Cui Xin-Yue, Mo Wu-Qiu, Liao Jian-Bo
Research Center for Eco-Environmental Engineering, Dongguan University of Technology, Dongguan 523808, China.
Huan Jing Ke Xue. 2022 Mar 8;43(3):1375-1383. doi: 10.13227/j.hjkx.202105225.
Simultaneous sampling and observation were conducted at 14 stations in typical intertidal zones of the Guangdong-Hong Kong-Macao greater bay area. The spatial distribution characteristics of Cd morphology in surface water, pore water, suspended matters, and sediments at each sampling site were analyzed, and the influencing factors of Cd morphology changes in each medium were discussed using statistical analyses based on environmental factors. The results showed that the total contents of Cd in surface water, pore water, suspended matters, and sediments in each intertidal zone ranged from 0.41-15.03 μg·L, 0.41-27.54 μg·L, 0.41-4.88 mg·kg, and 0.20-5.30 mg·kg, respectively. The contents of Cd in Shajiao Bay were significantly higher than those in other sampling sites, which should be related to the developed electronics and manufacturing industries in Dongguan. The concentration of Cd in surface water was slightly lower than that in pore water, whereas the content of Cd in suspended matter was comparable to that in sediment at the same sampling site. The results of morphological analysis showed that the ionic-state Cd was dominant in both surface water and pore water, accounting for 67.23%-97.56% and 33.33%-97.16%, respectively. In suspended matter and sediment, Cd was mainly in the residual state, accounting for 45.45%-96.36% and 45.80%-97.27%, respectively. Pearson correlation analysis showed that the complex-state Cd in the aqueous phase was negatively correlated with oxidation reduction potential (ORP) and pH and positively correlated with total organic carbon. The bioavailable Cd in solid sediment was significantly positively correlated with the proportion of clay, ORP, and solid organic carbon and significantly negatively correlated with pH. The single factor linear regression analysis showed that ORP had the greatest effect on the complex-state Cd in the aqueous phase, with regression coefficients of 0.864 and 0.824, respectively. The bioavailable Cd in solid sediment at different depths was significantly affected by the proportion of clay, and the regression coefficients were 0.968, 0.980, 0.977, and 0.877, respectively. The above results indicate that the distribution of total Cd content in the typical intertidal environment of the Greater Bay Area was affected by the characteristics of urban economic development, whereas the allocation of Cd morphology was closely related to environmental factors.
在粤港澳大湾区典型潮间带的14个站点进行了同步采样与观测。分析了各采样点地表水、孔隙水、悬浮物和沉积物中镉形态的空间分布特征,并基于环境因子,通过统计分析探讨了各介质中镉形态变化的影响因素。结果表明,各潮间带地表水、孔隙水、悬浮物和沉积物中镉的总含量分别为0.41 - 15.03 μg·L、0.41 - 27.54 μg·L、0.41 - 4.88 mg·kg和0.20 - 5.30 mg·kg。沙角湾的镉含量显著高于其他采样点,这应与东莞发达的电子和制造业有关。地表水镉浓度略低于孔隙水,而同一采样点悬浮物中镉含量与沉积物相当。形态分析结果表明,地表水和孔隙水中离子态镉占主导,分别占67.23% - 97.56%和33.33% - 97.16%。悬浮物和沉积物中,镉主要以残渣态存在,分别占45.45% - 96.36%和45.80% - 97.27%。Pearson相关性分析表明,水相中络合态镉与氧化还原电位(ORP)和pH呈负相关,与总有机碳呈正相关。固体沉积物中生物可利用镉与黏土比例、ORP和固体有机碳比例呈显著正相关,与pH呈显著负相关。单因素线性回归分析表明,ORP对水相中络合态镉影响最大,回归系数分别为0.864和0.824。不同深度固体沉积物中生物可利用镉受黏土比例影响显著,回归系数分别为0.968、0.980、0.977和0.877。上述结果表明,大湾区典型潮间带环境中总镉含量分布受城市经济发展特征影响,而镉形态分配与环境因子密切相关。