Considerable attention has been focused in recent decades on carbon dioxide emissions in view of detrimental environmental effects. In particular, two industries are a source of substantial carbon dioxide emissions: (1) Municipal and Industrial solid waste management and (2) Cement production. Municipal waste includes substantial quantities of organic material often referred to as organic municipal solid waste (MSW). Cement production is the most energy intensive phase of concrete generation. Both of these processes involve carbon dioxide (CO2) which can be leveraged for energy production and raw materials for concrete production.
A recycling and waste management process receives municipal solid waste (MSW) with substantial organic content to form a self-sustaining Hydrothermal Mineralization (HTM) process based on Supercritical Water Oxidation (SCWO) to receive supercritical steam and carbon dioxide with potential for electrical generation before forming calcium carbonate suitable for concrete production. Hydrothermal mineralization (HTM) provides a rapid elimination of organic wastes while simultaneously producing a non-emissive and thermally stable cement additive to act as a carbon sink. Hydrothermal mineralization (HTM) therefore provides a rapid disposal pathway for organic wastes, a green source of electricity and a final product that can be coupled with traditional and alternative cement productions to reduce carbon footprints of cement production.
Configurations herein are based, in part, on the observation that carbon dioxide sequestration and reduction is beneficial for environmental health. Excessive emissions of carbon dioxide from fossil fuel combustion and other causes has become a high profile concern for governments and environmentalists. Unfortunately, conventional approaches to carbon dioxide reduction focus on elimination of the source of CO2 generation through simply reducing output by urging or mandating elimination of sources, thus eliminating any benefits from the combustion as well. Accordingly, configurations herein substantially overcome the shortcomings of conventional approaches by providing a complementary consumer/receiver arrangement of CO2 related processes. MSW, itself posing environmental concerns by the need for disposal, feeds a SCWO process were, once water attains a supercritical state, a pathway for hydrothermal mineralization from CO2 generated from the SCWO feeds an HTM process for forming calcium carbonate directed to cement (concrete) production. Additionally, the high pressure water vapor and CO2 from the supercritical reaction can be used to power a turbine, or other use of vapor under pressure, prior to HTM.
In further detail, configurations herein present a method for obtaining calcium carbonate through mineralization of a waste stream, including heating an aqueous waste stream such as municipal solid waste to a temperature and pressure for attaining a supercritical state of the water, and reacting hydrocarbons in the waste stream with oxygen to form carbon dioxide and water resulting from supercritical water oxidation. A mineralization reaction combining the CO2 with calcium in the waste stream to form calcium carbonate, which is suitable for industrial and construction purposes such as concrete.
The foregoing and other objects, features and advantages of the invention will be apparent from the following description of particular embodiments of the invention, as illustrated in the accompanying drawings in which like reference characters refer to the same parts throughout the different views. The drawings are not necessarily to scale, emphasis instead being placed upon illustrating the principles of the invention.
The description below describes several configurations associated with the approach. Examples based on an experimental context are disclosed to illustrate the technical content of conversion of MSW to calcium carbonate and intermediate steps and compounds.
Supercritical water oxidation (SCWO) operates beyond the supercritical point of water (T>374° C., P>220 bar) under an oxidative environment to break down waste macromolecules to carbon dioxide in a matter of minutes. Due to the energy content of waste feeds (HHVfood waste=32.1 MJ/kg) the conversion to carbon dioxide is highly exothermic which means once steady state operation is achieved, the reaction requires no outside energy to operate. Once converted, the effluent stream is a high pressure, high temperature stream of supercritical carbon dioxide and water vapor. As an additional harvesting step, this stream can be expanded within a turbine to produce an excess of electricity that can be re-distributed back to the grid.
After leveraging the energy potential of the effluent stream, carbon dioxide will be sequestered in the form of calcium carbonate. This reaction takes place in an aqueous media under alkali conditions such that CO2 is converted to bicarbonate (HCO3−). From here, HCO3− will react with free calcium (Ca2+) to produce CaCO3. This conversion is thermodynamically favorable, however, the dissolution of CO2 into water to form HCO3− tends to be a rate limiting step. By leveraging the high pressure and purity of the effluent gas from the SCWO reaction, the disclosed approach overcomes issues surrounding dissolution rates.
Thus, the CO2 combines with calcium in the waste stream to form calcium carbonate.
Of the 292 million tons of MSW generated in the United States, more than 70% are a form of organic waste. Most MSW organics retain a varying amount of water. Unlike traditional waste-to-energy processes such as incineration, hydrothermal methods such as SCWO can take wet organic wastes because the working fluid is water, resulting in a positive energy balance when other processes require energy inputs.
The full benefit of integrating the disclosed approach depends on the feed being used. This proposal is based on using food waste which is only 20% of all MSW generated in the United States. With full conversion, food waste could offset nearly 20% of the national demand for CaCO3.
The disclosed approach therefore integrates SCWO and mineralization to produce CaCO3. The approach serves at least three needs or industries: 1) CaCO3 production, 2) Developers of CO2 sequestration technologies, and 3) Waste management industries.
In conventional approaches, CaCO3 demand is primarily satisfied in one of two forms. First is the mining of limestone directly. This production process revolves around mining limestone from open quarries or underground mines at which point it is ground down to a desired particle size. Secondly, is the precipitation of CaCO3. Typically, precipitated calcium carbonate (PCC) is formed by hydrating, or slaking, quicklime (CaO) which has already been of a CO2 molecule to form calcium hydroxide (Ca(OH)2). CO2 can then be converted to HCO3− and then react to form CaCO3. Both of these conventional processes ultimately require the mining of CaCO3 because quicklime is formed through the calcination of CaCO3 and produces nearly 1.3 kg of CO2/kg of CaO. To return to CaCO3 the emissions are slightly improved to ˜1 kg CO2/kg of PCC. In contrast, the disclosed approach requires no mining of CaCO3, nor any soluble form of calcium and alkali environment. An example configuration employs calcium chloride (CaCl2)) and sodium hydroxide (NaOH) as calcium and base sources, respectively. The use of traditional NaOH production our model shows a similar emission rate of ˜1 kg CO2/kg PCC. However, if greener energy sources (i.e., solar, wind, biomass, etc.) are considered, it can be seen that this approach can actually reduce emissions by 50% down to 0.5 kg CO2/kg PCC.
One approach is Direct Air Capture (DAC)/Point Source Capture (PSC), where the purpose for DAC and PSC technologies is to either remove or concentrate dilute CO2 from the atmosphere or process flue gas. These processes are broken down into two main chemistries: 1) Mineralization and 2) Amine-based.
Mineralization focuses on the permanent removal of CO2 through the formation of CaCO3 or MgCO3, two insoluble and thermally stable minerals. Deployed facilities have employed mineralization technology for DAC and purport to remove substantial quantities of CO2 per year. However, since the disclosed approach pulls from a carbon-dense feed, removal efficiency is projected to be substantially greater than DAC if utilizing waste on a sufficiently large scale, depending on the moisture and carbon content of the process feed.
Once landfilled, organic wastes are destined to degrade to CO2 and CH4 and are a significant Greenhouse Gas (GHG) emitter, shown by ratio 302. Traditional PCC production is often circular since it begins and ends with the mining of CaCO3, shown as ratio 304. A particular configuration disclosed herein provides linear and finite end of life for food waste as CaCO3 that is comparable to traditional PCC emissions, shown as ratio 306, however through the use of renewable energy sources (i.e., solar, wind, etc.), emissions can be reduced by 50%, shown as ratio 308.
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In the example configuration, the waste stream is an organic waste stream, and the containment is employed to commence a supercritical water oxidation (SCWO) reaction through heating to at least 373° C. at a pressure of at least 220 bar in an oxidative environment to generate CO2. The gaseous stream of carbon dioxide and water may be harvested by connecting a vessel or turbine input to the containment for powering an external load prior to mineralization. By engaging a vessel or conduit to the containment for receiving pressurized gases including carbon dioxide and water vapor, high pressure steam is available for powering a mechanical load.
Beyond mineralization, amine-based removal has proven to be effective at stripping CO2 from gas streams. However, amine reactions are reversible which limits their ability to sequester CO2. Amine-based removal is better for used for purification and transportation of CO2. Further amines are expensive and corrosive, making them impractical for many applications. Conventional approaches have not coupled SCWO and mineralization in this manner to produce CaCO3. The CO2 becomes effectively sequestered in bicarbonate, and then mineralization consumes the CO2 and free calcium to generate the calcium carbonate.
For 150 psi, between 20-120 minutes the process begins to plateau at ˜10% conversion. This is a result of being sub stoichiometric in base and the pH dropping below 5.5. With stoichiometric amounts of base to Ca2+ the process yields complete or near complete conversion. Once supercriticality is obtained, mineralizing becomes a self-sustaining, spontaneous reaction having a negative delta G.
While the system and methods defined herein have been particularly shown and described with references to embodiments thereof, it will be understood by those skilled in the art that various changes in form and details may be made therein without departing from the scope of the invention encompassed by the appended claims.
This patent application claims the benefit under 35 U.S.C. § 119 (e) of U.S. Provisional Patent App. No. 63/471,598, filed Jun. 7, 2023, entitled “LIMESTONE PRODUCTION,” incorporated herein by reference in entirety.
This invention was developed with U.S. Government support under contract No. DE-EE0009507, awarded by the Department of Energy. The Government has certain rights in the invention.
Number | Date | Country | |
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63471598 | Jun 2023 | US |