Soil Department, Federal Rural University of Rio de Janeiro, BR 465, km 7, Seropédica, Rio de Janeiro, CEP 23890-000, Brazil.
Chemosphere. 2012 Sep;89(1):121-7. doi: 10.1016/j.chemosphere.2012.04.060. Epub 2012 May 29.
Two assays were designed to obtain information about the influence of redox potential variations on barium mobility and bioavailability in soil. One assay was undertaken in leaching columns, and the other was conducted in pots cultivated with rice (Oryza sativa) using soil samples collected from the surface of Gleysol in both assays. Three doses of barium (100,300 mg kg(-1) and 3000 mg kg(-1)-soil dry weight) and two redox potential values (oxidizing and reducing) were evaluated. During the incubation period, the redox potential (Eh) was monitored in columns and pots until values of -250 mV were reached. After the incubation period, geochemical partitioning was conducted on the barium using the European Communities Bureau of Reference (BCR) method. Rainfall of 200 mm d(-1) was simulated in the columns and in the planting of rice seedlings in the pots. The results of the geochemical partitioning demonstrated that the condition of reduction favors increased barium concentrations in the more labile chemical forms and decreased levels in the chemical forms related to oxides. The highest barium concentrations in leached extracts (3.36 mg L(-1)) were observed at the highest dose and condition of reduction at approximately five times above the drinking water standard. The high concentrations of barium in the soil did not affect plant dry matter production. The highest levels and accumulation of barium in roots, leaves, and grains of rice were found at the highest dose and condition of reduction. These results demonstrate that reduction leads to solubilization of barium sulfate, thereby favoring greater mobility and bioavailability of this element.
设计了两种测定方法以获取关于氧化还原电位变化对土壤中钡的移动性和生物可利用性影响的信息。一种测定方法在淋滤柱中进行,另一种在使用取自两种测定中土壤表层的土壤样品的水稻(Oryza sativa)盆栽中进行。评估了三种钡剂量(100、300 mg kg(-1)和 3000 mg kg(-1)-土壤干重)和两种氧化还原电位值(氧化和还原)。在培养期间,柱和盆中的氧化还原电位(Eh)一直被监测,直到达到-250 mV 值。培养期结束后,使用欧洲共同体基准局(BCR)方法对钡进行地球化学分配。在柱中模拟了 200 mm d(-1)的降雨量,并在盆中种植了水稻幼苗。地球化学分配的结果表明,还原条件有利于增加更具活性的化学形态中钡的浓度,并降低与氧化物有关的化学形态中的浓度。在淋滤提取物中观察到的最高钡浓度(3.36 mg L(-1))出现在最高剂量和还原条件下,约为饮用水标准的五倍。土壤中高浓度的钡并没有影响植物干物质的生产。在根、叶和稻谷中,钡的最高浓度和积累出现在最高剂量和还原条件下。这些结果表明,还原导致硫酸钡的溶解,从而有利于该元素更大的移动性和生物可利用性。