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岩溶地下河沉积物对氨氮的等温吸附特征
摘要点击 1870  全文点击 1368  投稿时间:2010-02-15  修订日期:2010-06-25
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中文关键词  岩溶  地下河  沉积物  吸附  解吸
英文关键词  karst  underground river  sediment  adsorption  desorption
作者单位
郭芳 中国地质科学院岩溶地质研究所国土资源部岩溶动力学重点实验室桂林541004 
陈坤琨 江西省九江市环境科学研究所九江 332000 
姜光辉 中国地质科学院岩溶地质研究所国土资源部岩溶动力学重点实验室桂林541004 
中文摘要
      岩溶含水层是西南地区最重要的含水层之一.含水层的管道系统蕴藏着丰富的沉积物,这些沉积物可能成为污染物运移和转化的载体.以广西柳州市2个典型地下河系统为例,通过室内模拟的方法,研究地下河沉积物对氨氮的吸附特征.沉积物对氨氮的吸附平衡时间都小于2 h,最短的时间不足1 h,沉积物5 h平衡吸附量达到了最大吸附量的71%~98%.沉积物对氨氮吸附的最大吸附量Qmax为385.5 mg/kg.在实验设定的浓度范围内,NH+4吸附量随液相NH+4平衡浓度的增大而增大,沉积物对氨氮的吸附量与氨氮的吸附平衡浓度基本呈线性关系.吸附-解析平衡浓度都较低,表明地下河沉积物对氨氮具有较大的吸附潜力.在低浓度及高浓度条件下,Langmuir和Tempkin模型对数据无法拟合或拟合结果没有达到显著水平,而Linear模型和Freundlich模型的拟合效果均达到了极显著水平.对不同地质背景的2条地下河的不同沉积物类型、 不同取样时间和深度的研究表明,沉积物对氨氮的吸附特征并未按沉积物类型而分类,原因一是沉积物在发育的气候、 地质、 水文条件及污染历史、 现状上没有大的差别,二是下一步应增加pH、 盐度等因素对沉积物吸附解吸行为的影响研究.
英文摘要
      Karst aquifers are one of the most important aquifers in Southwestern China. One of the characteristics of karst aquifers is the enhanced permeability permits high flow velocities are capable of transporting suspended and bedload sediments. Mobile sediment in karst may act as a vector for the transport of contaminates. 14 sediment samples were collected from two underground rivers in two typical karst areas in Liuzhou city, Guangxi Autonomous Region, China. According to simulated experiment methods, characteristic of adsorption of ammonia nitrogen on sediment was studied. The results of ammonia nitrogen adsorption dynamics on sediments showed that the maximum adsorption velocity was less than 2 h. The adsorption balance quantity in 5 h accounted for 71%-98% of the maximum adsorption quantity. The maximum adsorption quantity of ammonia nitrogen was 385.5 mg/kg, which was sediment from a cave in the middle areas of Guancun underground river system. The study of isotherm adsorption indicated adsorption quantity of NH+4 increase followed by incremental balance concentration of NH+4 in the aquatic phase. Adsorption quantity of ammonia nitrogen in sediments has a relative linear relationship with adsorption balance concentrations. Adsorption-desorption balance concentrations were all low, indicating sediments from underground rivers have great adsorption potential. Under the condition of low and high concentrations of ammonia nitrogen in overlying water, Langmuir and Tempkin couldn't simulate or simulate results couldn't reach remarkable level, whilst Linear and Freundlich models could simulate well. Research on different type sediments, sampling times and depths from two underground rivers shows characteristic of ammonia nitrogen adsorption on karst underground river sediments doesn't have good correspondence with the type of sediments. One of the reasons is there is no big difference between sediments in the development of climate, geology, hydrological conditions and pollution history. The other reason maybe the article is lack of research on pH, salinity and others factors which may affect adsorption and desorption.

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