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. 2020 Feb 21;10:3174. doi: 10.1038/s41598-020-59702-z

Equilibrium Thermodynamic Properties of Aqueous Solutions of Ionic Liquid 1-Ethyl-3-Methylimidazolium Methanesulfonate [EMIM][MeSO3]

Chaolun Zheng 1, Jian Zhou 1, Yong Pei 1, Bao Yang 1,
PMCID: PMC7035425  PMID: 32081922

Abstract

The ionic liquid 1-ethyl-3-methylimidazolium methanesulfonate ([EMIM][MeSO3]) has been considered as a promising alternative desiccant to triethylene glycol and lithium bromide commonly used in the industry. In this paper, the water activity coefficient of this binary system was measured from 303 K to 363 K with water concentration from 18% to 92%. The interaction energies between the ionic liquid molecules (g22) and between the ionic liquid and water molecules (g12) for the [EMIM][MeSO3]/water binary system were determined from the water activity coefficient data using the Non-Random Two-Liquid (NRTL) model. The magnitude of the interaction energy between the [EMIM][MeSO3] and water molecules (g12) was found to be in the range of 45~49 kJ/mol, which was about 20% larger than that between the water molecules (g11) in the [EMIM][MeSO3]/water system. The large (g12) can explain many observed macroscopic thermodynamic properties such as strong hygroscopicity in the ionic liquid [EMIM][MeSO3]. These interaction energies were used to determine the heat of desorption of the [EMIM][MeSO3]/water system, and the obtained heat of desorption was in good agreement with that calculated from the conventional Clausius-Clapeyron Equation.

Subject terms: Mechanical engineering, Materials science

Introduction

Ionic liquids are compounds composed of organic cations and inorganic anions, and they show a negligible vapor pressure and good fluidity over a wide temperature range1,2. Some ionic liquids have been found to be highly hygroscopic, which makes them promising desiccants for applications in gas dehydration and absorption cooling. In contrast to triethylene glycol currently used in gas dehydration, losses by evaporation can be eliminated when the ionic liquids are used as desiccants. In addition, the use of ionic liquids can avoid the crystallization and corrosion problems3,4, which are the two major concerns of the most commonly used halide salt liquid desiccants5,6.

The ionic liquid 1-ethyl-3-methylimidazolium methanesulfonate ([EMIM][MeSO3]) is among those that are highly hygroscopic, and is a promising candidate for next generation of desiccants7,8. The determination of thermodynamic properties is important for performance evaluation for this special ionic liquid. Many researchers have conducted experiments to measure the important macroscopic thermodynamic properties, such as specific heat9,10, density7,912, viscosity7,9,11,13, electrical conductivity9, surface tension11,14, reflective index11, diffusion coefficient7, nuclear magnetic resonance (NMR) spectroscopy9,14,15, excess molar heats of mixing9,12,16, and water activity coefficient7,16.

Although the macroscopic thermodynamic properties of the [EMIM][MeSO3]/water binary system have been extensively investigated, the molecular thermodynamic properties of this binary system are not comprehensive. For example, the interaction energy or bonding energy between the ionic liquid molecules, and between the ionic liquid and water molecules are extremely scarce for the ionic liquid [EMIM][MeSO3]/water systems. These molecular interaction energy properties are related to many macroscopic thermodynamic properties such as heat of desorption, heat capacity, hygroscopicity, and water vapor pressure.

In this work, the Non-Random Two-Liquid (NRTL) model was used to determine the interaction energies between different molecule pairs inside the [EMIM][MeSO3]/water binary system from the measured water activity coefficients data. These interaction energies were used to determine the heat of desorption of the [EMIM][MeSO3]/water system, which was in good agreement with those calculated from the Clausius-Clapeyron Equation. A formula to predict heat of desorption from the interaction energies was also developed for the binary systems.

Theoretical Background

Water activity coefficient

The activity coefficient of water γH2o is a fundamental thermodynamic parameter that accounts for deviations from ideal behavior in non-ideal solutions, such as the aqueous ionic liquid solutions, which is defined as7,8:

γH2O=pH2O,nonidealpH2O,ideal=pH2O,nonidealxH2OpH2O,sat 1

where pH2O,ideal and pH2O,nonideal are the partial pressure of water above the ideal and non-ideal aqueous solutions, respectively, pH2O,sat is the saturation pressure of pure water, and xH2O is the molar fraction of water in the aqueous solutions. In Eq. (1), the ratio pH2O,nonideal/pH2O,sat is the relative humidity (RH) of the non-ideal aqueous solutions. In the ideal aqueous solutions, the partial pressure of water can be described by Raoult’s law7:

pH2O,ideal=xH2OpH2O,sat 2

However, the [EMIM][MeSO3]/water solution is a non-ideal solution, in which the interaction energy between [EMIM][MeSO3] and water is significantly stronger than those between water and water. A small value of water activity coefficient γH2O indicates a large intermolecular force between water and ionic liquid molecules and strong hygroscopicity for water absorption. The water activity coefficient at infinite dilution γH2O, is often used for the comparison of the hygroscopicity or absorption strength of different desiccants7.

Non-random two-liquid (NRTL) model

The NRTL model1720 correlates the activity coefficients γi of a compound i with its mole fractions xi in the liquid solutions:

lnγ1=x22(Δg1211RTexp(2α12Δg1211/RT)[x1+x2exp(α12Δg1211/RT)]2+Δg1222RTexp(α12Δg1222/RT)[x2+x1exp(α12Δg1222/RT)]2) 3
lnγ2=x12(Δg1222RTexp(2α12Δg1222/RT)[x2+x1exp(α12Δg1222/RT)]2+Δg1211RTexp(α12Δg1211/RT)[x1+x2exp(α12Δg1211/RT)]2) 4

where the subscripts 1 and 2 refer to component 1 and component 2 in the binary solution, respectively, Δg1211 and Δg1222are the exchange in the interaction energy between molecules, α12 is the non-randomness parameter, R is the molar gas constant, and T is the absolute temperature. In the case of infinite dilution, the NRTL equations reduce to

lnγ1,=Δg1211RT+Δg1222RTexp(α12Δg1222/RT) 5
lnγ2,=Δg1222RT+Δg1211RTexp(α12Δg1211/RT) 6

The water activity coefficient at infinite dilution γH2O, can be used to compare the hygroscopicity or absorption strength of different desiccants.

In the NRTL model, the exchange in the interaction energy Δg1211=g12g11, which is the interaction energy change as a result of breaking a 1-1 interaction g11 and forming a 1–2 interaction g12. In this study, components 1 and 2 refer to the water and the [EMIM][MeSO3], respectively. So g11, g22, and g12 are the interaction energies between the water molecules, between the ionic liquid [EMIM][MeSO3] molecules, and between the water and [EMIM][MeSO3] molecules. The interaction energy parameters Δg1211 and Δg1222 can be determined by data fitting using Eqs. (3) and (4) if the water activity coefficients γH2O with its mole fraction xH2O can be measured in the [EMIM][MeSO3]/water binary system. The interaction energy between the ionic liquid and water molecules g12 can be determined using the formula: g12=Δg1211+g11 if the interaction energy between water molecules g11 is known. Similarly, the interaction energy between the ionic liquid molecules g22 can be determined by g22=Δg1222+g12. These molecular interaction energy properties are related to many macroscopic thermodynamic properties such as heat of desorption, heat capacity, hygroscopicity, and water vapor pressure. One application of these molecular interaction energies is that they can be used to predict the heat of desorption of the aqueous ionic liquid solutions with water concentration from 0% to 100%. In comparison, the Clausius-Clapeyron Equation determines the heat of desorption at the water concentration where the vapor pressure and temperature are known.

Clausius-Clapeyron equation

The Clausius-Clapeyron Equation relates the vapor-liquid equilibrium (VLE) data (p and T) to the thermodynamic property, enthalpy of vaporization (ΔHv), which is given by21

ln(p)=ΔHvRT+C, 7

where p is the vapor pressure at the temperature T, ΔHv is enthalpy of vaporization, R is the molar gas constant, and C is a constant. In Eq. (7), ΔHv is assumed to be independent of T. However, the temperature dependence of ΔHv cannot be overlooked in the water and [EMIM][MeSO3] binary solutions due to the complex interaction between water and [EMIM][MeSO3]21,22. In a moderate temperature range, ΔHv can be assumed to change linearly with T,

ΔHv=ΔHv,0+aT, 8

where a is the temperature coefficient. So the modified Clausius–Clapeyron Equation for the ionic liquid solutions can be written as follows:

ln(pp0)=ΔHv,0R(1T1T0)+aRln(TT0). 9

Therefore ΔHv can be determined from Eqs. (8) and (9) when the VLE data are measured.

Uncertainty calculation

The experimental uncertainty in this experiment is estimated using the root-sum-square method suggested by Moffat23:

δR={i=1N(Rxiδxi)2}1/2 10

In particular, whenever the equation describing the result is a pure “product form”, as shown in Eq. (11):

R=X1aX2bX3cXMm 11

the relative uncertainty can be calculated by Eq. (12):

δRR={(aδX1X1)2+(bδX2X2)2++(mδXMXM)2}1/2 12

Experimental Methods

Materials

The 1-ethyl-3-methylimidazolium methanesulfonate ([EMIM][MeSO3]) was purchased from Sigma-Aldrich (purity higher than 95 wt. %). Deionized water was used in the experiment.

Experiment setup

The experiment setup for the vapor-liquid equilibrium (VLE) measurement is shown in Fig. 1. The temperature during experiments was controlled using a temperature-controlled oven (Yamato, DKN-402C). The [EMIM][MeSO3]/water solution was placed inside a reactant bottle, in which a humidity sensor (Rotronic HC2A-SM) was attached. The RH and temperature (T) of the gas phase inside the reactant bottle were measured simultaneously using this humidity sensor with an uncertainty of T = ±0.1 K and RH = ±0.8% of the RH reading. The water concentration in [EMIM][MeSO3]/water solutions was measured using the Karl Fisher Titrator (Mettler Toledo™ C20D) with a relative uncertainty less than 0.5%. A magnetic stirrer (Thermo Scientific Cimarec Micro Stirrers) was used to stir the [EMIM][MeSO3]/water solution inside the reactant bottle during the VLE measurement. The data logging and the conversion from RH and T to water vapor pressure were performed using the HW4-E software in a computer.

Figure 1.

Figure 1

Schematic of the experimental setup for the VLE Measurements. Legend: 1. temperature-controlled oven; 2. humidity sensor; 3. reagent bottle; 4. [EMIM][MeSO3]/water solution; 5. magnetic stirrer; 6. DAQ/computer.

VLE measurements

Twelve [EMIM][MeSO3]/water solutions with molar concentration of water from 18% to 92% were prepared in the VLE measurements. For each solution, its RH was measured at temperatures 303 K, 323 K, 343 K, and 363 K. The sample solution with an approximate volume of 100 ml was placed in the reactant bottle. The oven temperature was set to the desired temperature, and the sample solution was heated and stirred vigorously with magnetic stirrers to get homogeneous mixing. At the same time, the data logging was started. After the system reached the equilibrium and the RH stayed unchanged for 30 minutes, the equilibrium temperature and RH were recorded. A series of equilibrium temperature and water vapor pressure (or RH) data were obtained for the [EMIM][MeSO3]/water solutions.

Results and Discussion

Activity coefficient of water

The experimental VLE data for the [EMIM][MeSO3]/water binary solutions with water molar concentrations from 18% to 92% were measured and listed in Table 1. The vapor pressure pH2O were determined using the measured RH. The relative uncertainty of the measured mole fraction x(H2O) was found to be less than 5.02% using Eq. (12). The RH and T were measured simultaneously using the humidity sensor with an uncertainty of T = ±0.1 K and RH = ±0.8% of the RH reading. Figure 2 shows the measured water vapor pressure in [EMIM][MeSO3]/water binary solutions versus the molar fraction of water in a temperature range of 303 K to 363 K.

Table 1.

Experimental VLE data of the[EMIM][MeSO3]/water binary solutions at different temperatures.

x(H2O) Relative Humidity (%)
303 K 323 K 343 K 363 K
0.1855 2.31 2.68 3.04 3.44
0.2579 3.46 3.89 4.36 4.86
0.3207 4.87 5.40 6.00 6.67
0.3744 5.98 6.57 7.28 8.05
0.4840 9.86 10.60 11.47 12.45
0.5568 13.99 14.90 16.02 17.14
0.6602 22.42 23.71 25.14 26.45
0.7269 30.19 31.74 33.60 34.80
0.7752 38.94 40.33 42.00 43.35
0.8294 51.55 53.12 54.63 55.89
0.8821 68.20 68.84 69.76 70.82
0.9178 79.35 80.12 81.00 81.06
x(H2O) Water Vapor Pressure (Pa)
303K 323K 343K 363K
0.1855 98.01 330.71 947.63 2412.03
0.2579 146.81 480.03 1359.10 3407.69
0.3207 206.63 666.36 1870.32 4676.80
0.3744 253.73 810.74 2269.32 5644.42
0.4840 418.36 1308.04 3575.43 8729.57
0.5568 593.60 1838.66 4993.75 12018.05
0.6602 951.28 2925.81 7836.64 18545.95
0.7269 1280.96 3916.72 10473.79 24400.72
0.7752 1652.22 4976.72 13092.24 30395.72
0.8294 2187.27 6555.01 17029.26 39188.39
0.8821 2893.73 8494.86 21745.59 49656.86
0.9178 3366.82 9886.81 25249.32 56836.84

Figure 2.

Figure 2

Water vapor pressure in the [EMIM][MeSO3]/water binary solutions versus the molar fraction of water in the temperature range of 303 K to 363 K.

The effect of the ionic liquid on the non-ideality of the aqueous solutions can be expressed by the activity coefficients of water γH2O, which was calculated by Eq. (1). Table 2 shows the calculated activity coefficients of water γH2O in the [EMIM][MeSO3]/water binary solutions. The relative uncertainty of the water activity coefficient γH2O was found to be 5.09%. The plot of the activity coefficient γH2O versus the molar concentration of water is shown in Fig. 3. As shown in this figure, the water activity coefficient γH2O approaches a value of one when the water concentration is close to 100%, as expected by Raoult’s law. For water concentrations below about 30 mol.%, γH2O approaches almost constant values between 0.10 and 0.15. A small value of γH2Oindicates a large deviation from the ideal solution behavior or from Raoult’s law. A small value of γH2Ois desired for the application in gas dehydration. The influence of the temperature on γH2O is small in the temperature range of test, especially for low water concentrations. For a given water concentration, γH2O increases slightly when the temperature increases, which is consistent with the temperature dependence of the interaction energy Δg1211 in the [EMIM][MeSO3]/water binary solutions.

Table 2.

Water Activity Coefficient γH2O of the [EMIM][MeSO3]/water binary solutions at different temperatures.

x(H2O) Water Activity Coefficient γH2o
303 K 323 K 343 K 363 K
0.1855 0.1245 0.1445 0.1639 0.1854
0.2579 0.1342 0.1509 0.1691 0.1885
0.3207 0.1518 0.1684 0.1871 0.2080
0.3744 0.1597 0.1755 0.1944 0.2150
0.4840 0.2037 0.2190 0.2370 0.2572
0.5568 0.2512 0.2676 0.2877 0.3078
0.6602 0.3396 0.3592 0.3808 0.4007
0.7269 0.4153 0.4366 0.4622 0.4787
0.7752 0.5023 0.5202 0.5418 0.5592
0.8294 0.6215 0.6404 0.6586 0.6738
0.8821 0.7732 0.7804 0.7908 0.8029
0.9178 0.8645 0.8729 0.8825 0.8832

Figure 3.

Figure 3

Activity coefficient of water in the [EMIM][MeSO3]/water binary solutions versus the molar fraction of water in the temperature range of 303 K to 363 K.

The water activity coefficients at infinite dilution γH2O, for the [EMIM][MeSO3]/water binary solutions are listed in Table 3. It is found that the limiting water activity coefficients γH2O, is in the range of 0.102 to 0.151 at temperatures from 303 K to 363 K, more than 4 times lower than that for triethylene glycol, which indicates that the ionic liquid [EMIM][MeSO3] possesses much stronger ability of absorbing water vapor than the commonly used triethylene glycol desiccants.

Table 3.

Water activity coefficient at infinite dilution γH2O, for the [EMIM][MeSO3]/water binary system at different temperatures.

Temperature (K) 303 323 343 363
γH2O, 0.1015 0.1165 0.1322 0.1507

There exist some discrepancies in γH2O, in literature. For example, Krannich et al.7 reported the γH2O, around 0.20 that was determined using the boiling point method. Domanska et al.16 reported the γH2O, in the range 0.071~0.088, which were determined with the gas-liquid chromatography method. In this study, the limiting water activity coefficients γH2O, was found to be in the range of 0.102 to 0.151 at temperatures from 303 K to 363 K. The differences in the reported γH2O, data might be due to the different measurement techniques.

Interaction energy between molecules and non-randomness parameters

The exchange in interaction energy Δg1211, and Δg1222 and the non-randomness parameter α12 in the [EMIM][MeSO3]/water binary solutions can be extracted by fitting the experimental data γH2Oto the NRTL equations (Eqs. (34)). These parameters are listed in Table 4. In Table 4, the subscript “1” represents water, while the “2” represents the ionic liquid [EMIM][MeSO3]. Δg1211 is the interaction energy change as a result of breaking an H2O-H2O interaction and forming a [EMIM][MeSO3]-H2O interaction. As shown in Table 4, the interaction energy parameters Δg follow the order [EMIM][MeSO3]-[EMIM][MeSO3] > [EMIM][MeSO3]-H2O ≫ H2O-H2O. The large negative value of Δg1211 indicates that the intermolecular attractive force between [EMIM][MeSO3] and H2O is much stronger than that between H2O and H2O. The absolute value of interaction energy Δg1211 and Δg1222 decreases with increasing temperature, which could be attributed to the increasing thermal motion of the molecules18.

Table 4.

Interaction Energy and Non-Randomness parameters for the [EMIM][MeSO3]/water binary system at different temperatures.

Temperature (K) 303 323 343 363
α12 0.425 0.461 0.492 0.535
Δg1211 (J/mol) −7428 −7401 −7379 −7284
Δg1211 (J/mol) 2559 2490 2450 2405
g11 (J/mol) −41270 −40240 −39210 −38150
g12 (J/mol) −48698 −47641 −46589 −45434
g22 (J/mol) −51257 −50131 −49039 −47839
ARD 2.22% 2.64% 2.98% 3.13%

For comparison, the exchange in interaction energy Δg1211 and Δg1222 in some other ionic liquids/water binary solutions were summarized in Table 519,20,24,25. It should be noted that the Δg1211 in the [EMIM][MeSO3]/water binary solution was found to be larger than that in 1-ethyl-3-methylimidazolium ethylsulfate ([EMIM][EtSO4])/water solution25, which is another promising ionic liquid for moisture removal and shares similar chemical structure26,27. The difference in interaction energy may result from the shorter alkyl group in [EMIM][MeSO3] anion, which is favorable for the bonding with water molecule28,29.

Table 5.

Interaction Energy parameters for other ionic liquid/water binary systems.

Ionic Liquids Δg12−11 (J/mol) Δg12−22 (J/mol)
[EMIM][(CF3SO2)2N]19 −1458 12913
[BMIM][(CF3SO2)2N]19 −349 19436
[EMIM][DMP]20 −3925 5278
[MMIM][DMP]24 −9566 5065
[EMIM][DEP]24 −6535 11818
[EMIM][EtSO4]25 −1440 4439

The interaction energy between water molecules g11 is the molar vaporization energy of water (i.e., cohesive energy) but has a negative sign on it30, which is available in liteature31. The interaction energy between the ionic liquid and water molecules g12 can be calculated using the formula: g12=Δg1211+g11. Similarly, the interaction energy between the ionic liquid molecules g22 can be determined by g22=Δg1222+g12. The obtained interaction energies g11,g12 and g22 are summarized in Table 4. These molecular interaction energies have negative signs due to the intermolecular attractive forces. It is found in Table 4 that the molecular interaction energies become less negative when the temperature increases. The magnitude of the interaction energy between the [EMIM][MeSO3] and water molecules was found to be in the range of 45~49 kJ/mol, which was 20% larger than that between the water molecules in the [EMIM][MeSO3]/water system. The large interaction energy between the ionic liquid [EMIM][MeSO3] and water molecules can explain many reported macroscopic thermodynamic properties, such as small water activity coefficient and strong hygroscopicity.

The parameters α12 is related to the non-randomness in the liquid mixture; when α12 is zero, the local distribution around the center molecule is completely random. The non-randomness parameters α12 in the [EMIM][MeSO3]/water binary solutions were found to be around 0.5, as shown in Table 4. The values of α12 are generally consistent with those reported for other water/hygroscopic ionic liquid binary solutions17,20,24. The non-zero α12 in the [EMIM][MeSO3]/water binary solutions are mainly due to the difference in interaction energy and size between water and [EMIM][MeSO3].

The extent of the correlation between the experimental data and the NRTL model was evaluated by calculating the absolute relative deviation (ARD)24:

ARD=|γexpγNRTLγexp|n 13

where n is the number of data points, γexp is the γ value calculated from experimental data, and γNRTL is the γ value calculated from the NRTL model. The values of ARD are also listed in Table 4, which implies a satisfactory correlation in the test temperature range.

Heat of desorption

One application of these molecular interaction energies is that they can be used to determine the heat of desorption of the aqueous ionic liquid solutions. The internal energy in the aqueous ionic liquid solution Ul is the sum of the excess internal energy of the solution UE and the molar internal energy of the pure component Ui:

Ul=UE+n1U1+n2U2 14

where n1 and n2 are the mole number of component 1 (i.e., water) and component 2 (i.e., ionic liquid), respectively. In the evaporation process, the intermolecular interaction energy is dominant, and therefore the intramolecular interaction energy can be neglected in the internal energy. The excess internal energy of the aqueous ionic liquid solution UE can be evaluated as18,32:

UE=(g(1)g11)n1+(g(2)g22)n2 15

where g11 and g22 are the molar interaction energy between water molecules and between the ionic liquid and water molecules, respectively, and g(1) and g(2) represent the molar residual Gibbs energy for molecule cells having component 1 and component 2 at the center respectively33. g(1) and g(2) can be calculated as:

g(1)=x11g11+x21g12=g11+x21Δg1211 16
g(2)=x12g12+x22g22=g22+x12Δg1222 17

where x11, x22, x21 and x12 represent the local mole fractions. For example, x21 is the local mole fraction of component 2 around the center component 1. x21 and x12 depend on the global concentration according to the NRTL model,

x21=x2exp(α12Δg1211/RT)x1+x2exp(α12Δg1211/RT)=n2exp(α12Δg1211/RT)n1+n2exp(α12Δg1211/RT) 18
x12=x1exp(α12Δg1222/RT)x2+x1exp(α12Δg1222/RT)=n1exp(α12Δg1222/RT)n2+n1exp(α12Δg1222/RT) 19

Differentiating Eq. (14) leads to the change of internal energy in the liquid solution for the evaporation of one mole of water:

ΔUl=g11Δg1211x22exp(2α12Δg1211/RT)(x1+x2exp(α12Δg1211/RT))2Δg1222x22exp(α12Δg1222/RT)(x2+x1exp(α12Δg1222/RT))2 20

Considering the volume work in the evaporation process, which is equal to RT based on the ideal gas assumption, the heat of desorption can be calculated using the interaction energies:

ΔHv=g11+RTΔg1211x22exp(2α12Δg1211/RT)(x1+x2exp(α12Δg1211/RT))2Δg1222x22exp(α12Δg1222/RT)(x2+x1exp(α12Δg1222/RT))2 21

The formula can be used to predict the heat of desorption in the aqueous binary solutions when the interaction energies are given.

Figure 4 shows the heat of desorption calculated from the interaction energies in the [EMIM][MeSO3]/water binary solutions with water fraction from 0% to 100% at temperatures 303 K, 323 K, 343 K, and 363 K. The desorption heat calculated by the Clausius-Clapeyron Equation is also shown for comparison. As shown in Fig. 4, they are in good agreement. The desorption heat ΔHv decreases with increasing temperature for a given water concentration. This trend is consistent with the temperature dependence of the interaction energy parameters Δg1211 and Δg1222 listed in Table 4, which could be attributed to the increasing thermal motion of the molecules at elevated temperatures. Due to the strong bonding forces between water and [EMIM][MeSO3], the desorption heat or enthalpy of vaporization of water in the [EMIM][MeSO3]/water solutions is always higher than the enthalpy of vaporization of pure water at the same temperature, but the difference becomes smaller when the water concentration approaches 100%.

Figure 4.

Figure 4

Desorption heat calculated from the interaction energy in the temperature range of 303 K to 363 K and water fraction range of 0% to 100%. (The desorption heat calculated by the Clausius-Clapeyron Equation is also shown for comparison).

Conclusion

In this work, molecular thermodynamic properties such as interaction energies and non-randomness parameter of the [EMIM][MeSO3]/water binary system were determined from the water activity coefficient data using the Non-Random Two-Liquid (NRTL) model. The water activity coefficient of this binary system was measured with molar concentrations of water from 18% to 92% at temperatures 303 K, 323 K, 343 K, and 363 K. The interaction energy between the ionic liquid [EMIM][MeSO3] and water molecules (g12) was found to be ~20% larger than that between the water molecules (g11). The exchange in interaction energy Δg followed the order [EMIM][MeSO3]-[EMIM][MeSO3] > [EMIM][MeSO3]-H2O» H2O-H2O. The large negative value of Δg1211 (−7427.51 J/mol to −7283.79 J/mol) indicated that the intermolecular attractive force between [EMIM][MeSO3] and H2O was much stronger than that between H2O and H2O. This can explain the observed strong hygroscopicity in the ionic liquid [EMIM][MeSO3]. With the molecular interaction energies, the heat of desorption was predicted in the [EMIM][MeSO3]/water binary system. The obtained heat of desorption was in good agreement with that calculated from the conventional Clausius-Clapeyron Equation.

Acknowledgements

This research is financially supported by DOE under Grant DEEE0008672.

Author contributions

B.Y. and C.Z. conceived the experiment and developed the theoretical model. C.Z. set up the experimental system. C.Z. and J.Z. performed the experiments. C.Z. and Y.P. conducted the data analysis. C.Z. and B.Y. wrote the main manuscript. All authors reviewed the manuscript.

Data availability

All data generated or analyzed during this study are included in this published article.

Competing interests

The authors declare no competing interests.

Footnotes

Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

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Data Availability Statement

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