(Redox-)Biogeochemistry on the Microscale - Biofilms and Model Systems

微尺度（氧化还原）生物地球化学 - 生物膜和模型系统

• 批准号: 323566027
• 负责人: Professor Dr. Martin Obst
• 金额: --
• 依托单位: Lehrstuhl für Umweltgeochemie
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2017
• 资助国家: 德国
• 起止时间: 2016-12-31 至 2022-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/323566027?language=en
• 关键词: Redox; Biogeochemistry; Microscale; Biofilms; Model

We observe reduction and oxidation processes in the environment that cannot be explained by classical geochemical models. Often reactions are coupled that - based on their individual chemical requirements - should not occur together. However, one fundamental aspect that often has not been considered, mostly due to limitations in our experimental possibilities, is the heterogeneity of environmental systems.Die development of innovative experimental approaches, in particular in the fields of synchrotron-based X-ray spectromicroscopy and lab-based in-situ approaches such as the coupling of environmentally sensitive fluorescence probes with confocal laser scanning microscopy now became promising tools to study such heterogeneities.In this project, the influence of structural and chemical sub-micron scale heterogeneity in redox-active biofilms on biogeochemical reactions will be studied systematically. It will focus on the coupling between different redox-cycles (Fe, Mn, S) that - based on the macroscopic conditions - should not occur. The influence of these couplings on nutrient and contaminant cycling will be studied. In addition to studying natural and artificial biofilms, microfluidic model systems will help to gain a fundamental understanding of the underlying processes under controlled laboratory conditions.The goals of this project are:1) to characterize and parameterize both structural and chemical heterogeneities of redox-active biofilms at the micro-scale. This includes the organochemical composition (e.g. redox-active functional groups), inorganic constituents and chemical conditions with a focus on Fe, Mn and S species.2) to identify, to map and to quantify biogeochemical processes that occur in micro-niches, including the adsorption of nutrients or contaminants, mineral-precipitation and -dissolution, but also electron transfer reactions between the different constituents of the biofilm.3) to prove experimentally whether micro-scale heterogeneities can result in the same phenomena as temporal fluctuations, e.g. fluctuations in water levels.4) to identify individual parameters (i.e. pH, potential, metal concentrations, redox potential) that could induce the previously described structural and chemical heterogeneities.5) to characterize the organochemical composition of microbial exopolymers to study their potential for electron conductance and for acting as redox-buffer systems.6) to assess the importance of the previously determined reactions in microenvironments on the macroscopic scale.

我们观察到的还原和氧化过程中的环境，不能用经典的地球化学模型来解释。通常，反应是耦合的，基于它们各自的化学要求，它们不应该一起发生。然而，一个经常没有被考虑的基本方面是环境系统的异质性，这主要是由于我们实验可能性的限制。创新实验方法的发展，特别是在基于同步加速器的X射线光谱显微镜和基于实验室的干涉仪领域，原位方法，如环境敏感的荧光探针与共聚焦激光扫描显微镜的耦合，现在成为有前途的工具，在这个项目中，将系统地研究氧化还原活性生物膜中结构和化学亚微米尺度的不均匀性对生物地球化学反应的影响。它将集中在不同的氧化还原循环（铁，锰，硫）之间的耦合-基于宏观条件-不应该发生。将研究这些耦合对营养物和污染物循环的影响。除了研究天然和人工生物膜外，微流控模型系统将有助于在受控的实验室条件下获得对潜在过程的基本理解。本项目的目标是：1）在微观尺度上表征和参数化氧化还原活性生物膜的结构和化学异质性。这包括有机化学成分（例如氧化还原活性官能团）、无机成分和化学条件，重点是Fe、Mn和S物种。2）识别、绘制和量化微生态位中发生的地球化学过程，包括营养物或污染物的吸附、矿物沉淀和溶解，而且还包括生物膜的不同成分之间的电子转移反应。3）为了通过实验证明微尺度不均匀性是否可以导致与时间波动相同的现象，例如水位的波动。4）识别单个参数（即pH、电位、金属浓度，氧化还原电位），这可能会导致先前描述的结构和化学异质性。表征微生物外聚合物的有机化学组成，以研究其电子传导和作为氧化还原缓冲系统的潜力。以评估在宏观尺度上的微环境中的先前确定的反应的重要性。