Department of Civil and Architectural and Engineering Mechanics, University of Arizona, Tucson, AZ, 85721, USA.
Department of Chemical and Biological Engineering, South Dakota School of Mines and Technology, Rapid City, SD, 57701, USA.
Sci Rep. 2024 Jan 4;14(1):477. doi: 10.1038/s41598-023-51060-w.
The phase changes of soil water or porous media have a crucial influence on the performance of natural and man-made infrastructures in cold regions. While various methods have been explored to address the impacts of frost-action arising from these phase changes, conventional approaches often rely on chemicals, mechanical techniques, and the reuse of waste materials, which often exhibit certain limitations and environmental concerns. In contrast, certain organisms produce ice-binding proteins (IBPs) or antifreeze proteins (AFPs) to adapt to low temperatures, which can inhibit ice crystal growth by lowering the freezing point and preventing ice crystallization without the need for external intervention. This study explores the potential of three psychrophilic microbes: Sporosarcina psychrophile, Sporosarcina globispora, and Polaromonas hydrogenivorans, to induce non-equilibrium freezing point depression and thermal hysteresis in order to control ice lens growth in frost-susceptible soils. We hypothesize that the AFPs produced by psychrophiles will alter the phase changes of porous media in frost-susceptible soils. The growth profiles of the microbes, the concentration of released proteins in the extracellular solution, and the thermal properties of the protein-mixed soils are monitored at an interval of three days. The controlled soil showed a freezing point of - 4.59 °C and thermal hysteresis of 4.62 °C, whereas protein-treated soil showed a maximum freezing point depression of - 8.54 °C and thermal hysteresis of 7.71 °C. Interestingly, except for the controlled sample, all the protein-treated soil samples were thawed at a negative temperature (minimum recorded at - 0.85 °C). Further analysis showed that the treated soils compared to porous media mixed soil freeze (1.25 °C vs. 0.51 °C) and thaw (2.75 °C vs. 1.72 °C) at extensive temperature gap. This freezing and thawing temperature gap is the temperature difference between the beginning of ice core formation and completed frozen, and the beginning of ice core thawing and completed thawed for the treated soil samples selected from different incubation days. Overall, this study presents a novel bio-mediated approach using psychrophilic microbes to control ice formation in frost-susceptible soils.
土壤水或多孔介质的相变化对寒区自然和人为基础设施的性能有至关重要的影响。虽然已经探索了各种方法来解决这些相变化引起的冻融作用的影响,但传统方法通常依赖于化学物质、机械技术和废物的再利用,这些方法往往存在某些局限性和环境问题。相比之下,某些生物会产生冰结合蛋白(IBP)或抗冻蛋白(AFP)以适应低温,它们可以通过降低冰点和防止冰晶形成来抑制冰晶生长,而无需外部干预。本研究探索了三种嗜冷微生物(嗜冷球形芽孢杆菌、球形芽孢杆菌和极地氢噬胞菌)的潜力,以诱导非平衡冰点降低和热滞来控制易受霜冻影响的土壤中冰透镜的生长。我们假设嗜冷微生物产生的 AFP 将改变易受霜冻影响的土壤中多孔介质的相变化。每隔三天监测微生物的生长曲线、细胞外溶液中释放蛋白的浓度以及蛋白混合土壤的热特性。对照土壤的冰点为-4.59°C,热滞为 4.62°C,而蛋白处理土壤的最大冰点降低为-8.54°C,热滞为 7.71°C。有趣的是,除了对照样品外,所有蛋白处理的土壤样品在负温度下解冻(记录的最低温度为-0.85°C)。进一步分析表明,与多孔介质混合土壤相比,处理过的土壤在广泛的温度范围内冻结(1.25°C 对 0.51°C)和解冻(2.75°C 对 1.72°C)。这种冻结和解冻温度差是冰芯形成开始到完全冻结,以及所选不同培养天数的处理土壤样品的冰芯开始融化到完全融化的温度差。总的来说,本研究提出了一种使用嗜冷微生物控制易受霜冻影响的土壤中冰形成的新型生物介导方法。