首页> 外文期刊>Environmental Geochemistry and Health >Environmental biogeochemical behaviors of rare earth elements in soil-plant systems
【24h】

Environmental biogeochemical behaviors of rare earth elements in soil-plant systems

机译:土壤-植物系统中稀土元素的环境生物地球化学行为

获取原文
获取原文并翻译 | 示例
       

摘要

With the continual increase in the utilization of rare earth elements (REEs) for industrial and agricultural purposes in China, the research into the environmental biogeochemical behavior of REEs has become a pressing issue. The REEs' content in soil and various parts of wheat under different conditions in soil-plant systems were measured by INAA and ICP-MS. The results showed four aspects. (1) The mean value of total REEs in soil of China was 176.8 mg kg~(-1). The mean ratio of ΣLREE/ΣHREE in soils was 8.0 and cerium accounts for 42% of the total REEs. The content of REEs in wheat seed ranged between 10~(-11) and 10~(-8) g g~(-1), 3-4 orders of magnitude lower than that in soil. (2) The REEs contents in ryegrass, especially in roots, were significantly related to that of soil. The bioavailability of REEs in soil mainly depended on the exchangeable fraction of REEs, which was strongly affected by the physico-chemical properties of the soil. (3) Long-term foliage-dressing with Changle microfertilizer of REEs did not affect the contents and distribution patterns of REEs in soil. At the maturing stage of spring wheat, the REEs content was in the order of root > leaf > stem and crust. Compared with the control, foliage-dressing has a higher accumulation of REEs in root and leaf. However, no significant difference was found in stem and crust between the two treatments. (4) There was no significant accumulation with the soil-dressing method. When comparing controls in both foliage- and soil-dressing methods, no distinct residue of REEs in grains was found.
机译:随着中国工业和农业中稀土元素利用率的不断提高,对稀土元素的环境生物地球化学行为的研究成为迫切的问题。利用INAA和ICP-MS测定了土壤-植物系统中不同条件下土壤和小麦各部位的稀土元素含量。结果显示出四个方面。 (1)中国土壤的稀土元素平均值为176.8 mg kg〜(-1)。土壤中ΣLREE/ΣHREE的平均比率为8.0,铈占REE总量的42%。小麦种子中的稀土元素含量在10〜(-11)〜10〜(-8)g g〜(-1)之间,比土壤低3-4个数量级。 (2)黑麦草,尤其是根中的稀土元素含量与土壤含量显着相关。稀土元素在土壤中的生物利用度主要取决于稀土元素的可交换部分,而稀土元素的可交换部分受土壤理化性质的强烈影响。 (3)长期使用稀土元素长乐微肥不影响土壤中稀土元素的含量和分布格局。在春小麦成熟期,稀土元素的含量依次为根>叶>茎和地壳。与对照相比,观叶追根在根和叶中具有较高的稀土元素积累。然而,两种处理之间在茎和结皮上没有发现显着差异。 (4)追土方法无明显积累。当比较叶面和土壤追施方法的对照时,未发现谷物中有明显的稀土元素残留。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号