The ocean is a large sink of atmospheric carbon dioxide (CO2) since it can uptake 25% of the emitted CO2 by human activities (i.e., about 2 petagrams of carbon per year)1. Ocean iron fertilization (OIF) is one of several proposed methods to sequestrate atmospheric CO2 and mitigate its effect on the global climate2. Releasing iron at the upper level of the ocean (e.g., within the first 100 meters from the surface) stimulates the growth rate of phytoplankton, which are bacteria, protists, and plants in some areas of the ocean. Phytoplankton consume the atmospheric CO2 and release oxygen (O2) using photosynthesis. The consumed CO2 is proportional to the growth rate of phytoplankton, which depends on the available nutrients in the ocean such as iron. Experimental measurements have shown that increasing the iron concentration by 2 nM could almost double the specific growth rate of phytoplankton3. The expansion in the ecosystem of phytoplankton is proportional to the CO2 uptake in the ocean2,4,5 since the photosynthesis process is linearly proportional to the phytoplankton's cell volume5. This can have a major positive impact on global warming and climate change by stimulating the carbon (C) sequestration by expanding the growth and uptake of CO2 by phytoplankton and assuming that some fraction of the carbon reaches the deep ocean where it is stored for long periods of time out of contact with the atmosphere. For this purpose, earlier studies proposed different approaches to enhance the iron availability in the ocean for phytoplankton. Lauderdale et al.—2020 hypothesized that binding the ocean iron with organic molecules enhances the iron bioavailability6. The authors claim that this approach could form a reinforcing cycle between the biological activity of phytoplankton and iron cycling. However, this approach focuses only on the iron cycling in the ocean rather than increasing the ocean iron concentration through fertilization. Alternatively, Emerson-2019 proposed using biogenic iron dust for OIF7. The dust is made from Fe-oxides, which are produced by chemosynthetic iron-oxidizing bacteria. Then the formed dust would be dispersed, at altitude by an aircraft, into the open ocean. The author highlights that an extensive campaign of laboratory testing is needed to investigate the reactivity of the proposed biogenic oxide in both the atmosphere and the ocean. Therefore, in addition to the complexity of this approach, there could be restrictive legalization of dispersing dust in the atmosphere due to its unknown effect on atmospheric chemistry. To sum up, there is no well-established technique that has been optimized for the process of using OIF for C sequestration. Therefore, it would be desirable to find an efficient technique for OIF. Various embodiments disclosed herein relate to techniques combining both OIF and hydrogen (H2) gas generation in seawater using electrochemical reactions.
In accordance with one or more embodiments, a novel offshore mobile platform is disclosed for OIF and H2 gas generation using electrochemical processes. The platform uses an iron or iron-producing anode to generate ferrous iron for phytoplankton via electrolysis. In addition, the electrochemical reaction at the cathode produces H2 and hydroxide (OH—) species. The generated H2 gas at the cathode side is collected and stored on the platform for future reuse as a fuel (e.g., an energy source for the platform or transfer to onshore). The produced OH-increases the alkalinity of the ocean. Alternatively, the generated OH— can be converted to oxygen (O2) gas and coupled with any possible oxygen evolution at the anode as part of the iron electrolysis. The platform and its reactions can be powered by a variety of energy sources, including traditional electric sources (e.g., mechanical power generator or charged batteries onboard the platform or ship), renewable energy sources (e.g., solar, tidal, blue energies), or by reusing the generated and stored H2 as a fuel.
The design of the mobile platform provides extensive control over handling, transport, and running the platform. The platform can be either self-operated and free-standing in the ocean (i.e., floating and driven by the ocean current), or tugged by an external device such as a ship, underwater remote operating vehicle (ROV), or any floating device. Alternatively, the platform can be installed onboard a ship and carried out across the ocean to distribute the generated iron over a large scale. In these different scenarios, the electrodes can be either submerged or floating. Further, the electrode configuration and stacking can have various designs to provide more flexibility in handling the electrochemical reactions. The variety in selecting the shape and configuration of the electrode offer high flexibility, including applying the electrochemical process in a one-, two-, or three-dimensional (i.e., 1D, 2D, or 3D) arrangement, and handling the electrode offshore. Moreover, the electrochemical processes within the platform can be temporally varying to ensure efficient OIF and avoid any saturation in the growth rate of phytoplankton. This allows more accessibility to control the reaction and supply rates. For example, the OIF process can be applied continuously, intermittently (e.g., applied, stopped, or reversed in polarity over time), or as a function of time (e.g., simple pulse/alternating function). The applied current can be controlled by using a power supply unit on the platform. This electrochemical platform offers a wide range of flexible and dynamic features that allow the implementation and engineering of different processes. For example, the platform functionality is not restricted to OIF and H2 production but can be used in other electrochemical applications such as seawater desalination, blue energy harvesting, or mineral extraction.
At the anode 10, iron electrolysis takes place using either an iron or iron-production electrode. The standard potential of this electrolysis reaction is 0.44 V2. The reaction is given as:
Fe(s)→Fe(aq)+2+2e−.
In addition, O2 evolution reaction can occur at the anode as follows:
2H2O(l)→O2(g)+4H(aq)++4e−.
The generated oxygen gas can be collected and stored. Or, it can leave the ocean surface to the atmosphere.
At the cathode 12, seawater splitting takes place to produce H2 gas. The produced gas is be collected and stored using the installed tank at the platform as shown in
2H2O+2e−→H2(g)+2OH(aq)−.
The formed OH— increases the water's alkalinity. The overall reactions at the anode 10 and cathode 12 can involve additional secondary reactions as will be discussed below.
These electrochemical reactions are electrically powered by either a traditional electrical generator, a renewable energy device (e.g., solar PV cells 26, a tidal turbine 28, blue energy harvesting), or by reusing the generated hydrogen as fuel.
The electrodes 10, 12 can have various configurations and shapes to optimize the electrochemical processes and the engineering of the platform. The anode 10 and cathode 12 can be installed in various facing orientations such as vertical or horizontal configurations as exhibited in
For material selection, the anode 10 can be made from either iron or iron-producing materials. The cathode 12 can be made from iron, steel, or any other material. Both the anode 10 and cathode 12 can be made from iron with polarity reversal3. Additional materials, if necessary, can be used to enhance the chemical conditions such as using Aluminum. Finally, the electrolysis reaction and its mass transfer rate can be primarily controlled by manipulating the applied current at the electrodes. Continuous, intermittent, or time-varying current profiles can be applied. For example, a simple pulse current or temporal function of current application/reversal can be controlled using a controller associated with the power supply unit at the platform.
We computed the needed iron and electricity to increase the ocean iron concentration within the experimentally reported values4. We aim to increase the ferrous iron concentration (Fe+2) by 1 nM over a surface area of 100×100 km and depth of 30 m. Therefore, we performed theoretical analysis as follows:
where t is the reaction's time which is assumed to be five years (i.e., t=15.77×107s), Mw is the molecular mass of iron, n is the number of participating electrons, and F is Faraday's constant. Therefore, the needed current is I=(2×96,485 C/mole)×3×105 mole/(15.77×107s)=367 A.
We can install a 20 kW PV system of series panels to obtain the needed current. By assuming that each panel can output a current of ˜6-8 A, we roughly need about 70 panels to power the platform. The 70 panels will have a total equivalent area of 1400 sq ft with a cost of ˜$55,000. These calculations show the feasibility of our practical invention. We should highlight that the needed 16.75 tons can be supplied by running several platforms at the same time. This will reduce the overall needed time to complete the OIF process.
The main electrochemical reactions in the platform are shown in
Several approaches can be implemented to enhance the bioavailability of the produced iron at the anode 10. First, the electrode materials can be optimized to control the electron transfer and surface polarization conditions. For example, layered7 or hybrid electrodes can be used to enhance the chemical conditions if necessary. An array of alternating rods (e.g., Fe—Al—Fe—Al- . . . etc) can be used to improve the reaction conditions as shown in
Understanding the bioavailability and the reaction conditions of OIF and H2 gas production in seawater is crucial to engineer and optimize the efficiency of the platform. Computational tools can be used to investigate the fundamental aspects of these conditions. We can use computational chemistry simulations to study the molecular and atomistic features of the interacting chemical species. Also, computational fluid dynamics can be coupled with the ecosystem characteristics to model the chemical rates and transport of the produced chemical species in the ocean. The coupled ecosystem models can involve the growth and CO2 capturing by the phytoplankton system.
Having thus described several illustrative embodiments, it is to be appreciated that various alterations, modifications, and improvements will readily occur to those skilled in the art. Such alterations, modifications, and improvements are intended to form a part of this disclosure, and are intended to be within the spirit and scope of this disclosure. While some examples presented herein involve specific combinations of functions or structural elements, it should be understood that those functions and elements may be combined in other ways according to the present disclosure to accomplish the same or different objectives. In particular, acts, elements, and features discussed in connection with one embodiment are not intended to be excluded from similar or other roles in other embodiments. Additionally, elements and components described herein may be further divided into additional components or joined together to form fewer components for performing the same functions. Accordingly, the foregoing description and attached drawings are by way of example only, and are not intended to be limiting.
This application claims priority from U.S. Provisional Patent Application No. 63/288,771 filed on Dec. 13, 2021 entitled Offshore Mobile Platform for Electrochemical Ocean Iron Fertilization & Hydrogen Gas Generation, which is hereby incorporated by reference.
Number | Date | Country | |
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63288771 | Dec 2021 | US |