Zhang S, Shan X Q
Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, PO Box 2871, Beijing 100085, People's Republic of China.
Environ Pollut. 2001;112(3):395-405. doi: 10.1016/s0269-7491(00)00143-3.
A greenhouse study was conducted to investigate the accumulation of rare earth elements (REEs), La, Ce, Pr and Nd, in winter wheat (Triticum aestivum L.), and the speciation of these elements in soil following the application of REE-based fertilizers. Improved crop yield was confirmed by the experiment. The accumulation behavior of La, Ce, Pr and Nd in wheat varied depending on the concentration of REE fertilizer application, i.e. increased with increasing REE concentration at low fertilization application, constant over the medium REE range, and decreased with increasing REE concentration at high fertilizer application. Significant negative correlation was obtained between REE contents in roots and soil pH (r = -0.5787 to -0.8442 for La). REEs in both the fertilized and unfertilized soils were fractionated by a three-stage sequential extraction procedure into three chemically distinct fractions: water soluble, exchangeable and carbonate bound (B1), Fe-Mn oxide bound (B2), and organic and sulfide bound (B3). REEs in fertilized soils were found mainly in the B2 and B3 fractions, with only a small amount in the B1 fraction. REEs in B1 and B2 fractions were negatively correlated with soil pH (r = -0.6892 to -0.8927 and -0.7462 to -0.9482). Significant correlation was obtained between REEs in B1 fraction and REE contents in root. The correlation coefficients ranged from 0.6159 to 0.7410 when fertilizer application was lower than 20.0 mg/kg soil. No acceptable relationship was observed between REE contents in shoot and any of the extractable fractions in soils.
进行了一项温室研究,以调查稀土元素(REEs)镧(La)、铈(Ce)、镨(Pr)和钕(Nd)在冬小麦(Triticum aestivum L.)中的积累情况,以及施用稀土基肥料后这些元素在土壤中的形态。实验证实了作物产量有所提高。La、Ce、Pr和Nd在小麦中的积累行为因稀土肥料施用量的不同而有所变化,即在低施肥量时随稀土浓度增加而增加,在中等稀土范围内保持不变,在高施肥量时随稀土浓度增加而降低。根系中稀土元素含量与土壤pH值之间存在显著负相关(La的r值为-0.5787至-0.8442)。通过三阶段连续提取程序将施肥和未施肥土壤中的稀土元素分为三个化学性质不同的部分:水溶性、可交换性和碳酸盐结合态(B1)、铁锰氧化物结合态(B2)以及有机和硫化物结合态(B3)。发现施肥土壤中的稀土元素主要存在于B2和B3部分,B1部分含量很少。B1和B2部分中的稀土元素与土壤pH值呈负相关(r值分别为-0.6892至-0.8927和-0.7462至-0.9482)。B1部分中的稀土元素与根系中的稀土元素含量之间存在显著相关性。当施肥量低于20.0 mg/kg土壤时,相关系数范围为0.6159至0.7410。地上部分的稀土元素含量与土壤中任何可提取部分之间均未观察到可接受的关系。