Shujun Wang1, Caili Li1, Xiu Zhang1, Les Copeland2, Shuo Wang1. 1. Key Laboratory of Food Nutrition and Safety, Ministry of Education, College of Food Engineering and Biotechnology, Tianjin University of Science &Technology, Tianjin 300457, China. 2. Faculty of Agriculture and Environment, The University of Sydney, NSW 2006, Australia.
Abstract
Starch retrogradation is a term used to define the process in which gelatinized starch undergoes a disorder-to-order transition. A thorough understanding of starch retrogradation behavior plays an important role in maintaining the quality of starchy foods during storage. By means of DSC, we have demonstrated for the first time that at low water contents, the enthalpy change of retrograded starch is higher than that of native starch. In terms of FTIR and Raman spectroscopic results, we showed that the molecular order of reheated retrograded starch samples is lower than that of DSC gelatinized starch. These findings have led us to conclude that enthalpy change of retrograded starch at low water contents involves the melting of recrystallized starch during storage and residual starch crystallites after DSC gelatinization, and that the endothermic transition of retrograded starch gels at low water contents does not fully represent the retrogradation behavior of starch. Very low or high water contents do not favor the occurrence of starch retrogradation.
Starch retrogradation is a term used to define the process in which gelatinized starch undergoes a disorder-to-order transition. A thorough understanding of starch retrogradation behavior plays an important role in maintaining the quality of starchy foods during storage. By means of DSC, we have demonstrated for the first time that at low water contents, the enthalpy change of retrograded starch is higher than that of native starch. In terms of FTIR and Raman spectroscopic results, we showed that the molecular order of reheated retrograded starch samples is lower than that of DSC gelatinized starch. These findings have led us to conclude that enthalpy change of retrograded starch at low water contents involves the melting of recrystallized starch during storage and residual starch crystallites after DSC gelatinization, and that the endothermic transition of retrograded starch gels at low water contents does not fully represent the retrogradation behavior of starch. Very low or high water contents do not favor the occurrence of starch retrogradation.
Rice and wheat are two of the most economically important crops, contributing food for more than 90% of the world’s population1. The quality of food products made from these staple grains is largely dependent on the properties of their major component starch, which is the most abundant storage carbohydrate in plants. Starch is used widely in food and non-food industries and, due to its low cost and renewability, it is also used to fabricate biodegradable materials. Before consumption by humans or for its application in materials, starch is usually gelatinized, by undergoing an order-to-disorder transition brought about by heating in the presence of water. On storage after gelatinization, the disordered starch chains gradually reassociate into a different ordered structure in a process termed retrogradation. Starch retrogradation is accompanied by a series of physical changes such as increased viscosity and turbidity of pastes, gel formation, exudation of water and increased degree of crystallinity with the appearance of B-type crystalline polymorphs2. The changes that starch undergoes during gelatinization and retrogradation are irreversible and are major determinants of its functional properties for food processing, during digestion, and in industrial applications. These properties determine the quality, acceptability, nutritional value, and shelf-life of finished, starch-rich foods3.Gelatinization of starch causes loss of molecular order in both the amylose and amylopectin components. Subsequent retrogradation is the process in which the disaggregated starch chains reassociate into an ordered structure, which is different from the initial state4. Some of the partial crystallinity of amylopectin in native starch is restored during retrogradation5. Starch gelatinization and retrogradation are often characterized by differential scanning calorimentry (DSC), in combination with other structural or functional techniques36. The amount of water in the DSC pans plays an important role in the extent of starch gelatinization, which leads to the differential effects on subsequent retrogradation behavior. The effects of water availability on starch gelatinization have been investigated extensively, as reviewed recently by Wang and Copeland3. At low water content, the DSC endothermic transition only represents the limited swelling or incomplete gelatinization of starch granules78. Even at high water content (water:starch = 1.5:1 or higher), the DSC endotherm does not always represent the complete gelatinization of granules, as shown in studies with cereal and legume starches78910. In comparison to gelatinization, the effect of water content on starch retrogradation has attracted much less attention6. A comprehensive study on starch retrogradation over a wide range of water content is lacking despite its major significance for the quality of foods during storage6. As most food systems are processed under limited water conditions5 and then stored at 4 °C, an understanding of the changes that starch undergoes during gelatinization and retrogradation in such conditions is important to manipulate the textural and nutritional qualities of starchy foods. Under water-limited conditions, starch undergoes only partial gelatinization on DSC heating and will retrograde in a different way during subsequent storage compared with fully gelatinized starch8.Starch retrogradation may be characterized by determining the enthalpy change of retrograded starch gels after storage at 4 °C. The degree of retrogradation (DR) is often described by a parameter obtained by dividing the gelatinization enthalpy change of starch granules by the enthalpy change of reheated retrograded starch gels1112. In the present study, the retrogradation behavior of wheat and ricestarches over a wide range of water content was examined. To the best of our knowledge, this is the first study to investigate starch retrogradation over a wide range of water content by DSC in combination with ATR-FTIR and Raman spectroscopy. This study is aimed at gaining a better understanding of the effect of water content on starch retrogradation behavior in food and non-food applications.
Experimental Section
Materials
The wheat (Zhoumai 18) flour was kindly provided by the Institute of Crop Science, Chinese Academy of Agricultural Science. The rice (Oryza sativa) sample was purchased from a supermarket in Tianjin, China. Amylose (A0512) and amylopectin (A8515) from potatostarch were purchased from Sigma Chemical Co. (St. Louis, MO, USA). Other chemical reagents were of all analytical grade.
Isolation of Starch
Ricestarch (RS) was isolated according to the method of Spigno and De Faveri13, and wheatstarch (WS) according to a dough ball method814.
Chemical Analysis of Starch
The amount of damaged starch in the isolated starches was determined using the Megazyme Starch Damage Kit (Megazyme International Ireland Ltd. (Bray Co., Wicklow, Ireland). Amylose content was determined by iodine binding according to Chrastil15 using a standard curve of 10%, 20%, 25%, 30%, and 35% potatoamylose mixed with potato amylopectin. The crude lipid content of starch granules was determined gravimetrically by Soxhlet extraction using petroleum ether. The nitrogen content of wheat grains and starch granules were determined by standard Kjeldahl methodology. Crude protein content was estimated by multiplying the nitrogen content by a conversion factor of 6.25. Moisture content was determined by drying to constant weight at 105 °C and ash content was determined using a muffle furnace at 550 °C.
Differential Scanning Calorimetry
Differential scanning calorimetry (DSC) measurements were performed using a Differential Scanning Calorimeter (200 F3, Netzsch, Germany) equipped with a thermal analysis data station. Starch (approximately 3 mg wet weight) was weighed accurately into an aluminum sample pan. Distilled water was added with a pipette to obtain starch:water ratios of 1:0.5, 1:0.75, 1:1, 1:1.5, 1:2.5 and 1:4 (w/v) in the DSC pans, corresponding to the water content of 33, 43, 50, 60, 71 and 80%, respectively. The pans were sealed and allowed to stand overnight at room temperature before analysis. The pans were heated from 20 to 100 °C at a rate of 10 °C/min. An empty aluminum pan was used as the reference. Starch retrogradation was determined on the same gelatinized samples after storage at 4 °C for 7 days. The retrograded starch samples were re-scanned using the heating profiles described for starch gelatinization. Gelatinization enthalpy change of native starch (ΔHG) and enthalpy change on reheating of retrograded starch gels (ΔHR) were obtained using data recording software. All measurements were performed in triplicate. Degree of retrogradation (%DR) was calculated according to the formula:After DSC measurements, the sample pans were cooled to room temperature and reweighed. Those pans without any weight loss were collected and starch samples were freeze-dried and used for Fourier-transform infra-red (FTIR) and Raman spectroscopic analysis.To obtain sufficient material to gain a better understanding of starch retrogradation behavior, retrograded starches were also prepared by simulating the DSC heating conditions without stirring using the RVA to prepare starch gels followed by storage at 4 °C for 7 days. The retrograded starch samples prepared in this way were freeze-dried, ground using a mortar and pestle, and passed through a 100 μm sieve. The resulting retrograded starch powders were mixed with water in ratios of 1:0.5, 1:0.75, 1:1, and 1:1.5 (w/v) in the DSC pans and analyzed using the same procedures for DSC measurements as described above.
Attenuated Total Reflectance (ATR)-FTIR Spectroscopy
The residual molecular order of native starch after DSC heating and of retrograded starch gels after DSC reheating was determined directly using a Thermo Scientific Nicolet IS50 spectrometer (Thermo Fisher Scientific, USA). The ratio of absorbance at 1047/1022 cm−1 was used to estimate the short-range molecular order of starch.
The molecular order of native starch after DSC heating and of retrograded starch gels after DSC reheating was also determined by using a Renishaw Invia Raman microscope system (Renishaw, Gloucestershire, United Kingdom), which was equipped with a Leica microscope (Leica Biosystems, Wetzlar, Germany) and a 785 nm green diode laser source. Spectra were collected on at least five different spots of gelatinized and retrograded starch samples in the range of 3200–100 cm−1, with a resolution of approximately 7 cm−1. The full width at half height (FWHH) of the band at 480 cm−1, which can be used to characterize the molecular order of starch6, was calculated using the WiRE 2.0 software.
Statistical Analysis
Results are reported as the mean values and standard deviations of at least duplicate measurements. Analyses of variance (ANOVA) by Duncan’s test (p < 0.05) were conducted using the SPSS 17.0 Statistical Software Program (SPSS Inc. Chicago, IL, USA).
Results and Discussion
Basic Composition of Rice and Wheat starches
Amylose contents of the rice and wheatstarches were 11.5% and 25.0%, respectively (Table 1). The amylose content of starch from non-waxy rice varieties varies between 7% and 33%161718, whereas non-waxy wheatstarch usually contains 20–30% amylose19. Damaged starch contents of the rice and wheatstarches were 0.89% and 1.30%, respectively, whereas ash, protein, lipid and water contents of the two starches were all within the range of values reported in the literature20.
Table 1
Basic composition of wheat and rice starches.
Starch
Amylose (%)
DS (%)
Water (%)
Protein (%)
Lipid (%)
Ash (%)
Rice
11.5 ± 0.3
0.89 ± 0.07
11.72 ± 0.07
0.29 ± 0.04
0.07 ± 0.01
0.24 ± 0.09
Wheat
25.0 ± 0.6
1.30 ± 0.02
10.62 ± 0.21
0.36 ± 0.02
0.11 ± 0.01
0.15 ± 0.04
Values are means ± SD. DS: damaged starch.
Thermal Properties of Native and Retrograded Starches
The DSC curves of starch gelatinization and from reheated retrograded starch gels are presented in Fig. 1. Rice and wheatstarches displayed a typical gelatinization endothermic transition in the temperature ranges of 61.2–73.9 °C and 55.1–67.4 °C, respectively. With increasing water content, the gelatinization endothermic transition became progressively more pronounced and symmetrical (Fig. 1a,c). The area of this gelatinization endotherm increased with increasing water content. On reheating the retrograded starch, much broader but shallower endothermic transitions ranging from 42.9–68.9 °C and from 41.9–65.3 °C were noted for rice and wheatstarch, respectively (Fig. 1b,d). The area of this retrogradation endotherm increased initially and then decreased with increasing water content.
Thermal transition temperatures of native starch and retrograded starch gels at different water contents are listed in Table 2. There were small differences in the gelatinization transition temperatures of ricestarch as water content increased from 31% to 80%. The To, Tp and Tc of ricestarch were in the range of 61.2–62.1 °C, 66.9–68.3 °C and 71.0–73.9°, respectively. The transition temperature range (Tc–To) was from 9.8 to 11.7 °C. The To, Tp and Tc of wheatstarch ranged from 55.1, 60.8 and 64.6 °C to 56.8, 62.1 and 67.4 °C, respectively. The thermal transition broadened with Tc–To ranging from 9.5 to 11.3 °C. These observations are consistent with previous results, which showed that the conclusion temperature of pea and wheatstarches increased gradually with increasing water content78.
Table 2
Thermal transition temperatures of rice and wheat starch samples.
Temperatures
Water content/%
Rice starch
Wheat starch
G/oC
R/ oC
G/ oC
R/ oC
To
33
61.4 ± 0.6ab
44.1 ± 0.8a
55.1 ± 0.3a
42.8 ± 1.3ab
43
61.2 ± 0.3a
43.5 ± 1.1a
55.2 ± 0.5a
41.9 ± 0.4a
50
61.2 ± 0.2a
42.9 ± 0.6a
55.3 ± 1.3a
43.1 ± 0.7ab
60
61.8 ± 0.1abc
44.2 ± 0.2a
55.5 ± 0.1a
43.8 ± 1.9ab
71
62.1 ± 0.5c
44.2 ± 1.1a
56.0 ± 0.2a
43.1 ± 2.1ab
80
62.0 ± 0.3bc
nd
56.1 ± 0.4a
45.4 ± 0.9b
Tp
33
67.1 ± 0.7a
56.8 ± 0.5ab
61.0 ± 0.4a
58.3 ± 1.9c
43
67.3 ± 0.4a
58.2 ± 0.6b
60.8 ± 0.3a
57.6 ± 1.6bc
50
67.2 ± 0.3a
55.2 ± 0.9a
61.0 ± 0.2a
54.7 ± 1.5ab
60
66.9 ± 0.2a
53.9 ± 0.3a
61.1 ± 0.16a
55.6 ± 1.8abc
71
67.6 ± 0.4ab
54.7 ± 2.8a
61.8 ± 0.3b
53.6 ± 0.8a
80
68.3 ± 0.1b
nd
62.1 ± 0.0b
54.3 ± 0.1a
Tc
33
71.3 ± 0.7a
67.8 ± 1.8bc
64.6 ± 0.3b
65.3 ± 0.2d
43
71.0 ± 0.4a
68.9 ± 2.0c
64.8 ± 0.2ab
64.8 ± 0.2cd
50
71.3 ± 0.3a
65.9 ± 0.8b
65.6 ± 0.4b
64.5 ± 0.2cd
60
71.8 ± 0.6a
63.2 ± 0.4a
66.2 ± 0.2b
64.1 ± 0.9bc
71
73.9 ± 0.1b
62.5 ± 0.2a
67.0 ± 0.2c
63.4 ± 0.8ab
80
73.3 ± 0.3b
nd
67.4 ± 0.4c
62.7 ± 0.1a
Tc–To
33
9.9 ± 0.1a
23.2 ± 1.4b
9.5 ± 0.5a
22.5 ± 1.1b
43
9.8 ± 0.1a
25.4 ± 2.2b
9.6 ± 0.6a
22.9 ± 0.2b
50
10.1 ± 0.4a
23.0 ± 1.0b
10.3 ± 1.2a
21.4 ± 0.6b
60
10.0 ± 0.5a
19.0 ± 0.5a
10.7 ± 0.3ab
20.3 ± 2.2b
71
11.7 ± 0.6b
18.3 ± 0.9a
11.0 ± 0.2ab
20.3 ± 1.3b
80
11.3 ± 0.6b
nd
11.3 ± 0.3b
17.3 ± 0.9a
Values are means ± SD.Values with the same letters in the same column for each starch are not significantly different (p < 0.05).
G: gelatinization; R: retrogradation
nd: not determined.
After storage for 7 days, the transition temperatures of reheated retrograded starch gels, especially To and Tp, were much lower than those of native starch granules (Table 2), indicating that the melting of crystallites in retrograded starch gels occurred more readily than for native starch crystallites. The To of retrograded starch gels did not vary greatly with different water content, suggesting similarities in the onset of melting behavior of crystallites in retrograded starch gels. However, the Tp and Tc of retrograded ricestarch gels decreased from 56.8 to 53.9 °C and from 67.8 to 62.5 °C, respectively, as the water content increased from 33 to 71%. Similarly, the Tp and Tc of retrograded wheatstarch gels decreased from 58.3 to 53.6 °C and from 65.3 to 62.7 °C, respectively. With increasing water content, Tc–To decreased from 25.4 and 22.9 °C to 18.3 and 17.3 °C for rice and wheatstarch, respectively.Gelatinization enthalpy change increased from 2.6 to 14.4 J/g and from 2.9 to 10.7 J/g for rice and wheatstarch, respectively, as the water content increased from 33 to 71%, above which the enthalpy change remained essentially the same (Table 3). This observation was consistent with previous results8. Ricestarch presented a higher maximum enthalpy change of 14.4 J/g than did wheatstarch (10.7 J/g). The maximum enthalpy change of native starch granules has been shown to be variety dependent8.
Table 3
Enthalpy change of native and retrograded starches.
Starch
Water content/%
ΔHGJ/g
aΔHR J/g
bΔHR J/g
DR%
Rice starch
33
2.6 ± 0.1a
3.9 ± 0.0c
4.2 ± 0.2a
153.1 ± 5.7f
43
4.6 ± 0.1b
5.6 ± 0.2e
5.2 ± 0.4b
121.9 ± 3.4e
50
5.5 ± 0.1c
7.0 ± 0.4f
6.6 ± 0.0b
82.8 ± 5.0d
60
14.0 ± 0.2d
4.7 ± 0.4d
4.6 ± 0.1a
33.3 ± 2.7c
71
14.4 ± 0.7d
1.4 ± 0.2b
nm
9.9 ± 0.6b
80
14.3 ± 0.2d
0a
nm
0a
Wheat starch
33
2.9 ± 0.0a
6.2 ± 0.2e
4.4 ± 0.5b
214.8 ± 5.0e
43
4.1 ± 0.1b
6.0 ± 0.0e
4.6 ± 0.7b
146.1 ± 2.5d
50
5.5 ± 0.0c
5.5 ± 0.1d
4.1 ± 0.3b
100.1 ± 2.3c
60
8.5 ± 0.1d
2.6 ± 0.4c
3.3 ± 0.1a
30.5 ± 4.4b
71
10.7 ± 0.4e
1.8 ± 0.1b
nm
16.4 ± 0.3a
80
10.7 ± 1.1e
0.5 ± 0.0a
nm
4.7 ± 0.3a
Values are means ± SD. Values with the same letters in the same column for each starch are not significantly different (p < 0.05).
a: reheating retrograded starch gels; b: reheating retrograded starch powders/water mixtures; DR% was calculated based on the enthalpy change of regrograded starch gels.
nm: not measured.
After retrogradation, the enthalpy change of rice and wheatstarch gels varied according to water content (Table 3). Enthalpy change of ricestarch gels increased from 3.9 J/g at a water content of 33% to a maximum value of 7.0 J/g at a water content of 50%, and then decreased to zero at a water content of 80%. In comparison, the retrogradation enthalpy change of wheatstarch gels reached a maximum value of 6.2 J/g at a water content of 33%, and then decreased progressively to 0.5 J/g at a water content of 80%. When the water content was above 80%, no retrogradation of wheatstarch gel was observed by DSC (data not shown), consistent with previous reports212223.Interestingly, the enthalpy change of retrograded starch gels was greater than that of native starch granules when the water content was between 33 and 50% (Table 3), resulting in a calculated value for the degree of retrogradation of the starch gels greater than 100% (Table 3, Fig. 2). This suggests that the broad endothermic transition of retrograded starch gels involves not only the melting of recrystallized starch formed during retrogradation, but the further melting of residual crystallites that remained in the retrograded starch gels. As proposed8, the DSC endothermic transition does not represent the full gelatinization of starch granules at DSC water-limited conditions.
Figure 2
Gelatinization enthalpy change of RS (A), retrogradation enthalpy change of RS (B), DR of RS (C), Gelatinization enthalpy change of WS (D), retrogradation enthalpy change of WS (E), DR of WS (F).
To further substantiate the above hypothesis, the thermal transition of freeze-dried retrograded starch powders was determined (Fig. 3). Two separated endothermic transitions were noted in the range of 40~65 °C and 70~100 °C. The lower temperature endotherms are proposed to be the melting of retrograded starch crystallites, whereas the ones at higher temperature are proposed to be due to the melting of residual crystallites remaining after DSC gelatinization. The observation of two separated endotherms indicated that melting of recrystallized starch formed during retrogradation and residual crystallites after DSC gelatinization occurred separately rather than simultaneously. The second endothermic transition is unlikely to be due to the melting of amylose-lipid complexes, which occurs at higher temperatures. Moreover, the lipid content of the starches was very low. The broad endothermic transitions noted for retrograded starch gels are consistent with the consecutive melting of recrystallized starch and residual starch crystallites. However, unlike the freeze-dried material, the endotherms of the reheated starch gels in the DSC pans may overlap because water is likely to migrate more readily from recrystallized starch to residual starch crystallites in gels than in rehydrated powders. Interestingly, the enthalpy change of freeze-dried retrograded starch powers was lower than that of retrograded starch gels (Table 3), consistent with the findings that freeze drying can disrupt the crystalline and molecular order of starch24. At higher water content of 60–80%, the degree of retrogradation was between 0–32.3% and between 4.7–34.1% for rice and wheatstarch, respectively.
Figure 3
DSC curves of retrograded rice starch powders (a), retrograded wheat starch powders (b). p1: represents the melting of recrystallized starch during retrogradation; p2: represents the melting of residual starch crystallites after DSC gelatinization.
Short-range Molecular Order of Starch by ATR-FTIR and Raman Spectroscopy
The short-range molecular order of double helices in starch can be characterized by the ratio of absorbances at 1047/1022 cm−1 obtained from FTIR spectroscopy of starch25262728. To verify the further melting of starch granule crystallites remaining in retrograded starch on DSC reheating, the molecular order of native starch after DSC heating and retrograded starch gels after DSC reheating was determined by ATR-FTIR and Raman spectroscopy. To identify the differences in the molecular order of these starch samples, the deconvoluted FTIR spectra of wheatstarch in the range of 1200–800 cm−1 were obtained (Fig. 4). The ratios of 1047/1022 cm−1 of starch after gelatinization decreased with increasing water content (Table 4), indicating that the degree of disruption of molecular order in starch after DSC heating increased with increasing water content. Similar results were also observed with retrograded starch gels after DSC reheating, although in some cases no significant differences were observed. The ratios of 1047/1022 cm−1R were lower than those of 1047/1022 cm−1G over the whole range of water content, although the difference was small in some cases. This result showed that the molecular order of the retrograded starch gels after DSC reheating was lower than that of gelatinized starch, providing evidence to support the conclusion from the DSC data that there was further melting of starch crystallites remaining in retrograded starch gels.
Figure 4
The deconvoluted FTIR spectra of gelatinized WS after DSC heating (a), reheated retrograded WS (b).
Table 4
The ratios of 1047/1022 cm−1 and FWHMs of the band at 480 cm−1 of starch samples.
Starch
Water content/%
1047/1022cm−1G
1047/1022cm−1R
FWHMG
FWHMR
Rice starch
33
0.695 ± 0.017c
0.649 ± 0.023c
15.47 ± 0.08a
15.54 ± 0.09a
43
0.647 ± 0.008b
0.625 ± 0.007abc
15.45 ± 0.54a
16.38 ± 0.44b
50
0.657 ± 0.006b
0.635 ± 0.005bc
15.59 ± 0.05a
15.84 ± 0.36ab
60
0.646 ± 0.009b
0.645 ± 0.007c
15.73 ± 0.01a
15.77 ± 0.07ab
71
0.595 ± 0.014a
0.595 ± 0.032ab
15.31 ± 0.09a
15.36 ± 0.58a
80
0.604 ± 0.012a
0.586 ± 0.011a
15.66 ± 0.23a
16.38 ± 0.25ab
Wheat starch
33
0.694 ± 0.015b
0.652 ± 0.006b
15.94 ± 0.35ab
16.32 ± 0.08b
43
0.687 ± 0.010b
0.655 ± 0.007b
16.53 ± 0.02b
16.99 ± 0.24c
50
0.680 ± 0.001b
0.664 ± 0.008b
15.92 ± 0.04ab
16.23 ± 0.24b
60
0.689 ± 0.017b
0.660 ± 0.016b
15.67 ± 0.35a
15.78 ± 0.25a
71
0.662 ± 0.014a
0.658 ± 0.014b
16.32 ± 0.41b
16.40 ± 0.04b
80
0.647 ± 0.037a
0.623 ± 0.005a
15.53 ± 0.50a
16.44 ± 0.28b
Values are means ± SD. Values with the same letters in the same column for each starch are not significantly different (p < 0.05).
G represents native starch after DSC heating; R represents retrograded starch gels after DSC reheating.
As the LCM-Raman spectra of starch samples were similar, only those of wheatstarch are presented (Fig. 5). Several clear bands can be seen at 480, 865, 943, 1264 and 2900 cm−1, which are related to δ (CH2), νs (C1-O-C4), νs (C1-O-C5), skeletal (C-C-O), and ν (C-H) modes, respectively293031. Of these bands, the ones at 480 and 2900 cm−1 are often used to characterize the molecular order of native starch granules or the changes in molecular order of starch samples during gelatinization or retrogradation629323334. Full width at half maximum height (FWHM) of the strong band at 480 cm−1 is often used to characterize the relative crystallinity of starch samples; this parameter is most responsive to changes in crystallinity29. Values for FWHMR were higher than those for FWHMG over the whole range of water content (although the difference was small at high water content), indicating that the relative crystallinity of retrograded starch gels after DSC reheating was lower than that of gelatinized starch samples, consistent with the ATR-FTIR results.
Figure 5
LCM-Raman spectra of gelatinized WS after DSC heating (a), reheated retrograded WS (b).
The maximum enthalpy change of retrograded starch gels was observed at water content around 50%, which does not correspond to the maximum degree of starch retrogradation. The crystallites formed during retrogradation are less ordered and less stable than crystallites in native starch granules. The observed higher enthalpy change of retrograded starch gels at low water content indicated that the enthalpy change of retrograded starch gels involves not only the melting of new starch crystallites formed on storage, but also further melting of starch crystallites remaining after gelatinization. This conclusion was supported by the ATR-FTIR and Raman spectroscopy analysis of molecular order of starch after gelatinization and after reheating of retrograded starch gels. Several studies investigated the effect of water content on retrogradation of starch212223353637, but none reported an apparent value greater than 100% for the degree of retrogradation. The effect of water content on starch retrogradation, as determined by measuring DSC enthalpy change of recrystallized amylopectin, displayed a parabolic shape, with maximum retrogradation occurring in starch gels at 40–45% water content212237.Another interesting finding from the present study is the decreasing Tp and Tc of retrograded starch gels with increasing water content. Two hypotheses, not mutually exclusive, are proposed to interpret this observation. The crystallites formed during retrogradation could become progressively less stable with increasing water content, leading to lower Tp and Tc of retrograded starch gels. Another explanation is that the higher Tp and Tc of retrograded starch gels at low water content is due to further melting of residual starch crystallites that remained in retrograded starch gels. The melting of starch crystallites is not complete at the end of DSC heating, especially at low water content3839. This interpretation is supported by the observation that the Tc of retrograded rice and wheatstarch gels was slightly lower than those of native starch granules at low water content, and that the transition temperature range of retrograded starch gels decreased with increasing water content (Table 2). Taken together, we can conclude that the endothermic transition of retrograded starch gels at low water content does not reflect accurately the retrogradation behavior of gelatinized starch.It is also interesting to note that the enthalpy change of starch gelatinization remained essentially unchanged at a water content above 71%, whereas the enthalpy change of starch retrogradation decreased progressively up to a water content of 80%. This result indicated that although the enthalpy change reached a maximum value, presumably corresponding to the complete gelatinization of starch, the retrogradation behavior of fully gelatinized starch was different at different water contents. The high water content brought about low degree of retrogradation, indicating that with increasing water content, the coming together and realignment of dispersed starch chains becomes progressively more difficult.
Conclusions
Differential scanning calorimetry studies over a wide range of water content have shown that water strongly influences retrogradation behavior of rice and wheatstarches. The DSC thermal transition parameters have demonstrated for the first time that the enthalpy change of retrograded starch gels was greater than that of native starch at water content of 33 to 50%. In combination with ATR-FTIR and Raman results, we conclude that the DSC endothermic transition of retrograded starch gels at low water content does not truly reflect the retrogradation behavior of gelatinized starch. The enthalpy change of retrograded starch gels at low water contents represents the melting of starch crystallites formed by retrogradation and of residual crystallites remaining after gelatinization. At high water content, when complete gelatinization of starch may occur, the degree of retrogradation is influenced by water content, whereas at very low and very high water content, the DSC enthalpy change indicated that little retrogradation of starch occurred.
Additional Information
How to cite this article: Wang, S. et al. Retrogradation enthalpy does not always reflect the retrogradation behavior of gelatinized starch. Sci. Rep.
6, 20965; doi: 10.1038/srep20965 (2016).
Authors: Rudi Vermeylen; Veerle Derycke; Jan A Delcour; Bart Goderis; Harry Reynaers; Michel H J Koch Journal: Biomacromolecules Date: 2006-04 Impact factor: 6.988
Authors: Rudi Vermeylen; Veerle Derycke; Jan A Delcour; Bart Goderis; Harry Reynaers; Michel H J Koch Journal: Biomacromolecules Date: 2006-09 Impact factor: 6.988