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孙银磊, 李志妃, 张先伟. 岩土新发现——高原淡水藻类诱导产生碳酸钙[J]. 岩土工程学报. DOI: 10.11779/CJGE20240851
引用本文: 孙银磊, 李志妃, 张先伟. 岩土新发现——高原淡水藻类诱导产生碳酸钙[J]. 岩土工程学报. DOI: 10.11779/CJGE20240851
A new discovery of rock and soil - calcium carbonate induced by Plateau freshwater algae[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20240851
Citation: A new discovery of rock and soil - calcium carbonate induced by Plateau freshwater algae[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20240851

岩土新发现——高原淡水藻类诱导产生碳酸钙

A new discovery of rock and soil - calcium carbonate induced by Plateau freshwater algae

  • 摘要: 鉴于高原淡水藻类诱导产生碳酸钙的研究领域尚属探索初期,本文聚焦于高原独特环境下淡水藻类在岩石表面的生物矿化作用,重点分析了藻类诱导产生的沉积物特性及其对岩石力学性质的影响。通过X射线衍射(XRD)试验,确认了该沉积物的主要成分为碳酸钙沉淀。进一步,利用扫描电子显微镜(SEM)观察了碳酸钙的微观结构,并结合点荷载试验分析了碳酸钙沉积对岩石抗压强度的具体影响。研究结果表明,高原淡水藻类具备诱导产生碳酸钙的功能,但诱导产生碳酸钙的抗压强度弱于附着的岩石,并揭示了碳酸钙沉积的微观结构特征与其对岩石力学性质影响之间的内在联系。作为一项岩土新发现——高原环境下淡水藻类诱导碳酸钙,可以为理解生物矿化作用在岩石风化、沉积及地质工程稳定性评估中的潜在作用提供了科学依据。

     

    Abstract: Since the research field of calcium carbonate induced by freshwater algae in the plateau is still in the early stage of exploration, this paper focuses on the biological mineralization of freshwater algae on the rock surface under the unique environment of the plateau, and focuses on analyzing the characteristics of sediments induced by algae and their effects on rock mechanical properties. By X-ray diffraction (XRD) test, it is confirmed that the sediment is mainly composed of calcium carbonate precipitation. Furthermore, the microstructure of calcium carbonate was observed by scanning electron microscope (SEM), and the effect of calcium carbonate deposition on compressive strength of rock was analyzed by point load test. The results show that freshwater algae can induce calcium carbonate, but the compressive strength of induced calcium carbonate is weaker than that of attached rocks, and the intrinsic relationship between the microstructure of calcium carbonate deposits and its effect on rock mechanical properties is revealed. As a new geotechnical discovery, calcium carbonate induced by freshwater algae in plateau environment can provide scientific basis for understanding the potential role of biommineralization in rock weathering, sedimentation and geological engineering stability assessment.

     

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