湖南某水库锰异常事件成因及其土壤和沉积物锰释放影响因素研究

Causes of Manganese Anomaly Event in a Reservoir in Hunan Province and Influencing Factors of Manganese Release in Soil and Sediment

  • 摘要:
      目的  为了解湖南地区某水库冬季锰浓度异常及研究区土壤和沉积物中锰污染特性及其释放影响因素,分析锰异常的成因,并评价研究区土壤和沉积物中锰的污染水平和潜在生态风险。
      方法  采用小试试验、现场监测、历史数据调查与实地勘查调研等方法,测定了研究区土壤、沉积物锰含量,分析了土壤、沉积物中锰释放与影响因素之间的关系并探索其解吸动力学特征;调查水库水质季节性变化规律,分析气象数据变化规律及周边环境现状,综合研判本次湖南地区某水库冬季锰异常事件的成因;采用地累积指数、潜在生态风险系数评价研究区土壤、沉积物锰污染水平和潜在生态风险。
      结果  研究区各处土壤、沉积物中锰含量均超过相应背景值;研究区土壤、沉积物中锰的释放与pH、溶解氧、水温、电导率、扰动等理化性质的变化密切相关;研究区土壤、沉积物除个别实验组外,锰的解吸过程均符合准一级动力学模型,解吸时间、空间环境、锰含量及存在形态等差异均会对解吸过程产生不同影响;各个点位锰震荡条件下解吸平衡量在0.026 mg g−1 ~ 0.195 mg g−1之间且均高于相应静置状态;研究区各处土壤、沉积物污染程度处于无污染至轻度污染之间,潜在生态风险均处于低风险。
      结论  研究区内源锰污染较为严重,事件发生前水库各项理化性质剧烈变化及临时施工扰动,加剧了内源锰释放;除此之外,历史监测数据的局限性、水库库容的季节变化及温跃层的消失也导致了锰浓度监测值的异常变化。风险评价结果显示,研究区土壤、沉积物锰污染风险总体可控。

     

    Abstract:
      Objective  The aim of this study was to understand the characteristics and release factors of manganese pollution in soil and sediment of a reservoir in Hunan Province, analyze the causes of this event, and evaluate the level and potential ecological risk of manganese pollution in soil and sediment.
      Method  The manganese content in soil and sediment of the study area was determined by small scale experiment, field monitoring, historical data investigation and field investigation, and the relationship between the release of manganese in soil and sediment and its influencing factors was analyzed, and the desorption kinetics was explored. The seasonal variation law of reservoir water quality was investigated, the variation law of meteorological data and the surrounding environment were analyzed, and the causes of the winter manganese anomaly event in a reservoir in Hunan Province were comprehensively analyzed. Soil accumulation index and potential ecological risk coefficient were used to evaluate the manganese pollution level and potential ecological risk in soil or sediment in the study area.
      Result  The contents of manganese in soils or sediments in the study area all exceeded their respective background values. The release of manganese from soil or sediment is closely related to the changes of pH, dissolved oxygen, water temperature, electrical conductivity, disturbance and other physical and chemical properties. The desorption process of manganese from soil or sediment in the study area was in accordance with the quasi-first-order kinetic model except for few experimental group. The desorption time, space environment, manganese content and morphology had different effects on the desorption process. The equilibrium amount of Mn desorption is between 0.026 mg g−1 to 0.195 mg g−1 and higher than their static condition under the condition of oscillation at each sample. The degree of soil or sediment pollution in the study area ranged from pollution-free to mildly polluted, and the potential ecological risks were all at low risk.
      Conclusion  The pollution of endogenous manganese in the study area is serious. The dramatic changes of physical and chemical properties of the reservoir and the construction disturbance during the occurrence of abnormal events promote the release of endogenous manganese. In addition, the limitation of historical monitoring data, the seasonal variation of reservoir capacity and the disappearance of thermocline also lead to the abnormal variation of manganese concentration monitoring values. The result of risk assessment shows that the risk of manganese pollution in soil or sediment in the study area is generally controllable.

     

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