Browsing by Author "Tutolo, Benjamin M"
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- ItemOpen AccessAlkalinity Generation Constraints on Basalt Carbonation for Carbon Dioxide Removal at the Gigaton-per-Year Scale(2021-08-20) Tutolo, Benjamin M; Awolayo, Adedapo; Brown, CalistaThe world adds about 51 Gt of greenhouse gases to the atmosphere each year, which will yield dire global consequences without aggressive action in the form of carbon dioxide removal (CDR) and other technologies. A suggested guideline requires that proposed CDR technologies be capable of removing at least 1% of current annual emissions, about half a gigaton, from the atmosphere each year once fully implemented for them to be worthy of pursuit. Basalt carbonation coupled to direct air capture (DAC) can exceed this baseline, but it is likely that implementation at the gigaton-per-year scale will require increasing per-well CO2 injection rates to a point where CO2 forms a persistent, free-phase CO2 plume in the basaltic subsurface. Here, we use a series of thermodynamic calculations and basalt dissolution simulations to show that the development of a persistent plume will reduce carbonation efficiency (i.e., the amount of CO2 mineralized per kilogram of basalt dissolved) relative to existing field projects and experimental studies. We show that variations in carbonation efficiency are directly related to carbonate mineral solubility, which is a function of solution alkalinity and pH/CO2 fugacity. The simulations demonstrate the sensitivity of carbonation efficiency to solution alkalinity and caution against directly extrapolating carbonation efficiencies inferred from laboratory studies and small-injection-rate field studies conducted under elevated alkalinity and/or pH conditions to gigaton-per-year scale basalt carbonation. Nevertheless, all simulations demonstrate significant carbonate mineralization and thus imply that significant mineral carbonation can be expected even at the gigaton-per-year scale if basalts are given time to react.
- ItemOpen AccessAssimilation of carbon and nitrogen by microbial mats from alkaline soda lakes(2020-11-19) Liu, Yihua; Strous, Marc; Hubert, Casey R J; Tutolo, Benjamin M; Hu, JinguangBackground:Soda lakes are extreme terrestrial ecosystems characterized by high pH, alkalinity, and sodium carbonate concentration. Despite the extreme environment, soda lakes host diverse microbial communities with high primary productivity, carried out by fast-growing phototrophic microbes such as cyanobacteria. In Goodenough Lake, a soda lake on the Cariboo Plateau in BC Canada, carbon isotope analysis indicated that the photosynthetic rate but not bicarbonate availability controlled carbon dioxide assimilation. However, the roles of individual cyanobacteria populations in carbon fixation remain unknown. Despite the rapid growth of microbial mat communities, common nitrogen sources, ammonium and nitrate, were detected only occasionally and in trace amounts in lake water. Mat communities may use alternative nitrogen sources like urea and dinitrogen gas as enzymes for urea assimilation and dinitrogen fixation were highly expressed.Objective:The objective is to measure carbon and nitrogen assimilation by microbial populations in mat communities.Approaches:Incubation of microbial mats from Goodenough Lake with heavy stable isotope labelled bicarbonate, and nitrogen sources, followed by isotope ratio mass spectrometry and proteomics.Results and conclusions:Over 90 different microbial populations were detected in microbial mat communities using proteomics. The sampled mat microbial communities were different from each other, even if samples were close together, but the most abundant populations were the same across samples. The two most abundant cyanobacterial populations exhibited different carbon fixation dynamics, and their abundance was negatively correlated, suggesting that they occupy different ecological niches. Among nitrogen sources, urea was consumed at the highest rate, followed by ammonia. The nitrate consumption rate was much lower, and the fixation of nitrogen was not detected. Urea was consumed mainly during the day. Rates for nitrate and ammonia consumption were similar during the day and the night.