ARTICLE IN PRESS Energy 32 (2007) 1660–1669 www.elsevier.com/locate/energy Thermodynamic equilibrium model and second law analysis of a downdraft waste gasifier S. Jarungthammachote, A. Dutta Energy Field of Study, School of Environment, Resources and Development, Asian Institute of Technology, P.O. Box 4, Klongluang, Pathumthani 12120, Thailand Received 9 August 2006 Abstract The management of municipal solid waste (MSW) and the current status of world energy resources crisis are important problems. Gasification is a kind of waste-to- energy conversion scheme that offers the most attractive solution to both waste disposal and energy problems. In this study, the thermodynamic equilibrium model based on equilibrium constant for predicting the composition of producer gas in a downdraft waste gasifier was developed. To enhance the performance of the model, further modification was made by multiplying the equilibrium constants with coefficients. The modified model was validated with the data reported by different researchers. MSW in Thailand was then used to simulate and to study the effects of moisture content (MC) of the waste on the gasifier’s performance. The results showed that the mole fraction of H2 gradually increases; CO decreases; CH4, which has a very low percentage in the producer gas increases; N2 slightly decreases; and CO2 increases with increasing MC. The reaction temperature, the calorific value, and the second law efficiency, decrease when MC increases. r 2007 Elsevier Ltd. All rights reserved. Keywords: Downdraft waste gasifier; Thermodynamic equilibrium model; Second law analysis; Municipal solid waste; Waste to energy 1. Introduction The management of municipal solid waste (MSW) is one of the most important problems especially for developing countries. The quantity of solid waste generated by human activities has increased dramatically and its characteristics depend on the location and people’s lifestyles. In general, there are five main categories of acceptable waste handling options available; namely (1) prevention, (2) re-use and recycling, (3) composting, (4) incineration, and (5) landfilling. In many countries, landfills are the most frequently used option to dispose MSW. Lately, incineration is considered to be one of the most effective means of dealing with waste [1]. Incineration not only reduces volume of solid waste but also converts wastes to an energy form. This scheme is popularly known as waste-to-energy (WTE) conversion. However, due to the environmental problems that go hand-in-hand with incineration, waste incinerators Corresponding author. Tel.: +66 2 524 5403; fax: +66 2 524 5439. E-mail address: [email protected] (A. Dutta). 0360-5442/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.energy.2007.01.010 are required to install with sophisticated exhaust gas cleaning equipment. Depending on the regulations of the country, this gas cleaning equipment can be large and expensive [2]. Gasification is another kind of WTE conversion that is very attractive. In the old days, gasification was widely used for producing gases from coal and biomass but now gasification of waste has become one of the growing interests of many organizations and researchers. Moreover, due to the world’s energy crisis, finding new energy resources is very important. For these reasons, it is apparent that gasification of waste is a solution for both MSW management and finding option for new energy resources. Furthermore, it also proves to be more environmental friendly compared to other options. Since waste is inherently non-homogeneous material, the composition of MSW varies significantly and depends on many factors. These are location, local policy, origin of the waste, etc. For a techno-economical evaluation, actual construction of a gasifier is not always feasible and economically sound because experimentation usually ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 Nomenclature C C̄ p D E Exp Dḡof DGTo o h̄f Dh̄T H HHV K LHV m Mod n N O P R̄ RMS s̄ mass fraction of carbon specific heat at constant pressure, kJ/kmol K number of data exergy, kJ experimental data standard Gibbs function of formation standard Gibbs function of reaction at temperature T enthalpy of formation, kJ/kmol enthalpy difference in any given T and at 298 K, 1 atm, kJ/kmol mass fraction of hydrogen higher heating value, MJ/kg equilibrium constants lower heating value, kJ/kmol kmol of oxygen per kmol of feedstock predicted value from model numbers of mole mass fraction of nitrogen mass fraction of oxygen pressure, atm universal gas constant, 8.314 kJ/kmol K root-mean-square specific entropy, kJ/kmol K involves much greater time, effort, and cost. Thus, a mathematical model for such analysis is more useful. The equilibrium model has been used by many researchers for the analysis of the gasification process. Those models were based on the minimization of Gibbs free energy [3–7]. This is a constrained optimization problem that generally uses the Lagrange multiplier method. An understanding of some mathematical theories is necessary for solving optimization and non-linear equation problems. The other kind of equilibrium model is based on equilibrium constant. However, it is important to note that an equilibrium model based on the minimization of Gibbs free energy and one based on equilibrium constants are of the same concept. Zainal et al. [8] used the latter type of equilibrium model to predict the composition of the producer gas for different biomass materials. The amount of oxygen in that model was eliminated by defining it in terms of some components in the producer gas; however, it was not shown when they compared their model with the experimental data. This is what makes the model developed in this study different. The relationship between the amount of oxygen and the reaction temperature has been explored. This model can predict the reaction temperature by knowing the amount of oxygen, and vice versa. To further improve the model, the equilibrium constants were multiplied by the coefficients determined from the comparison of the predicted results with the experimental results S T w x 1661 mass fraction of sulfur temperature, K kmol of moisture per kmol of feedstock mole fraction Greek letters n e Z stoichiometric number specific exergy, kJ/kmol efficiency Superscripts quantity per unit mole Subscripts ch dry ex feed fg i, j, k ph o chemical dry basis exergy feedstock difference in property between saturated liquid and saturated vapor i, j, kth gas species physical standard reference state from other works. Data on MSW of Thailand was used in the modified model for the simulation to study the effects of moisture content on the composition of the producer gas, on the reaction temperature, and on the calorific value. Finally, the second law efficiency of the gasification process was estimated for the solid waste with 20%, 25%, and 30% moisture content. 2. The model To develop the model, the chemical formula of feedstock is defined as CHxOyNz. The global gasification reaction can be written as follows: CHx Oy Nz þ wH2 O þ mðO2 þ 3:76N2 Þ ¼ nH2 H2 þ nCO CO þ nCO2 CO2 þ nH2 O H2 O z þ 3:76m N2 , þ nCH4 CH4 þ 2 ð1Þ where x, y, and z are the number of atoms of hydrogen, oxygen, and nitrogen per number of atom of carbon in the feedstock, respectively; w is the amount of moisture per kmol of feedstock; and m is the amount of oxygen per kmol of feedstock. All inputs on the left-hand side of Eq. (1) are defined at 25 1C. On the right-hand side, ni are the numbers of mole of the species i that are also unknown. ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 1662 2.1. Mass balance To find the five unknown species of the producer gas, five equations were required. Those equations were generated using mass balance and equilibrium constant relationships. Considering the global gasification reaction in Eq. (1), the first three equations were formulated by balancing each chemical element as shown in Eqs. (2)–(4). Carbon balance: f 1 ¼ 0 ¼ nCO þ nCO2 þ nCH4 1. f 4 ¼ 0 ¼ K 1 ðnCO ÞðnH2 O Þ ðnCO2 ÞðnH2 Þ, (11) f 5 ¼ 0 ¼ K 2 ðnH2 Þ2 ðnCH4 Þðntotal Þ. (12) (2) Eqs. (13) and (14) were used for the equilibrium state of ideal gas mixture because of the requirements of K1 and K2 values (3) DG oT , R̄T X ni Dḡof;T;i , DG oT ¼ Hydrogen balance: f 2 ¼ 0 ¼ 2nH2 þ 2nH2 O þ 4nCH4 x 2w. where xi is mole fraction of species i in the ideal gas mixture, n is stoichiometric number (positive value for products and negative value for reactants), Po is standard pressure, 1 atm, and ntotal is total mole of producer gas. Eqs. (9) and (10) can be modified as ln K ¼ Oxygen balance: f 3 ¼ 0 ¼ nCO þ 2nCO2 þ nH2 O w 2m y. (4) (13) (14) i 2.2. Thermodynamic equilibrium Chemical equilibrium is usually explained either by minimization of Gibbs free energy or by using an equilibrium constant. To minimize the Gibbs free energy, constrained optimization methods are generally used which requires an understanding of complex mathematical theories. For that reason, the present thermodynamic equilibrium model is developed based on the equilibrium constant and not on the Gibbs free energy. The remaining two equations, were obtained from the equilibrium constant of the reactions occurring in the gasification zone as shown below Boudouard reaction : C þ CO2 ¼ 2CO; (5) Water2gas reaction : C þ H2 O ¼ CO þ H2 , (6) Methane reaction : C þ 2H2 ¼ CH4 . CO2 þ H2 O ¼ CO2 þ H2 . (8) For the model in this study, the thermodynamic equilibrium was assumed for all chemical reactions in the gasification zone. All gases were assumed to be ideal and all reactions form at pressure 1 atm. Therefore, the equilibrium constants, which are functions of temperature for the water–gas shift reaction and the methane reaction are: The equilibrium constant for water–gas shift reaction P ni Y i P ðnCO2 ÞðnH2 Þ K1 ¼ . (9) ðxi Þni ¼ o P ðnCO ÞðnH2 O Þ i The equilibrium constant for methane reaction P ni Y i P ðnCH4 Þðntotal Þ ni K2 ¼ ðxi Þ ¼ , o P ðnH2 Þ2 i The values of coefficients a0 –g0 and the enthalpy of formation of the gases are presented in Table 1 [10]. For calculating K1 and K2, the temperature in the gasification or reduction zone must be known. In this study, it was determined using energy balance method as explained in Section 2.3. (7) Zainal et al. [8] and Higman and van der Burgt [9] presented that Eqs. (5) and (6) can be combined to give the water–gas shift reaction by subtracting Eq. (5) from Eq. (6) Water2gas shift reaction : where R̄ is the universal gas constant, 8.314 kJ/(kmol K), DGTo is the standard Gibbs function of reaction, and Dḡof;T;i represents the standard Gibbs function of formation at given temperature T of the gas species i which can be expressed by the empirical equation below 0 0 c d o Dḡof;T ¼ h̄f a0 T lnðTÞ b0 T 2 T3 T4 2 3 0 e þ ð15Þ þ f 0 þ g0 T. 2T (10) 2.3. Energy balance The temperature of the gasification zone needs to be calculated in order to calculate the equilibrium constants (Eqs. (13)–(15)). For this reason, either energy or enthalpy balance was performed for the gasification process which was usually assumed to be an adiabatic process [8]. When the temperature in gasification zone is T and the temperature at inlet state is assumed to be 298 K (25 1C), the enthalpy balance for this process can be written as X o X o o ni ðh̄f;i þ Dh̄T;i Þ, (16) h̄f;j ¼ j¼react i¼prod o h̄f where is the enthalpy of formation in kJ/kmol and its value is zero for all chemical elements at reference state (298 K, 1 atm), and Dh̄T represents the enthalpy difference between any given state and at reference state. It can be approximated by Z T C̄ p ðTÞ dT, Dh̄T ¼ (17) 298 ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 1663 Table 1 o The value of h̄f (kJ/mol) and coefficients of the empirical equation for Dḡof;T (kJ/mol) o Compound h̄f a0 b0 c0 d0 e0 f0 g0 CO CO2 H2O CH4 110.5 393.5 241.8 74.8 5.619 103 1.949 102 8.950 103 4.620 102 1.190 105 3.122 105 3.672 106 1.130 105 6.383 109 2.448 108 5.209 109 1.319 108 1.846 1012 6.946 1012 1.478 1012 6.647 1012 4.891 102 4.891 102 0.0 4.891 102 8.684 101 5.270 2.868 1.411 101 6.131 102 1.207 101 1.722 102 2.234 101 Table 2 The coefficients of specific heat for the empirical equation Gas species a b c d Temperature range (K) Hydrogen Carbon monoxide Carbon dioxide Water vapor Methane Nitrogen 29.11 28.16 22.26 32.24 19.89 28.90 0.1916 102 0.1675 102 5.981 102 0.1923 102 5.204 102 0.1571 102 0.4003 105 0.5372 105 3.501 105 1.055 105 1.269 105 0.8081 105 0.8704 109 2.222 109 7.469 109 3.595 109 11.01 109 2.873 109 273–1800 273–1800 273–1800 273–1800 273–1500 273–1800 where C̄ p ðTÞ is specific heat at constant pressure in kJ/kmol K and is a function of temperature. It can be defined by the empirical equation below C̄ p ðTÞ ¼ a þ bT þ cT 2 þ dT 3 , (18) where T is the temperature in K and Z T C̄ p ðTÞdT ¼ aT þ bT 2 þ cT 3 þ dT 4 þ k, (19) 2.4. Calculation procedure 298 where k is a constant obtained from the integration and a, b, c, and d are the specific gas species coefficients, which are shown in Table 2 [11]. Eq. (16) can be rewritten as X o X o h̄f;j ¼ ni h̄f;i j¼react i¼prod 2 3 P P 2 3 n a n b þ n c T þ T i i i i i i T 7 6 i i 6 i 7 7. þ6 6 P 7 P 4þ 5 4 nd T þ nk P i i i To solve the values of nH 2 ; nCO ; nCO2 ; nH2 O and nCH4 an initial temperature was assumed and substituted into Eqs. (13) and (15) to initially calculate K1 and K2. Then, both equilibrium constants were substituted into Eqs. (11) and (12), respectively. Finally, the five simultaneous equations, Eqs. (2), (3), (4), (11), and (12), were used and solved by Newton–Raphson method. For calculating the new value of temperature, Eq. (20) was used. The outlined procedure was repeated until the temperature value was converged. The detail of the calculation procedure is illustrated in Fig. 1. i i i 3. Validation and modification of the model ð20Þ De Souza-Santos [12] suggested the relationship for finding the enthalpy of formation for solid fuel in reactant that is X o o h̄f;fuel ¼ LHV þ ½nk ðh̄f Þk , (21) k¼prod o ðh̄f Þk calculated from Eq. (20) using Newton–Raphson method. This relationship can predict the reaction temperature by knowing the amount of air. This makes the model a good tool to show the variation of reaction temperature when mole of air is changed. where is the enthalpy of formation of product k under complete combustion of the solid fuel and LHV is the lower heating value of the solid fuel in kJ/kmol. Now that the enthalpies of formation in Eq. (16) can be solved, the temperature in the gasification zone can finally be 3.1. Validation The model developed in this study was tested by comparing the calculation results with data from other researchers. Nine experimental data reported by Jayah et al. [13] were used to compare with the results from the model developed. The comparison is shown in Table 3. The comparison was done by setting the temperature used for the developed model fixed at 1100 K as reported by Jayah et al. [13]. Table 4 shows the comparisons of results between the model developed and the experimental data. These two comparisons are the best and the worst cases ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 1664 INPUT: initial temperature T m, and w START CALCULATE: the equilibrium K1 and K2 by using Eqs. (15), (14), and (13) T=Tnew Abs (T-Tnew) <0.1 K END CALCULATE: ni by using Eqs. (2), (3), (4), (11), and (12) CALCULATE: the temperature Tnew by using Eq. (20) Fig. 1. The calculation procedure. Table 3 The RMS error from comparison between predicted results and data from [13] Run no. RMS error 1 2 3 4 5 6 7 8 9 Avg RMS error 1.585 1.484 1.066 0.882 2.474 3.917 1.219 2.746 2.717 2.010 Table 4 The comparison of predicted results with the experimental data from [13] Gas composition % mol dry basis The present model Experimental data RMS error MC 16.0% MC 14.0% MC 16.0% MC 14.0% 16.0% 14.0% H2 CO CH4 CO2 N2 ma 18.04 17.86 0.11 11.84 52.15 0.4647 18.03 18.51 0.11 11.43 51.92 0.4591 17.00 18.40 1.30 10.60 52.70 0.3361 12.50 18.90 1.20 8.50 59.10 0.3927 a Tables 3 and 4 show that the predicted results generally agree with other experimental data, except for the case of CH4. The slight difference in the results may have came from the assumptions defined in simplifying the model, such as all gases are assumed to be ideal, no residue, absence of tar, etc. The interesting points in the comparisons are the amount of H2 and CH4. The model predicted higher amounts of H2, but the predicted amounts of CH4 are lower than all experimental data. It is important to note that equilibrium models from the literatures reviewed [3–6,8,14] predicted the H2 concentration higher and the CH4 concentration lower than the measured data from experiment. Bacon et al. [14] also reported a substantially higher CH4 in the product gas than what was estimated from his equilibrium model calculation. A possible explanation to this is that the state of equilibrium was not met during the experiment. Gumz [15] as cited by Bacon et al. [14] stated that a modified equilibrium constant can be defined as the true equilibrium constant multiplied by the degree of approach to equilibrium. In calibrating the model of Jayah et al. [13], the amount of methane predicted was adjusted in such a way that it was equal to the amount of methane measured in the product gas. 0.882 3.917 The amount of oxygen in Eq. (1). chosen from Table 3, correspond to the highest and the lowest error. The error in this comparison is estimated by the root-mean-square (RMS), defined as sffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi PN 2 i ðExpi Modi Þ , (22) RMS ¼ D where Exp is the value from the experimental results, Mod is the predicted value from the model, and D is the number of data. 3.2. The modified model Since downdraft gasifiers are different in designs, the producer gases generated by them are also different in composition. To increase the results’ accuracy, some models were developed and modified for specific gasifier. Jayah et al.’s model was calibrated by fixing the amount of methane in the model to a value derived from one of their experimental results [13]. Experimental data reported at Zainal et al. [8], Altafini et al. [5], and Jayah et al. [13] were used to modify the model. This combination gives a total of eleven cases to use as experimental data. A coefficient of 11.28, was used to multiply with K2 in the calculation procedure in order to improve the performance of the model. This coefficient came from the average value of the ratio of CH4 from the eleven experimental data and CH4 ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 calculated from the model. For CO concentration, the equilibrium model normally predicts a slightly lower value than that from the experiments. In some cases the equilibrium model also predicts the CO2 concentration barely higher than those from the experiments [3–6,8]. Therefore, a coefficient less than 1.0 was multiplied with K1 which was obtained the same way as finding the coefficient for K2 based on the amount of CO. A value 0.91 was defined to be the coefficient for modifying K1. The modified model was then used to simulate and compare with Jayah et al’s work. Furthermore, the modified model was also compared with SynGas model and the experimental data at 1073 K, 10% MC from Altafini et al. [5]. As presented in previous sections, the amount of oxygen used in the gasification process is the necessary input for the model simulation. Thus, the experimental result from Zainal et al.’s work was not used for the comparison because the amount of air used was not indicated. The results of the comparisons are shown in Tables 5–7, respectively. Table 5 shows that after modifying the model, the amount of H2 significantly reduced as compared to the predicted value from the unmodified model. The amount of CH4 dramatically increased and was found closer to the experimental values. For some cases, CO remained constant, while for other cases it predicted slight increase Table 5 The comparison of results from modified model with the data from [13] Gas composition % mol dry basis The present model Experimental data RMS error MC 16.0% MC 14.0% MC 16.0% MC 14.0% 16.0% 14.0% H2 CO CH4 CO2 N2 m 16.81 17.86 1.05 12.10 52.18 0.4472 16.8 18.52 1.06 11.68 51.94 0.4415 17.00 18.40 1.30 10.60 52.70 0.3361 12.50 18.90 1.20 8.50 59.10 0.3927 0.700 3.652 Table 6 The RMS error from comparison between modified model and data from [13] Run no. RMS 1 2 3 4 5 6 7 8 9 Avg RMS error 1.555 1.615 1.021 0.700 2.057 3.652 0.747 2.334 2.333 1.779 1665 Table 7 The comparison of results from modified model with the data from [5] Gas composition % mol dry basis Modified model H2 CO CH4 CO2 N2 m 18.24 23.34 1.66 9.82 46.93 0.3578 Altafini et al. RMS error SynGas model Experiment Modified model 20.06 19.70 0.00 10.15 50.10 0.329 14.00 20.14 2.31 12.06 50.79 0.307 2.845 SynGas model 2.780 in values from the unmodified model. One reason is that the coefficient used to modify K1 is 0.91, which is almost close to unity, thus, the value of CO in modified model should not dramatically change. Some of the values were the same as that of unmodified model because of the fact that equation forming K1 has a direct relationship with the amount of H2 produced, which is also depended on K2. When K2 was modified using the coefficient 11.28, the value of H2 reduced. However, since hydrogen has to be conserved, amount of H2O is increased. In addition, the amount of K1 has a specific value at a certain temperature (around 0.82 for 1100 K after modification). Thus, the amount of CO did not increase much and some values are the same as predicted by the unmodified model. This effect can be observed from the increasing values of CO2, though the increment was insignificant. Table 6 presents that the predicted results of the modified model were better compared to unmodified model. The results from the modified model are satisfactorily close to the experimental value as shown in Table 7. The predicted mole fractions of H2 and CO are higher but the predicted mole fraction of CO2 is lower than the experimental data. The RMS error between the modified model and SynGas model were also found comparable. Another important parameter of gasification process is HHV of producer gas. In the experiment of Altafini et al.’s study, the average HHV measured from the experiment was 5.276 MJ/N m3 while the HHV calculated from this model was 5.507 MJ/N m3. The data from Tables 6 and 7 confirm that the modified model developed in this study can predict agreeable results with experimental values. 4. The effect of moisture content The municipal solid waste from developing countries normally has high level of moisture when compared to those from developed countries [16]. As for the case of Thailand, the main composition of municipal solid waste is food [17], thus it mainly consists of moisture. Therefore, the effect of moisture content on the composition of producer gas from waste gasification is an interesting ARTICLE IN PRESS 1666 S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 aspect. Table 8 shows the average composition of MSW from eleven provinces in Thailand. In this study, all noncombustible and recyclable materials except paper were excluded. Paper was included because it can produce high levels of H2, CO, and CH4 [8]. Table 8 The average composition of MSW in eleven provinces in Thailand (2002) [17] Component (wt%) Food Plastic Paper Glass, stone and can Yard waste Metal Cloth Rubber/leather Other 54.17 12.24 9.80 7.95 3.98 3.15 2.61 2.47 4.13 Table 9 The chemical composition of solid waste on dry ash-free basis Element (wt%) C H O N S 51.034 6.776 39.178 2.642 0.370 In estimating the chemical compositions on dry ash-free basis, the information from Tchobanoglous et al. [18] were employed and the results are shown in Table 9. The chemical formula of this solid waste, based on a single atom of carbon, is defined as CH1.5932O0.5758N0.0444. Sulfur was neglected in this study. The enthalpy of formation for the waste calculated using Eq. (21) is 107306.269 kJ/kmol. The lower heating value of solid fuel in MJ/kg was derived using the higher heating value formula presented by Channiwala and Parikh [19], that is HHV ¼ 0:3491C þ 1:1783H þ 0:1005S 0:1034O 0:0151N 0:0211Ash; LHV ¼ HHV ¼ 9mH hfg , ð23Þ where C, H, O, N, S, and Ash are percentages of mass of carbon, hydrogen, oxygen, nitrogen, sulfur and ash in the dry solid fuel, mH is mass fraction of hydrogen in solid fuel, and hfg is enthalpy of vaporization of water. To study the effect of moisture content of the waste, the amount of air was fixed at 0.4 of the stoichiometic requirement (m ¼ 0.444). Fig. 2 shows the effect of moisture content on the composition of producer gas. It can be seen that the fraction of H2 gradually increases from 16.04% to 20.11% when MC increases from 0% to 40%. In the case of CO, it showed an inverse tendency. CO decreases from 25.01% to 12.01% with an increase in moisture content. The useful gas CH4, has a very low percentage in the producer gas, though it showed an increase from 0.134% to 1.86%. Fig. 2 also illustrates the fraction of N2 in the producer gas which was almost Fig. 2. The effect of moisture content on the composition of producer gas. ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 1667 Fig. 3. The effect of moisture content on the reaction temperature. Fig. 4. The effect of moisture content on the calorific value. constant with only a slight change from 52.80% to 50.25%. For CO2, it increases from 6.00% to 15.74%. Fig. 3 shows the variation of the reaction temperature. The temperature decreases from 1374.0 to 1064.3 K when the MC increases from 0% to 40%. Fig. 4 displays the effect of moisture content on the calorific value of producer gas. It can be observed that the calorific value decreases from 4.93 to 4.42 MJ/N m3 when varying MC from 0% to 40%. ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 1668 5. Second law efficiency Table 11 Second law efficiencies of waste gasification As mentioned before, developing countries like Thailand have a high level of moisture in their MSW. For Thailand, the moisture content of MSW in some provinces is around 20–22% and can be as high as 40% for some provinces popular to tourists [17]. In the previous section, we have seen that the moisture content negatively affects the calorific value of producer gas. For this part of the study, exergy analysis was used to evaluate the effect of moisture content on the performance of the gasification process. In real processes, exergy is not conserved because of irreversibilities. Exergy efficiency or second law efficiency is defined as Zex ¼ E prod , E feed þ E medium (24) where Eprod and Efeed are exergies of producer gas and feedstock, respectively. Emedium is the exergy of the gasifying medium, which in this study can be neglected because it is the air at atmospheric conditions [20]. In this case, kinetic exergy and potential exergy are also negligible, thus the exergy can be divided into two major components shown below E ¼ E ch þ E ph , (25) where Ech and Eph are chemical exergy and physical exergy, respectively. The dead state used in the following calculation is defined at Po ¼ 1 atm, To ¼ 298 K. Kotas [21] suggested that the specific chemical exergy of ideal mixture gas, in kJ/kmol, can be calculated by X X ¯ ch;M ¼ xi ¯ch;i þ R̄T o xi ln xi , (26) i i where xi is mole fraction of ith component and ech,i is standard chemical exergy of ith component, in kJ/kmol and they are presented in Table 10 [21]. The physical exergy of each gas species can be calculated by ¯ ph ¼ ðh̄ h̄o Þ T o ðs̄ s̄o Þ, (27) where h̄ and s̄ are enthalpy and entropy at any pressure (P), temperature (T), h̄o and s̄o are enthalpy and entropy at Po, To. Kotas [21] also presented the equation for estimating exergy of solid fuel with mass ratio 2:674O=C40:667, Table 10 Standard chemical exergy of some substances [21] Substance ch;i (kJ/kmol) H2 CO CO2 H2O (g) CH4 N2 238,490 275,430 20,140 11,710 836,510 720 Moisture content (%) Second law efficiencies (%) 20 25 30 81.54 80.28 78.62 expressed in kJ/kg, as shown solid ¼ jdry ½LHV þ mw hfg , (28a) where jdry ¼ 1:0438 þ 0:1882ðH=CÞ 0:2509ð1 þ 0:7256ðH=CÞÞ þ 0:0383ðN=CÞ 1 0:3035ðO=CÞ ð28bÞ and mw is mass fraction of moisture in the fuel, and hfg is enthalpy of vaporization, in kJ/kg. Table 11 presents the second law efficiencies of waste gasification at moisture contents 20%, 25% and 30%, respectively. The simulation was performed at temperature equal to 1073 K. From Table 11, it can be observed that second law efficiency slightly decreases from 81.54% to 78.62% when moisture content increases from 20% to 30%. The reason of decreasing second law efficiency can be attributed to the reduction of chemical exergy as the moisture content is increased. Table 10 shows that the standard chemical exergies of CH4, CO, and H2 are first, second, and third highest values among the gases. When MC is increased, more air is required to maintain the temperature at 1073 K. This results in a decrease in the mole fraction of useful gases such as CO, CH4, and H2 when simulations were performed. Consequently, the first term in the right-hand side of chemical exergy equation, Eq. (26) also decreased. The results of this study agree with Kaupp’s study [22] as he mentioned that in practice, in order to provide the necessary heat of reaction to reach gasification temperature, an increasing MC necessitates an increasing amount of air. The disadvantages of increasing the amount of air shown in this section cause reduction of useful gases, CH4, CO, and H2. This results in a significant reduction of the heating value of the producer gas. These all lead to a conclusion that MC is a very important factor. Therefore, waste should be suitably dried when it will be used for gasification purposes. Drying by exposing the waste to solar radiation is a simple way but it is suitable only under clear sky and could take about one or two days. Under this condition, hygienic problems and foul odor also come up and post major concerns. Therefore, solar drying of waste before gasification process should be accompanied with waste segregation and proper management. ARTICLE IN PRESS S. Jarungthammachote, A. Dutta / Energy 32 (2007) 1660–1669 6. Conclusion The thermodynamic equilibrium model was developed for downdraft gasifier in order to calculate the composition of producer gas. The coefficients for correcting the equilibrium constant of water–gas shift reaction and methane reaction were used to improve the model. Those coefficients were obtained from the comparison between the model and the results of the experiments of other researches. The predicted results from the modified model satisfactorily agree with experimental results reported by other researchers. The modified model was then employed to simulate the gasification of Thailand MSW. The results showed that the mole fraction of H2 gradually increases and CO decreases, when MC increases. CH4, which has a very low percentage in the producer gas increases, N2 slightly decreases and CO2 increases with increasing MC. The reaction temperature and the calorific value decrease when MC increases. Finally, at a constant temperature of gasification process for waste with MCs of 20%, 25%, and 30%, the second law efficiency decreases with the increase in MCs. This is because amount of required air increases when MC increases in order to maintain the required reaction temperature, which in this case is 1073 K. 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