Abstract
Water scarcity is a growing global and systematic problem in regions with low groundwater availability. Atmospheric water generation (AWG) technologies are an innovative solution to the water shortage problem, as atmospheric water vapor is a readily available resource even in arid regions, with the drawback of high energy consumption. In this paper, the viability of AWG technologies on an energy and economic level is investigated by thermodynamic modeling of three main active AWG systems consisting of cooling condensation, adsorption and absorption processes. A location analysis model is developed to evaluate the performance based on representative weather data of temperature, pressure and relative humidity over a period of one year to account for seasonal shifts and daily variations in climatic conditions. The specific energy consumption kWh/kg, water production trend and total specific cost are calculated for each technology. Water production by seawater desalination at the nearest coastline and transportation to the site by tanker truck, as well as bottled water prices, are used as benchmarks to assess economic viability. The results show that active AWG systems can only be an economically viable alternative if the water consumption site is relatively far from the coast or other water-rich regions and low electricity costs are available (distance >600 km, electricity price <0.10 US$/kWh). Compared to bottled water, all AWG technologies are in a competitive price range. Absorption systems have an energy efficiency advantage over conventional cooling condensation and adsorption systems (cooling condensation: average 0.42 kWh/kg; absorption: average 0.38 kWh/kg; adsorption: average 1.16 kWh/kg), but require a higher degree of process and plant design development. However, because of the high fluctuation in water production, atmospheric water generation technologies should be considered as a complementary supply to conventional water sources.
Article Highlights
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Modelling of three main atmospheric water generation systems using thermodynamic models to compare energy efficiency.
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Active atmospheric water generation systems can be energetically and economically feasible in beneficial circumstances.
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Due to the high fluctuation in water production, atmospheric water generation technologies should be seen as an additional supply to conventional water sources.
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1 Introduction
Securing the world’s water supply is a major challenge for future generations [1, 2]. Freshwater scarcity is recognised as a global, systemic problem worldwide [3]. Already, two-thirds of the world’s population experiences water scarcity for one month of the year, and half a billion people live in water-stressed areas throughout the year [4]. Total global water consumption increased by 13% from 3973 km\(^{3}\)/year in 2000 to 4489 km\(^{3}\)/year in 2021 [5]. During the same period, domestic water consumption increased by 33% from 384 km\(^{3}\)/year to 514 km\(^{3}\)/year, with a similar trend for future consumption [5, 6]. Due to population growth and rising average temperatures, water supplies are already severely constrained, especially in semi-arid and arid areas, as groundwater levels in many regions are being depleted faster than they can regenerate as a result of over-exploitation [7,8,9]. As a result, the transport and sale of water in tanker trucks or as bottled water is often the only supply option for people and industry in arid and non-coastal areas [10, 11]. In particular, the use of bottled water has increased dramatically in recent years, from about 200 million tons/year in 2010 to 355 million tons/year in 2021, with continued annual growth of 10% expected until 2026 [12]. The benefits of bottled water are consistent water quality, but high carbon emissions and plastic waste are important disadvantages [6, 12].
Seawater desalination, especially by reverse osmosis, is already a widely used water source in arid coastal regions such as the Arabian Gulf or the South American coast [13] , with more than 18,000 desalination plants in operation worldwide, producing about 40 billion m\(^{3}\) of water per year [14, 15]. Its advantages are relatively low specific energy consumption of 3–5 kWh per m\(^{3}\) of water produced [16, 17] and overall low production costs of 0.5\(-\)1.5 US\({\$}\)/m\(^{3}\) [18,19,20], as well as large production capacities of up to 1 million m\(^{3}\) per day [18, 20]. However, there are several environmental concerns, in particular the amount of chemicals used to pre-treat seawater and the large quantities of highly saline brine produced, which is discharged into the sea, endangering local coastal regions and marine life [21,22,23]. In addition, fossil fuels are often used to power desalination plants, resulting in a significant carbon footprint for the water produced of 2 \(kg_{CO_2}\)/m\(^{3}\) [14, 17].
Atmospheric water generation (AWG) or atmospheric water harvesting is an emerging technology that has gained interest in recent years as an additional source of potable water in water stressed areas. Concepts are being explored in which AWGs can provide an additional source of water to increase the resilience of the overall water supply [24]. The global market for AWG systems is estimated at USD 2.1 billion for 2019 [25]. For the following years 2020 to 2027, market forecasts predict strong growth with an annual growth rate of 19.5% [25], which means that a global AWG market volume of around USD 10 billion can be expected by the end of the decade. AWG technologies can be divided into active and passive systems [3, 26]. Active systems allow greater scalability and more consistent water production from air, but require more energy and process engineering. Passive systems can operate independently of local infrastructural conditions such as power sources , etc., but are often very locally applicable (e.g. fog nets) or highly dependent on climatic conditions (e.g. solar radiation). Due to these disadvantages in scalability and high dependence on local conditions, only active AWGs are considered in this research article. Active AWGs can be divided into cooling and desiccant based systems. Cooling Condensation AWGs (CC AWGs) are an established technology and are widely available in the AWG market, where they account for 98.9% of global revenues [25]. However, CC AWGs have a limited application range in terms of climatic conditions due to the need to sub-cool the air below its dew point and high energy consumption ranging from 0.2\(-\)1.5 kWh/m\(^{3}\) depending on climatic conditions [26, 27]. Desiccant based systems use either adsorption or absorption of atmospheric water. The adsorption process uses porous solid materials such as MOFs or zeolites to bind the water molecules and is the subject of much active research in terms of materials used and process application [28,29,30,31]. These adsorbents have highly variable water uptake potentials ranging from 0.2 to 1.6 \(kg_{water}/kg_{desiccant}\) [30, 32], and optimization of the materials in terms of uptake potential and energy efficiency is a major area of current academic research. Energy requirements for adsorption–desorption AWG vary widely, ranging from 0.9–4 kWh/kg [26]. Absorptive processes use hygroscopic liquid salt solutions, for which various salts have been investigated for their process potential [33, 34], but the process engineering implementation of this technology has been sparsely explored [34] , with reported specific energy requirements of 0.15–1 kWh/kg [34].
The progress and comparison of different AWG technologies regarding their energy efficiency has been studied by several authors [3, 26, 35,36,37,38], which promises a possible implementation in the global water supply, although the high energy consumption is prominent in all active AWG technologies.
Lord et al. [39] explored the potential of cooling based AWGs for global application. Moghimi et al. [40] analyzed the profitability of a CC AWG machine in terms of its production and potential production and financial risks. However, in the current scientific literature, there is no comparison of the different active AWG technologies on a global scale in terms of performance evaluation (water production, energy efficiency) as well as economic comparison (water cost, production volatility). Furthermore, seasonal and intraday climatic variations have not been taken into account in the above mentioned research articles.
In this work, we present a modeling framework for a systematic comparison of the three defined active AWG technologies. These technologies are modeled and evaluated using hourly weather data over a representative year at 18 sites worldwide in terms of water production, energy consumption, water cost, and production volatility. From the results, considerations for the possible implementation of AWG technologies can be directly derived: On the one hand, the best choice of technology as well as the economic validity compared to conventional water sources such as seawater desalination or bottled water. Furthermore, the risk of fluctuating water production of the different technologies over the year is identified and the cost distribution of energy costs to investment costs in relation to the specific amount of water produced is compared in order to highlight possible optimization potentials with regard to the price of water.
2 Thermodynamic principles for water vapour extraction from air
The amount of water in the air is primarily affected by temperature, as warmer air has a greater capacity to hold moisture. The water content of air can be accurately measured by water vapour pressure, since the total pressure of gases is equal to the sum of their partial pressures. The saturation vapour pressure of air \(p_{s}\) corresponds to the liquid/gas phase boundary of water. Relative humidity \(\phi _{rel}\) is expressed as the fraction of the actual vapour pressure over the saturation vapour pressure [41].
The absolute amount of water in the air is given by the absolute humidity \(\phi _{abs}\), which measures the mass of water per volume of air. It is calculated from the vapour pressure, the specific gas constant \(R_{v}\) (461.51\(\frac{J}{kg*K}\) for water) and the air temperature T in Kelvin [41].
Changes in the moisture content of the air during extraction processes can be described energetically by the enthalpy of humid air.
with the specific enthalpy \(h_{humid air}\), the specific isobaric heat capacities of air and steam \(c_{p,air}\) and \(c_{p,wv}\), the mass fraction of water in the air \(x_{w,air}\), the enthalpy of vaporisation \(\Delta h_{v}\) of water at 0 \(^\circ\)C, and the air temperature T [41].
The density of humid air is calculated from the absolute humidity and the specific volume \(\nu _{humid air}\) [41].
The specific energy consumption (SEC) is used for the evaluation of thermal processes in terms of their energy efficiency [3, 26]. The SEC is calculated from the required energy input E per produced amount of water \({\dot{m}}_{w}\).
3 State of the art—air water generation technologies
Existing technologies for harvesting water from atmospheric moisture can be divided into passive and active systems [3], as shown in Fig. 1. Passive systems, such as fog or dew collectors, have the advantage of being simple to operate with low capital and maintenance costs, but are highly dependent on local climatic conditions [42]. Active systems, in contrast, are more scalable and less dependent on environmental conditions such as fog or sunlight [3]. Active technologies for extracting water from atmospheric moisture can be divided into two categories [34]: cooling-based systems and desiccant-based systems, which are further subdivided into adsorption-based processes using solid desiccants and absorption-based processes using liquid desiccants.
3.1 Passive air water generation technologies
Passive air water harvesting systems collect water from the air using natural processes without the need for external energy [3, 26]. These systems have the advantage of using simple technology, which means lower investment and operating costs. However, the low-tech nature of the systems also results in poorer adaptability to the environment . The yield is highly unpredictable due to weather and location dependency [3, 26, 42], as these systems are highly dependent on environmental conditions such as fog, dew or rain. Examples of passive air water harvesting systems are fog or dew nets, which collect the supersaturated water vapour in the air and allow it to condense on their surface, collecting the precipitating water [42]. These technologies are only suitable for use in regions with high humidity or precipitation, which are not typically regions affected by severe water scarcity, and are therefore not considered further in this study.
3.2 Active air water generation technologies
3.2.1 Active cooling condensation
Cooling condensation is the most widely used process to date for extracting water from atmospheric moisture [43] and is also commonly used in air conditioning systems to dehumidify the air. In this process, as shown schematically in Fig. 2, fans are used to bring air into contact with a cooled heat exchanger (condenser). In this condenser, the air is cooled below its dew point, condensating the atmospheric water in the air. The water is then discharged from the condenser and treated for the specific application. The yield of cooling condensation is highly dependent on relative humidity and air temperature and has limited application in cold dry areas where the dew point of the air is below the freezing point of water [27, 44]. Most refrigeration condensation processes are electrically powered. Cooling is provided by a vapour compression refrigeration cycle using refrigerants such as R-134a [45], where the electrical power requirement is determined by the energy efficiency ratio (EER) , which is defined as the ratio of the cooling energy supplied to the system to the electrical energy required as input [27]. The use of membranes to concentrate moisture in the incoming air can increase the efficiency and climatic range of application for the technology [46]. For reasons of simplicity in modelling the system, this addition is not considered in this study.
Typical machines available on the market, including their operating parameters as specified by the manufacturer, are listed in Table 1. An average of these parameters is used in the model to represent a representative machine.
3.2.2 Active adsorption–desorption using solid desiccants
Adsorption-based methods use a solid bed of microporous, hydrophilic material as the sorbent [28, 52]. Ambient air is passed through the adsorbent bed using a fan and the water molecules in the air are bound by physisorption in the hygroscopic pores of the adsorbent [52]. Unlike the cooling condensation method, the air does not have to be in a saturated state to collect the gaseous water, but it can be adsorbed directly from the air without the need for cooling. This process can be reversed by applying heat to the adsorbents. Novel metal-organic frameworks (MOFs) or special zeolite groups are commonly used as adsorbents [28,29,30,31]. Once maximum storage saturation is reached, the adsorbent is regenerated by heating the adsorbent bed. The produced water vapour is condensed in a condenser and the produced water can be treated. The process, as shown in the Fig. 3, must be cyclic when using a single adsorbent bed, e.g. a day-night cycle, where water is adsorbed at night and solar energy is used for desorption during the day [28]. Quasi-continuous operation can be achieved by using more than one adsorbent bed, which increases the complexity of the system. The commercialisation of this technology is still at the research stage, so there are no market-ready products.
3.2.3 Active absorption–desorption using liquid desiccants
Absorption-based systems use highly concentrated aqueous electrolyte solutions as liquid sorbents, which have hygroscopic properties. Similar to the adsorption process, no cooling or saturation of the air is required for the absorption to take place. The driving force for the mass transfer of the water between the gas and liquid phases is the difference between the vapour pressures of the gaseous and liquid water in each phase. When the vapour pressures are in equilibrium, no mass transfer takes place. This equilibrium describes the boundary between the absorption and desorption processes. Hygroscopic salts reduce the vapour pressure of the aqueous solution with increasing concentration, shifting the equilibrium in favour of absorption of water from the air into the liquid phase. The most commonly used salts for air dehumidification are lithium chloride (LiCl), magnesium chloride (MgCl2) or potassium acetate (KAC) [53,54,55]. Glycols such as triethylene glycol [54, 55] and ionic liquids [56, 57] are also used as hygroscopic sorbents. Compared to glycols, salts have the advantage that they have no vapour pressure and therefore remain in the aqueous phase when heated. However, a disadvantage is that they typically have corrosive properties, which necessitates the use of more durable materials and results in higher investment costs [55]. Research into composite adsorbents using caged silica impregnated with lithium chloride or calcium chloride has shown that the corrosivity of these salts can be reduced while also improving the uptake kinetics [58, 59]. Further research in this area would help to drastically improve investment costs through the possible use of more cost effective material selection.
The schematic concept of an absorption–desorption system is shown in Fig. 4. The hygroscopic absorbent is brought into contact with the ambient air to allow the absorption of atmospheric water into the saline solution. In terms of process technology, the sorbent is either sprayed directly into the air to be dehumidified or distributed on the surface of solid structures, most commonly packed beds with loose packing [34]. The dilute electrolyte solution is then thermally heated so that the water can be evaporated, condensed and recovered. The concentrated electrolyte solution is recirculated to the absorption, allowing the process to be continuous [60]. Advantages over adsorption based processes are better scalability and continuous operation [60]. Compared to the cooling condensation process, higher energy efficiency and a wider climatic range are possible [3]. Similar to adsorption–desorption AWG, this technology is still at the research stage and no market-ready products are available.
3.2.4 Dessicant water uptake potential comparison
Figure 5 shows the water uptake potential of different desiccants per kg of adsorbent or per kg of absorbent solution at equilibrium at a fixed temperature of 15 \(^\circ\)C (left) and 30 \(^\circ\)C (right). At higher temperatures and humidity levels, a much higher sorption capacity can be achieved with liquid sorbents than with solid sorbents. However, in drier and colder conditions, the solid sorbents have a higher sorption capacity. Liquid sorbents are more sensitive to temperature than solid sorbents in terms of uptake potential. Comparatively, lithium chloride solution has a higher uptake potential than potassium acetate solution, but has significant other downsides such as high corrosiveness and toxicity, requiring more corrosion resistant materials and higher safety standards. For solid desiccants, the metal-organic framework MIL-101(Cr) has the highest absorption potential at higher relative humidities. At lower relative humidities, various solid desiccants such as MIL-160 have a higher water absorption potential. The complete adsorption–desorption cycle is illustrated in Fig. 20, showing the shift of the adsorption isotherm for the higher desorption temperature at 70 \(^\circ\)C.
4 Modelling of active AWG technologies and location analysis
4.1 Cooling condensation model
Cooling condensation works by lowering the ambient air temperature below its dew point. The model consists of mass and energy balances of this process to calculate the outlet air temperature and the specific energy consumption, as shown in Fig. 6. Table 2 lists the required input data for the cooling condensation AWG (CC AWG) model; Table 3 lists the model parameters with their chosen values.
The power required for the fan is given by the pressure drop in the CC AWG \(\delta p\) and the inlet airflow.
The absolute humidity, enthalpy and density of the inlet air are calculated according to the thermodynamic principles of water vapour extraction from air as described in Sect. 2. The inlet air mass flow rate is calculated from the inlet air volumetric flow rate and the air density.
The dry air mass flow rate at the inlet and outlet of the AWG is constant, as only water is condensed during the process.
The total mass balance and the water mass balance are used to calculate the exhaust air mass flow and the exhaust air absolute humidity and temperature.
The enthalpy of the outgoing air stream is calculated from the temperature and absolute humidity. The cooling energy required is calculated from the total energy balance.
The electrical energy input can be expressed using the EER and the required cooling energy as
The total specific energy consumption of the CC AWG is given by
4.2 Adsorption–desorption model
The model is divided into two parts, one being the adsorption of humidity during the night and the other being the desorption and condensation of water during the day, as shown in Fig. 7. The reasonable assumption is that the adsorption and desorption kinetics are fast enough to allow for a day-night cycle [52]. The assumed cycle lengths are 12 h each (desorption 8 am–8 pm, adsorption 8pm-8am). Climatic data averaged over the cycles are then used as input to the model. Assumptions made for modelling the absorption–desorption system:
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Adsorption and desorption kinetics are fast enough to be completed in a 12 h cycle [26, 30].
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Uniform airflow through the adsorbent bed.
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Uniform heating of the adsorbent bed.
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Ambient temperature is used as condensation temperature in the desorption stage.
Table 4 lists the required input data for the adsorption–desorption AWG model. Table 5 lists the model parameters with their selected values.
To simplify the model, the reasonable assumption of the Polanyi principle of temperature invariance for the water adsorption equilibrium is used [61]. Thus, the Polanyi adsorption potential \(\Delta F_{ad}\) is given by
using the ambient vapour pressure \(P_{v}\) and the saturation vapour pressure \(P_{s}(T)\) at the ambient temperature T. The amount of water adsorbed per mass of adsorbent is then calculated as follows [61].
where A, B, \(k_{1}\), \(x_{1}\), \(k_{2}\) and \(x_{2}\) are adsorbent material parameters as described by Gordeeva et al. [61] for different bed materials.
The desorption temperature depends on the adsorbent material and the target water collection fraction, which describes the fraction of water collected during the desorption phase and can be calculated from the saturation pressure of water and the outlet vapour pressure at the desorption temperature [61].
The water collection fraction is set to a reasonable value of 0.7 [61]. The desorption potential \(\Delta F_{des}\) is calculated using the desorption temperature, similar to the adsorption potential. The amount of water harvested per cycle is then given by
The total amount of water produced per cycle depends on the amount of adsorbent used.
The total amount of air required for the desorption cycle also depends on the absolute humidity before (a) and after (b) the condensation step.
The desorption cycle time is calculated with Eq. (22).
Using the heat capacities of the adsorbent and binder materials, the required amounts of heating of the adsorbent bed and air as well as the adsorption energy and the energy losses to the environment can be calculated as [32]
The electrical demand for the heating is assumed to be supplied by a heat pump system, whose energy performance is defined by the coefficient of performance (COP), which describes the ratio of the electrical energy to the thermal energy supplied to the system. The COP value depends on the temperature rise required by the heat pump system. A value of 5 is chosen for the lower desorption temperatures of the adsorption–desorption AWG [64].
The power requirement for the fan is calculated as
With the different energy consumption, the total specific energy requirement of the adsorption–desorption AWG model is calculated as follows.
4.3 Absorption–desorption model
The absorption–desorption model consists of two stages, an absorption stage and a desorption stage, see Fig. 8. In the absorption unit, a loose packing column with a high enough packing height is used so that the contact time between the air and the salt solution is long enough for equilibrium between the two phases to be reached [34, 60]. The diluted brine is then heated to its boiling point and the outlet concentration is set to a fixed value chosen to be close to the solubility limit. Assumptions made for modelling of the absorption–desorption system:
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The height of the absorption column is long enough to absorb atmospheric water up to the equilibrium state of air and salt solution [34, 60].
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The salt solution has the same temperature as the ambient air at the solution outlet of the absorption stage due to the high flow rate of air compared to the flow rate of salt solution and the large contact area.
Table 6 lists the required input data for the absorption–desorption AWG model. Table 7 lists the model parameters with their selected values.
In the absorption phase of the model, the equilibrium state of the solution and the corresponding humidity are calculated from the vapour pressure data (see Sect. 3.2.3). If no absorption is possible, i.e. the operating point would be on the desorption side of equilibrium and there would be mass transfer of water from the brine to the air, all variables are set to zero. The mass concentration of the saline solution after the absorption unit is calculated as
where \({\dot{m}}_{air}\) is the air mass flow rate, \({\dot{m}}_{sol,ab,in}\) the solution inlet flow rate, \(w_{ab,in}\) the solution inlet salt mass fraction, \(w_{ab,out}\) the solution outlet salt mass fraction, \(y_{air,in}\) the air inlet water mass fraction and \(y_{air,out}\) the air outlet water mass fraction. The air inlet mass flow rate is calculated from the air volume flow rate.
The mass flow rate of the brine leaving the absorption unit is calculated from the total mass balance
with
and
The required temperature in the evaporation unit and the outlet concentration of the absorption unit is calculated from the vapour pressure data of the absorption solution (physical property data of lithium chloride solution as described by Chaudhari and Patil [62], physical property data of potassium acetate from measurements of vapour pressure and heat capacity as described by Kölking [34]).
The amount of water evaporated is calculated from the total mass balance of the desorption unit.
The energy balance of the desorption unit is used to calculate the required heating energy \({\dot{Q}}_{des}\), which is provided by a heat pump with a fixed COP set to a value of 3, since the temperature rise is higher compared to the adsorption–desorption AWG [64]. The salt solution enthalpies are calculated using aforementioned physical property data [34, 62].
The inlet temperature to the evaporator after heat exchange of the desorption outlet solution flow and the inlet solution flow is calculated using a simple heat exchanger calculation.
where \(\Delta T_{hx}\) is the temperature difference between the heat exchanger inlet and outlet flows. Using the hydrostatic pressure \(p_{hyd}\) and the hydraulic work \(W_{hyd}\), the eletrical power consumption for pum** is calculated as
with
and
The total specific energy consumption of the absorption–desorption AWG is then given by
4.4 Reverse osmosis water production and transport model
The cost of producing water by reverse osmosis (RO) plant depends on the annual/daily water production capacity. With increasing capacity, the specific production cost decreases to a lower limit of about 0.50 $/m\(^{3}\) at 320,000 m\(^{3}\)/day. The specific cost is higher at lower production capacities, increasing significantly to about 2 $/m\(^{3}\) at 3000 m\(^{3}\)/day, with a maximum of 10–12 $/m\(^{3}\) at very low production capacities of around 100 m\(^{3}\)/day [18, 65, 66]. A fitted function of RO plant specific production costs in $/m\(^{3}\) as a function of daily water production in m\(^{3}\), regressed from data in Al-Karaghouli and Kazmerski [18], Caldera et al. [19] and Ghaffour et al. [20]:
The cost of transporting the produced water from the onshore RO plant to the site is calculated using a water tanker transport model [18, 67,68,69,70]. Tanker truck specific cost \(Cost_{transport,truck}\) is calculated using the model developed by Marufuzzaman et al. [67] and Berwick as well as Farooq [68] and Pootakham et al. [69, 70] using the physical properties of water. Figure 9 shows the schematic of the RO and transport model. Table 8 lists the parameters required for the cost estimation model of water transport by truck.
The total cost of the produced and transported water is as follows.
4.5 Overall location analysis and economic analysis model
All models are implemented in Matlab. Representative annual hourly weather data (temperature, relative humidity, air pressure) are generated for each site using Meteonorm 8.0 [71]. The location data and climatic conditions are used as an input to the model. With the calculated SEC over the whole year, the specific electricity cost per produced amount of water is calculate as
The three different AWG technologies are compared from an energy and economic point of view using the benchmark technology of RO water production and truck transport to the point of use. Figure 10 shows the schematic of the overall model with input and output data with the four sub-models.
To assess the potential for atmospheric water production, characteristic locations around the world are selected with a variety of different climatic conditions, distances from the coast, and different energy and fuel costs. Different economic and environmental zones, climatic conditions and levels of drinking water scarcity have been considered on all continents to provide a representative assessment, as listed in Table 9. Electricity and fuel costs were researched for a fixed date in 8/2023 [72]. The road distance to the site from the nearest coast was estimated using Google Maps [73]. Representative hourly climate data (temperature, relative humidity, pressure) were generated using Meteonorm 8.0 software [71].
The economic performance of the AWG technologies is assessed by calculating the total specific cost of produced water and a risk assessment of the volatility of production over the course of a year. The total specific water cost \(Cost_{water,tot}\) is the sum of the specific electricity cost \(Cost^{el}_{water}\) and the fixed annual cost \(FC_{AWG,year}\) divided by the annual water demand \(W_{year}\).
The fixed costs include the annual price of the AWG, \(P_{AWG,annual}\), and the maintenance costs, \(Cost_{maint,annual}\), as a percentage of the investment costs. It is set at 3% of the annual investment cost for all AWG technologies [75].
The annual depreciation is calculated using the total cost per AWG unit \(P_{AWG}\), the total number of AWG units \(n_{AWG,req}\) required to produce the specified amount of water, and the operating life of the AWG unit \(OL_{AWG}\). The operating life of all AWG technologies is set to 15 years with no salvage value at the end.
The ratio of energy cost to total water cost is calculated to evaluate the impact of optimising energy consumption versus production cost savings. A higher value indicates a greater impact of energy costs on total water costs. It can therefore be concluded that either optimising energy consumption or reducing production costs will have a greater impact on the resulting total water costs and should be pursued with higher priority.
Table 10 lists the parameters chosen for the economic calculations. The purchase price for the CC AWG is chosen as an average of the values in Table 1. For the adsorption–desorption AWG and the absorption–desorption AWG there are no products on the market yet, therefore the purchase prices have to be estimated and are assumed to be twice as high as for the CC AWG due to the higher complexity of the technologies involved.
The volatility of AWG water production due to seasonal climatic variations poses a risk to the availability and reliability of water supplies. This is considered to be one of the major barriers to the adoption of AWG technologies [40]. The mean hourly water production and standard deviation of each site are calculated to assess the production risk [40]. The standard deviation is used to analyse the \(\sigma\) and 2\(\sigma\) confidence intervals, above which 83.7% and 97.5% of water production lies. A higher number indicates more reliable water production over the course of the year.
5 Results and discussion of AWG-technology evaluation and location analysis performance evaluation for different technologies
The energy performance of active AWG technologies is highly dependent on the climatic conditions of the site.First, the three active AWG technologies are compared in terms of their specific energy consumption and water production. The annual performance of the technologies is then analysed using the site analysis model described above, using hourly weather data to evaluate production efficiencies for different geological sites and climates. The calculated specific water costs are used for economic evaluation and comparison with seawater desalination and bottled water. Finally, an analysis of the volatility of water production is carried out to assess the risk of having inconsistent water production over the year.
5.1 Thermodynamic performance and efficiency evaluation of AWG technologies
5.1.1 Active cooling condensation AWG results
The efficiency of active cooling condensation is highly dependent on the ambient climatic conditions. Figure 11 (left) shows the specific energy consumption for different temperatures and relative humidities. In very hot and humid climatic conditions, the lowest possible specific energy consumption is around 0.17 kWh/kg. The limit of the climate range in which water can be produced depends on the condensation temperature. If it is below freezing point, the AWG machine would freeze, requiring the machine to be heated and significantly reducing its energy efficiency. Figure 11 (right) shows the lowest possible operating points in terms of temperature and relative humidity for the CC AWG model.
5.1.2 Active adsorption–desorption AWG results
In sorptive AWG technologies, the largest energy requirement is for desorption of the water from the desiccant. As the water is extracted from the sorbent by heating the air and the adsorbent bed, the composition of the air plays an inverse role in the energy efficiency of the system compared to CC AWG. Referring to Fig. 12, higher relative humidity levels result in higher specific energy consumption because more total air has to be heated to remove the adsorbed water from the adsorbent bed. Drier and warmer conditions favour the desorption process energetically, resulting in lower specific energy consumption, as less desorption air needs to be heated to reach the desorption temperature of the desiccant. At a low relative humidity of 20% for both materials considered, the SEC increases again at higher daytime temperatures. This is because, assuming the same absolute humidity at night and a temperature decrease of 7 \(^\circ\)C compared to the daytime temperature, the absorption potential of the materials is lower, as shown in Fig. 5. Over the climatic range considered, the SECs are significantly higher compared to the other AWG technologies. However, the required desorption temperatures are at a relatively low level, so the required energy can be provided by solar thermal systems, as shown in Fig. 13 for MIL-101(Cr).
5.1.3 Active absorption–desorption AWG results
The specific energy consumption of highly concentrated lithium chloride and potassium acetate aqueous solutions are analysed, as shown in Fig. 14. The use of lithium chloride solution shows a lower specific energy consumption than the use of potassium acetate salt solution with the lowest SEC at about 0.1 kWh/kg (lithium chloride solution) and 0.13 kWh/kg (potassium acetate solution). However, due to the high corrosiveness of lithium chloride, higher quality materials must be used, resulting in higher unit costs. The lower limit of relative humidity is around 40% for both solutions, which is higher compared to other AWGs, but a steeper drop in SEC is calculated with increasing relative humidity due to the higher water uptake potential, see Fig. 5. Lower specific energy requirements are achieved even in drier conditions compared to the CC AWG and the adsorption–desorption AWG. However, the SEC range is higher than that of the CC AWG and the adsorption–desorption AWG.
Similar to the adsorption–desorption process, most of the energy is used to heat the solvent to evaporate the absorbed water out of solution. The required regeneration temperature is calculated to be 135 \(^\circ\)C for the lithium chloride solution and 132 \(^\circ\)C for the potassium acetate solution. The distribution of energy required for the three active AWG processes under different climatic conditions is shown in Fig. 15. About 90 % of the energy is used to cool the ambient air (CC AWG) or about 80% to heat the air and the adsorbent bed or desiccant liquid for desorption of the bound water. The remaining energy is used to generate the required air flow and to account for thermal losses to the environment. Thermal losses are significantly higher for the desiccant based AWGs because the temperature difference with the air is much greater. The energy required for pumps in absorption–desorption AWGs is not included in this graph as it represents less than 1% of the total energy requirement. The results show that different AWG technologies can be energetically advantageous for different climatic conditions. For colder temperatures and high humidity (top right), the absorption–desorption AWG and the CC AWG are most energy efficient. In colder and dry conditions (top left), the adsorption–desorption AWGs have the lowest specific energy demand, while in warmer conditions either the CC AWG (bottom left) or the absorption–desorption AWG (bottom right) are energetically more efficient. This indicates that for realistic, fluctuating climatic conditions between day and night , as well as different seasonal periods, an overall analysis for different locations over a whole year is useful.
5.2 Location performance analysis and economical evaluation of AWG technologies
The analysis of the AWG technologies is carried out using the models previously described for the selected global sites over a full year period to compare the energy efficiency of the systems and to assess the resulting water costs in relation to water production via desalination and transport and bottled water. Water production over the year is analysed and discussed in terms of production risks for a stable water supply.
5.2.1 Truck and pipeline water transport
The specific costs of water production and transport depend linearly on the fuel price at the location and the distance to the destination of water use, as shown in Fig. 16. For each site analysed, the specific cost of water is calculated using the parameters from Table 9. The water production cost is a small percentage of the total cost compared to the transport cost. For short distances, the production cost is about 20% (1.53 US$/m\(^{3}\) for an annual water production of 50,000 m\(^{3}\)) of the total cost, which share decreases significantly with increasing distance.
5.2.2 Specific energy consumption analysis
Comparing the SECs for the AWG technologies in the location analysis, it can be seen that the adsorption–desorption AWG also has the highest specific energy demand for all sites, as shown in Fig. 17. The specific energy demand of the CC AWG is in the same order of magnitude as that of the absorption–desorption AWG. The specific energy demand of the CC AWG model is on average about 30% higher than that of the absorption–desorption AWG model with 0.422 kWh/kg compared to 0.386 kWh/kg. The strongest influencing parameter for the specific energy demand of both CC AWG and absorption–desorption AWG is the absolute humidity for which a clear tendency of an increasing specific energy demand with decreasing absolute humidity can be observed. This tendency is not so clear for the absorption–desorption AWGs, as a lot of water can be absorbed into the liquid phase at particularly high peak humidity (see Fig. 5), and thus a short-term high absolute humidity greatly increases water production and efficiency. This effect also applies to the comparison with the adsorption–desorption AWG. With an average SEC of 1.156 kWh/kg across all sites, the adsorption–desorption AWG significantly higher in terms of energy demand than the other AWGs. However, the required desorption temperature level is relatively low and a day-night cycle is applied, so that meeting the energy demand with solar thermal energy is a reasonable alternative to drawing electricity from the grid. This would result in a fully off-grid solution, as proposed by most research, for example Kim et al [52].
5.2.3 Specific water cost analysis
The results of the cost calculation for each location are shown in Fig. 18, including the costs of bottled water and water production by desalination and transport. The specific cost of water increases with distance from the coast. Local fuel costs have a direct impact on transport costs. For coastal sites, only RO production costs are considered, resulting in a low specific water production cost of about 1.50 US$/t. Even in locations with very low electricity costs (e.g. Dubai, Doha), which proportionally influence the specific water production costs for AWG systems, this threshold is not reached, but is at least one order of magnitude higher. For longer water transport distances, the energy costs of AWG technologies are closer to the water costs. For Bloemfontein and other locations with distances to the coast greater than 600 km, the water production costs of absorption–desorption AWG and CC AWG are about the same as the specific water costs of truck transport. For Khartoum, absorption–desorption AWG and CC AWG are cheaper than water transport due to very low energy costs and favourable climatic conditions for atmospheric water production. On average for the locations analysed, the absorption–desorption AWG has the lowest operating cost at 61.88 US$/t, followed by the CC AWG at 89.32 US$/t and the adsorption–desorption AWG at 306.16 US$/t. Compared to bottled water with an average of 581.11 US$/t , all three AWG technologies analysed are advantageous in terms of cost.
The ratio of energy costs to total water costs is shown in Table 11. As expected, the results show that in locations with higher water production and lower energy costs, the energy costs far exceed the investment costs, e.g. in Dakar, where energy costs represent 92% (CC), 95% (absorption–desorption) and 63% (adsorption–desorption) of the total costs. On average over all sites, energy costs are the driving cost factors for CC AWG and absorption–desorption AWG at 68% and 82% respectively, while energy and investment costs are equal on average for adsorption–desorption AWG. These results, together with the cost analysis of the sites, make it clear that the primary focus for optimisation must be on increasing energy efficiency or implementing alternative energy supply concepts such as renewable energy. Although reducing production costs is also a viable option, it represents only a small part of the total water production costs.
5.2.4 Water production and availability risk analysis
Mean water production and confidence intervals of production are shown in Tables 12, 13, 14 for each technology. Using these confidence intervals, we can analyse how much water production varies over the year. As the volatility increases, so does the risk of having no water production for an extended period of time. For the CC AWG and the absorption–desorption AWG, large standard deviations were found for most sites, which implies a high risk of inconsistent water production throughout the year. The most promising location for constant water production is Dakar with a 2\(\sigma\) value of 102.27 L per hour (CC) or 119.72 L per hour (absorption–desorption), meaning that at least this amount of water can be produced 97.5% of the time. For the \(\sigma\) confidence levels, more locations such as Dubai or Lima can produce more than 60 L per h (CC) or 100 L per h (absorption–desorption) for 83.7% of the days. The large variation in production and the differences between the different locations can also be seen in Figs. 19, 21 and 22, which show the water production over the year for the three AWG technologies for the three distinct locations of Dakar, Khartoum and Los Angeles. In Dakar, where climatic conditions vary less over the year, water production is more stable than in Khartoum or Los Angeles. At these sites, water can be produced mainly during the warm and humid summer months. In contrast, the adsorption–desorption analysis (Fig. 21) shows a much more constant water production. This is due to the fact that the upper water capacity limit of the adsorbent is constantly reached at most sites and therefore the production is stable throughout the year, as shown by the high \(\sigma\) and 2\(\sigma\) values. Only a few sites, such as Khartoum or Denver, do not achieve this and experience larger fluctuations in water production.
In summary, the high volatility of production must be taken into account when planning the implementation of AWG technologies to ensure a constant water supply. Therefore, AWG technologies work best when used as an additional source of water to complement conventional options. Relying solely on AWG technologies for water supply in these locations is not a viable option.
6 Limitations of study
This chapter discusses the limitations, simplifying assumptions, and potential biases of this study.
Basic economical evaluation: Only a relatively simple economic analysis is considered in this study to provide a baseline analysis. More in-depth analysis of cash flow, financing risks, etc. is not included.
Modell parameters and assumptions: Many model parameters such as the purchase price of adsorption–desorption and absorption–desorption AWGs or operating parameters had to be estimated as no data points are available in the literature. These parameters may change in the future as more research is published or technologies become commercially available.
No exergy efficiency analysis for second law efficiency of AWG technologies: The models developed use only the first law of thermodynamics. Further studies implementing exergy efficiency analysis in the global analysis could prove useful to evaluate the second law efficiency of the AWG systems (e.g., Kim et al. [32] for second law efficiency analysis for adsorption–desorption AWG, Bahman and Groll [76] for second law analysis of air cooling units).
Not considering advanced plant design and control strategies: The efficiency of the technologies could be significantly increased by more complex plant designs, such as multi-stage concepts of adsorption–desorption AWG or different solution management concepts for absorption–desorption AWG [30, 34]. These are current areas of research that will become increasingly important in the future.
Life cycle analysis, environmental impact: A life cycle analysis would be useful to assess the overall impacts, including economic and environmental impacts, of AWG technologies. For example, the impacts and costs of disposal are not considered in this study.
Local regulatory guidelines, subsidies or government legislation: This study did not consider local government subsidies or barriers to the implementation of AWG technologies at the sites analysed.
Focus on bottled water and desalination for price comparisons; neglect of comparison with tap water: An economic comparison with tap water was not made because tap water is often locally subsidised and varies widely in quality, making it less comparable between sites.
7 Conclusion and outlook on future research
Water scarcity is one of the global challenges facing politics, business and science in the twenty-first century, threatening the livelihoods and quality of life of millions of people. Climate change will make water scarcity an even greater global systemic challenge in the future. Harnessing atmospheric moisture can make an important contribution to solving this challenge. In addition to water supply in water scarce areas, the use of decentralised and possibly self-sufficient water supply is an important requirement in the future scenarios of many technological fields. The scientific literature on the evaluation of the economic performance of AWGs, especially for desiccant-based AWGs, is limited. While existing scientific research mainly deals with technical aspects, there is no global analysis that evaluates the performance of AWGs taking into account seasonal and intra-day variations in climatic conditions. Therefore, this paper takes a first step towards comparing different active AWG technologies by implementing a framework for analysing the energetic and economic efficiency on a global scale.
Our results show that active AWG systems could be used as an alternative to water production and truck transport, as long as the location of water use is far from coasts or other water-rich regions. Compared to the price of bottled water, it is economically advantageous in all locations analysed. Absorptive systems were shown to have an energy efficiency advantage over conventional cooling condensation systems, but require a higher level of technology and process and plant design development. Adsorption-desorption AWGs are best suited for off-grid operation with solar power due to low desorption temperature requirements and convenient use of the day-night cycle. Overall, the cost of energy is still significantly higher than the cost of desalinating and transporting seawater to most locations around the world. This shows that AWG technologies are only economically competitive in the premium water market, e.g. bottled water. The analysis of the ratio of energy cost to total cost of water produced by the AWG technologies showed that most of the cost is produced by energy consumption (CC AWG: 68%, absorption–desorption AWG: 82%, adsorption–desorption AWG: 50%). This indicates that improving energy efficiency would significantly reduce the cost of water production.
A risk analysis of water production showed that at most of the sites analysed, there is a significant variation in water production over the course of a year for all of the AWG technologies. Relying solely on AWG technologies for water supply at these sites is not a viable option.
The current study can be extended by future research that could further investigate the overall environmental impact of AWG technologies using life cycle analysis to assess the carbon footprint. Investigations into local regulatory guidelines, subsidies or policies that could prove to be supportive or hindering to the implementation would also be beneficial to the realisation of future AWG technology projects.
Data availability
Data publicly available: Global electricity and fuel prices for the analysed locations are available at: https://www.globalpetrolprices.com/ [72]. Bottled water prices for the analysed locations are available at: https://www.globalproductprices.com/ [74]. Hourly temperature, relative humidity and air pressure data are generated using Meteonorm 8.0 [71]. Data available with the paper or supplementary information: The authors declare that the data supporting the findings of this study are available within the paper.
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JP and AD conceived of the presented idea. JP designed the model and the computational framework and analysed the data. JP performed the calculations and wrote the manuscript with reviews from all authors. All authors provided critical feedback and helped shape the research, analysis and manuscript.
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Potyka, J., Dalibard, A. & Tovar, G. Energetic analysis and economic viability of active atmospheric water generation technologies. Discov Appl Sci 6, 153 (2024). https://doi.org/10.1007/s42452-024-05746-z
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DOI: https://doi.org/10.1007/s42452-024-05746-z