# Thermally Stimulated Depolarization Current from HCl-Doped Ice

Authors: Yoon Young Choi
Journal: Physics Research International
 (2011)

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## Abstract

Thermally stimulated depolarization current (TSDC) technique has been applied to investigate the dielectric properties of the HCl-doped ice. Three TSDC peaks were found from HCl-doped ice as well as ice of pure water. Among three peaks, theα and γ peaks are affected strongly by the concentrations of HCl. We found that the pH numbers are linearly proportioned to the ratios of the areas of the peaks. The relation between xα (the ratio of the area of α peak to the area of β peak) and  pHHCl,α was found to be pHHCl,α=7.77−2.86xα. This result suggests the possibility of the development of an apparatus to measure the pH number of acid contaminated water. The activation energies correspond to depolarization processes reflected in the α, β,  and γ peaks that were found to be 267±19 meV, 431±30 meV, and 635±44 meV, respectively.


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## Body

## 1. Introduction

Water is one of the most abundant substances in nature and essential to human’s life and industries. Polluted water will cause a serious threat of life in nature and industries. Despite stricter grovel environmental regulations, frequency of acid rain increases as industry grows, and impacts of acid rain in forest degradation, surface water contamination, and corrosion of building materials become a serious environmental problem. Therefore it is important to investigate dielectric property of acid polluted water [1].If a strong electric field is applied to a dielectric material, dipoles in the material will be arranged in a certain direction and the materialis polarized. If that material is cooled down while applying the electric field, the arranged dipoles are frozen in a metastable state and stay in ordered phase even if the electric field is removed. If the material is warmed up, the material is depolarized by thermal energy. During the depolarization process, current flows in the external circuit. This current is called the thermally stimulated depolarization current (TSDC) [2]. In case of a perfect crystal phase dielectric material it is hard to rearrange dipoles by an external electric field. It is known that in crystals with vacancies, interstitials or impurity ions of other types dipolar complexes are formed near impurities. Such dipolar defects are the origin of the TSDC. This TSDC method has been extensively used for many crystals that contain dipolar defects that can be oriented by an external electric field [3–8].In this paper we studied dielectric properties of HCl polluted ice using TSDC technique. We found that there are three peaks in TSDS measurement as a function of temperature which indicate existence of three metastable sites of dipoles in ice. The area of the peaks is logarithmically proportional to concentration of HCl.The reported TSDC results show that it is very sensitive to the materials contained in water [9, 10]. Therefore, TSDC technique is also good for investigating the physical properties such as the trap density of water dipole in the electric field, the activation energy of the trapped water dipole, and the relation between TSDC peak area and the concentration of the HCl in the water. This technique can be applied to the development of the dosimeter for the various physical or chemical quantities. But this technique has no practical use because there are relative simple methods for similar measurements, and the TSDC method is relatively expensive and complex. Further study may enable this technique to be practical.


## 2. Experiment

HCl-doped water samples were prepared by diluting 10% HCl with deionized water to the target concentrations. To measure TSDC, a Pt parallel-plate capacitor was used in this experiment. The dimension of the parallel-plate was 10 mm × 10 mm, and the distance between two plates was 1 mm. The experimental apparatus (the capacitor and a liquid nitrogen tank) was shielded by an aluminum box to reduce electrical noise. This shielding also helps in keeping steady heating rate for each experiment. After filling the capacitor with the liquid sample at room temperature, the capacitor was cooled down to 220 K, and electric field was applied to the capacitor for 1 minute. Then the capacitor was immersed in liquid nitrogen to cool the sample down to liquid nitrogen temperature while the electric field was applied. The polling voltage is 1000 V which is equivalent to 1.0 MV/m electric field applied to the sample. During the polling treatment the current in the circuit was less than 0.1 nA.This means that the liquid sample was not electrically decomposed. After reaching the liquid nitrogen temperature, the two ends of the lead wire were connected to the Pt plates to discharge residue charge induced during the polling treatment. After discharging, the capacitor was taken out of liquid nitrogen tank, and TSDC was measured as a function of temperature using a current amplifier and a voltage amplifier connected to the A-D converter. The heating rate of the sample wasη=0.9759-0.0028T in K/sec units where T is the temperature of the sample in Kelvin degree.


## 3. Results and Analysis

It is known that ice has Ih structure at 1 atm and temperature 80 K–273 K, and ice of Ih structure has H–O bonding axes [11]. Water molecules in pure ice are tightly bound to each other to form crystal, and it is hard to polarize the molecules by the external electric field. However if there are broken bonds due to defects or impurities water molecules can be oriented along the external electric field. By cooling to much lower temperature this metastable ordered phase may be locked in. This is the origin of the TSDC peaks in the water ice.Figure1 shows TSDC graphs as a function of temperature for ice doped by the various concentrations of HCl. In this figure, the currents are normalized to compare the relative intensities of the peaks. In the case of pure water as well as HCl-doped water, three peaks appeared at 110 K, 130 K, and 160 K. The presence of three peaks means that there are three kinds of defects in the ice made of pure or HCl- doped water, or there are excited states for a dipole in the electric field. The TSDC from pure water shows that the β peak was strong and the α and γ peaks were relatively weak. Note the β peak of 1.0×10-3%  mole concentration is smaller than that of 2.5×10-5% mole concentration. This is because of the volume of the sample solutions. However, with an increasing concentration of HCl, the α and γ peaks became stronger, and no peak appeared except these three peaks.Figure 1
TSDC graphs from the ice doped with various concentrations of HCl. As increasing the concentration of HCl, theα and γ peaks become stronger and the β peak is affected weekly by the concentration of HCl. The strong currents for the concentrations 5.0×10-6% and  2.5×10-5%  at the temperature higher than 200 K are due to the space charges. For the concentration1.0×10-3%, the γ peaks are overlapped by the space charge current.On the other hand, the H+ and the Cl− ions can be strongly hydrated, with water dipoles arranged spherically around the ions. This hydration would form a new type of crystal, and it would make a new TSDC peak. However, as shown in this figure, a new TSDC peak was not found in the HCl-doped ice. Therefore it is concluded that the hydrations induced by the H+ or the Cl− ions do not make new type defect. As described above, the β peak of the ice made of pure water was the strongest. However, as the concentration of HCl increased, the α and γ peaks became stronger than the β peak. This occurrence of this phenomenon means that the dipoles inducing the β peak were more stable than those inducing the α and γ peaks. So to speak, the H+ or Cl− ions affect strongly on the densities of defects (broken H–O bondings) inducing the α and γ peaks but affect relatively weekly on the density of defect inducing the β peak.Various methods were tried to investigate the relationship between the pH number and TSDC peaks. Because the TSDC depends on the volume of the sample solution and the electrodes surrounding the sample solution, it is difficult to determine the relationship between the TSDC and the pH number. Figure1 shows that the areas of peaks were strongly affected on the concentration of HCl. Therefore, the areas of peaks were focused to find the relationship.In the HCl-doped water, some portion of the H+ or Cl− ions would contribute to make the defects, and some portion of H+ or Cl− ions would remain as the space charge. If we set n as the number of defectsin the iceper unit volume, C as the concentration of HCl, ΔC as the infinitesimal concentration of HCl contributes to make the infinitesimal defect Δn then, ΔC is proportion alto C andΔn, that is, ΔC=ACΔn. Here, A is a proportional constant. This equation can be expressed as following integral form. The negative sign means that increment of ΔC results in decrement of C,(1)∫C0C1CdC=-∫n0ndn.
The result of (1) is (2)ln⁡C=ln⁡C0-An0-An.The unit oflnC is the unit of pH number. This equation reveals that pH concentration is linearly proportional to the number of the defects. The equation (2) can be written as follows:(3)pH=B-An.
Here, B is a constant.To investigate the relationship between the concentration of HCl and TSDC peaks, the areas of peaks were estimated using curve fitting method. It was found that the number of the defects is not proportional to the intensity of the TSDC peak, but it is proportional to the area of the TSDC peak. With try and error, we found the consistent relationship. As explained above, theβ peak is relatively stable and affected weekly by HCl. Therefore the area of the β peak was chosen as a reference area. It is found that the ratios of the areas of the α peaks to the areas of the β peaks were linearly proportional to the pH concentration. Figure 2 shows the relationship between the pH concentrations of HCl and the ratios of the areas of the α peaks to the areas of the β peaks.Figure 2
The relationship between the pH concentrations of HCl-doped water and the ratio of areas (the area of theα peak divided by the area of the β peak). Although the data points are slightly scattered, the ratios of the peak areas are linearly proportional to the pH concentrations of HCl. The dashed line is the linear fit.If we letxα be the ratio of areas (the area of the α peak divided by the area of the β peak), the pH concentration estimated by the α peak is given by following equation:(4)pHHCl,α=7.77-2.86xα.This result is in good agreement with the theoretical equation shown in (3). It is expected that the similar analysis for the γ peaks would show similar result as (1). But as shown in Figure 1, the γ peak at the high concentration of HCl was too strong to estimate the area. However, because of the lack of the data points, the similar analysis was not tried for the γ peaks. However, if we measure the ratios of the areas of peaks, we can determine the pH numbers without considering the volume of samples. Therefore this result suggests the possibility of the development of the pH dosimeter using TSDC technique.Although it is known that there are at least three hydrogen bonds per water molecule [11], the number of TSDC peaks present depended on the experimental conditions. The structure of interfacial water differs from that of bulk water because of changes in the hydrogen bond network at a phase boundary, depending on the nature of the second phase. The number of TSDC peaks and the intensities of the individual peaks should be dependent on the electrode surrounding the water. Gun’ko and his coworker found only two TDSC peaks from water. They used water samples absorbed in a porous SiO2 absorbent tablet. In this study the water samples were placed in a Pt parallel-plate capacitor. There should be more defects on the surface of the water than in the bulk of the water. The physical properties of the surface are quite different from those of the bulk, and the physical properties of a water surface in contact with SiO2 should also be different from those of a water surface in contact with Pt. Therefore, the type of defects present at the interface between water and SiO2 may be different from those at the interface between water and Pt. The different interfaces may shift the peaks, the peak intensities, or the number of peaks. Gun’ko also indicated that the interaction of water with solid surfaces results in the displacement of peaks. Riehl  [11] found three strong peaks at 120 K, 130 K, and 171 K and a weak peak at 140 K. Although they did not indicate the type of material used for the electrode surrounding the ice made of pure water, their results were similar to these results. The difference between Bishop’s results and these results may have come from the different heating rate and the different materials used for the electrode. In this case, the water molecules were in contact with Pt plates. Therefore, it is to be expected that these TSDC results from water were different from other results.It is well known that the thermally stimulated current is given by a general equation [12], (5)I(T)=Aexp⁡[-EtkT-Bη∫T0Texp⁡(-EtkT)dT],
where parameters A and B are constant, Et is the activation energy, η is the heating rate, T0 is the initial temperature, and T will be T0+ηt. If T0≈T, (5) can be written as(6)ln⁡(I)=ln⁡(A)-EtkT.
The slope of the plot of ln(I) versus 1/T reveals the activation energy. This approximation can accompany some error. To check the error range due to this approximation, two slopes obtained using two theoretical curves plotted using (5) and (6) are compared. Figure 3 shows two semilogarithm graphs plotted using (5) and the graph plotted using (6).These plots  correspond to the α peak in Figure 1.Figure 3
Arrhenius plots against1000/T. Open circles denote the graph plotted using (5), and small closed circles denote the graph plotted using (6). The slopes of two graphs in the temperature region 85 K~100 K are almost same.In the temperature region 85 K~100 K, this figure reveals that the slope of the graph plotted using (5) is bigger by 0.2% than that of the graph plotted using (6). But the experimental error was found to be ~5%. Therefore the error occurred by the approximation can be ignored, and so (6) is a good approximation in the low temperature region of a peak. It is expected that the activation energy would change according to the concentration of HCl. However, the activation energy does not change. This means that the interaction between H+ or Cl- ion and water molecules is not strong enough to change the activation energy of the water dipole. The activation energies correspond to depolarization processes reflected in the α, β, and γ peaks in Figure 1 calculated using (6) which are 267±19meV, 431±30meV, and 635±44meV. Bishop and his coworkers reported that the activation energy of the peak appearing at 120 K is 250±20meV. This value is in good agreement with this result. Reports describing the activation energies of other peaks were not found. However, we think that these results are reasonable.


## 4. Conclusion

In summary, the dielectric properties of the HCl-doped ice have been investigated using TSDC technique. Three TSDC peaks were found that for the HCl-doped ice as well as the pure water ice. It is found H+ or Cl- ion does not make new type defect (broken hydrogen bond) in the ice. The α peak and the γ peak are affected strongly, but the β peak is affected weakly by the concentrations of HCl. The relation between xα (the ratio of the area of the α peak to the area of the β peak) and the pH concentration of HCl-doped water was found to be pHHCl,α=7.77-2.86Xα. The activation energies correspond to depolarization processes reflected in the α, β and γ peaks which are found to be 267 ± 19 meV, 431±30meV and 635 ± 44 meV.



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*Source: 930406-2011-08-08.xml*