, the relationship between precipitation ion concentrations and urbanization shifted from synergy to trade-off. After 2005, the dominant decoupling status of major ion concentrations relative to urbanization shifted from expansive negative decoupling (up to 62.93%) to strong decoupling (up to 75.86%). This shift indicates that the antagonism between urbanization and precipitation pollution has gradually transitioned toward equilibrium. However, this equilibrium exhibits spatiotemporal non-stationarity. These findings highlight the complex nonlinear interactions between urbanization and precipitation chemistry. Identifying spatial heterogeneity in decoupling between urbanization and environmental pollution facilitates the formulation of differentiated zoning management strategies.