Li X David, Schwartz Franklin W
Department of Geological Sciences, The Ohio State University, Columbus, OH 43210, USA.
J Contam Hydrol. 2004 Jan;68(1-2):39-53. doi: 10.1016/S0169-7722(03)00144-X.
Previous studies on in situ chemical oxidation of trichloroethylene (TCE) with potassium permanganate indicated that the solid reaction product, Mn oxide, could reduce the permeability of the porous medium and impact the success of dense non-aqueous phase liquid (DNAPL) removal. In order to address the issue of permeability reduction caused by precipitation, this study investigated the mineralogy of Mn oxides and the possibilities of removing the solid precipitates by dissolution. The solid reaction product from the oxidation of TCE by permanganate is semi-amorphous potassium-rich birnessite, which has a layered mineral structure with an interlayer spacing of 7.3 A. The chemical formula is K(0.854)Mn(1.786)O(4).1.55H(2)O. It has a relatively small specific surface area at 23.6+/-0.82 m(2)/g. Its point of zero charge (pzc) was measured as 3.7+/-0.4. This birnessite is a relatively active species and could participate in various reactions with existing organic and inorganic matter. The dissolution kinetics of Mn oxide was evaluated in batch experiments using solutions of citric acid, oxalic acid, and ethylenediaminetetraacetic acid (EDTA). Initial dissolution rates were determined to be 0.126 mM/m(2)/h for citric acid, 1.35 mM/m(2)/h for oxalic acid, and 5.176 mM/m(2)/h for EDTA. These rates compare with 0.0025 mM/m(2)/h for nitric acid at pH=2. Organic acids dissolve Mn oxide quickly. Reaction rates increase with acid concentration, as tested with citric acid. The dissolution mechanism likely involves proton and ligand-promoted dissolution and reductive dissolution. Citric and oxalic acid can induce ligand-promoted dissolution, while EDTA can induce ligand-promoted and reductive dissolutions. At low pH, proton-promoted dissolution seems to occur with all the acids tested, but this process is not dominant. Reductive dissolution appears to be the most effective process in dissolving the solid, followed by ligand-promoted dissolution. These experiments indicate the significant potential in using these organic acids to remove precipitates formed during the oxidation reaction.
先前关于用高锰酸钾对三氯乙烯(TCE)进行原位化学氧化的研究表明,固体反应产物氧化锰会降低多孔介质的渗透率,并影响致密非水相液体(DNAPL)去除的效果。为了解决沉淀导致渗透率降低的问题,本研究调查了氧化锰的矿物学以及通过溶解去除固体沉淀物的可能性。高锰酸钾氧化TCE产生的固体反应产物是半无定形的富钾水钠锰矿,它具有层状矿物结构,层间距为7.3埃。化学式为K(0.854)Mn(1.786)O(4).1.55H(2)O。其比表面积相对较小,为23.6±0.82平方米/克。测得其零电荷点(pzc)为3.7±0.4。这种水钠锰矿是一种相对活跃的物质,能够与现有的有机和无机物质发生各种反应。在分批实验中,使用柠檬酸、草酸和乙二胺四乙酸(EDTA)溶液评估了氧化锰的溶解动力学。确定柠檬酸的初始溶解速率为0.126毫摩尔/平方米/小时,草酸为1.35毫摩尔/平方米/小时,EDTA为5.176毫摩尔/平方米/小时。这些速率与pH = 2时硝酸的0.0025毫摩尔/平方米/小时相比。有机酸能快速溶解氧化锰。如用柠檬酸测试,反应速率随酸浓度增加而提高。溶解机制可能涉及质子和配体促进的溶解以及还原溶解。柠檬酸和草酸可诱导配体促进的溶解,而EDTA可诱导配体促进的溶解和还原溶解。在低pH值下,所有测试的酸似乎都会发生质子促进的溶解,但这个过程并非主导。还原溶解似乎是溶解固体最有效的过程,其次是配体促进的溶解。这些实验表明,使用这些有机酸去除氧化反应过程中形成的沉淀物具有巨大潜力。