Farmer John G, Thomas Rhodri P, Graham Margaret C, Geelhoed Jeanine S, Lumsdon David G, Paterson Edward
Department of Chemistry, University of Edinburgh, UK.
J Environ Monit. 2002 Apr;4(2):235-43. doi: 10.1039/b108681m.
Chromium concentrations of up to 91 mg l(-1) were found by ICP-OES for ground water from nine boreholes at four landfill sites in an area of S.E. Glasgow/S. Lanarkshire where high-lime chromite ore processing residue (COPR) from a local chemical works had been deposited from 1830 to 1968. Surface water concentrations of up to 6.7 mg l(-1) in a local tributary stream fell to 0.11 mg l(-1) in the River Clyde. Two independent techniques of complexation/colorimetry and speciated isotope dilution mass spectrometry (SIDMS) showed that Cr was predominantly (>90%) in hexavalent form (CrVI) as CrO4(2-), as anticipated at the high pH (7.5-12.5) of the sites. Some differences between the implied and directly determined concentrations of dissolved CrIII, however, appeared related to the total organic carbon (TOC) content. This was most significant for the ground water from one borehole that had the highest TOC concentration of 300 mg l(-1) and at which < 3% of Cr was in the form of CrVI. Subsequent ultrafiltration produced significant decreases in Cr concentration with decreasing size fractions, e.g. <0.45 microm, < 100 kDa, <30 kDa and < 1 kDa by the tangential-flow method. As this appeared related more to concentrations of humic substances than of TOC per se, horizontal bed gel electrophoresis of freeze-dried ultrafilter retentates was carried out to further characterise the CrIII-organic complex. This showed for the main Cr-containing fraction, 100 kDa-0.45 microm, that the Cr was associated with a dark brown band characteristic of organic (humic) matter. Comparison of gel electrophoresis and FTIR results for ultrafilter retentates of ground water from this borehole with those for a borehole at another site where CrVI predominated suggested the influence of carboxylate groups, both in reducing CrVI and in forming soluble CrIII-humic complexes. The implications of this for remediation strategies (especially those based on the addition of organic matter) designed to reduce highly mobile and carcinogenic Cr(VI)O4(2-) to the much less harmful CrIII as insoluble Cr(OH)3 are discussed.
通过电感耦合等离子体发射光谱法(ICP - OES)测定发现,在格拉斯哥东南部/南拉纳克郡某区域四个垃圾填埋场的九个钻孔的地下水中,铬浓度高达91毫克/升。该区域从1830年至1968年曾堆放当地一家化工厂的高钙铬铁矿加工残渣(COPR)。当地一条支流的地表水铬浓度高达6.7毫克/升,而在克莱德河中则降至0.11毫克/升。络合/比色法和特定同位素稀释质谱法(SIDMS)这两种独立技术表明,正如在这些场地高pH值(7.5 - 12.5)条件下所预期的那样,铬主要(>90%)以六价形式(CrVI)存在,即CrO4(2-)。然而,溶解态CrIII的隐含浓度和直接测定浓度之间存在一些差异,这似乎与总有机碳(TOC)含量有关。对于一个钻孔的地下水来说,这种情况最为显著,该钻孔的TOC浓度最高,为300毫克/升,且其中<3%的铬以CrVI形式存在。随后通过切向流方法进行超滤,随着粒径分数减小,如<0.45微米、<100 kDa、<30 kDa和<1 kDa,铬浓度显著降低。由于这似乎更多地与腐殖物质的浓度而非TOC本身有关,因此对冻干超滤截留物进行了水平床凝胶电泳,以进一步表征CrIII - 有机络合物。结果表明,对于主要含铬部分,即100 kDa - 0.45微米,铬与一条深棕色条带相关,该条带具有有机物(腐殖质)的特征。将该钻孔地下水超滤截留物的凝胶电泳和傅里叶变换红外光谱(FTIR)结果与另一个以CrVI为主的场地钻孔的结果进行比较,表明羧基在还原CrVI以及形成可溶性CrIII - 腐殖质络合物方面都有影响。本文讨论了这对修复策略(特别是基于添加有机物的策略)的影响,这些策略旨在将高迁移性和致癌性的Cr(VI)O4(2-)还原为危害小得多的CrIII,即不溶性的Cr(OH)3。