Casas Carla C, Graf Alexander, Brüggemann Nicolas, Schaschke Carl J, Jorat M Ehsan
School of Applied Sciences, Abertay University, Dundee, United Kingdom.
Institute for Bio- and Geosciences, IBG-3: Agrosphere, Forschungszentrum Jülich, Jülich, Germany.
Front Microbiol. 2020 Sep 8;11:557119. doi: 10.3389/fmicb.2020.557119. eCollection 2020.
Microbial-Induced Calcite Precipitation (MICP) stimulates soil microbiota to induce a cementation of the soil matrix. Urea, calcium and simple carbon nutrients are supplied to produce carbonates via urea hydrolysis and induce the precipitation of the mineral calcite. Calcium chloride (CaCl) is typically used as a source for calcium, but basic silicate rocks and other materials have been investigated as alternatives. Weathering of calcium-rich silicate rocks (e.g., basalt and dolerite) releases calcium, magnesium and iron; this process is associated with sequestration of atmospheric CO and formation of pedogenic carbonates. We investigated atmospheric carbon fluxes of a MICP treated sandy soil using CaCl and dolerite fines applied on the soil surface as sources for calcium. Soil-atmosphere carbon fluxes were monitored over 2 months and determined with an infrared gas analyser connected to a soil chamber. Soil inorganic carbon content and isotopic composition were determined with isotope-ratio mass spectrometry. In addition, soil-atmosphere CO fluxes during chemical weathering of dolerite fines were investigated in incubation experiments with gas chromatography. Larger CO emissions resulted from the application of dolerite fines (116 g CO-C m) compared to CaCl (79 g CO-C m) but larger inorganic carbon precipitation also occurred (172.8 and 76.9 g C m, respectively). Normalising to the emitted carbon to precipitated carbon, the environmental carbon cost was reduced with dolerite fines (0.67) compared to the traditional MICP treatment (1.01). The carbon isotopic signature indicated pedogenic carbonates (δC = -8.2 ± 5.0‰) formed when dolerite was applied and carbon originating from urea (δC = -46.4 ± 1.0‰) precipitated when CaCl was used. Dolerite fines had a large but short-lived (<2 d) carbon sequestration potential, and results indicated peak CO emissions during MICP could be balanced optimising the application of dolerite fines.
微生物诱导碳酸钙沉淀(MICP)刺激土壤微生物群,促使土壤基质发生胶结作用。通过提供尿素、钙和简单的碳养分,经尿素水解产生碳酸盐,从而诱导矿物方解石沉淀。氯化钙(CaCl)通常用作钙源,但碱性硅酸盐岩石和其他材料也已作为替代物进行了研究。富含钙的硅酸盐岩石(如玄武岩和辉绿岩)的风化会释放钙、镁和铁;此过程与大气CO的固存和成土碳酸盐的形成有关。我们研究了使用CaCl和施加在土壤表面的辉绿岩细粉作为钙源时,经MICP处理的砂质土壤的大气碳通量。在2个月内监测土壤-大气碳通量,并通过连接到土壤箱的红外气体分析仪进行测定。用同位素比率质谱法测定土壤无机碳含量和同位素组成。此外,在气相色谱的培养实验中,研究了辉绿岩细粉化学风化过程中的土壤-大气CO通量。与CaCl(79 g CO-C m)相比,施加辉绿岩细粉(116 g CO-C m)导致更大的CO排放,但也发生了更大的无机碳沉淀(分别为172.8和76.9 g C m)。将排放的碳归一化为沉淀的碳后,与传统的MICP处理(1.01)相比,辉绿岩细粉的环境碳成本降低(0.67)。碳同位素特征表明,施加辉绿岩时形成了成土碳酸盐(δC = -8.2 ± 5.0‰),使用CaCl时沉淀出源自尿素的碳(δC = -46.4 ± 1.0‰)。辉绿岩细粉具有较大但短暂(<2天)的碳固存潜力,结果表明,在MICP过程中,通过优化辉绿岩细粉的施用,可以平衡CO排放峰值。