Moisture sorption isotherms of chickpea seeds at several temperatures

Moisture sorption isotherms of chickpea seeds at several temperatures

Journal of Food Engineering 45 (2000) 189±194 www.elsevier.com/locate/jfoodeng Moisture sorption isotherms of chickpea seeds at several temperatures...

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Journal of Food Engineering 45 (2000) 189±194

www.elsevier.com/locate/jfoodeng

Moisture sorption isotherms of chickpea seeds at several temperatures Nikolay D. Menkov * Department of Process Engineering, Higher Institute of Food and Flavour Industries, 26 Maritza Blvd., 4000 Plovdiv, Bulgaria Received 15 October 1999; accepted 28 February 2000

Abstract The equilibrium moisture contents of chickpea seeds were determined using the gravimetric static method at 5°C, 20°C, 40°C and 60°C over a range of water activities from 0.110 to 0.877. The sorption capacity of seeds decreased with the increase in temperature at constant water activity. Six models, modi®ed Chung±Pfost, modi®ed Halsey, modi®ed Oswin, modi®ed Henderson, Guggenheim±Anderson±de Boer (GAB), and a new Fraction±linear (FL), were applied to analyze the experimental data. The FL model was found to be the most suitable for describing the sorption data. For practical considerations a single monolayer value (in water activity (aW ) range 0.16±0.18) can be assumed. Ó 2000 Elsevier Science Ltd. All rights reserved.

1. Introduction Chickpea (Cicer arietinum L.) is a valuable foodstu€ due to its high content of vegetable protein with essential amino acids (Chavan, Kadam & Salunke, 1986; Clemente, Sanchez-Vioque, Vioque, Bautista & Millan, 1998; Jood, Bichnoi & Sharma, 1998; Rincon, Martinez & Iba nez, 1998; Sanchez-Vioque, Clemente, Vioque, Bautista & Millan, 1999). The legume seeds meant for food or sowing are normally subjected to long-term storage. During that time, important physico-chemical and biological changes take place with a strong impact on the nutrient properties. To a large extent, these changes depend on the moisture content of the seeds (Burr, Kon & Morris, 1968; Garcia-Vela & Stanley, 1989; Hentges, Weaver & Nielsen, 1991). The storage conditions of the legume seeds have a substantial in¯uence on their germination and longevity (Roberts, 1972; Vertucci, Roos & Crane, 1994). A number of models have been suggested in the literature to describe the relationship between the equilibrium moisture content (EMC) and the water activity (aW ) of food (Van den Berg & Bruin, 1981). Some of them take into account the e€ect of temperature. The modi®ed Chung±Pfost (Chung & Pfost, 1967; Pfost, Mourer, Chung & Milliken, 1976), modi*

Tel.: +359-32-449-393; fax: +359-32-440-102. E-mail address: nimenkov@hi-plovdiv.acad.bg (N.D. Menkov).

®ed Henderson (Henderson, 1952; Thompson, Peart & Foster, 1968), modi®ed Halsey (Halsey, 1948; Iglesias & Chirife, 1976a), modi®ed Oswin (Oswin, 1946; Chen & Morey, 1989) and GAB (Van den Berg, 1984; Labuza, Kaanane & Chen, 1985) equations have been adopted by the American Society of Agricultural Engineers as standard equations for describing sorption isotherms (ASAE, 1995). Veltchev and Menkov (2000) applied successfully a new four-parameter, Fraction±linear (FL) model, for describing the S-shape desorption isotherms of apples. The monolayer moisture content (MMC) which is of signi®cant importance to the physical and chemical stability of dehydrated materials with regard to lipid oxidation, enzyme activity, non-enzymatic browning, ¯avour components preservation, and structural characteristics (Labuza, Tannenbaum & Karel, 1970; Karel & Yong, 1981), can be determined from the equilibrium sorption isotherms by means of the two-parameter BET (Brunauer±Emmett±Teller) equation (Brunauer, Emmett & Teller, 1938). The knowledge of the equilibrium moisture content of chickpea seeds at various temperatures would allow to specify the storage conditions for the seeds. The object of this work is to: (1) determine experimentally the equilibrium sorption isotherms of chickpea seeds at 5°C, 20°C, 40°C and 60°C; (2) select the most suitable model describing the isotherms; (3) calculate the monolayer moisture content as a function of temperature.

0260-8774/00/$ - see front matter Ó 2000 Elsevier Science Ltd. All rights reserved. PII: S 0 2 6 0 - 8 7 7 4 ( 0 0 ) 0 0 0 5 2 - 2

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N.D. Menkov / Journal of Food Engineering 45 (2000) 189±194

Modi®ed Halsey   ÿ exp …A ‡ Bt† aW ˆ exp : MC

2. Material and methods 2.1. Material Chickpea seeds of the Resurs 1 variety (provided by the Agricultural University, Plovdiv, Bulgaria, 1998) were tested. The seeds had been gathered 6 months in advance. After harvest they were sun-dried to approximately 12% dry basis (d.b.) and kept in a dry place (aW < 0.55) at room temperature. The mass of 1000 seeds was about 270 g. The seeds contained 58.4% d.b. carbohydrate, 23.1% d.b. protein, 4.0% d.b. fat and 2.8% d.b. ash.

Modi®ed Henderson   1 ÿ aW ˆ exp ÿ A…t ‡ B†M C :

…1 ÿ

B0 a 

The water vapor sorption equilibrium of the chickpea seeds was determined at 5°C, 20°C, 40°C and 60°C, using the static gravimetric method (Wolf, Spiess & Jung, 1985). For the adsorption process, seeds were ®rst dehydrated in a desiccator over P2 O5 at room temperature for 20 days to an initial moisture content below 1% d.b. Samples for desorption measurements were ®rst hydrated in a glass jar over distilled water at 4°C for 20 days to approximately 32% d.b. For sorption measurements samples of 4  0:2 g were weighed in weighing bottles. The weighing bottles were then put in 10 hygrostats with di€erent saturated salt solutions (LiCl, CH3 COOK, MgCl2 , K2 CO3 , NaBr, Mg(NO3 )2 , SrCl2 , NaCl, KBr, KCl), to obtain constant water activities (Greenspan, 1977; Weisser, 1986; Maroulis, Tsami, Marinos-Kouris & Saravacos, 1988). All used salts were of reagent grade. At high water activities …aW > 0:70† crystalline thymol was placed in the hygrostats to prevent microbial spoilage of the seeds (Wolf et al., 1985). The hygrostats were kept in thermostats at 5°C, 20°C, 40°C and 60 ‹ 0.2°C. Samples were weighed (balance, sensitivity ‹ 0.0001 g) every 3 days. Equilibrium was acknowledged when three consecutive weight measurements showed a di€erence less than 0.001 g. The moisture content of each sample was determined by the vacuum oven method (AOAC, 1990). The time for the samples to reach equilibrium varied from 5 to 40 days, depending on the temperature and water activity. The equilibrium moisture contents were determined by means of triplicate measurements. 2.3. Analysis of data The description of the relationship between EMC, aW and temperature was veri®ed according to the following six models:

…1†

…3†

…4†

GAB Mˆ

2.2. Sorption isotherms

Modi®ed Chung±Pfost   ÿA exp … ÿ CM † : aW ˆ exp t‡B

Modi®ed Oswin  C aW : M ˆ … A ‡ Bt† 1 ÿ aW

…2†

B0 ˆ B exp

h1 RT

 C 0 ˆ C exp

AB0 C 0 aW ; 0 0 0 W † … 1 ÿ B aW ‡ B C aW †

h2 RT

…5†

 ;

…6†

 :

…7†

FL Mˆ

A ‡ BT ‡ DaW ; 1 ÿ CaW

…8†

where M is the moisture content (% d.b.); aW the water activity; A, B, C, D, h1 , h2 the model coecients; t the temperature (°C); T the absolute temperature (K) and R ˆ 8:314 is the universal gas constant (J molÿ1 Kÿ1 ). A nonlinear, least-squares regression program was used to ®t the six models to the experimental data (all replications). The suitability of the equations was evaluated using the mean relative error (MRE, %), standard error of moisture (SEM) and randomness of residual (Chen & Morey, 1989): ^ i 100 X Mi ÿ M …9† MRE ˆ ; Mi N s P ^ i †2 …Mi ÿ M SEM ˆ : df

…10†

Residual ^i; ei ˆ Mi ÿ M

…11†

^ i are experimental and predicted values, where Mi and M N is the number of data points and df is the degree of freedom (number of data points minus number of coecients in the model). The residuals obtained for each model with its respective coecients were plotted against measured EMC and assessed visually as random or patterned. In order to determine the monolayer moisture content, the two-parameter BET equation which is valid for aW < 0:45 (Labuza et al., 1985) was applied:

N.D. Menkov / Journal of Food Engineering 45 (2000) 189±194

191

rithm described in the literature (Iglesias & Chirife, 1976b; Menkov, Paskalev, Galyazkov & KerezievaRakova, 1999).

BET

Mm CaW ; …12† Mˆ …1 ÿ aW †…1 ÿ aW ‡ CaW † where Mm is the MMC (% d.b.). The MMC values for each temperature were calculated following an algo-

3. Results and discussion In Fig. 1, the adsorption and desorption isotherms of chickpea seeds at 5°C and 60°C are presented. The sorption isotherms have an S-shape pro®le typical for legume seeds (Vertucci & Leopold, 1987; Pappas & Rao, 1987; Mazza & Jayas, 1991). The hysteresis e€ect was distinctly expressed at 5°C. At 60°C the di€erences between the experimental data obtained after adsorption and desorption are not statistically signi®cant (level of signi®cance 0.05) for the most experimental points. The experimental data of all measurements are given in Table 1. The EMC values decreased with an increase in the temperature at constant aW . Similar trends for many seeds and food materials have been reported in the literature (Labuza, 1968; Menkov, 1997; Walters & Hill, 1998). The comparison between the results obtained and the data provided by Sethi, Soni and Chopra (1977) for chickpea ¯our shows that the seeds had a lower water sorption capacity. Similar observations were reported by

Fig. 1. Desorption and adsorption isotherms of chickpea seeds at 5°C and 60°C showing the hysteresis e€ect.

Table 1 Adsorption (ads) and desorption (des) data (M, % d.b.) of chickpea seeds at di€erent temperatures 5°C aW

a b

20°C Ma

SDb

aW

40°C M

SD

aW

60°C M

SD

aW

M

SD

ads des

0.113 0.113

4.94 6.58

0.12 0.11

0.113 0.113

4.58 4.40

0.07 0.06

0.112 0.112

3.27 3.71

0.11 0.08

0.110 0.110

3.08 3.25

0.10 0.17

ads des

0.245 0.245

7.20 8.73

0.14 0.14

0.231 0.231

6.67 7.26

0.05 0.09

0.201 0.201

4.99 5.72

0.08 0.19

0.160 0.160

4.13 4.18

0.03 0.06

ads des

0.336 0.336

8.16 9.63

0.18 0.11

0.331 0.331

7.62 9.05

0.06 0.21

0.316 0.316

5.57 6.74

0.05 0.14

0.293 0.293

5.37 5.19

0.10 0.17

ads des

0.431 0.431

9.22 10.66

0.08 0.12

0.432 0.432

8.88 10.12

0.14 0.12

0.432 0.432

7.48 8.53

0.19 0.10

0.432 0.432

6.84 6.64

0.06 0.18

ads des

0.589 0.589

10.89 12.63

0.16 0.08

0.544 0.544

10.15 11.28

0.21 0.12

0.484 0.484

7.90 8.75

0.14 0.24

0.440 0.440

7.03 6.95

0.12 0.06

ads des

0.635 0.635

12.74 15.19

0.20 0.15

0.591 0.591

10.87 12.51

0.12 0.19

0.532 0.532

9.02 9.65

0.07 0.13

0.497 0.497

7.78 8.11

0.18 0.17

ads des

0.757 0.757

17.80 20.53

0.14 0.10

0.725 0.725

14.55 17.24

0.11 0.08

0.658 0.658

12.20 12.57

0.14 0.17

0.580 0.580

8.85 9.22

0.11 0.12

ads des

0.771 0.771

18.38 21.44

0.09 0.20

0.755 0.755

17.39 18.16

0.16 0.22

0.747 0.747

15.33 16.09

0.23 0.07

0.745 0.745

13.50 12.44

0.08 0.20

ads des

0.851 0.851

24.72 25.44

0.20 0.07

0.817 0.817

21.83 23.52

0.15 0.14

0.794 0.794

17.11 16.60

0.23 0.22

0.789 0.789

14.34 14.09

0.22 0.17

ads des

0.877 0.877

28.70 29.15

0.22 0.25

0.851 0.851

24.65 24.51

0.21 0.21

0.823 0.823

19.34 19.12

0.06 0.17

0.803 0.803

14.95 16.29

0.28 0.09

Mean of n ˆ 3 replications. Standard deviations.

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N.D. Menkov / Journal of Food Engineering 45 (2000) 189±194

Chhinnan and Beuchat (1985) with whole cowpeas and cowpea ¯ours. The coecients for the three- and four-parameter models together with the corresponding MRE and SEM values are presented in Table 2. The parameters of the GAB models are presented in Table 3. Example of

the analysis of the residuals are presented in Fig. 2. For the modi®ed Chung±Pfost (for adsorption and desorption as well) and modi®ed Henderson equations (for adsorption), the residual plots were patterned, which makes them unsuitable. The residuals obtained by all the other models were randomly distributed. For these

Table 2 Estimated values of model coecients (A, B, C, D); mean relative error (MRE, %) and standard error of moisture (SEM) of three- and fourparameter models for adsorption (ads) and desorption (des) Parameter

Model Modi®ed Chung±Pfost

Modi®ed Halsey

Modi®ed Oswin

Modi®ed Henderson

FL

A

ads des

455.2110 308.1214

3.337690 4.098313

10.79086 12.71118

0.000138 0.000328

10.35033 15.70636

B

ads des

101.6365 52.78201

)0.007900 )0.012647

)0.05010 )0.07701

12.82720 48.96227

)0.022551 )0.038772

C

ads des

0.166102 0.159547

1.582279 1.777402

0.49602 0.43913

2.138215 1.415975

0.954224 0.910345

D

ads des

± ±

± ±

± ±

± ±

4.469358 5.778511

MRE

ads des

12.13 10.76

4.63 6.20

6.71 5.01

15.31 10.40

4.88 5.24

SEM

ads des

2.16 1.81

0.59 0.78

0.77 0.75

3.01 1.30

0.58 0.70

Residual

ads des

Patterned Patterned

Random Random

Random Random

Patterned Random

Random Random

Table 3 Estimated values of model coecients (A, B, C, h1 , h2 ); mean relative error (MRE, %) and standard error of moisture (SEM) of the GAB model

Adsorption Desorption

A

B

C

h1

h2

MRE

SEM

Residual

5.372119 6.976963

0.547510 0.356268

0.000561 0.000490

1225.049 2071.703

26279.24 25363.67

5.06 6.19

0.65 0.80

Random Random

Fig. 2. Plot of residuals ®t of Chung±Pfost and FL models to adsorption data of chickpea seeds.

N.D. Menkov / Journal of Food Engineering 45 (2000) 189±194

models the respective MRE and SEM values were similar. For the desorption data at 60°C the MRE values obtained by the modi®ed Halsey and the GAB models were high: 8.3% and 9.8%, respectively. For adsorption data at 20°C the MRE value obtained by the modi®ed Oswin model was 9.1%. The MRE values obtained by the FL model at the studied temperatures varied small: from 4.2% to 5.3% for adsorption and from 4.8 to 6.3 for desorption. This gives us grounds to recommend the FL model for description of the equilibrium isotherms of chickpea seeds. The temperature in¯uence on the monolayer moisture content values is shown in Fig. 3. There is also a hysteresis e€ect with respect to the monolayer moisture content. The values diminish with the increase in temperature. Menkov et al. (1999) have shown for a large number of biological products that the dependence between MMC and temperature can be described by a linear equation. A modi®cation of the BET model yields: Modi®ed BET … A ‡ Bt†CaW ; Mˆ …1 ÿ aW †…1 ÿ aW ‡ CaW †

…13†

Mm ˆ A ‡ Bt;

…14†

where A, B and C are coecients independent of temperature. Applying the chickpea data the coecients of Eq. (13) were determined direct, using a nonlinear, leastsquares regression program on the basis of experimental data at aW < 0:45 (all replications): for adsorption A ˆ 5:9589; B ˆ ÿ0:0322; C ˆ 23:13263; for desorption A ˆ 7:10650; B ˆ ÿ0:0514; C ˆ 25:66617. Fig. 3 shows a comparison of the MMC values obtained by the stan-

193

dard procedure with Eq. (12) and Eqs. (13) and (14). It can be seen from the ®gures that in this case the linear equation provides a very good description of the data obtained. The corresponding water activity was determined by Eq. (13) after putting M ˆ Mm ˆ A ‡ Bt p Cÿ1 : …15† …aW † m ˆ Cÿ1 Despite the hysteresis e€ect, the (aW )m values obtained are close: for adsorption …aW †m ˆ 0:165; for desorption …aW †m ˆ 0:172. The (aW )m value is independent of temperature (the coecient C in Eq. (13) is independent of temperature). For practical considerations a single monolayer value (in the aW range 0.16±0.18) can be assumed, with respective EMC values from 4.1% to 5.7% for adsorption and from 4.2% to 6.7% for desorption.

4. Conclusions The sorption capacity of chickpea seeds decreased with an increase in temperature at constant water activity. The FL model is the most suitable for describing the relationship between the equilibrium moisture content and the water activity for the seeds under study. For practical considerations a single monolayer value (in the aW range 0.16±0.18) can be assumed.

Acknowledgements This study was conducted with the kind support of the National Research Fund, Bulgaria. References

Fig. 3. E€ect of temperature on the monolayer moisture content.

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