# Application of Dynamic Temperature-Humidity Chamber for Measuring Moisture Sorption Isotherms of Biomaterials as Compared to the Conventional Isopiestic Method

Authors: Maha Al-Khalili; Nasser Al-Habsi; Mohammad Shafiur Rahman
Journal: Adsorption Science & Technology
 (2021)

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## Abstract

Measurement of water activity and moisture sorption isotherms of foods and biomaterials are important to determine the state of water. In this work, a dynamic temperature-humidity (DTH) controlled chamber was used to measure water sorption isotherm and compared with the conventional isopiestic method. Temperature and relative humidity of DTH chamber can be controlled in the range of -15 to 100°C and 0 to 98%, respectively; thus, measurement of water activity at any point can be measured within the above ranges. The DTH chamber method showed high reproducibility as compared with the conventional isopiestic method when measured isotherms of cellulose, lignin, and hemicellulase were compared at 30°C. Finally, isotherm data of cellulose, lignin, and hemicellulase were generated in the temperature range of 10-90°C using DTH chamber, and these were modelled by BET and GAB equations. The model parameters were correlated with the temperature.


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## Body

## 1. Introduction

Water activity indicates the states of water in foods, and it is a crucial indicator of food stability [1–4]. Moisture sorption isotherm at a certain temperature indicates the relationship of the water activity and moisture content. Water activity of a food is primarily a tool to assess the microbial growth, rancidity, nonenzymatic and enzymatic reactions, vitamin losses, and textural attributes [5–9].The conventional static isopiestic method uses desiccator (i.e., an enclosed atmospheric environment of a specific relative humidity) and saturated salt solutions (i.e., creating specific relative humidity environments). It is the most basic and popular method, and it is widely used to measure moisture sorption isotherm of foods. The isopiestic method has been developed by Bousfield, and it is defined as the transport of solvent from a solution with higher vapor pressure to a solution with lower vapor pressure [10]. The principle of isopiestic method mainly relays on the creation of humid environment in an air tight closed desiccator at a constant temperature [8, 11, 12]. Initially, desiccator was commonly used, and then, different types of cells, such as glass and metal jars, and plastic containers were also used. It is a simple method and needs a simple setup (i.e., a desiccator or air tight chamber, different types of salts, and sample holder) [13]. Temperatures of the jars or cells with sample and saturated salt solutions are mainly controlled by placing these in water bath or air oven. The long equilibration time of several weeks to months is one of the major issues of this method [13–16]. The maintenance of the saturated salt solution plays an important role in maintaining specific relative humidity in the chamber [14]. A layer of salt crystals needs to be maintained to ensure saturated condition of the salt solution during whole equilibrium time. However, salts should be a soft mixture, and it is important to avoid fossil formation (i.e., rock like mass) [16, 17]. In order to check the equilibrium condition of the sample and environment in the desiccator, it needs to be opened and closed time to time. This breaks the equilibrium relative humidity in the desiccator, and it needs time to reach at the set specific relative humidity after reclosing the desiccator. Samples and salts are susceptible for microbial growth during the long equilibrium period, especially at high water activity [13, 18, 19]. In order to control the microbial growth, thymol and other chemicals (e.g., toluene) in a small beaker are placed inside the desiccator; however, these are toxic and hazardous.Over the years, a wide range of isopiestic setups with improved designs were reported in the literature. The jars with evacuated system (i.e., under vacuum) were then introduced to enhance the equilibrium time [19–21]. It can equilibrate samples faster and act as thermal insulation; however, it is higher in cost due to its construction and required additional instruments. Another improvement was performed by placing an in situ balance to record mass without opening and closing the jars or chambers. This could avoid the disruption of equilibrium atmosphere by avoiding the opening and closing of jar [11, 22].An apparatus of circulating air chamber was also developed earlier. It consists of equilibrium chamber, magnetic stirrer for air circulation, and an in situ sensitive balance to record the mass. The complete setup was then placed in a constant temperature bath [11, 23, 24]. Gal. [20] used a system to create air with specific relative humidity, and then, air is supplied to the isotherm measurement chamber. The air humidity was controlled either by cooling air to condense out water or high pressure air was expanded in a chamber. Recently, commercial Dynamic Vapor Sorption (DVS) systems are being used, and it is built with a temperature-humidity controlled chamber and an in-build microbalance. The relative humidity of the chamber was maintained by circulating nitrogen gas at a specific relative humidity. In this system, moisture was sprayed over dry nitrogen gas in a separate chamber to attain a specific relative humidity before circulating it into the isotherm chamber [13, 25]. In this case, opening and closing of the chamber can be avoided. Rapid equilibrium was the main advantage of this method, and the same sample can be used for entire isotherm measurement (i.e., complete water activity range). A very small sample needs to be used (i.e., microgram) in the DVS system. However, complete DVS system is very costly.Isotherms of spray dried tomato pulp, texturized soy protein, hazelnut, rice, barley malt, cookies, and crackers were investigated within a narrow range of temperature, mainly 20-60°C [26–34]. In the literature, isotherm data of foods within a wide range of temperature (i.e., chilled condition and above 60°C) are limited. Sorption isotherms of cellulose and lignin were reported by Mihranyan et al. [35] and Volkova et al. [36]. However, limited data are presented for hemicellulase. In this study, these materials were used to test the proposed dynamic temperature-humidity (DTH) chamber for measuring moisture sorption isotherm and to develop their prediction models.According to the literature, more than 200 different equations have been developed to shape the sorption isotherms at different temperature [37]. Some of these models relay on the theoretical basis, while others are considered as semiempirical or empirical [26, 30, 38]. The GAB (Guggenheim–Anderson–de Boer) and BET (Brunauer–Emmett–Teller) are the most commonly used models for the prediction of the sorption isotherms of different foods [39–41]. This is mainly due to their theoretical basis, and model parameters have physical meaning.At present, different types of temperature-humidity controlled chambers are commercially available and these could be used to measure the water sorption isotherm. The objective of this study was to use a dynamic temperature-humidity (DTH) controlled chamber for measuring water sorption isotherms of foods. The adsorption isotherms of cellulose, lignin, and hemicellulase were measured by DTH chamber, and these isotherms were compared with the conventional isopiestic method (i.e., 30°C). In addition, isotherm data were generated in the temperature range of 10-90°C using DTH chamber, and these were modelled by BET and GAB equations.


## 2. Materials and Methods

### 2.1. Materials

Commercial cellulose (C6H10O5)n, lignin (C81H92O28), and hemicellulase (β-(1-4)-D-xylopyranosyl) were purchased from Sigma-Aldrich, USA. Seven saturated salt solutions, namely, lithium chloride (LiCl), magnesium chloride (MgCl2), magnesium nitrate (Mg(NO3)2), sodium bromide (NaBr), strontium chloride (SrCl2), potassium chloride (KCl), and potassium nitrate (KNO3), were used to create relative humidity environments: 11.5, 32.7, 52.9, 57.7, 70.8, 84.3, and 95.0%, respectively. Water activity values for these saturated salt solutions were obtained from Rahman [8]. In the conventional isopiestic method, thymol was used to overcome the microbial growth in the samples and saturated salt solutions.


### 2.2. Moisture Content

Moisture content of the sample was measured in triplicates by drying samples at 70°C for 18 h in a vacuum oven at pressure 10 kPa (VD 23, Binder, Germany).


### 2.3. Conventional Isopiestic Method

Sample (0.2 g) in a glass dish was placed inside a tightly closed glass jar, which was maintained at a specific relative humidity. The specific relative of the jar was created by placing a saturated salt solution in a beaker. Seven saturated salt solutions as mentioned in the earlier section were used to create relative humidity. A layer of salts at the bottom of the beaker was maintained during the whole equilibrium period to ensure the saturated condition of the salt solutions. Thymol in a 5 ml beaker was placed inside the jar to avoid any microbial growth in the sample or solution. Jars containing samples, saturated salt solutions, and thymol were kept in an oven (Gallenkamp, UK; model: 300 plus series) at 30°C, and mass of the sample in each jar was recoded every two days until a constant weight was achieved.


### 2.4. Dynamic Temperature-Humidity Chamber

In this proposed method, a dynamic temperature-humidity (DTH) chamber (Model 240, Binder, Germany) was used to measure the sorption isotherm. A schematic diagram of the DTH is shown in Figure1. DTH chamber applies APT-line™ technology to maintain homogeneous climate conditions. It stands for “Advanced Preheating Technology” and a unique heating system that ensures homogeneous air and temperature distribution inside a chamber. Its controller allows it to operate in the condensation free region and special air flow (i.e., turbine) to ensure high level of temperature homogeneity, short heating up time, and rapid heat transfer. At the same time, this technology also ensures fast recovery of the humidity and temperature after opening and closing [42]. In this technology, water spray in a premixing chamber and mix with air (i.e., desire relative humidity) and then circulate to the humidity chamber at a specified relative humidity. The air relative humidity and temperature are automatically controlled by the system. The temperature and humidity of the chamber can be controlled in the range of -15 to 100°C and 0 to 98%, respectively. The temperature of the chamber was maintained with a thermostat, and humidity was maintained at a desired level by automatic water spray through a nozzle.Figure 1
Schematic diagram of the dynamic temperature-humidity (DTH) chamber.


### 2.5. Dynamic Temperature-Humidity (DTH) Chamber Method

#### 2.5.1. Initial Conditioning

Sample (0.2 g) was placed uniformly in a glass dish, and it was then conditioned in the DTH chamber, which was set at 30°C and 5% relative humidity. Weight of the sample was recorded until 60 min, initially every 5 min and then every 10 min. This procedure was used to bring the sample at the start of the adsorption isotherm. Triplicate samples were used in this procedure. The adsorption data was fitted to the Weibull equation to determine actual equilibrium moisture. Weibull equation can be written as follows:(1)Mw−MeMo−Me=exp−tβα,where Mo, Mw, and Me are the moisture at initial, time t, and equilibrium (g/100 dry-solids), respectively, t is the time (min), and α and β are the model parameters. The data was fitted to Equation (1) using the NLREG software, and model parameters were determined [43]. The moisture after 30 min was compared with the equilibrium moisture as determined from the Weibull equation.


#### 2.5.2. Equilibration Time Determination

Required equilibrium time at each step increase in humidity (i.e., 10% RH) was determined by measuring adsorption kinetics by changing relative humidity from 5 to 15% (i.e., 10% increase in relative humidity). In this procedure, weight of the sample was recorded after changing relative humidity from 5 to 15%, initially every 5 min and then every 10 min. Samples were used in triplicates.


#### 2.5.3. Isotherm Measurement

First, DTH chamber was set at 30°C and 5% relative humidity and started the experiment after it was reached at the set condition. Samples (0.2 g) were placed uniformly in three glass dishes, and these were placed inside the DTH chamber. These were then conditioned for 30 min, and the weight was recorded. The relative humidity of the DTH chamber was then set to 10% relative humidity, and weight of the sample was recorded after 30 min. The same procedure was followed after changing the relative humidity of the chamber at 10% increment up to 90% relative humidity. Finally, DTH chamber was set at 95% relative humidity. The same procedures were repeated for other isotherm measurement at different temperatures (i.e., 10, 30, 50, 70, and 90°C).


### 2.6. Isotherm Models

Moisture adsorption isotherms were modelled by commonly used fundamental BET and GAB equations. BET equation can be written as follows [44]:
(2)Me=MbBaw1−aw1+B−1aw,where Me and Mb are the equilibrium moisture and BET monolayer moisture contents (dry basis: g water/100 g dry solids) and B is a constant related to the net heat of sorption. The BET isotherm is valid up to water activity 0.45, and it would be enough to determine the parameters Mb and B [45]. BET parameters were estimated graphically by plotting aw/1−awMw versus water activity within water activity 0.45. The values of B and Mb were estimated from the slope B−1/MbB and intercept 1/MbB of the best fitted line.GAB equation was used to model the isotherm data from water activity 0.05 to 0.95. The GAB model was modified from BET equation considering multilayer sorption, and it is the extended isotherm considering water activity beyond 0.45 [46]. This modified equation was treated kinetically by DeBoer [47] and statically by Guggenheim [48], and it was then known as GAB equation. It is one of the most widely used models in the food domains. GAB equation can be written as follows:
(3)Me=MgCKaw1−Kaw1−Kaw+CKaw,where Mg is the GAB monolayer moisture content (dry basis, g/100 g dry solids), C is a constant related to the monolayer heat of sorption, and K is a factor related to the heat of sorption of multilayer.Clausius-Clapeyron equation was used to calculate the isosteric heat of adsorption [49]:
(4)dlnawd1/T=−QsT,where aw is the water activity, T is temperature (K), Qs is the net isosteric heat of sorption (kJ/kg). It can be defined as the energy required to remove a unit mass of adsorpted water at a specific temperature [50]. The net isosteric heat of sorption (Qs) was estimated from the slope of lnaw versus 1/T plots at a specific moisture content, and it can be estimated at each temperature [51].


### 2.7. Statistical Analysis

Data are presented as average and standard deviation. Reproducibility of the measurement by each method was determined from the standard deviation divided by average value, and it was presented as percent. Nonlinear regression was used to predict the GAB model parameters, and the NLREG software was used (Sherrod, 1991). Accuracy of the models was evaluated considering regression coefficient,R2.


## 2.1. Materials

Commercial cellulose (C6H10O5)n, lignin (C81H92O28), and hemicellulase (β-(1-4)-D-xylopyranosyl) were purchased from Sigma-Aldrich, USA. Seven saturated salt solutions, namely, lithium chloride (LiCl), magnesium chloride (MgCl2), magnesium nitrate (Mg(NO3)2), sodium bromide (NaBr), strontium chloride (SrCl2), potassium chloride (KCl), and potassium nitrate (KNO3), were used to create relative humidity environments: 11.5, 32.7, 52.9, 57.7, 70.8, 84.3, and 95.0%, respectively. Water activity values for these saturated salt solutions were obtained from Rahman [8]. In the conventional isopiestic method, thymol was used to overcome the microbial growth in the samples and saturated salt solutions.


## 2.2. Moisture Content

Moisture content of the sample was measured in triplicates by drying samples at 70°C for 18 h in a vacuum oven at pressure 10 kPa (VD 23, Binder, Germany).


## 2.3. Conventional Isopiestic Method

Sample (0.2 g) in a glass dish was placed inside a tightly closed glass jar, which was maintained at a specific relative humidity. The specific relative of the jar was created by placing a saturated salt solution in a beaker. Seven saturated salt solutions as mentioned in the earlier section were used to create relative humidity. A layer of salts at the bottom of the beaker was maintained during the whole equilibrium period to ensure the saturated condition of the salt solutions. Thymol in a 5 ml beaker was placed inside the jar to avoid any microbial growth in the sample or solution. Jars containing samples, saturated salt solutions, and thymol were kept in an oven (Gallenkamp, UK; model: 300 plus series) at 30°C, and mass of the sample in each jar was recoded every two days until a constant weight was achieved.


## 2.4. Dynamic Temperature-Humidity Chamber

In this proposed method, a dynamic temperature-humidity (DTH) chamber (Model 240, Binder, Germany) was used to measure the sorption isotherm. A schematic diagram of the DTH is shown in Figure1. DTH chamber applies APT-line™ technology to maintain homogeneous climate conditions. It stands for “Advanced Preheating Technology” and a unique heating system that ensures homogeneous air and temperature distribution inside a chamber. Its controller allows it to operate in the condensation free region and special air flow (i.e., turbine) to ensure high level of temperature homogeneity, short heating up time, and rapid heat transfer. At the same time, this technology also ensures fast recovery of the humidity and temperature after opening and closing [42]. In this technology, water spray in a premixing chamber and mix with air (i.e., desire relative humidity) and then circulate to the humidity chamber at a specified relative humidity. The air relative humidity and temperature are automatically controlled by the system. The temperature and humidity of the chamber can be controlled in the range of -15 to 100°C and 0 to 98%, respectively. The temperature of the chamber was maintained with a thermostat, and humidity was maintained at a desired level by automatic water spray through a nozzle.Figure 1
Schematic diagram of the dynamic temperature-humidity (DTH) chamber.


## 2.5. Dynamic Temperature-Humidity (DTH) Chamber Method

### 2.5.1. Initial Conditioning

Sample (0.2 g) was placed uniformly in a glass dish, and it was then conditioned in the DTH chamber, which was set at 30°C and 5% relative humidity. Weight of the sample was recorded until 60 min, initially every 5 min and then every 10 min. This procedure was used to bring the sample at the start of the adsorption isotherm. Triplicate samples were used in this procedure. The adsorption data was fitted to the Weibull equation to determine actual equilibrium moisture. Weibull equation can be written as follows:(1)Mw−MeMo−Me=exp−tβα,where Mo, Mw, and Me are the moisture at initial, time t, and equilibrium (g/100 dry-solids), respectively, t is the time (min), and α and β are the model parameters. The data was fitted to Equation (1) using the NLREG software, and model parameters were determined [43]. The moisture after 30 min was compared with the equilibrium moisture as determined from the Weibull equation.


### 2.5.2. Equilibration Time Determination

Required equilibrium time at each step increase in humidity (i.e., 10% RH) was determined by measuring adsorption kinetics by changing relative humidity from 5 to 15% (i.e., 10% increase in relative humidity). In this procedure, weight of the sample was recorded after changing relative humidity from 5 to 15%, initially every 5 min and then every 10 min. Samples were used in triplicates.


### 2.5.3. Isotherm Measurement

First, DTH chamber was set at 30°C and 5% relative humidity and started the experiment after it was reached at the set condition. Samples (0.2 g) were placed uniformly in three glass dishes, and these were placed inside the DTH chamber. These were then conditioned for 30 min, and the weight was recorded. The relative humidity of the DTH chamber was then set to 10% relative humidity, and weight of the sample was recorded after 30 min. The same procedure was followed after changing the relative humidity of the chamber at 10% increment up to 90% relative humidity. Finally, DTH chamber was set at 95% relative humidity. The same procedures were repeated for other isotherm measurement at different temperatures (i.e., 10, 30, 50, 70, and 90°C).


## 2.5.1. Initial Conditioning

Sample (0.2 g) was placed uniformly in a glass dish, and it was then conditioned in the DTH chamber, which was set at 30°C and 5% relative humidity. Weight of the sample was recorded until 60 min, initially every 5 min and then every 10 min. This procedure was used to bring the sample at the start of the adsorption isotherm. Triplicate samples were used in this procedure. The adsorption data was fitted to the Weibull equation to determine actual equilibrium moisture. Weibull equation can be written as follows:(1)Mw−MeMo−Me=exp−tβα,where Mo, Mw, and Me are the moisture at initial, time t, and equilibrium (g/100 dry-solids), respectively, t is the time (min), and α and β are the model parameters. The data was fitted to Equation (1) using the NLREG software, and model parameters were determined [43]. The moisture after 30 min was compared with the equilibrium moisture as determined from the Weibull equation.


## 2.5.2. Equilibration Time Determination

Required equilibrium time at each step increase in humidity (i.e., 10% RH) was determined by measuring adsorption kinetics by changing relative humidity from 5 to 15% (i.e., 10% increase in relative humidity). In this procedure, weight of the sample was recorded after changing relative humidity from 5 to 15%, initially every 5 min and then every 10 min. Samples were used in triplicates.


## 2.5.3. Isotherm Measurement

First, DTH chamber was set at 30°C and 5% relative humidity and started the experiment after it was reached at the set condition. Samples (0.2 g) were placed uniformly in three glass dishes, and these were placed inside the DTH chamber. These were then conditioned for 30 min, and the weight was recorded. The relative humidity of the DTH chamber was then set to 10% relative humidity, and weight of the sample was recorded after 30 min. The same procedure was followed after changing the relative humidity of the chamber at 10% increment up to 90% relative humidity. Finally, DTH chamber was set at 95% relative humidity. The same procedures were repeated for other isotherm measurement at different temperatures (i.e., 10, 30, 50, 70, and 90°C).


## 2.6. Isotherm Models

Moisture adsorption isotherms were modelled by commonly used fundamental BET and GAB equations. BET equation can be written as follows [44]:
(2)Me=MbBaw1−aw1+B−1aw,where Me and Mb are the equilibrium moisture and BET monolayer moisture contents (dry basis: g water/100 g dry solids) and B is a constant related to the net heat of sorption. The BET isotherm is valid up to water activity 0.45, and it would be enough to determine the parameters Mb and B [45]. BET parameters were estimated graphically by plotting aw/1−awMw versus water activity within water activity 0.45. The values of B and Mb were estimated from the slope B−1/MbB and intercept 1/MbB of the best fitted line.GAB equation was used to model the isotherm data from water activity 0.05 to 0.95. The GAB model was modified from BET equation considering multilayer sorption, and it is the extended isotherm considering water activity beyond 0.45 [46]. This modified equation was treated kinetically by DeBoer [47] and statically by Guggenheim [48], and it was then known as GAB equation. It is one of the most widely used models in the food domains. GAB equation can be written as follows:
(3)Me=MgCKaw1−Kaw1−Kaw+CKaw,where Mg is the GAB monolayer moisture content (dry basis, g/100 g dry solids), C is a constant related to the monolayer heat of sorption, and K is a factor related to the heat of sorption of multilayer.Clausius-Clapeyron equation was used to calculate the isosteric heat of adsorption [49]:
(4)dlnawd1/T=−QsT,where aw is the water activity, T is temperature (K), Qs is the net isosteric heat of sorption (kJ/kg). It can be defined as the energy required to remove a unit mass of adsorpted water at a specific temperature [50]. The net isosteric heat of sorption (Qs) was estimated from the slope of lnaw versus 1/T plots at a specific moisture content, and it can be estimated at each temperature [51].


## 2.7. Statistical Analysis

Data are presented as average and standard deviation. Reproducibility of the measurement by each method was determined from the standard deviation divided by average value, and it was presented as percent. Nonlinear regression was used to predict the GAB model parameters, and the NLREG software was used (Sherrod, 1991). Accuracy of the models was evaluated considering regression coefficient,R2.


## 3. Results and Discussion

### 3.1. Adsorption Kinetics

Figure2 illustrates the initial conditioning of a sample at 30°C and 5% relative humidity. The initial moisture contents of cellulose, lignin, and hemicellulase were 8.0, 3.9, and 0.7 g/100 g sample, respectively (Table 1). In the case of cellulose, Figure 2(a) shows a sharp decrease of moisture content as a function of time and after 10 min, moisture remained nearly constant. Similar change was also observed in the case of lignin, and moisture content was also remained nearly the same after 10 min (Figure 2(b)). In the case of hemicellullase, moisture content remained the same after 20 min (Figure 2(c)), since it was already contained very low moisture (i.e., low driving force for moisture adsorption). This indicated that the initial moisture content played a role to achieve the required equilibration time to reach initial conditioning. Tereshchenko [16] also identified that initial water activity (i.e., moisture) of a sample indicated the required equilibrium time. The moisture adsorption as a function of time was fitted to the Weibull equation, and moisture after 30 min and equilibrium moisture from the Weibull equation were determined. The percent deviation was observed below 0.14% when cellulose, lignin, and hemicellulase were considered. Therefore, 30 min was considered as the equilibration time.Figure 2
Sorption kinetics of the dried samples for initial conditioning before starting the adsorption isotherm ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)Table 1
BET and GAB models’ parameters for commercial fibers and the enzyme hemicellulase.
SampleXwBET model parametersGAB model parameters(g/100 g)T (°C)Mb (g/100 g dry solids)BR2Mg (g/100 g dry solids)CKR2Cellulose8.0106.37120.690.988.30106.830.570.99304.8225.910.995.8323.090.720.99504.264.090.974.307.130.770.99701.424.550.993.005.000.390.97901.541.670.992.501.000.760.97Lignin3.9107.28196.140.998.00400.000.870.99306.07412.000.996.26200.000.950.99505.6870.440.995.8860.000.950.85703.7441.170.993.7840.000.980.88902.2020.220.992.5220.000.990.96Hemicellulase0.7103.989.650.994.7510.000.720.99304.396.780.994.857.120.820.99503.214.250.993.394.380.910.99702.093.330.992.503.250.830.99901.311.400.991.701.220.880.99Xw: initial moisture content (g/100 g sample).Figure3 shows the moisture adsorption kinetics at 30°C, when relative humidity of the chamber was changed from the condition 5% to 15% (i.e., 10% increment). It shows that moisture increased exponentially and then reached to equilibrium. This shows that 30 min equilibration time was enough to reach equilibrium state for all 3 samples. However, in the case of isopiestic method, the equilibration time was observed more than 3 weeks at each relative humidity. Similarly, reported literature shows that the conventional isopiestic method took long equilibration time. In many instances, it took more than 4 weeks [26, 29, 30, 52].Figure 3
Adsorption kinetics of the dried samples at 15% relative humidity at 30°C ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


### 3.2. Comparison between Isopiestic and Controlled Humidity Chamber Methods

Moisture adsorption isotherms as measured by DTH chamber and conventional method are shown in Figure4. The measured values by both methods were correlated, and R2 were observed as 0.95, 0.96, and 0.91, respectively, for cellulose, lignin, and hemicellulase. The reproducibility of the DTH and conventional methods varied from 0.0074 to 7.6% and 0.75 to 21%, respectively, considering different equilibrium relative humidity used in this experiment. In addition, data points in the conventional method showed more random considering the whole trend of the curve as compared to DTH methods (i.e., DTH isotherm followed a smooth curve if the points are joined). This could be due to the fact that the DTH method used the same sample to measure adsorption isotherm for all relative humidity condition, while conventional method used different sample at each relative humidity. In addition, in the case of conventional method, physicochemical properties of the samples could be changed when stored for 3 weeks inside the glass jar, and more variability of the relative humidity (i.e., created by saturated salt solutions) and temperature in the glass jar could exist. Moreover, DTH chamber had the ability to maintain precise control of the relative humidity in the temperature-humidity chamber due to dynamic air circulation as compared to the static air in the conventional isopiestic chamber.Figure 4
Adsorption isotherms as measured by DTH chamber and conventional isopiestic method ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


### 3.3. Advantages of the Dynamic Temperature-Humidity (DTH) Chamber

The main advantage of DTH was the shorter equilibrium time, as discussed in the earlier section. Faster equilibration was observed in the DTH chamber as compared to the conventional isopiestic method although 0.2 g was used in both methods. It was due to the mechanical air circulation used in the DTH, which accelerated the mass transfer. In addition, DTH chamber did not open during the specific equilibration experiment, while conventional ones needed to open and close time to time in order to check the mass (i.e., it took long time to attain again to the desire relative humidity). In addition, the required longer equilibrium time by conventional method can change the physical and chemical characteristics of the sample, especially at high water activity [8]. For example, in the case of lignin at high water activity, conventional method showed much higher water adsorption as compared to the DTH method (Figure 4). This could be due to the transformation of physicochemical changes occurred in lignin at high relative humidity for longer equilibrium time.In the case of conventional method, specific salt is required to maintain a specific relative humidity [53–56]. Therefore, salts for all relative humidity values are required. However, salts for all relative humidity may not be readily available, and this could restrict the conventional method for all relative humidity conditions. In addition, any incremental level of relative humidity within 0 to 0.98% and temperature within -15 to 100°C can be achieved in the case of DTH chamber. In the case of conventional method, oven or water bath needs to be used for longer period (i.e., more than 4 weeks) [13, 18, 19]. This needs more energy consumption by the oven, and oven would be unable to use for other purposes.In the conventional method, it is important to monitor the saturated conditions (i.e., a layer of deposited salt at the bottom) of the salt solution during complete experimental period to ensure a constant relative humidity [16]. In the process of moisture desorption from the sample (i.e., high moisture sample), salts can be dissolved over time and saturation could not be maintained. This needs the addition of salts time to time [56]. In addition, fossilization of salts could deviate the desired relative humidity [13]. Contamination of salts from the sample could also affect the desired relative humidity. In the proposed DTH method, all these issues could be avoided.In the DTH method, there is no need to check equilibrium conditions time to time by opening and closing the chamber. In this case, weight of the sample needs to be taken after predetermined equilibrium time of 30 min (i.e., at each relative humidity). Metal cells, used at higher temperature, could be susceptible to corrosion [24, 57]. Replacing metal cells with glass could be a favourable choice to overcome these issues, but it limits the isotherm measurement at lower temperatures [58–61]. In conventional method, handling of 9 to 10 cells for more than 4 weeks needs lots of handling time, whereas in the case of DTH chamber, minimal handling of the samples is required. In addition, lots of space is required for handling 9 to 10 jars in the case of conventional method. In the case of the DTH method, the same sample could be used for measuring water activity within the complete range of 0.05 to 0.98 relative humidity.


### 3.4. Water Adsorption Isotherm

Figure5 show the measured adsorption isotherms of cellulose, lignin, and hemicellulase using DTH chamber and predicted model by GAB equation at different temperatures (10, 30, 50, 70, and 90°C). Isotherms showed sigmoid shape, as observed and reported in the literature for foods [13, 38, 39, 52, 62, 63]. In cases of lignin and hemicellulase, a sharp increase was observed after water activity 0.8, indicating more swelling with the adsorption of water as compared to the cellulose. These isotherms shifted down as a function of increasing temperature from 10 to 90°C. This was due to the increase of escaping tendency of water molecule at higher temperature [62]. Kapsalis [64] pointed that temperature affects the mobility of water molecules and enhanced dynamic equilibrium between water vapor and adsorbed phases. Similar observations were also stated for starchy foods [27, 65, 66]. Literature isotherms were mainly reported within 20-60°C; however, the DTH chamber method can be used to measure isotherm up to 100°C as well as chilled conditions up to -15°C. This could be one of the major advantage of the proposed DTH method.Figure 5
Adsorption isotherms of cellulose, lignin, and hemicellulase at temperature from 10 to 90°C.The measured absorption isotherm data of the three samples were fitted linearly with the BET model (Equation (2)) up to water activity 0.4, and the regression coefficients (R2) were varied from 0.97 to 0.99. The model parameters are shown in Table 1. The BET monolayer values of Mb exhibited a decreasing trend with increasing temperature for all samples (i.e., R2 0.920, 0.882, and 0.961 for cellulose, lignin, and hemicellulase, respectively) (Figures 6(a)–6(c)). The decrease in Mb could be due to the chemical and physical changes induced by elevated temperature [67]. Similar findings were also reported for rice, barley malt, cookies, and crackers [27, 28, 32]. The prediction of Mb values is crucial since deterioration of foods is minimal at Mb (i.e., strongly bound water cannot be involved in any deteriorative reaction either as solvent or as one of the substrates) [68]. The BET monolayer is an effective method that estimates the amount of bound water to specific polar sites in dehydrated food systems.Figure 6
BET ((a) cellulose, (b) lignin, and (c) hemicellulase) and GAB ((d) cellulose, (e) lignin, and (f) hemicellulase) monolayer values as a function of temperature.
(a)(b)(c)(d)(e)(f)At 10°C,B values were 120.7, 196.1, and 9.7 J/g, respectively, in the cases of cellulose, lignin, and hemicellulase (Table 1). The B values were observed as 502.8 J/g (22°C) for the corn flour [69], 101.5 and 5.7 J/g for blueberries in the case of desorption and adsorption isotherms at 40°C, respectively [70], 7.4 J/g in the desorption isotherm and 9.2 J/g in the adsorption isotherm at 30°C for dried potato [31], and 2.9 J/g at 45°C for yams [34]. The heat of adsorption (i.e., B) showed a decreasing trend as a function of increasing temperature. The values of B were plotted as Arrhenius equation as a function of 1/T (Figures 7(a)–7(c)).Figure 7
BET modelB values ((a) cellulose, (b) lignin, and (c) hemicellulase), GAB model C values ((d) cellulose, (e) lignin, and (f) hemicellulase), and K values ((g) cellulose, (h) lignin, and (i) hemicellulase) as a function of temperature.
(a)(b)(c)(d)(e)(f)(g)(h)(i)The nonlinear regression was implemented for the GAB model for the whole range of water activity (i.e., 0.05 to 0.95) with a regression coefficient (R2) varied from 0.85 to 0.99 (Table 1). The Mg values from the GAB model decreased with the increase of temperature, and it was correlated linearly with temperature (i.e., R2 of 0.943, 0.938, and 0.938 for cellulose, lignin, and hemicellulase, respectively) (Figures 6(d)–6(f)). The GAB model was used to predict sorption isotherms of many food products [41, 71, 72], vegetables like dried-onions and green beans [40], and fruit like apple, blackcurrant, sour cherries, apricots, and coffee fruit [73, 74].lnC value was plotted as a function of inverse temperature (1/T), and regression coefficient showed more than 0.9 (Figures 7(d)–7(f)). However, regression coefficients of lnK versus 1/T plots showed lower than 0.6, in the case of cellulose and lignin (Figures 7(g)–7(i)). Chirife [75] and Rahman [8] also pointed that K values should be less than unity and less affected by temperature.


### 3.5. Isosteric Heat of Adsorption

Equation (4) was used to calculate the isosteric heat of adsorption, and it decreased with the increase of moisture (Figure 8). This behaviour was also observed in other studies for quinoa, dried fruit, cassava, orange juice powder, and jasmine rice crackers [62, 66, 76–79]. A steeped increase in heat of sorption was observed below moisture 4.0 to 10.0 g/100 g sample depending on the sample. This was because water binding energy increased at lower water content [79]. Similar justification was also proposed by other researches [65, 67, 80, 81]. Therefore, removal of bound water from the surface can be tougher [76].Figure 8
Isosteric heat of adsorption as a function of moisture content ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


## 3.1. Adsorption Kinetics

Figure2 illustrates the initial conditioning of a sample at 30°C and 5% relative humidity. The initial moisture contents of cellulose, lignin, and hemicellulase were 8.0, 3.9, and 0.7 g/100 g sample, respectively (Table 1). In the case of cellulose, Figure 2(a) shows a sharp decrease of moisture content as a function of time and after 10 min, moisture remained nearly constant. Similar change was also observed in the case of lignin, and moisture content was also remained nearly the same after 10 min (Figure 2(b)). In the case of hemicellullase, moisture content remained the same after 20 min (Figure 2(c)), since it was already contained very low moisture (i.e., low driving force for moisture adsorption). This indicated that the initial moisture content played a role to achieve the required equilibration time to reach initial conditioning. Tereshchenko [16] also identified that initial water activity (i.e., moisture) of a sample indicated the required equilibrium time. The moisture adsorption as a function of time was fitted to the Weibull equation, and moisture after 30 min and equilibrium moisture from the Weibull equation were determined. The percent deviation was observed below 0.14% when cellulose, lignin, and hemicellulase were considered. Therefore, 30 min was considered as the equilibration time.Figure 2
Sorption kinetics of the dried samples for initial conditioning before starting the adsorption isotherm ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)Table 1
BET and GAB models’ parameters for commercial fibers and the enzyme hemicellulase.
SampleXwBET model parametersGAB model parameters(g/100 g)T (°C)Mb (g/100 g dry solids)BR2Mg (g/100 g dry solids)CKR2Cellulose8.0106.37120.690.988.30106.830.570.99304.8225.910.995.8323.090.720.99504.264.090.974.307.130.770.99701.424.550.993.005.000.390.97901.541.670.992.501.000.760.97Lignin3.9107.28196.140.998.00400.000.870.99306.07412.000.996.26200.000.950.99505.6870.440.995.8860.000.950.85703.7441.170.993.7840.000.980.88902.2020.220.992.5220.000.990.96Hemicellulase0.7103.989.650.994.7510.000.720.99304.396.780.994.857.120.820.99503.214.250.993.394.380.910.99702.093.330.992.503.250.830.99901.311.400.991.701.220.880.99Xw: initial moisture content (g/100 g sample).Figure3 shows the moisture adsorption kinetics at 30°C, when relative humidity of the chamber was changed from the condition 5% to 15% (i.e., 10% increment). It shows that moisture increased exponentially and then reached to equilibrium. This shows that 30 min equilibration time was enough to reach equilibrium state for all 3 samples. However, in the case of isopiestic method, the equilibration time was observed more than 3 weeks at each relative humidity. Similarly, reported literature shows that the conventional isopiestic method took long equilibration time. In many instances, it took more than 4 weeks [26, 29, 30, 52].Figure 3
Adsorption kinetics of the dried samples at 15% relative humidity at 30°C ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


## 3.2. Comparison between Isopiestic and Controlled Humidity Chamber Methods

Moisture adsorption isotherms as measured by DTH chamber and conventional method are shown in Figure4. The measured values by both methods were correlated, and R2 were observed as 0.95, 0.96, and 0.91, respectively, for cellulose, lignin, and hemicellulase. The reproducibility of the DTH and conventional methods varied from 0.0074 to 7.6% and 0.75 to 21%, respectively, considering different equilibrium relative humidity used in this experiment. In addition, data points in the conventional method showed more random considering the whole trend of the curve as compared to DTH methods (i.e., DTH isotherm followed a smooth curve if the points are joined). This could be due to the fact that the DTH method used the same sample to measure adsorption isotherm for all relative humidity condition, while conventional method used different sample at each relative humidity. In addition, in the case of conventional method, physicochemical properties of the samples could be changed when stored for 3 weeks inside the glass jar, and more variability of the relative humidity (i.e., created by saturated salt solutions) and temperature in the glass jar could exist. Moreover, DTH chamber had the ability to maintain precise control of the relative humidity in the temperature-humidity chamber due to dynamic air circulation as compared to the static air in the conventional isopiestic chamber.Figure 4
Adsorption isotherms as measured by DTH chamber and conventional isopiestic method ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


## 3.3. Advantages of the Dynamic Temperature-Humidity (DTH) Chamber

The main advantage of DTH was the shorter equilibrium time, as discussed in the earlier section. Faster equilibration was observed in the DTH chamber as compared to the conventional isopiestic method although 0.2 g was used in both methods. It was due to the mechanical air circulation used in the DTH, which accelerated the mass transfer. In addition, DTH chamber did not open during the specific equilibration experiment, while conventional ones needed to open and close time to time in order to check the mass (i.e., it took long time to attain again to the desire relative humidity). In addition, the required longer equilibrium time by conventional method can change the physical and chemical characteristics of the sample, especially at high water activity [8]. For example, in the case of lignin at high water activity, conventional method showed much higher water adsorption as compared to the DTH method (Figure 4). This could be due to the transformation of physicochemical changes occurred in lignin at high relative humidity for longer equilibrium time.In the case of conventional method, specific salt is required to maintain a specific relative humidity [53–56]. Therefore, salts for all relative humidity values are required. However, salts for all relative humidity may not be readily available, and this could restrict the conventional method for all relative humidity conditions. In addition, any incremental level of relative humidity within 0 to 0.98% and temperature within -15 to 100°C can be achieved in the case of DTH chamber. In the case of conventional method, oven or water bath needs to be used for longer period (i.e., more than 4 weeks) [13, 18, 19]. This needs more energy consumption by the oven, and oven would be unable to use for other purposes.In the conventional method, it is important to monitor the saturated conditions (i.e., a layer of deposited salt at the bottom) of the salt solution during complete experimental period to ensure a constant relative humidity [16]. In the process of moisture desorption from the sample (i.e., high moisture sample), salts can be dissolved over time and saturation could not be maintained. This needs the addition of salts time to time [56]. In addition, fossilization of salts could deviate the desired relative humidity [13]. Contamination of salts from the sample could also affect the desired relative humidity. In the proposed DTH method, all these issues could be avoided.In the DTH method, there is no need to check equilibrium conditions time to time by opening and closing the chamber. In this case, weight of the sample needs to be taken after predetermined equilibrium time of 30 min (i.e., at each relative humidity). Metal cells, used at higher temperature, could be susceptible to corrosion [24, 57]. Replacing metal cells with glass could be a favourable choice to overcome these issues, but it limits the isotherm measurement at lower temperatures [58–61]. In conventional method, handling of 9 to 10 cells for more than 4 weeks needs lots of handling time, whereas in the case of DTH chamber, minimal handling of the samples is required. In addition, lots of space is required for handling 9 to 10 jars in the case of conventional method. In the case of the DTH method, the same sample could be used for measuring water activity within the complete range of 0.05 to 0.98 relative humidity.


## 3.4. Water Adsorption Isotherm

Figure5 show the measured adsorption isotherms of cellulose, lignin, and hemicellulase using DTH chamber and predicted model by GAB equation at different temperatures (10, 30, 50, 70, and 90°C). Isotherms showed sigmoid shape, as observed and reported in the literature for foods [13, 38, 39, 52, 62, 63]. In cases of lignin and hemicellulase, a sharp increase was observed after water activity 0.8, indicating more swelling with the adsorption of water as compared to the cellulose. These isotherms shifted down as a function of increasing temperature from 10 to 90°C. This was due to the increase of escaping tendency of water molecule at higher temperature [62]. Kapsalis [64] pointed that temperature affects the mobility of water molecules and enhanced dynamic equilibrium between water vapor and adsorbed phases. Similar observations were also stated for starchy foods [27, 65, 66]. Literature isotherms were mainly reported within 20-60°C; however, the DTH chamber method can be used to measure isotherm up to 100°C as well as chilled conditions up to -15°C. This could be one of the major advantage of the proposed DTH method.Figure 5
Adsorption isotherms of cellulose, lignin, and hemicellulase at temperature from 10 to 90°C.The measured absorption isotherm data of the three samples were fitted linearly with the BET model (Equation (2)) up to water activity 0.4, and the regression coefficients (R2) were varied from 0.97 to 0.99. The model parameters are shown in Table 1. The BET monolayer values of Mb exhibited a decreasing trend with increasing temperature for all samples (i.e., R2 0.920, 0.882, and 0.961 for cellulose, lignin, and hemicellulase, respectively) (Figures 6(a)–6(c)). The decrease in Mb could be due to the chemical and physical changes induced by elevated temperature [67]. Similar findings were also reported for rice, barley malt, cookies, and crackers [27, 28, 32]. The prediction of Mb values is crucial since deterioration of foods is minimal at Mb (i.e., strongly bound water cannot be involved in any deteriorative reaction either as solvent or as one of the substrates) [68]. The BET monolayer is an effective method that estimates the amount of bound water to specific polar sites in dehydrated food systems.Figure 6
BET ((a) cellulose, (b) lignin, and (c) hemicellulase) and GAB ((d) cellulose, (e) lignin, and (f) hemicellulase) monolayer values as a function of temperature.
(a)(b)(c)(d)(e)(f)At 10°C,B values were 120.7, 196.1, and 9.7 J/g, respectively, in the cases of cellulose, lignin, and hemicellulase (Table 1). The B values were observed as 502.8 J/g (22°C) for the corn flour [69], 101.5 and 5.7 J/g for blueberries in the case of desorption and adsorption isotherms at 40°C, respectively [70], 7.4 J/g in the desorption isotherm and 9.2 J/g in the adsorption isotherm at 30°C for dried potato [31], and 2.9 J/g at 45°C for yams [34]. The heat of adsorption (i.e., B) showed a decreasing trend as a function of increasing temperature. The values of B were plotted as Arrhenius equation as a function of 1/T (Figures 7(a)–7(c)).Figure 7
BET modelB values ((a) cellulose, (b) lignin, and (c) hemicellulase), GAB model C values ((d) cellulose, (e) lignin, and (f) hemicellulase), and K values ((g) cellulose, (h) lignin, and (i) hemicellulase) as a function of temperature.
(a)(b)(c)(d)(e)(f)(g)(h)(i)The nonlinear regression was implemented for the GAB model for the whole range of water activity (i.e., 0.05 to 0.95) with a regression coefficient (R2) varied from 0.85 to 0.99 (Table 1). The Mg values from the GAB model decreased with the increase of temperature, and it was correlated linearly with temperature (i.e., R2 of 0.943, 0.938, and 0.938 for cellulose, lignin, and hemicellulase, respectively) (Figures 6(d)–6(f)). The GAB model was used to predict sorption isotherms of many food products [41, 71, 72], vegetables like dried-onions and green beans [40], and fruit like apple, blackcurrant, sour cherries, apricots, and coffee fruit [73, 74].lnC value was plotted as a function of inverse temperature (1/T), and regression coefficient showed more than 0.9 (Figures 7(d)–7(f)). However, regression coefficients of lnK versus 1/T plots showed lower than 0.6, in the case of cellulose and lignin (Figures 7(g)–7(i)). Chirife [75] and Rahman [8] also pointed that K values should be less than unity and less affected by temperature.


## 3.5. Isosteric Heat of Adsorption

Equation (4) was used to calculate the isosteric heat of adsorption, and it decreased with the increase of moisture (Figure 8). This behaviour was also observed in other studies for quinoa, dried fruit, cassava, orange juice powder, and jasmine rice crackers [62, 66, 76–79]. A steeped increase in heat of sorption was observed below moisture 4.0 to 10.0 g/100 g sample depending on the sample. This was because water binding energy increased at lower water content [79]. Similar justification was also proposed by other researches [65, 67, 80, 81]. Therefore, removal of bound water from the surface can be tougher [76].Figure 8
Isosteric heat of adsorption as a function of moisture content ((a) cellulose, (b) lignin, and (c) hemicellulase).
(a)(b)(c)


## 4. Conclusion

The DTH chamber method showed several advantages over conventional isopiestic method. It showed high reproducibility (i.e., 0.0074 to 7.6%) as compared to the conventional isopiestic method (i.e., 0.75 to 21%) at different equilibrium relative humidity. In addition, DTH chamber method can be used to achieve quick equilibration time (i.e., 30 min); temperature and relative humidity could be selected at any point within the relative humidity 0 to 98% and temperature from -15 to 100°C, respectively. The adsorption isotherm of cellulose, lignin, and hemicellulase was measured within the temperature of 10-90°C and relative humidity from 5 to 95%. The adsorption isotherm was modelled by BET and GAB models, and these model parameters were correlated with the temperature. At 10°C, BET monolayer values were 6.37, 7.28, and 3.98 g/100 ds, respectively, for cellulose, lignin, and hemicellulase.



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*Source: 1236427-2021-12-30.xml*