Characteristics of Environmental Geochemistry in the Arseniasis Area of the Inner Mongolia of China

• Published in: Environmental geochemistry and health Vol. 24; no. 3; pp. 249 - 259
• Main Authors: Lin, Nian-Feng, Tang, Jie, Bian, Jian-Min
• Format: Journal Article
• Language: English
• Published: Kew Kluwer Academic Publishers 01.09.2002; Springer Nature B.V
• Subjects: Arsenic; basins; China, People's Rep., Inner Mongolia; China, People's Rep., Shanxi; China, People's Rep., Xinjiang Uygur; Coastal plains; Decomposing organic matter; Deep wells; Drinking water; exhibitions; Floodplains; Freshwater; Geochemistry; Humus; lakes; methane; people; risk; Taiwan; villages; Water pollution; wells; China; Taiwan; Yellow River; China, People's Rep., Shanxi Prov; China, People's Rep., Huang He R; China, People's Rep., Xinjiang; ISEW, Taiwan
• ISSN: 0269-4042; 1573-2983
• DOI: 10.1023/A:1016079216654

In China, endemic arseniasis attributable to the geological-geochemistry environment is mainly found in the plain of the Great Bend of the Yellow River and the Hu-Bao plain in the Inner Mongolia Autonomous Region, in the Datong basin of Shanxi Province, the floodplain of the northern side of the Tian Mountain of Xinjiang Uygur Autonomous Region, and in the southwest coastal plain of Taiwan. These areas share many similar characteristics including widespread occurrences, a large population being affected, and the magnitude of risk involved. The population living in these areas is estimated to be around 5.5 × 10⁵, of which of 2.5 × 10⁵ are resident in Inner Mongolia. Based on our systematic research and comparison of various areas, we found the different types of arseniasis are often associated with different regions. The neural arseniasis is distributed in Xinjiang Uygur Autonomous Region and Shanxi Province, caused by inorganic arsenic in drinking water while the cycling-obstacle arseniasis is mainly found in Inner Mongolia and Taiwan, associated with organic arsenic in water. The distribution of arsenic affected villages in Inner Mongolia exhibits orientation and focus on low-lying land in the subsiding centre of the Great Bend basin, which was enriched with humus in the lake and limnetic deposits. Much CH₄ gas can be detected in the water of shallow and deep wells in these villages. Some of the wells with higher concentrations of CH₄ can even be ignited. This is a typical reductive geochemical environment. We tested the total amount of arsenic (ΣAs), As³⁺, and methyl arsenate in all types of water sources. It is found that the number of arseniasis cases is not clearly related to the total amount of arsenic (ΣAs) in the water. However, it is related to the ratio of As³⁺ plus methyl arsenic to the total amount of arsenic (ΣAs). The higher the ratio, the higher the number of people affected and the more serious the illness. The statistical results also indicate that good drinking water accounts for 60% of the drinking water source while the arsenic contaminated water makes up about 25% of the drinking water in the study area. This research reveals that the local geochemical environment is responsible for the spreading of the endemic arseniasis in the area and thus suggests a new direction of how to prevent such disease.