Gao Lei, Chen Jian-Yao, Ke Zhi-Ting, Wang Jiang, Yang Xue-Yun, Shimizu Yuta
Geography and Planning School, Sun Yat-Sen University, Guangzhou 510275, China.
Huan Jing Ke Xue. 2013 Aug;34(8):3079-87.
Shima River, a tributary of Dongjiang River, located in Dongguan City of Guangdong Province, has been seriously polluted in the last 30 years. Water samples were collected from the river and the aquifer and the soil samples were collected as well in the wet (June) and dry (February) season to investigate the temporal and spatial variations of water quality in terms of heavy metal concentrations and inhibition rate of the luminescent bacterium (Vibrio fischeri, LUMIStox 300). Heavy metal concentrations and inhibition rate in river water were found decreasing from the upstream to the downstream, with metal concentrations exceeding the national surface water quality standard (Class I) for all samples and a highest inhibition of 38.34% (equivalent to moderate toxic) at R1 in the dry season. Significant difference (P < 0.01 or P < 0.001) in the wet and dry season was identified in both metal concentrations and inhibition rate, except at R11, which showed a inhibition rate of 15.56%, higher than those in all other samples in the wet season. Inhibition rate at GW4, GW5 and GW6 showed significant difference (P < 0.01 or P < 0.001) in the two periods, and the highest inhibition rate (15.88%) at GW6 in the dry season was considered as low in toxicity. The positive correlations (P < 0.05 or P < 0.01) between heavy metals (Zn, Fe, Mn and Ni) and inhibition rate were identified with correlation coefficients of 0.452, 0.567, 0.726 and 0.475, respectively. Heavy metal pollution of soil (Cu, Ni and Zn) near the river was due to the interaction between the river and the groundwater. Cd was heavily accumulated in the soil, while elevated concentrations of Fe and Mn were found in the river and the groundwater was heavily polluted by Ni.
石马河是东江的一条支流,位于广东省东莞市,在过去30年里受到了严重污染。在雨季(6月)和旱季(2月)从该河流和含水层采集了水样,并采集了土壤样本,以研究水质在重金属浓度和发光细菌(费氏弧菌,LUMIStox 300)抑制率方面的时空变化。发现河水中的重金属浓度和抑制率从上游到下游逐渐降低,所有样本的金属浓度均超过国家地表水水质标准(Ⅰ类),旱季R1处的最高抑制率为38.34%(相当于中度毒性)。除R11外,雨季和旱季的金属浓度和抑制率均存在显著差异(P<0.01或P<0.001),R11的抑制率为15.56%,高于雨季的所有其他样本。GW4、GW5和GW6处的抑制率在两个时期存在显著差异(P<0.01或P<0.001),旱季GW6处的最高抑制率(15.88%)被认为毒性较低。重金属(锌、铁、锰和镍)与抑制率之间存在正相关(P<0.05或P<0.01),相关系数分别为0.452、0.567、0.726和0.475。河流附近土壤(铜、镍和锌)的重金属污染是河流与地下水相互作用的结果。镉在土壤中大量积累,而河流中发现铁和锰的浓度升高,地下水受到镍的严重污染。