Department of Animal Ecology, Faculty of Earth and Life Sciences, VU University, Amsterdam, The Netherlands.
Chemosphere. 2011 Mar;82(11):1614-9. doi: 10.1016/j.chemosphere.2010.11.047. Epub 2010 Dec 13.
Mo bioaccumulation in the earthworm Eisenia andrei was determined after 28 d exposure in ten different European field soils (pH 4.4-7.8) and an artificial soil, freshly spiked with Na₂MoO₄ at concentrations between 3.2 and 3200 mg Mo kg⁻¹ dry soil. Three field soils were also tested after ageing for 11 months. Earthworm Mo concentrations generally levelled off at high exposure levels but in most soils showed a (nearly) linear increase with increasing soil concentrations in the lower, non-toxic range (below EC10 or NOEC for reproduction effects). Bioaccumulation (BAF) and Bioconcentration factors (BCF) were calculated as the ratio of earthworm concentration to soil and estimated porewater concentrations, respectively. BAFs (0.35-3.44) and BCFs (1.31-276) did not seem much affected by soil concentration, suggesting that earthworms are not capable of regulating their internal Mo concentrations. BAF was best predicted by ammonium oxalate-extractable iron (Fe(ox)) and phosphor (P(ox)) contents of the soils.
在 28 天暴露于十种不同的欧洲田间土壤(pH 值为 4.4-7.8)和一种人工土壤中后,测定了蚯蚓 Eisenia andrei 中的钼生物积累。新鲜添加 Na₂MoO₄,浓度在 3.2 至 3200mg Mo kg⁻¹干土之间。还对三种田间土壤进行了 11 个月老化后的测试。蚯蚓中的 Mo 浓度通常在高暴露水平下趋于稳定,但在大多数土壤中,在较低的、非毒性范围内(低于对生殖效应的 EC10 或 NOEC),随着土壤浓度的增加呈(几乎)线性增加。生物积累(BAF)和生物浓缩因子(BCF)分别作为蚯蚓浓度与土壤和估计的孔隙水浓度的比值来计算。BAF(0.35-3.44)和 BCF(1.31-276)似乎不受土壤浓度的影响很大,这表明蚯蚓不能调节其内部 Mo 浓度。BAF 最好通过土壤中草酸铵可提取的铁(Fe(ox))和磷(P(ox))含量来预测。