Biogeochemical Weathering of Layer Silicates

层状硅酸盐的生物地球化学风化

• 批准号: 9706382
• 负责人: Jillian Banfield
• 金额: $ 24.46万
• 依托单位: University of Wisconsin-Madison
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1997
• 资助国家: 美国
• 起止时间: 1997-07-01 至 2001-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9706382&HistoricalAwards=false
• 关键词: Biogeochemical; Weathering; Layer; Silicates

9706382 Banfield The proposed research will investigate the inorganic and biological mechanisms by which layer silicates are weathered, with implications for geochemical cycles, soil fertility, and plant nutrition. Specifically, work will focus on interactions between biotite, chlorite, muscovite, and rhizosphere microorganisms and the reactions that convert these minerals to clays. This work builds on our previous studies of inorganically and biogeochemically mediated alteration of chain silicates and extensive studies of layer silicate structures, microstructures, chemistry, and reaction mechanisms in hydrothermally altered rocks. Layer silicates partially transformed to clay minerals will be characterized using atomic-resolution transmission electron microscopy and state of the art energy-filtered electron microscopic techniques. Atomic-resolution and low dose image capture capabilities will be used to determine whether structural details of clay products are consistent with a transformation mechanism that involves structural inheritance. Our work will employ both weathered layer silicates from the rhizosphere region of natural soils and layer silicates weathered in a laboratory rhizosphere. The distribution of microorganisms on mineral surfaces will be studied using domain level and more specific oligonucleotide probes. The hypothesis that microorganisms in soils accelerate mineral dissolution by production of extracellular enzymes (e.g. "mineralases" , analogous to cellulases and chitinases microbes produce to degrade wood, chitin, and related organic substrates) will be tested. This work involves collaboration with Prof. Robert Goodman (Plant Pathology, UW-Madison.

小行星9706382 拟议的研究将调查层状硅酸盐风化的无机和生物机制，对地球化学循环，土壤肥力和植物营养的影响。 具体来说，工作将集中在黑云母，白云母，和根际微生物之间的相互作用和这些矿物转化为粘土的反应。 这项工作建立在我们以前的研究无机和地球化学介导的链硅酸盐蚀变和广泛的研究层硅酸盐结构，微观结构，化学和反应机制的热液蚀变岩石。 层状硅酸盐部分转化为粘土矿物将使用原子分辨率透射电子显微镜和最先进的能量过滤电子显微镜技术的特点。 原子分辨率和低剂量图像捕获能力将用于确定粘土产品的结构细节是否与涉及结构遗传的转化机制一致。 我们的工作将采用两个风化层硅酸盐从根际地区的天然土壤和层硅酸盐风化在实验室根际。 微生物在矿物表面的分布将使用域水平和更特异的寡核苷酸探针进行研究。 土壤中的微生物通过产生胞外酶（例如“矿化酶”，类似于微生物产生的降解木材、几丁质和相关有机底物的纤维素酶和几丁质酶）来加速矿物溶解的假设将得到检验。 这项工作涉及与教授罗伯特古德曼（植物病理学，威斯康星大学麦迪逊分校。