Shan Xiao-Quan, Wang Zhongwen, Wang Weisheng, Zhang Shuzhen, Wen Bei
Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, P.O. Box 2871, Beijing, 100085, China.
Anal Bioanal Chem. 2003 Feb;375(3):400-7. doi: 10.1007/s00216-002-1711-2. Epub 2003 Jan 28.
A labile rhizosphere soil solution fraction has been recommended to predict the bioavailability of heavy metals and rare earth elements to plants. This method used moist rhizosphere soil in combination with a mixture of 0.01 mol L(-1) of low-molecular-weight organic acids (LMWOAs) as extractant. The extracted soil solutions were fractionated into two colloidal fractions of <0.45 microm (F(3)) and <0.2 microm (F(2)), and one truly dissolved fraction including free metal ions and inorganic and organic complexes (fraction<molecular weight cutoff of 1 kD). Hereafter, the fraction of the truly dissolved fraction refers to labile rhizosphere soil solution fraction, F(lrss). For the soil solutions extracted with a mixture of LMWOAs the concentrations of heavy metals and rare earth elements in F(2) and F(3) were quite similar. However, the mean concentrations of Cr, Ni, Zn, Cu, Pb, Cd, La, Ce, Pr, and Nd in F(lrss) accounted for 79.9%, 91.3%, 90.8%, 60.1%, 77.5%, 75.3%, 81.2%, 77.2%, 80.3%, and 79.5%, respectively, of their concentrations in F(2). In contrast, there were no differences in the extractable metal concentrations between the three fractions while the first step of the method recommended by the European Community of Reference (BCR), where 0.1 mol L(-1) acetic acid was used as an extractant. The single correlation analysis was made between metal concentrations in the different fractions of soil solutions and their concentrations in wheat. If the first step of BCR method was used there was no good correlation between heavy metals in soil pools and that in wheat shoots and roots. When LMWAOs were used a good correlation was obtained between the concentrations of heavy metals in soil pools and that in wheat roots, which followed a general order of r(1 kD, LMWOAs) >r(0.2 microm, LMWOAs) approximately r(0.45 microm, LMWOAs). In the case of rare earth elements the good correlation was obtained for both the wheat roots and shoots. Generally, the correlation coefficients obtained by LMWAOs were better than that obtained by the first step of BCR method. Therefore, LMWAOs and F(lrss) were strongly recommended to predict the bioavailability of metals in soil pools to plants.
一种不稳定的根际土壤溶液组分已被推荐用于预测重金属和稀土元素对植物的生物有效性。该方法使用湿润的根际土壤与0.01 mol L(-1)的低分子量有机酸(LMWOAs)混合物作为提取剂。提取的土壤溶液被分离为两个胶体组分,<0.45微米(F(3))和<0.2微米(F(2)),以及一个真正溶解的组分,包括游离金属离子、无机和有机络合物(分子量截止<1 kD的组分)。此后,真正溶解组分的部分指不稳定的根际土壤溶液组分,F(lrss)。对于用LMWOAs混合物提取的土壤溶液,F(2)和F(3)中重金属和稀土元素的浓度相当相似。然而,F(lrss)中Cr、Ni、Zn、Cu、Pb、Cd、La、Ce、Pr和Nd的平均浓度分别占其在F(2)中浓度的79.9%、91.3%、90.8%、60.1%、77.5%、75.3%、81.2%、77.2%、80.3%和79.5%。相比之下,当使用欧洲共同体参考(BCR)推荐方法的第一步,即使用0.1 mol L(-1)乙酸作为提取剂时,三个组分之间的可提取金属浓度没有差异。对土壤溶液不同组分中的金属浓度与其在小麦中的浓度进行了单相关分析。如果使用BCR方法的第一步,土壤库中的重金属与小麦地上部和根部的重金属之间没有良好的相关性。当使用LMWOAs时,土壤库中的重金属浓度与小麦根部的重金属浓度之间获得了良好的相关性,其一般顺序为r(1 kD, LMWOAs) >r(0.2微米, LMWOAs) ≈ r(0.45微米, LMWOAs)。对于稀土元素,小麦根部和地上部都获得了良好的相关性。一般来说,LMWOAs获得的相关系数优于BCR方法第一步获得的相关系数。因此,强烈推荐使用LMWOAs和F(lrss)来预测土壤库中金属对植物的生物有效性。