环境地球化学国家重点实验室知识库

The quality changes of shallow groundwater from karst hilly areas in Guiyang region of China impacted by the urbanization were investigated. The results show that the major ions in shallow groundwater from the karst hilly areas are mainly composed of HCO₃ ⁻, SO₄ ²⁻, Ca²⁺ and Mg²⁺, and the concentrations scopes of NO₃ ⁻, Cl⁻, K⁺ and Na⁺ of the groundwater in agricultural, residential and industrial areas are 4.5–9.6, 2.8–7.1, 3.9–6.3 and 2.5–4.9 times higher than those in the forest areas, respectively. The concentrations of As, Pb and Cd of shallow groundwater in the industrial areas are also significantly enhanced, followed by those in the residential areas and the agricultural areas. The concentrations of NO₃ ⁻, SO₄ ²⁻, As, Pb and Cd of the groundwater in the industrial areas and those of NO₃ ⁻, SO₄ ²⁻, As and Cd of shallow groundwater in the residential areas reach grade III of the Groundwater Quality Standard of China (GB/T 14848-93), while the concentration of NO₃ ⁻ in the groundwater from the industrial areas exceeds grade V. With the process of urbanization, NO₃ ⁻ is the key factor to influence the groundwater quality in karst hilly areas, followed by SO₄ ²⁻, As, Pb and Cd.