Fu F, Akagi T, Shinotsuka K
Faculty of Agriculture, Tokyo University of Agriculture and Technology, Fuchu, Japan.
Biol Trace Elem Res. 1998 Summer;64(1-3):13-26. doi: 10.1007/BF02783321.
All the lanthanide elements (REE) in fern (Matteuccia) and in soil were determined with inductively coupled plasma mass spectrometer (ICP-MS) in order to discuss REE behavior in fern. The fern sample was divided into three parts: root, stem, and leaf; the soil of the same site was also sampled and the soil sample was divided into two parts: HCl and HNO3 soluble part (soil[HCl]) and HF soluble part (soil[HF]). REE in each part was determined by ICP-MS after solvent extraction separation. The overall variation of the REE pattern of the root does not resemble that of the whole soil, but that of the HF soluble part. A tetrad effect variation (W-type) was found in the REE patterns of root, stem and leaf; more conspicuous tetrad effect variation was observed in HREE region than in LREE region, and was so in stem and leaf than in root. Negative anomalies of Ce were observed in the REE patterns of root, stem and leaf, with bigger anomalies in stem and leaf than in root. The results of this study suggest that REE in fern has come from silicates of soil and has once been in dissolved state.
为了探讨稀土元素(REE)在蕨类植物中的行为,采用电感耦合等离子体质谱仪(ICP-MS)测定了蕨类植物(荚果蕨)和土壤中的所有镧系元素。将蕨类植物样本分为根、茎、叶三部分;采集同一地点的土壤样本,并将土壤样本分为两部分:盐酸和硝酸可溶部分(soil[HCl])和氢氟酸可溶部分(soil[HF])。各部分的稀土元素经溶剂萃取分离后,用ICP-MS测定。根中稀土元素模式的总体变化与全土不同,而与氢氟酸可溶部分相似。在根、茎、叶的稀土元素模式中发现了四重效应变化(W型);重稀土区域的四重效应变化比轻稀土区域更明显,茎和叶中的四重效应变化比根中更明显。在根、茎、叶的稀土元素模式中均观察到铈的负异常,茎和叶中的异常比根中更大。本研究结果表明,蕨类植物中的稀土元素来自土壤硅酸盐,且曾经处于溶解状态。