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Kalina cycle

The Kalina cycle is a thermodynamic power generation that employs a working fluid consisting of and to convert low- to medium-temperature heat sources (typically below 400°C) into , achieving thermal efficiencies 15–50% higher than conventional Rankine cycles through better thermal matching via variable boiling and condensation temperatures during phase changes. Invented by Aleksandr I. Kalina in the mid-1980s, the was developed as an to single-component fluid cycles like the Rankine or (ORC), particularly for recovery where traditional systems suffer from low efficiency due to mismatched temperature profiles. In operation, the ammonia-water mixture—often around 70% and 30% —is heated in a , where vaporizes preferentially owing to its lower (approximately -33°C compared to 's 100°C at standard pressure), producing a high-concentration vapor that drives a high-pressure for power generation. The remaining water-rich liquid is separated via a and , then recombined after a low-pressure stage to facilitate recuperative preheating, before in a cooler and repressurization by a to close the loop; this process enables a gliding temperature change that closely follows the heat source's profile, minimizing losses. The cycle's advantages include reduced fuel consumption leading to 15–20% lower emissions of , , and compared to Rankine systems, as well as lower of $1,100–$1,500 per kW for installations under 10 MW, making it suitable for decentralized power production. It excels in recovering from like steelworks, cement kilns, and gas turbine exhausts, as well as in geothermal and applications, with demonstrated efficiencies up to 25% for heat sources around 100–200°C where systems might achieve only 10–15%. Key commercial deployments highlight its viability, including a 4.5 MW in Fukuoka, Japan, operational since 1999, a 2 MW geothermal facility in , , since 2000, and a 3.5 MW unit at the Kashima steelworks in since 1999, collectively proving its reliability and scalability for global improvements.

Overview

Definition and Principles

The Kalina cycle is a designed for converting low- to medium-temperature into mechanical power, utilizing a binary mixture such as ammonia-water. This cycle operates by leveraging the properties of a zeotropic mixture, where the working fluid exhibits a composition-dependent and behavior over a range of temperatures rather than at a single point. The core principle of the Kalina cycle relies on the zeotropic mixture's ability to achieve better matching with variable-temperature heat sources and sinks, thereby minimizing losses during heat transfer processes. In contrast to single-component fluids in traditional , the ammonia-water mixture allows for a glide during and , which reduces irreversibilities and enhances overall . This variable characteristic enables more effective utilization of heat from sources like or geothermal fluids in the 100–200°C range. Operationally, the cycle involves pressurizing the mixture, heating it to produce vapor-rich phases for expansion in a to generate power, followed by separation, condensation, and recombination to recycle the fluid. For low-temperature sources (100–200°C), the Kalina cycle typically achieves efficiencies of 15–20%, representing an improvement of 10–50% over conventional Rankine cycles in comparable applications due to its superior heat recovery.

Key Advantages

The Kalina cycle offers significant efficiency improvements over the conventional , particularly for low-temperature sources below 200°C, where it can achieve 10–50% higher . This gain stems from the zeotropic properties of the ammonia-water mixture, which enable a closer match between the and the source in the , minimizing losses due to reduced differences in heat exchangers. As a result, the cycle extracts more usable energy from low-grade , such as industrial exhaust or geothermal fluids, compared to steam-based systems that suffer from larger pinch points and irreversibilities. A key advantage is the cycle's operational flexibility, achieved through adjustable concentrations of the , allowing adaptation to fluctuating heat source temperatures without requiring major system redesigns. By varying the mixture composition—typically between 50% and 90% —the boiling and condensation processes can be tuned to match variable inlet conditions, such as seasonal changes in geothermal output or intermittent heat, enhancing overall system responsiveness and utilization rates. The Kalina cycle also provides reduced complexity relative to gas-steam combined cycles while approaching similar levels, with reported net efficiencies up to 50% in optimized configurations for recovery. Unlike multi-stage combined setups that demand separate gas and turbines, the Kalina cycle integrates power generation in a single loop using a binary fluid, simplifying installation and maintenance for low- to medium-grade heat applications. Environmentally, the cycle contributes to lower per generated in scenarios by maximizing from existing thermal streams, thereby reducing the need for additional fossil fuel-based power. The ammonia-water mixture is non-ozone-depleting and has a low , avoiding the environmental drawbacks of synthetic refrigerants used in some alternative cycles. Economically, the Kalina cycle features lower for low-grade heat recovery systems, primarily due to smaller sizes enabled by the efficient temperature gliding of the . In industrial settings, such as or plants, payback periods can range from 3 to 5 years in optimized configurations, driven by higher power output and reduced operational expenses compared to organic Rankine cycles.

Thermodynamic Principles

Cycle Processes

The Kalina cycle is a closed-loop that utilizes an ammonia-water mixture as the to convert low-grade into mechanical power, with key steps involving addition, , , and recombination. The cycle's stems from the zeotropic nature of the mixture, which allows for a temperature glide during and , better matching the heat source and sink profiles and reducing destruction. A is often incorporated to control the composition of the vapor by distilling the mixture prior to , ensuring optimal enrichment in the vapor stream. The cycle begins with heat addition in the , where the high-pressure liquid is heated and undergoes over a temperature range (process 4-1 in typical numbering), transitioning from subcooled liquid to a two-phase with the component vaporizing preferentially due to its higher . This nonlinear curve on the temperature-entropy (T-s) diagram reflects the zeotropic behavior, where the and temperatures differ, enabling progressive heat absorption that minimizes irreversibilities compared to isothermal phase changes in pure cycles. The resulting two-phase then enters a , where the ammonia-rich vapor is isolated from the water-rich liquid. The ammonia-rich vapor from the separator undergoes isentropic expansion in the turbine (process 1-2), converting into mechanical work while dropping to lower ; during this expansion, partial may occur as the enters the wet region, with the exiting stream being a vapor-liquid at lower and . The separated water-rich liquid is throttled isenthalpically to the low (process 3-4), maintaining its nearly constant while reducing , before it is directed to the absorber for recombination. The turbine exhaust is cooled in a , rejecting to the environment and fully condensing the ammonia-rich portion. In the absorber, the throttled water-rich liquid absorbs the condensed ammonia-rich stream from the , recombining into a uniform mixture at intermediate concentration, which is then pumped back to for preheating in a before returning to the to close the loop. On the T-s diagram, the process exhibits a glide similar to but in reverse, with the nonlinear curves for both phases ensuring closer matching to the cooling medium, further minimizing losses; overall, the diagram illustrates a rounded shape with reduced area under the curve for rejection relative to traditional Rankine cycles using pure fluids.

Working Fluid Characteristics

The primary working fluid employed in the Kalina cycle is an ammonia-water binary mixture, typically comprising 50-80% ammonia by mass fraction. This composition is selected for its advantageous thermophysical properties, including a high latent heat of vaporization and a pronounced temperature glide during evaporation and condensation, which enable superior thermal matching with variable-temperature heat sources compared to single-component fluids like water or pure ammonia. The displays zeotropic behavior, characterized by non-isothermal phase changes where the and differ, resulting in a glide of up to several tens of degrees depending on and concentration. Specifically, the saturation decreases with increasing concentration at a given , allowing the mixture to absorb more gradually and closely follow the profile of the heat source. This zeotropic nature also supports in the cycle's phase separator, where the vapor phase becomes enriched in (often exceeding 90% mass fraction) while the liquid remains depleted, facilitating efficient separation without additional energy input. Key thermophysical attributes of the ammonia-water mixture include an effective that exceeds that of pure components in the relevant operating ranges, aiding in transfer during preheating and desuperheating stages. The critical point varies with ammonia mass fraction, spanning from approximately 132°C and 11.3 for pure to 374°C and 22.1 for pure , which permits subcritical operation across low- to medium-temperature applications (typically below 200°C) without entering the supercritical regime. While the ammonia-water mixture remains the standard due to its commercial availability and manageable handling in closed systems, alternative working fluids such as zeotropic blends (e.g., propane-isobutane) or other pairs have been investigated for specific conditions, though they have not achieved widespread adoption owing to compatibility and performance trade-offs. Optimization of the concentration, commonly tuned to around 70% for many configurations, maximizes the cycle's approach to the Carnot , often reaching up to 70% relative by aligning the mixture's glide with the heat source profile.

System Design

Main Components

The , often integrated with a in Kalina cycle systems, serves as the primary absorption component where the ammonia-water mixture is heated and partially boiled using a low-grade source, such as or geothermal fluids. This process occurs over a temperature range due to the zeotropic nature of the mixture, enabling better thermal matching with the source compared to single-component fluids. Design typically employs a counterflow configuration to maximize efficiency, with the section preheating the incoming lean mixture using residual from the exhaust before it enters the main zone. The is a gravity-based or mechanical device positioned after the , functioning to divide the two-phase - mixture into an ammonia-rich vapor stream, which proceeds to the for work extraction, and a -rich stream, which is throttled and directed toward the absorber. This separation exploits the differing volatilities of and , typically achieving a dryness around 0.3 at the , and is designed as a simple vertical vessel to minimize losses while ensuring purity for downstream processes. The , or expander, extracts mechanical work from the high-, ammonia-enriched vapor exiting the by expanding it to lower , driving a for power output. It is usually implemented as a single-stage suitable for the relatively low drops in Kalina cycles, with inlet conditions often around 35-50 and 160°C, and designed for high isentropic efficiency to handle the wet vapor without excessive . The and absorber work in tandem at the cycle's low-temperature, low- end to recombine the vapor and liquid phases of the . The absorber mixes the exhaust vapor with the throttled water-rich liquid, facilitating ammonia absorption into the through cooling with an external medium like cooling , while the handles any residual vapor ; this combined often includes provisions for a desorber to strip trace ammonia from the lean solution, ensuring complete phase recombination and minimizing losses. Designs emphasize adiabatic mixing in the absorber to temperature rise, with rejection via shell-and-tube exchangers. The pump, or compressor in some variants, recirculates the recombined lean ammonia-water mixture from the absorber back to the evaporator by increasing its pressure from the condenser outlet (typically 1-4 bar) to the high-side operating pressure (e.g., 35-50 bar). Due to the predominantly liquid state of the fluid, it requires relatively low power input and is designed with high isentropic efficiency, often as a centrifugal pump to handle the solution's properties without cavitation. Auxiliary components enhance overall efficiency, including the rectifier column, which purifies the ammonia-rich vapor post-separator or evaporator by fractional distillation to remove residual water, producing a higher-concentration vapor for the turbine without additional external heat; it is typically a packed or tray column operating on the sensible heat of the incoming mixture. The solution heat exchanger recovers internal heat between the strong (ammonia-rich) solution leaving the absorber and the weak (water-rich) solution returning from the separator, preheating the former to reduce evaporator duty; this is usually a counterflow plate or shell-and-tube exchanger integrated into the cycle piping.

Typical Configurations

The basic single-effect configuration of the Kalina cycle employs a closed loop comprising an , , , , and , where the ammonia-water mixture is heated in the evaporator, separated into vapor and liquid streams, expanded through the turbine for power generation, condensed, and pumped back to the evaporator. This layout is particularly suitable for small-scale recovery applications, such as those ranging from 50 kW to 5 MW, including with moderate sources. A common enhancement is the recuperated design, which incorporates an internal —often positioned between the exhaust and the incoming mixture—to recover heat from the hot process stream to the cold return stream, thereby improving overall system performance by approximately 5-10%. This configuration maintains the core loop of the basic setup while adding the to minimize losses, making it ideal for applications where heat source temperatures are between 100°C and 300°C, such as exhaust. Multi-stage variants extend the basic design by incorporating series evaporators or multiple separators and mixers, allowing the cycle to accommodate broader temperature ranges in the heat source by stepwise and . These setups, such as the KC12 with dual recuperators and condensers, are commonly applied in generation, where variable fluid temperatures require phased heat absorption to optimize matching with the source profile. In bottoming cycle setups, the Kalina cycle is integrated downstream of an existing power plant to utilize low-grade exhaust heat, forming a combined system where the Kalina captures residual thermal energy from the Rankine or stack gases. The flow arrangement typically includes 4-6 major loops: the primary Rankine steam loop (boiler-turbine--pump), the Kalina loop (-separator-turbine--pump), an absorption/mixing path for the ammonia-water blend, and interconnecting conduits between the cycles, enabling enhanced overall plant output without major modifications to the host system. Scale adaptations of these configurations allow the Kalina cycle to fit diverse deployment needs; micro-scale systems under 100 kW, often based on the basic or recuperated layouts, support in remote or small industrial settings like utilization. In contrast, utility-scale implementations exceeding 10 MW incorporate multi-stage or bottoming designs with multiple turbines in parallel or series to handle larger heat inputs, such as those from combined-cycle gas plants.

Performance and Efficiency

Theoretical Analysis

The of the Kalina cycle is defined as \eta = \frac{W_{\text{net}}}{Q_{\text{in}}} = 1 - \frac{Q_{\text{out}}}{Q_{\text{in}}}, where W_{\text{net}} represents the net work output, calculated as the work minus the work, and Q_{\text{in}} and Q_{\text{out}} are the heat input and rejection, respectively. This formulation derives directly from the first law of applied to the closed cycle, assuming steady-state conditions and negligible kinetic and changes. Exergy efficiency provides a second-law perspective, expressed as \eta_{\text{ex}} = 1 - \frac{I}{E_{\text{in}}}, where I denotes the total exergy destruction across cycle components and E_{\text{in}} is the exergy input from the heat source. This metric underscores the Kalina cycle's advantage in minimizing irreversibilities through better temperature matching between the working fluid and the heat source, resulting in lower exergy losses compared to single-component cycles. The working fluid, an ammonia-water , exhibits non-ideal characterized by T_b = f(x_{\text{NH}_3}) and dew point T_d = f(x_{\text{NH}_3}), where x_{\text{NH}_3} is the ammonia mass fraction. The glide \Delta T = T_d - T_b typically ranges from 20–50°C for optimal mixtures, enabling closer thermal matching during heat addition and rejection. For low-temperature heat sources, the Kalina cycle approximates 70–80% of the Carnot efficiency, outperforming the Rankine cycle's typical 50% attainment due to the 's variable boiling characteristics. Accurate of the cycle necessitates iterative numerical methods to handle the non-ideal vapor-liquid of the , often employing the Peng-Robinson .

Practical Considerations

The ammonia-water working fluid in the Kalina cycle is highly corrosive, particularly due to its alkaline nature ( approximately 12.3 at ambient conditions), necessitating the use of corrosion-resistant materials such as stainless steels (e.g., 304, 316) or duplex alloys like Nitronic 60 to mitigate and erosion-corrosion in components like turbines and heat exchangers. Impurities such as dissolved oxygen or can exacerbate cracking in milder steels, while control through regular fluid monitoring and adjustment is essential to maintain system integrity and prevent material degradation. Safety concerns arise primarily from ammonia's toxicity, classified as a high-risk substance by standards like those from the , requiring enclosed systems, advanced (e.g., via its pungent or fixed gas detectors), and strict pressure management to avoid hazards like autoignition at elevated temperatures above 651°C. Maintenance challenges include fouling in the separator due to impurities in the working fluid, which can reduce separation efficiency, alongside the need for periodic analysis of the ammonia-water mixture concentration to ensure optimal performance and prevent shifts that degrade cycle efficiency. The Kalina cycle is most scalable in the 100 kW to 50 MW power range, where its complexity is manageable for applications like geothermal or recovery, but larger installations often incorporate hybrids with other cycles (e.g., ) to address escalating design and operational intricacies. Economically, the Kalina cycle offers a levelized cost of energy (LCOE) approximately 5-10% lower than (ORC) systems in geothermal contexts (e.g., 0.18 €/kWh vs. 0.22 €/kWh), driven by superior efficiency at low temperatures, though higher upfront costs stem from custom fluid handling and specialized components. Environmentally, the closed-loop design minimizes water consumption compared to open steam cycles, using negligible makeup water for the ammonia-water mixture, and lends itself to integration with CO2 capture processes by recovering to drive or liquefaction units, potentially reducing emissions by 15-23%.

History and Development

Invention and Early Work

The Kalina cycle was invented by Aleksandr I. Kalina, a Russian engineer who emigrated to the in 1978 after holding a senior position in the . Kalina, born in 1933 near , (then part of the USSR), drew on his expertise in to develop the cycle while working independently and later founding , Inc., to advance its commercialization. His work built on earlier concepts from the 1970s, which aimed to enhance power generation from low-enthalpy geothermal and sources using multi-component fluids, but sought to address their limitations in efficiency and temperature matching. The core concept emerged in the late , with Kalina proposing a thermodynamic power cycle that utilized an ammonia-water mixture as the to improve from low-temperature sources below 200°C, where traditional Rankine cycles perform poorly. Inspired by the variable-temperature boiling characteristics of ammonia-water mixtures in absorption refrigeration systems, the cycle allows for better thermal matching between the working fluid and heat source, reducing irreversibilities during . This motivation addressed the inefficiencies of conventional cycles in recovering , potentially increasing overall plant efficiency by optimizing the utilization of low-grade . Kalina filed the foundational patent in 1980, which was granted as US Patent 4,346,561 in , describing a for energy generation using a multi-component with regenerative preheating. In the early , initial focused on modeling the behavior and thermodynamic properties of ammonia-water mixtures for applications, involving theoretical analyses published in journals. Collaborations with academic institutions, such as those contributing to exergy-based studies, helped validate the cycle's potential through simulations of mixture compositions and designs. By the mid-1980s, lab-scale prototypes and bench tests confirmed the cycle's advantages, demonstrating improvements of 10-20% over equivalent Rankine cycles for low-temperature heat recovery, primarily due to reduced losses in the and . These early experiments, often using simplified configurations like the Kalina Cycle System 11 (KCS-11), highlighted gains of around 15% in second-law efficiency for sources around 100-150°C, establishing a foundation for further development without venturing into full-scale implementation.

Key Milestones

A significant early occurred in 1992 at the U.S. Department of Energy's Energy Technology Engineering Center in Canoga Park, , where a ~3 MW prototype plant validated the cycle using nuclear , paving the way for commercial applications. The first commercial implementation of the Kalina cycle occurred in 1998 at the Kashima Steel Works of in , where a 3.5 MW recovery plant was commissioned, marking the transition from experimental to operational use. This facility utilized low-grade from production processes, demonstrating the cycle's viability for industrial applications and achieving reliable power generation over subsequent years. Geothermal adoption advanced significantly with the 2000 commissioning of a 2 MW electric in , , by Orkuveita Húsavíkur, which harnessed low-temperature at around 121°C to supply over 80% of the town's needs with minimal environmental impact through full fluid reinjection. By 2010, the system had been expanded to a 17 MW thermal capacity, incorporating additional modules to enhance output while maintaining high efficiency in variable geothermal conditions. In , a notable project commissioned in 2009 at , , featured a 3.4 MW Kalina cycle plant integrated with geothermal resources for combined heat and power generation, operational until its 2017 shutdown due to gradual resource depletion in the . This installation highlighted the cycle's adaptability to moderate-temperature geothermal sources but also underscored challenges in long-term resource sustainability. The 2000s saw the introduction of second-generation Kalina cycle systems by Kalex LLC, founded by Alexander Kalina, focusing on enhanced low-temperature efficiency through optimized working fluid mixtures and process configurations, supported by key patents filed between 2004 and 2010. For instance, U.S. Patent 6,820,421 (granted 2004) detailed a low-temperature geothermal system improving energy conversion from sources below 150°C, while subsequent filings like U.S. Patent 6,923,000 (2005) addressed dual-pressure operations for broader applicability. These innovations achieved up to 20-30% higher efficiency compared to first-generation designs in low-grade heat scenarios. In the 2020s, advancements continued with hybrid integrations of Kalina cycles with systems and modifications for improved efficiency in recovery, as detailed in thermodynamic studies and literature reviews published through 2025. Market analyses as of 2025 project compound annual growth rates of 8-10% for Kalina-based and geothermal systems through 2033, driven by demands. The lapse of first-generation Kalina cycle patents around 2015, including several original filings from the 1990s, facilitated wider licensing and independent implementations by reducing barriers to technology access.

Applications

Waste Heat Recovery

The Kalina cycle is particularly suited for recovering low- to medium-grade waste heat from industrial processes, with optimal source temperatures ranging from 80°C to 250°C, including exhaust streams from steel mills, oil refineries, and cement plants. This application leverages the ammonia-water working fluid's variable boiling point to achieve superior thermal matching compared to single-component cycles, enabling the conversion of 10-20% of the available waste heat into electrical power. In such systems, the cycle typically operates as a bottoming process, either recovering heat from gas turbine exhaust or via direct flue gas exchangers, with reported thermal efficiencies reaching up to 18% for a 150°C source temperature. A notable example is the 4 MW installation at Fuji Oil's Tokyo Bay Refinery in , commissioned in 2005, which utilizes from refinery operations at approximately 116°C to generate power and offset over 60 million kWh of grid electricity annually. Similar implementations, such as the 3.5 MW system at a steelworks in 1999 recovering from 98°C cooling water, demonstrate reductions in host process consumption by 5-10% through enhanced overall utilization. These cases highlight the cycle's ability to integrate seamlessly into existing industrial infrastructure, producing reliable baseload power while improving site-wide efficiency. Optimization strategies for the Kalina cycle in waste heat applications include adjusting the ammonia-water mixture concentration to accommodate fluctuating heat loads, which minimizes irreversibilities and maintains performance under variable conditions. Hybrid configurations combining the Kalina cycle with organic Rankine cycles (ORC) have also been explored to broaden recovery across temperature gradients, enhancing exergy efficiency to around 68% in low-temperature steel industry streams. Benefits include short payback periods of 2-4 years due to low operational costs and electricity sales, alongside emission reductions of 1-2 tons of CO2 per MWh generated by displacing fossil fuel-based power. However, challenges arise from heat source variability, often necessitating buffer storage systems to stabilize input temperatures and ensure consistent output.

Geothermal and Renewable Energy

The Kalina cycle is well-suited for generation from low-enthalpy resources, typically in the 60–150°C range, where it functions as a alternative to flash plants by employing an ammonia-water zeotropic mixture to more closely match the temperature profile of the heat source. This configuration allows efficient extraction of from geothermal brines that are too cool for direct production, with the cycle's variable enhancing heat recovery compared to single-phase working fluids. In practice, the cycle has demonstrated superior performance over organic Rankine cycles () in handling low-grade geothermal fluids, particularly by better managing non-condensable gases that can reduce efficiency in systems. A prominent example is the 2 MW geothermal power plant in , which utilizes at approximately 120–124°C to produce electricity while co-generating 20 MW of thermal power for , achieving an overall utilization efficiency exceeding 80% of the available . The plant's integration into the local geothermal system highlights the cycle's ability to maximize resource value from moderate-temperature sources, with the ammonia-water mixture enabling operation at lower pressures and temperatures than traditional cycles. In applications, the Kalina cycle pairs effectively with collectors delivering at around 200°C, converting it to dispatchable with efficiencies of 12–15% when combined with for continuous operation. This integration leverages the cycle's adaptability to variable inputs, outperforming Rankine cycles in economic terms for mid-temperature by reducing capital costs through optimized composition. The cycle also extends to other renewables, such as (OTEC), where ammonia-water variants boost Carnot efficiency by up to 50% over pure-fluid closed cycles by minimizing irreversibilities in the and . In , Kalina systems recover low-grade heat from combustion processes, enhancing overall plant efficiency in decentralized setups. Scalability is a key advantage, with modular Kalina units enabling deployment in remote geothermal sites and facilitating solar-geothermal configurations that provide 24/7 baseload power by compensating for intermittency, as explored in recent 2025 studies on multi-generation systems combining low-enthalpy geothermal with . These improve system reliability and output in variable-resource environments, with ongoing research as of 2025 focusing on integrations for and . Environmentally, Kalina cycle applications in renewables contribute to low-carbon production with minimal —often less than km² per MW for geothermal installations—and enhanced resource utilization in water-scarce areas through reduced cooling water needs compared to evaporative systems. By integrating with renewables, the cycle supports emission reductions and in regions with abundant but underutilized thermal resources.

Commercialization

Licensing and Patents

The Kalina cycle's intellectual property framework originated with patents filed by Alexander I. Kalina in the early 1980s, including the foundational U.S. No. 4,346,561 issued in 1982 for generating using a zeotropic as the . Additional key patents, such as U.S. No. 4,548,043 granted in 1985, covered methods for and thermodynamic processes integral to the cycle's design. These first-generation patents, primarily focused on ammonia-water mixtures and basic cycle configurations, generally expired in the early 2000s, approximately 20 years after their filing dates, allowing for broader access to core concepts. A second generation of Kalina cycle technology emerged in the mid-2000s, developed by Kalina through Kalex LLC, which he co-founded. This iteration introduced optimizations like reduced structural losses and enhanced for low-temperature heat sources, with patents such as U.S. Patent No. 6,923,000 issued in 2005 for dual-pressure geothermal systems. These second-generation patents, assigned to Kalex LLC, remain active and are projected to hold validity through the 2030s, protecting advanced variants including cascade and multi-stage configurations. Ownership of first-generation rights transitioned to Wasabi Energy plc and its subsidiary Global Geothermal Ltd. in the late , which acquired global licensing control over remaining active patents and the Kalina Cycle . Some rights were restructured or transferred during Wasabi Energy's financial challenges in the , including administration proceedings in , leading to partnerships that distributed usage in specific sectors. Following Wasabi Energy's voluntary administration in , licensing rights were restructured, with Kalina Power Limited acquiring control over key patents and trademarks by the late . As of 2025, Kalina Power Ltd. (ASX: KPO) continues to license the technology globally, focusing on and geothermal applications. Kalex LLC retains exclusive control over second-generation advancements, enabling independent commercialization of improved systems without overlapping claims on expired foundational patents. Licensing has been central to the technology's dissemination, with exclusive agreements facilitating integration into industrial applications. In the 2000s, Global Geothermal Ltd. entered a partnership with AG for turbine integration in geothermal projects, exemplified by the 2009 licensing for the plant in , which combined Kalina cycles with Siemens equipment. For Asian markets, a 2009 exclusive was granted to Shanghai New Energy Technology Co., Ltd. (SSNE) by Global Geothermal, covering waste heat recovery and applications in through 2024, with royalties tied to installed capacity. In 2011, secured global exclusive rights from Wasabi Energy for Kalina cycle deployment in the cement and lime industries (excluding ), including a $2 million upfront fee and ongoing royalties to support recovery systems. Following the expiration of original patents, generic implementations of first-generation Kalina cycles have proliferated in academic and research settings, enabling open experimentation with basic ammonia-water systems without licensing fees. Commercial deployments, however, typically involve royalty-based models for patented variants, with rates ranging from $35,000 to $150,000 per megawatt of installed capacity annually, equating to approximately 2-5% of plant revenue depending on operational scale. By 2025, the Kalina cycle supports dozens of licensed projects worldwide, with a growing emphasis on emerging markets like and for and geothermal applications, driven by mandates and agreements.

Notable Installations

One of the earliest commercial implementations of the Kalina cycle is the Kashima Steel Works in , commissioned in 1999 by . This 3.45 MW facility recovers from a revolving at approximately 98°C, marking the first fully commercial application of the technology and demonstrating its viability for industrial processes. The has operated continuously for over 20 years with minimal downtime, producing reliable from low-grade heat sources that would otherwise be wasted. The geothermal power plant in , operational since July 2001, represents a pioneering use of the Kalina cycle for , with a design capacity of 2 MW electric output from a 121°C geothermal flow of 90 kg/s. The facility achieves a of approximately 10%, utilizing about 17 MW of thermal input while enabling full reinjection of the geothermal fluid and integration with . As of 2025, the plant remains operational, now functioning as a that combines Kalina cycle power generation with additional low-temperature resource utilization for enhanced overall efficiency. In , the geothermal plant, started in 2006, generated 3.4 MW of electricity from a 123°C at 150 kg/s, supported by a capacity of up to 70 MW for combined and power applications. The system demonstrated a net efficiency of around 15%, outperforming traditional organic Rankine cycles in low-temperature conditions. Operations ceased in 2017 due to depletion of the geothermal resource, but the provided valuable data on long-term performance and scalability for geothermal projects. The pilot plant in , commissioned in December 2009, is a smaller-scale with 580 kW electric output integrated into a network using geothermal resources. Developed by and with Energent's Euler turbine technology, it validated the Kalina cycle's effectiveness for micro-scale applications, achieving stable operation and proving the feasibility of modular systems for localized heat recovery. As of 2021, the plant continued operations, including a pilot for extraction from geothermal . A notable example of modularity is the 50 kW EcoGen unit installed at Matsunoyama Onsen hot spring in Niigata, Japan, in December 2011 by Wasabi Energy. This compact, packaged system harnesses low-temperature hot spring fluid below 100°C to provide remote power generation, highlighting the Kalina cycle's adaptability for off-grid and small-scale renewable installations with field-tested stability over initial operations. Recent developments include hybrid enhancements at existing sites, such as at , further integrating the Kalina cycle with advanced for sustained geothermal output.

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