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水介质中微生物诱导碳酸钙沉淀的长期可持续性。

Long-term sustainability of microbial-induced CaCO precipitation in aqueous media.

作者信息

Gat Daniella, Ronen Zeev, Tsesarsky Michael

机构信息

Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, P.O Box 653, Beer-Sheva 8410501, Israel.

Department of Environmental Hydrology and Microbiology, The Zuckerberg Institute for Water Research, Ben-Gurion University of the Negev, Sede-Boqer Campus, Sede-Boqer 8499000, Israel.

出版信息

Chemosphere. 2017 Oct;184:524-531. doi: 10.1016/j.chemosphere.2017.06.015. Epub 2017 Jun 7.

DOI:10.1016/j.chemosphere.2017.06.015
PMID:28622648
Abstract

Microbially induced CaCO precipitation (MICP) via urea hydrolysis is an emerging technique for soil amelioration, building materials rehabilitation and pollutants sequestration amongst other various environmental applications. The successful application of MICP requires the sustainability of the precipitated CaCO; to which the fate of ammonia, the main by-product of ureolysis, is potentially significante. Ammonia volatilization and biological ammonia oxidation both induce a pH decrease, which, in turn, might cause CaCO dissolution. To examine the potential effect of accumulated ammonia on precipitated CaCO, we conducted a long-term MICP batch experiment, using environmental enrichment cultures of ureolytic bacteria. Here we show that CaCO precipitation was completed within 15-27 days, along with a rise in ammonium concentration. Following completion of ureolysis and precipitation, ammonium concentrations decreased, leading to a pH decrease. About 30 days after precipitation was completed, as much as 30% CaCO dissolution, was observed. A two-step model, describing urea hydrolysis followed by the removal of ammonia from the precipitation solution, predicted CaCO dissolution due to ammonia volatilization. We suggest that ureolytic MICP might result in ammonia volatilization, leading to significant CaCO dissolution. These results provide basic insights into the sustainability of ureolytic MICP and should further encourage removal of the accumulated ammonia from the treated site.

摘要

通过尿素水解进行的微生物诱导碳酸钙沉淀(MICP)是一种新兴技术,可用于土壤改良、建筑材料修复和污染物封存等多种环境应用。MICP的成功应用需要沉淀的碳酸钙具有可持续性;而尿素分解的主要副产物氨的去向可能具有重要意义。氨的挥发和生物氨氧化都会导致pH值下降,进而可能导致碳酸钙溶解。为了研究积累的氨对沉淀碳酸钙的潜在影响,我们使用尿素分解细菌的环境富集培养物进行了长期的MICP批次实验。在此我们表明,碳酸钙沉淀在15-27天内完成,同时铵浓度升高。尿素分解和沉淀完成后,铵浓度下降,导致pH值降低。沉淀完成约30天后,观察到高达30%的碳酸钙溶解。一个描述尿素水解然后从沉淀溶液中去除氨的两步模型预测了由于氨挥发导致的碳酸钙溶解。我们认为尿素分解MICP可能导致氨挥发,从而导致大量碳酸钙溶解。这些结果为尿素分解MICP的可持续性提供了基本见解,并应进一步鼓励从处理过的场地去除积累的氨。

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