Hengli Zhang,
Chunjiang Yu and
Zhongyang Luo*
State Key Laboratory of Clean Energy Utilization, Zhejiang University, Hangzhou 310027, China. E-mail: zyluo@zju.edu.cn
First published on 4th June 2020
Biomass direct combustion for power generation is used widely in China. The circulating fluidized bed (CFB) boiler has a lower combustion temperature and a wide fuel adaptability, which is suitable for biomass combustion. The dynamic process of ash deposition in a CFB boiler is different from that in a grate furnace because it has a lower combustion temperature and a higher flue gas flow. In this work, the dynamic process of ash deposition on a superheater in a 50 MW biomass CFB boiler was studied by a deposit sampling system at different deposition times. Multiple deposit samples with different deposition times were observed and analysed to obtain an indication of deposit changes with time to understand the entire deposit build-up process. This study differs from previous studies on ash deposition and the deposition process could be identified as occurring in three stages: (1) initial deposition, (2) KCI deposition and (3) capturing of fly ash particles. In the first stage, the temperature gradient near the superheater led to the deposition of fine particles smaller than 2 μm from the flue gas through thermophoretic deposition. In the second stage, the surface became rough, which led to an increase in gas-phase KCl condensation rate and the formation of a dense and continuous KCl layer after the initial deposition. In the third stage, KCI provided a sticky layer to capture larger particles in the flue gas. Thus, more large particles were captured in the flue gas and the KCl continued to condense. As the surface temperature was increased, the condensation rate of the gas-phase KCl decreased. The higher surface temperature enhanced KCI melting and captured more fly ash particles, which led to a rapid build-up of ash deposits on the heating surfaces.
Elements that are deposited on the superheater in biomass-fired boilers include mainly K, Ca, Mg, Si, S and Cl, whereas Na, Al, P occur as minor elements.18 K, Cl and S are the dominant elements during deposition. Elemental K in biomass fuel is released to the gas phase as KCl, KOH and K2SO4 during combustion.7,14,17,19 KCl and K2SO4 deposit on the superheater mainly through condensation and thermophoresis, and the innermost deposition layer is formed.3,20–24 Sticky potassium salts with a low melting point capture fly ash particles to form the outer deposit layer.8 Nevertheless, most previous research on biomass ash deposition was based mainly on an analysis of mature deposits that are derived directly from heating surfaces during boiler maintenance. These mature deposits have gone through a long-term in situ reaction, which differs from their initial formation state. Hence, it is difficult to stratify and analyse deposit changes with time.
The literature indicates that ash deposition probes with temperature control have been used to study the deposit composition, deposit formation rate and corrosion that is caused by alkali deposits. To date, the influence of flue gas temperature, deposition exposure time and alkali content in fuel on the deposit formation rate has been investigated.25–28 Deposit shedding events were also considered during long-term experiments.25,28,29 The deposit composition of ash deposition probes was analysed by X-ray diffractometry (XRD) and scanning electron microscopy (SEM).30 The deposit samples were divided into an inner and outer layer. Chlorine- or sulphur-rich alkali particles were found in the early deposition stage, then larger particles from fly ash began to deposit through inertial impact.20,31,32 Corrosion caused by alkali metal deposits was investigated at different flue gas temperatures33 and probe surface temperatures on three types of superheater steels.34
Different from the literature mentioned above, in this work, we focused only on the dynamic deposition process. The deposit build-up process on an ash deposition probe at different deposition times was investigated based on a full-scale 50 MW biomass CFB boiler. The deposit samples with different deposition times, which indicate different intermediate deposition states, can be analysed directly to obtain more information on the deposition process. However, previous research on ash sampling probe experiments analysed only the inner- and outer-layer samples.30–32
Proximate analysis | Moisture (%, ar) | 44.28 |
Ash (%, dry) | 6.97 | |
Volatile (%, dry) | 71.74 | |
Fixed carbon (%, dry) | 21.28 | |
Ultimate analysis | C (%, dry) | 40.77 |
H (%, dry) | 5.38 | |
N (%, dry) | 0.35 | |
S (%, dry) | 0.33 | |
O (%, dry) | 46.19 | |
Lower heating value | Q (MJ kg−1, ar) | 7.63 |
Inorganic elements | Ca (%, dry) | 2.34 |
K (%, dry) | 0.69 | |
Na (%, dry) | 0.16 | |
Cl (%, dry) | 0.86 |
As shown in Table 2, the elemental composition of the fly ash was analysed from the energy spectrum. Combined with the X-ray diffraction (XRD) analysis in Fig. 3, the main components of the fly ash were identified as CaCO3, SiO2 and KCl. Because of the low content of other components, no obvious diffraction peak was found in the XRD diagram.
Na | Mg | Al | Si | P | S | Cl | K | Ca | Fe |
---|---|---|---|---|---|---|---|---|---|
1.4 | 2.2 | 5.7 | 9.9 | 0.9 | 0.6 | 5.2 | 5.4 | 17.3 | 3.9 |
A sketch of the ash deposit probe is shown in Fig. 4. The system includes a fan, electric control valve, digital display controller, thermocouple and stainless-steel sampling probe. The probe was 2.5 m long with a 38 mm outer diameter. A thin stainless-steel ring was attached to the probe to sample the ash deposit. To simulate the high-temperature superheater condition, the probe was cooled by air to maintain a stable sampling ring surface temperature. Because the main steam temperature of the boiler and flue gas temperature in the high temperature superheater region was 540 °C and 720 °C, respectively, the estimated surface temperature of the high-temperature superheater was 600 °C. Hence, the sampling ring surface temperature was set to 600 °C.
The sampling lasted 1, 2, 5, 15, 24 and 48 h for each test. After deposits sampling, there was no need to take the deposits off the ring. The deposit samples were analysed directly, together with the sampling ring. The ash deposit micromorphology was observed by scanning electron microscope (SEM). The microstructure elemental content was measured by energy dispersive spectrometer (EDS).
Element | Na | Mg | Al | Si | P | S | Cl | K | Ca |
---|---|---|---|---|---|---|---|---|---|
1 h | 1.61 | 6.9 | 5.6 | 8.7 | 3.0 | 6.3 | 8.6 | 3.8 | 55.5 |
2 h S1 | 1.6 | 0.9 | 0.8 | 1.0 | 0.3 | 0.4 | 41.4 | 50.2 | 3.4 |
2 h S2 | 2.2 | 8.2 | 6.5 | 8.7 | 4.4 | 8.1 | 7.7 | 4.6 | 49.6 |
5 h | 2.2 | 0.7 | 0.4 | 0.6 | 0.1 | 0.2 | 46.8 | 47.9 | 1.2 |
15 h S1 | 1.5 | 1.2 | 0.4 | 0.7 | 0.3 | 0.1 | 45.4 | 48.3 | 2.2 |
15 h S2 | 2.4 | 0.5 | 0.4 | 0.4 | 0.5 | 0.1 | 46.1 | 48.4 | 1.3 |
15 h S3 | 2.2 | 4.3 | 4.9 | 11.3 | 2.4 | 4.0 | 12.3 | 12.1 | 46.5 |
1 day | 3.0 | 3.0 | 4.1 | 6.7 | 2.4 | 6.0 | 23.2 | 26.1 | 25.5 |
2 days | 1.7 | 3.0 | 5.9 | 9.9 | 2.5 | 6.3 | 12.7 | 14.1 | 43.9 |
Since some deposit layers are very thin, a large amount of Fe, Cr, Ni from sampling ring appears in EDS measurement results. Consequently, the EDS results were calibrated by removing C, O, Fe, Cr and Ni content, and the datas were normalized.
According to deposition theories, fine particles deposit on the probe mainly through thermophoretic deposition. In a region with a large temperature gradient, fine particles are affected by the thermophoretic force that pushes the particles from the high-to the low-temperature zone. To verify the source of these 2 μm particles, particles less than 2 μm in the fly ash were chosen for tests by using EDS. Their average elemental content is listed in Table 4. The elemental composition is similar to that of the 1 h deposition sample, which indicates that the initial deposition layer may originate directly from the thermophoretic deposition of fine particles in the fly ash. This initial layer is different from previous research on the elemental composition and deposition mechanism.
Na | Mg | Al | Si | P | S | Cl | K | Ca |
---|---|---|---|---|---|---|---|---|
1.6 | 8.2 | 5.7 | 9.8 | 4.7 | 4.7 | 7.0 | 4.0 | 54.3 |
It has been reported in literature that the initial or innermost deposition layer is rich in K, Cl and S. Jensen found that pure KCl and K2SO4 form an initial deposition layer through condensation; however, FexOy was derived from superheater surface corrosion.21 Lianming Li suggested that the innermost layer composition was KCl, K2SO4, SiO2, K2Ca(SO4)2 and Fe2O3.3 KCl originated from condensation and reacted slowly with SO2 in flue gas to form K2SO4, whereas the reaction of K2SO4 and CaSO4 generated K2Ca(SO4)2. All results mentioned above are somewhat different from 1 h deposits in measurements in the 50 MW biomass CFB boiler. In this case, 1 h ash deposits on the sampling probe is a short deposition process before KCl condensation. This layer is so thin that it cannot be observed in mature deposits. KCl condensation also occurred in this study, which will be discussed in the next section. Fine-particle deposition also existed in Skrifvars's deposition probe experiment.31 The results suggest that submicron particles also deposited on the rear of the probe, including Ca, Mg, Na, K, S and Cl. These deposits could help form a thin initial layer. Inertial impaction rarely occurred on the rear of the probe. Except for potassium salt condensation, other submicron particles in flue gas may deposit through thermophoresis in the early stage of deposition. It is remarkable that the deposition of fine particles in Skrifvars's report differs from this study. The K, Cl and S are much lower in the 1 h deposits, most likely because the low combustion temperature and high Cl content of fuel in this study prevent K2SO4 release into the gas phase. Consequently, no significant S content (K2SO4) was found in all stages of deposition in this study. Cl and K increased rapidly in deposits of 2, 5 and 15 h.
KCl has a relatively low melting temperature and presents in the gas phase after combustion. The initial deposit layer after 1 h makes the surface rough, which may increase the KCl condensation speed.
A small tube furnace experiment (Fig. 6) was conducted to investigate the KCl condensation on surfaces of different roughness. The furnace was heated to 800 °C (higher than the melting point of KCl) to accelerate KCl migration to the gas phase. A water-cooled metal tube whose surface temperature was kept at 600 °C was placed inside the tube furnace to collect KCl by condensation. KCl in the gas phase mixed with carrier gas and condensed on a water-cooled metal tube. The deposition time was set as 1, 5, 10, 20 and 40 min. The deposited KCl was collected and weighed to obtain mass–change curves (Fig. 7). At the beginning of condensation, KCl condensed much faster on the rough surface than on the smooth surface. When the surface was covered with KCl, the condensation rates tended to be equal, which explains why the KCl content is low in the initial deposits and increases rapidly in the following hours.
The deposition process in the second stage of KCI condensation can be described as follows: the sampling ring surface becomes rough after 1 h of deposition, which accelerates the KCI condensation rate in the gas phase, and allows KCl condensation to be the dominant deposition method in place of thermophoretic deposition. After 2 h, most part of area, such as Spot 1, was covered with the condensed KCl. Some part of the area, such as Spot 2, was not covered by the KCI layer. The deposit sample of 5 h had a thicker KCl layer than that at 2 h. The dominant KCl condensation lasted up to 15 h when the main part of the 15 h deposit sample remained as the KCl layer [Table 3 and Fig. 5(d)]. The EDS results show that smooth particles, such as Spot 2 in Fig. 5(d) are KCl, whereas flocculated particles, such as Spot 3 are mainly calcium-containing salts, which may originate from CaCO3 and Ca2SiO4 in the fly ash. It can be concluded that at this stage, the dominant deposition mechanism remains KCl gas-phase condensation. However, because of the existence of the sticky KCl layer, other ash particles in the fly ash were captured and settled on the existing deposition layer.
As an important factor for gas-phase KCl condensation and subsequent deposition growth, the temperature of the deposit surface was calculated. The convection heat transfer formula of the flue gas that swept across the deposit sampling ring is:
Re = V·d/ν | (1) |
Nu = C·Ren·Pr1/3 | (2) |
(3) |
The radiation heat transfer formula of the deposit can be expressed as:
(4) |
The sum of convection heat transfer and radiation heat transfer on the deposit surface was equal to the heat flow inside the deposit.
(5) |
Deposits of 2, 5 and 15 h consist mainly of KCl, thus k is approximately equal to the thermal conductivity of KCl. In longer deposition times, k is 0.57 w/m·K, which is approximate experimental measurement value of deposits sample derived from high-temperature superheater (measured by the thermal conductivity meter). Td = 620 °C was chosen as the initial value for iteration and the iteration value of Td can be calculated from eqn (1)–(5). When the difference between two iteration values of Td was less than 1 °C, the iteration stopped. The final surface temperature was obtained in Table 5.
1 h | 2 h | 5 h | 15 h | 1 day | 2 days | |
---|---|---|---|---|---|---|
Thickness (mm) | 0.06 | 0.11 | 0.27 | 0.50 | 1.0 | 1.6 |
During the first 15 h, deposition was dominated by KCl with a large thermal conductivity, which is relatively pure, dense and less porous. The surface temperature does not increase significantly. However, with the development of deposits, KCl captures other fly ash particles in the flue gas to form a porous structure, which lowers the thermal conductivity coefficient. Thus, the surface temperature increased rapidly to 633 °C in 1 day and 645 °C in 2 days. Because of the increase in surface temperature, the condensation rate of the gas-phase KCl decreased. The higher surface temperature leads to a higher tendency for KCI melting and therefore, an easier capture of fly ash particles. Thus, the 2 day deposit sample has a significantly lower content of KCl than that of the 1 day deposits, and a higher particle content with calcium salt from flue gas.
It has been reported that biomass ash deposition presents at least two layers visible to us.20,35 The inner layer formed by condensation of potassium salts, and the outer layer consisting of KCl and fly ash particles captured by sticky KCl. These results were similar to that of the conclusions drawn by Lianming Li3 and Yanqing Niu.35 They also found that the content of KCl was gradually decreased and the content of Ca, Si was increased from inner deposition layer to outer layer.
The initial deposits were caused by the thermophoretic deposition of fine particles from the flue gas, rather than the condensation of alkali species as reported previously. Then, gas-phase KCl condensation dominates the deposition and forms a dense KCl layer. Hence, KCl provides a sticky layer to capture larger particles in the flue gas. At this stage, an obvious trend of decrease in KCl and increase in calcium salts on the deposit surface resulted.
It is worth noticing that the elemental composition of the biomass fuel affects the ash deposition process significantly. The K content of biomass fuel is high in Chinese biomass power plants and the Cl content can vary greatly. Because the Cl content affects K migration during combustion, the deposition mechanism in the CFB boiler requires further research. Detailed research should be undertaken in a CFB boiler that burns high alkali and a low chlorine biomass fuel.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d0ra04370b |
This journal is © The Royal Society of Chemistry 2020 |