Surface Treatment of Rammed Earth Heritage Sites Using MICP Technology: An Investigation of Rainwater Erosion Resistance via Indoor Experiments and In Situ Testing

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-10-19 DOI:10.1155/2024/2083124
Liang Liu, Yun Zhang, Wanting Chen, Haiying Cao, Lianjun Guo, Lingling Zheng, Tianli Li, Rong Shu, Dongdong Li
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Abstract

Rammed earth, a commonly used building material in ancient times, differs from natural sedimentary layers in that it is more compact. Buildings constructed from historical rammed earth sites frequently encounter the issue of rainwater erosion. Microbially induced calcium carbonate precipitation (MICP) is commonly applied to sand soil treatment, yet reports on its use for stabilizing rammed earth are scarce. This study focused on the rammed earth of the Shanhaiguan Great Wall and explored the efficacy of MICP in mitigating rain erosion through permeation tests, splash experiments, and scouring trials. The findings indicate that the forms of rain erosion damage under MICP treatment vary across different operational conditions. In laboratory experiments, as the concentration of the cementation solution increases, the amount of calcium carbonate crystals also increases. However, the permeability, splash resistance, and rain erosion resistance initially increase and then decrease. When the cementation solution concentration is 1.0 mol/L, the penetration rate is the highest, lasting 712.55 s. The splash pit rate is the lowest, at only 1.2 mm, and the soil erosion rate is the lowest, at only 4.13%. The rain erosion resistance in the field test exhibit the same trend, and the optimal concentration is 1.2 mol/L. The optimal concentration mechanism involves the aggregation of calcium carbonate crystals at suitable cementation solution concentrations, which begin to fill the soil particle pores, effectively resisting rainwater erosion. At lower concentrations of the cementation solution, calcium carbonate crystals are merely adsorbed by soil particles without blocking the pores. Due to the high compressibility of rammed earth, which results in lower porosity, a higher concentration of the cementation solution leads to rapid pore clogging by excessive calcium carbonate crystals, which accumulate on the surface to form a white crust layer. The MICP technique can effectively alleviate rainwater erosion in rammed earth, and the optimal concentration needs to be tailored to the porosity of the rammed earth. This mechanism was also validated in field scouring experiments on the Shanhaiguan Great Wall’s rammed earth.

Abstract Image

利用 MICP 技术对夯土遗址进行表面处理:通过室内实验和现场测试研究抗雨水侵蚀能力
夯土是古代常用的建筑材料,它与天然沉积层的不同之处在于它更加密实。用夯土建造的建筑经常会遇到雨水侵蚀的问题。微生物诱导碳酸钙沉淀法(MICP)通常用于砂土处理,但将其用于稳定夯土的报道却很少。本研究以山海关长城的夯土为研究对象,通过渗透试验、飞溅试验和冲刷试验,探讨了微生物诱导碳酸钙沉淀法在减轻雨水侵蚀方面的功效。研究结果表明,在不同的运行条件下,MICP 处理对雨水侵蚀的破坏形式各不相同。在实验室实验中,随着固结溶液浓度的增加,碳酸钙晶体的数量也随之增加。然而,渗透性、抗飞溅性和抗雨水侵蚀性最初会增加,然后会降低。当胶结溶液浓度为 1.0 mol/L 时,渗透率最高,持续时间为 712.55 秒。溅坑率最低,仅为 1.2 mm,土壤侵蚀率最低,仅为 4.13%。实地试验中的抗雨水侵蚀能力也呈现出同样的趋势,最佳浓度为 1.2 mol/L。最佳浓度的机理是碳酸钙晶体在适当的固结溶液浓度下聚集,开始填充土壤颗粒孔隙,从而有效抵抗雨水侵蚀。在较低浓度的固结溶液中,碳酸钙晶体只是被土壤颗粒吸附,不会堵塞孔隙。由于夯土的压缩性较高,孔隙率较低,如果胶结溶液的浓度较高,过多的碳酸钙晶体就会迅速堵塞孔隙,并在表面堆积形成白色结壳层。MICP 技术可有效缓解夯土中的雨水侵蚀,但最佳浓度需要根据夯土的孔隙率来确定。这一机制也在山海关长城夯土的实地冲刷实验中得到了验证。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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