文献类型：期刊文献

英文题名：Hydrochemical Characteristics and Risk Assessment of Tongzi River, Guizhou Province, Southwest China

作者：Lu, Jiemei An, Yanling

第一作者：Lu, Jiemei

通信作者：An, YL[1];An, YL[2]

机构：[1]Guizhou Inst Technol, Coll Resources & Environm Engn, Guiyang 550003, Peoples R China;[2]Guizhou Univ, Coll Resources & Environm Engn, Key Lab Karst Georesources & Environm, Minist Educ, Guiyang 500025, Peoples R China

第一机构：贵州理工学院资源与环境工程学院

通信机构：corresponding author), Guizhou Inst Technol, Coll Resources & Environm Engn, Guiyang 550003, Peoples R China;corresponding author), Guizhou Univ, Coll Resources & Environm Engn, Key Lab Karst Georesources & Environm, Minist Educ, Guiyang 500025, Peoples R China.|贵州理工学院资源与环境工程学院;贵州理工学院;

年份：2023

卷号：15

期号：4

外文期刊名：WATER

收录：;EI(收录号：20231013672881);Scopus(收录号：2-s2.0-85149254159);WOS:【SCI-EXPANDED(收录号:WOS:000940032000001)】；

基金：This research was funded by the High-Level Talent Introduction Program for the Guizhou Institute of Technology (2019 [45]). The funder had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

语种：英文

外文关键词：hydrochemical characteristics; major ion sources; agricultural activities; risk assessment

摘要：This study collected 31 water samples from the Tongzi River, Guizhou Province, Southwest China to conduct a risk assessment to understand the hydrochemical characteristics and major ion sources of irrigation and drinking water quality and their effects on human health. The results showed that ion abundance in the Tongzi River is Ca2+ (66%) > Mg2+ (24%) > K++Na+ (10%) for cations and HCO3- (75%) > SO42-(21%) > Cl- (4%) for anions. Additionally, the hydrochemical type of the water is Ca-Mg-HCO3, controlled by carbonate weathering. Methods including ion ratios, principal component analysis (PCA), and correlation analysis (CA) were used to analyze the source of main ions in the river water. PC1, with the most significant variance (54.9%), decides the hydrochemical characteristics and is affected by the positive loadings of SO42- (0.92), pH (0.85), Ca2+ (0.80), Cl- (0.72), Na+(0.66), NO3- (0.65), and K+ (0.57). PC2 explains 19.2% of the total variance, with strong positive loadings of Na+ (0.75), K+ (0.63) and Cl- (0.59). Mg2+ (0.84) and HCO3- (0.85) exhibits high loadings in PC3, explaining 9.3% of the variance. The results showed that intensive agricultural activities in the basin were the main source of nitrate NO3-, whereas SO42- was mainly derived from mining activities. The lower concentrations of Na+, K+, and Cl- were from coal combustion, domestic wastewater discharge, and agricultural fertilizer applications. The study area was mainly affected by carbonate rock weathering; natural processes (mainly the weathering of carbonate rocks) were still the main origin of Ca2+, Mg2+, and HCO3-. Moreover, the United States Salinity Laboratory (USSL) diagram and the Wilcox diagram showed that 100% of the samples fell in the C2S1 zones, and the water quality had good suitability for irrigation. The health risk assessment (HRA) results showed that HQ(NO)(3)(-) was much larger than HQ(NH4+) and indicated that nitrate pollution dominated non-health hazards. About 6.5% of the samples in the tributaries represented an unacceptable risk for infants and children, and the HQ value for infants and children was always higher than that for adults. Additionally, the non-carcinogenic health risk of riverine ions for infants and children in the Tongzi River was very noteworthy, especially in the tributaries.