从水表沉积物中使用氨增强动员
Wei Xiu1,2,3,4, Ruixuan Gai1,2, Songze Chen5,6
1State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, PR China.
Environmental science & technology
|February 6, 2024
概括
氨氧化刺激铁的减少,调动地下水中的. 这种涉及细菌和古生物的合成过程对于理解含水层中的丰富至关重要.
科学领域:
- 环境微生物学 环境微生物学
- 地质化学 地质化学
- 生物地质化学生物地质化学
背景情况:
- 氨会影响地下水的 (As) 丰富,特别是通过微生物的铁降解与无氧氧化相结合.
- 具体的途径和微生物驱动氨诱导的铁 (III) 减少和随后的动员仍然在很大程度上是未知的.
研究的目的:
- 调查关键的微生物通路和微生物负责诱导的铁 (III) 减少和动员在高地下水.
- 量化氨在含水层沉积物中释放的贡献.
主要方法:
- 用15N标记的和有机碳来源 (葡萄糖,乳酸盐,乳酸盐/乙酸盐) 化地下水层沉积物.
- 测量,铁和的度.
- 头部空间N2.2.的稳定同位素分析 (δ15N)
- 用基因组解析的基因组分析来识别微生物参与者.
主要成果:
- 氨度的降低与铁度的增加和释放的相关.
- 铁和氧化氨的摩尔比率在3.1到3.7之间.
- 15N标签证实了N2是氨氧化的主要产物.
- 的添加使的释放增加了16.1%49.6%,由有机电子捐赠者增强.
- 甲基因组学表明,细菌铁降解剂和古老氧化剂之间的合成相互作用.
结论:
- 合成刺激的铁降解是高地下水中动员的重要,低估的驱动因素.
- 这一过程涉及细菌铁降解和古老氧化之间的代谢伙伴关系.
更多相关视频
06:52Experimental Column Setup for Studying Anaerobic Biogeochemical Interactions Between Iron OxyHydroxides, Trace Elements, and Bacteria
Published on: December 19, 2017
7.8K
10:05Integrated Field Lysimetry and Porewater Sampling for Evaluation of Chemical Mobility in Soils and Established Vegetation
Published on: July 4, 2014
14.3K
相关概念视频
Extraction: Advanced Methods
447
Metal ions can be separated from one another by complexation with organic ligands–the chelating agent– to form uncharged chelates. Here, the chelating agent must contain hydrophobic groups and behave as a weak acid, losing a proton to bind with the metal. Since most organic ligands used in this process are insoluble or undergo oxidation in the aqueous phase, the chelating agent is initially added to the organic phase and extracted into the aqueous phase. The metal-ligand complex is...
447
Qualitative Analysis
22.4K
For solutions containing mixtures of different cations, the identity of each cation can be determined by qualitative analysis. This technique involves a series of selective precipitations with different chemical reagents, each reaction producing a characteristic precipitate for a specific group of cations. Metal ions within a group are further separated by varying the pH, heating the mixture to redissolve a precipitate, or adding other reagents to form complex ions.
For instance, group IV...
For instance, group IV...
22.4K
Precipitation and Co-precipitation
1.8K
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
1.8K
