a. statistical data at 2008; b. statistical data at 2007; c. n.a. stands for data not applicable
Summary of the general statistic information and the periods with data available for analysis
Open access peer-reviewed chapter
By Mang Lin, Iat-Neng Chan, Chuen-Yu Chan, Xue-Mei Wang and Han-Ying Dong
Submitted: October 24th 2010Reviewed: April 22nd 2011Published: September 26th 2011
The Pearl River Delta (PRD) in Southern China is one of the most developed regions in China. Administratively, the delta region is constituted by nine cities in Guangdong Province, and the Special Administrative Regions of Hong Kong and Macao. The PRD has developed into a manufacturing center of the world since the onset of China’s economic reform in the late 1970‘s. The important role of this region in China is highlighted by the high percentage contribution of gross domestic product (GDP) of Guangdong Province, which is mostly contributed by the PRD cities in the mainland, to that of the nation (>10%, National Bureau of Statistics China, 2009).
As an important manufacturing center and city cluster, the PRD region is inevitably affected by severe air pollution problems, which attract much public attention. In response to this situation, a regional air quality monitoring network compositing of 16 automatic stations has been established by the joint effort from Guangdong and Hong Kong governments since late 2005 with an aim to examine the air pollution problem of the region (GDEPMC & HKEPD, 2008). A series of large scale research programs including comprehensive aircraft and ground-base measurements and modeling exercises have been conducted by the scientific community to better characterize and analyse the problem and to find scientific evidence for formulating possible control strategies (e.g. the Program of Regional Integrated Experiments on Air Quality over the PRD of China-PRIDE-PRD in 2004 and 2006) (Zhang et al., 2008; Hua et al., 2008).
Fig. 1 depicts the land use change of the PRD from 1992 to 2004. The major urban areas were mainly found in the capital Guangzhou and the former British colony Hong Kong in the early 1990’s. However, in the 21st century, almost the whole PRD region was characterized by urban areas. This dramatic urban expansion was found to be one of the most key factors affecting the air quality and climate of the region (Wang et al., 2007; Kaufmann et al., 2007). Furthermore, the steady increasing trends of GDP and electricity consumption also highlight the tremendous progress of urbanization and industrialization of this region(Fig. 2). Concurrent atmospheric composition changes and air quality degradation have been observed by space-borne satellite (e.g., Richter et al., 2005; Van der A et al., 2006; Ghude et al., 2009) and limited long-term ground-based measurements. Chan et al. (2004) first deduced that the regional background ozone (O3) concentration in south China including the PRD region had been increased at a rate of 1.5% per year from 1984 to 1999 based on the urban measurements in Hong Kong. This finding was recently proven by Wang et al. (2009) using the data recorded from a background station in Hong Kong during the period 1994 to 2007. Besides, the metropolitan Guangzhou was also inevitably suffered from the air quality and visibility degradation during recent half century (Deng et al., 2008).
The China‘s “12th five-year’s plan” intends the PRD to transform its labor intensive and resource consuming light industry to heavy industry, telecom, equipment manufacture, auto and petrochemical industries for examples. With such a strategy, the traditional industry and enterprises are forced to move out from this region. Moreover, “cleaner” fuels such as liquefied petroleum gas (LPG) and low sulfur gasoline have been promoted by the government. Such massive changes of industry structure and prevalent fuel are anticipated to have strong effects on air quality. For instance, Tang et al. (2008) reported that there have been around 1.5 times increases in propane concentration in Guangzhou due to the introduction of LPG to the city in 2003. This pilot study highlights the scientific importance of clear understanding of the emerging air pollution issues along with these economic and industrial changes.
The objective of this chapter is to unveil the long-term air pollution changes in three typical commercial and industrial cities of the PRD region, Hong Kong, Macao and Foshan. The possible impacts of these changes on the atmospheric environment and their implications on the regional and urban air quality control strategy will be discussed. These cities are selected simply because they are the cities that we have accessible data. Hong Kong and Macao are located at the southern part of the PRD (Fig. 1). With the second-largest stock market in Asia, Hong Kong is well-known as an international financial center, while Macao is famous as a gambling city with flourishing tourism. On the other hand, Foshan is located at the central-western of the region, where urbanization process is most rapid (Fig. 1). This city is highly industrialized as reflected by its high industrial production value compared with those of Hong Kong and Macao (Table 1). The city is especially famous for ceramic industry, which produced approximately one fourth of the world’s ceramic products in 2007 (Peng 2007; Yin 2008). A statistical summary on the general information of these three cities and data available periods are shown in Table 1.
Fig. 3 and Fig. 4 summarize the mean concentrations of major air pollutants and the occurrence of episode days in Hong Kong, Macao and Foshan. As expected, the highest SO2 and PM10 concentrations were found in the industrial city Foshan due to the high SO2 and PM10 emissions from industrial activities. Note that the average SO2 concentration (60 μg m-3) reached the National Ambient Air Quality Standard (Level II) (GB3095-1996) (NAAQS II) of 60 μg m-3 (monthly mean). In fact, more than 50% of the days during the period 2001-2007 in Foshan had daily SO2 concentrations exceeding the NAAQS I of 50 μg m-3 (Table 2 and Fig. 4). Besides, the high percentages of PM10 episode days in Foshan highlight the severe
|Populationa||7.0 million||0.5 million||5.7 million|
|Areaa||1100 km2||21 km2||3800 km2|
|Vehicle numbera||0.70 million||0.18 million||0.60 million|
|Value of industrial productionb||160 billion (HKD)||16 billion (MOP)||940 billion (CNY)|
particle pollution at this industrial region. Hong Kong and Macao are both commercial cities with limited manufacturing industries. The SO2, PM10 and O3 concentrations of Macao were slightly higher, which could be attributed to the fact that Macao is located at the southeast of Hong Kong (Fig. 1). The prevailing northeasterly wind from September to April will carry aged and polluted air from Hong Kong and other PRD cities like Shenzhen and Dongguan to Macao to deteriorate air quality.
The average NO2 concentration was highest in Hong Kong and lowest in Foshan. This result is reasonable as Hong Kong is a commercial city with dense traffic (Table 1), which results in the elevated NOx emission and ambient NO2 concentration. However, it is noted particularly that the average NO2 concentration of Foshan during the period of 2006-2008 (60 μg m-3, not shown) was higher than that in Hong Kong and Macao, which suggested that the remarkable increases of vehicle number and vehicular emission in Foshan was becoming more important (Wan et al., 2011). Moreover, although the number of episode day with daily NO2 concentration larger than 80 μg m-3 (NAAQS I & II) in Foshan was close to that in Macao (~7.3%), the frequency of daily NO2 concentration exceeding 120 μg m-3 (NAAQS III) in Foshan was significantly higher than that in Macao (Fig. 3). This fact emphasizes the needs of implementation of stricter NO2 control measures in Foshan.
|Level I||Level II||Level III|
|SO2 (Daily Mean)||50||150||250|
|NO2 (Daily Mean)||80||80||120|
|O3 (Hourly Mean)||120||160||200|
|PM10 (Daily Mean)||50||150||250|
Ozone concentrations in Hong Kong and Macao both showed substantial increases with rates of 1.00 (R2=0.752) and 1.06 (R2=0.324) μg m-3 per year respectively (Fig. 5). The observed increasing trends are mostly caused by the regional increases in surface O3 concentrations due to transport of its precursors from south China and East Asia as the urban area of Hong Kong is shown to be a net sink of inflowing O3 due to the titration effect of nitrogen monoxide freshly emitted from traffic (Chan et al. 2004; Wang et al. 2009). NO2 concentration in Macao showed a smoothly increasing trend with a rate of 1.26 μg m-3 per year (R2=0.712). We believe that this change is probably accounted by the simultaneous increasing trend of vehicle number in Macao, which increased from 0.11 million in 2000 to 0.18 million in 2007 (Macao Statistics and Census Service,
Although long-term O3 data were not available in Foshan, NO2 concentration showed sharp increases from 18 μg m-3 in mid 2005 to 80 μg m-3 in late 2006 contradicting to the general decreases before 2005 (Fig. 5). This increasing rate reached 440% although NO2 decreased to lower levels from 2007 to 2008. The overall increasing rate during 2001-2008 was 6.34 μg m-3 per year (R2=0.496). The continuous increases in coal burning and road traffic, as well as lack of an efficient NO2 control strategy, led to the remarkable increases of NO2 level. More detailed discussions can be found in Wan et al (2011).
In Macau, PM10 concentrations showed a steady increasing trend with a rate of 2.39 μg m-3 per year (R2=0.716, Fig. 6). As high portion of organic carbon, which is one of the important species in particle primarily emitted by automobile in urban area, was found in PM10 in Macao (Wu et al., 2003), the increases of PM10 concentration were probably attributed to the increases of vehicle emission as mentioned above. Apart from the local emission, the airborne particulate matter in Macao was also influenced by transported secondary aerosols of regional scale (Wu et al., 2002, 2003). On the contrary, PM10 concentrations in Foshan displayed a steady decreasing trend with an overall rate of 3.47 μg m-3 per year in 2001-2008, which was believed to be due to continuous implementation of stricter emission control measures on various industrial sources. For instance, many high emitting factories including cement plants and small-scale ceramic plants were forced to close down by the city government in the past decades (Wan et al., 2011).
The SO2 concentrations in Hong Kong showed a growth rate of 0.28 μg m-3 per year in the period of 1984-2008 (Fig. 6). Specifically, the decreases from 1993 were due to the effective banns of high-sulfur fuel usage and reduction of power plant emissions in Hong Kong (HKEPD,
Given that O3 is a vital atmospheric oxidant and NO2 is one of the most important O3 precursors, the remarkable increases of O3 in Hong Kong and Macao as well as the tremendous augment of NO2 in Foshan highlight the enhancement of atmospheric oxidizing power in the PRD region. It is reasonable to hypothesize that such changes would exert impacts on atmospheric environmental quality and chemistry. In this section, we used visibility as a proxy of atmospheric environmental quality changes to investigate the impacts of air pollution changes on the atmospheric chemical processes. Following the definition of the Hong Kong Observatory, the observed visibility data were transformed to Reduced Visibility (RV) which is defined as the percentage of hours with visibility below 8 km, excluding the data of rainy days or those affected by fog or high relative humidity (≥95%) (Leung et al., 2007). With this definition, the resulted RV would better indicate the frequency of visibility degradation caused by elevated pollutant level in the atmosphere. As expected, the highest RV was found in Foshan while the lowest RV occurred in Hong Kong (Fig. 3).
Three multiple regression models and the partial correlations between RV and each air pollutant were calculated. The model results were subjected to the F-test and student t-test with a significant level p<0.05. After that, the air pollutants with significant partial correlation were kept at the model equations while others were removed from the equations (Table 3). Generally, visibility in Hong Kong is primarily influenced by concentration levels of O3, SO2 and NO2 in recent 16 years. Particularly, RV would increase 0.28%, 0.27% and 0.15% if concentrations of SO2, NO2 and O3 increase 1 μg m-3 respectively. In Macao, the RV was significantly affected by PM10 concentration with a value of increasing 0.33% of RV per
1 μg m-3 of PM10. Similar relationship exists in Foshan with a value of increasing 0.50% of RV per 1 μg m-3 of PM10. Besides, the RV in Foshan correlated with NO2 concentration with a value of increasing 0.14% of RV per 1 μg m-3 of NO2.
It is well-known that visibility impairment is always proportion to the loading of fine particles owing to the scattering capacity of aerosol. Besides, NO2 is another important species in the atmosphere which can degrade visibility due to its strong blue-light-absorbing capacity. Therefore, it is easy to explain the correlation between RV and PM10 as well as NO2.
|Regression Model||Independent Variables||Equationa|
|1 (Hong Kong 1993 – 2008)||O3, SO2, NO2, PM10||[RV] = 0.28 [SO2] + 0.27 [NO2] + 0.15 [O3] – 15.80|
|2 (Macao 1999 - 2007)||O3, SO2, NO2, PM10||[RV] = 0.33 [PM10] – 5.70|
|3 (Foshan 2001 - 2008)||SO2, NO2, PM10||[RV] = 0.14 [NO2] + 0.50 [PM10] - 21.24|
However, the correlation between RV and SO2 as well as O3 can hardly be directly interpreted because both O3 and SO2 are rather weak in absorbing and scattering visible light, and they thus will not produce strong influence on visibility directly. In fact, this result highlights the changes of atmospheric chemistry due to the tremendous increases of O3 concentration in Hong Kong and Macao. In the enhanced O3 atmosphere, the increasing oxidation rate would transform SO2 to secondary fine sulfate particles more rapidly, which could effectively degrade visibility (Fig. 8, Meng et al. 1997, Shao et al. 2006). The chemical mechanism of S(IV) to S(VI) transformation has been extensively studied in literatures (e.g. Penkett et al, 1979; Stockwell and Calvert, 1983; Seinfeld and Pandis, 1997; Liang and Jacobson, 2000). The enhanced formation of secondary sulfate in the O3-rich atmosphere mentioned above actually agrees with the findings from a recent study, in which SO4 2- concentrations in East Asia were found to increase at a greater rate than SO2 emissions and SO2 concentrations because “East Asia is a less oxidant-limited area than other parts of the world” (Lu et al. 2010).
In addition, although long-term O3 data in Foshan were not available, the elevated level of NO2 concentration more or less highlights the enhancement of oxidizing power of atmosphere in this region as well. It is well known that O3 is generated from the photolysis of NO2 and reacts mainly with NO to regenerate NO2 quickly. If CO or VOCs are present, the simply photostationary state mentioned above is modified in a way that NO2 can be regenerated through the reaction between NO and HO2 (or RO2). Net formation of O3 occurs because the conversion of NO to NO2 is accomplished by the HO2 (or RO2) radical rather than by O3 itself. Therefore, the enhanced NO2 concentration in the atmosphere also reflects the presences of other secondary pollutants like fine particle which significantly contributes to visibility impairment. The significant correlations between RV and NO2 concentration in Hong Kong and Foshan thus underline the important role of NO2, or even secondary pollutants, play in visibility reduction. In Macao, RV did not correlate well with O3 and NO2 concentrations. However, the high portion of secondary aerosols in PM10 and steady increasing trends of O3 and NO2 also emphasize the vital role of high O3 levels play in photochemical formation of secondary pollutants such as sulfate, which would exert notable impacts on visibility, public health and climate.
Changes of major atmospheric compositions and air pollution levels due to the rapid economic and industrial development have been observed in the PRD region. The data such as those presented in this paper suggest that these long-term air pollution trends have vital implications on the formulation of regional air quality control strategies. Generally, the elevated concentration levels of NO2 and O3 in the three commercial and industrial cities highlight the enhancement of atmospheric oxidizing power in the PRD region, which may exert profound effects on atmospheric chemistry, public health as well as regional climate.
Specifically, both of SO2 and O3 concentrations in Hong Kong show significant increasing trends. Given that SO2 would be oxidized to secondary sulfate more easily in the O3 enhanced atmosphere, the simultaneously increasing O3 and SO2 are reasonably expected to trigger the formation of secondary sulfate and resulted in the pronounced visibility degradation. Wang et al. (2009) have suggested that short-term O3 control strategies should be aimed at O3 precursor sources in Hong Kong and the adjacent PRD while the long-term ones need to consider distant sources. Given that the increase of SO2 concentration was due to the enhanced local SO2 emissions of Hong Kong and Shenzhen (Chan and Yao, 2008) as well as elevated regional SO2 emissions in East Asia (Lu et al., 2010), similar strategy should be adopted for SO2 control.
In Macao, the increasing trends of secondary pollutants like O3 and NO2 highlight the influences of increasing O3 precursor emission in its upwind regions such as eastern PRD and the east Chinese coast. Therefore, the air pollution controls of Hong Kong, as well as other upwind regions are vital. Furthermore, the augment of NO2 concentration also implies that the local vehicular emission control of Macao should not be neglected. As PM10 in Macao was mainly affected by local vehicular emission and regional transport, its increasing trend also emphasized the importance of both local and regional controls.
On the other hand, decreasing trends of PM10 and SO2 were observed in Foshan. These are due to the efforts of more efficient control in industrial sectors. In a recent paper, Wan et al. (2011) emphasized that the implementation of stricter PM10 and SO2 control measures in industrial exhaust had resulted in reduced ambient air pollution level. However, this industrial city is still severely polluted compared to the commercial cities like Hong Kong and Macao due to its high coal burning and industrial emissions. Such fact suggested that the SO2 as well as particles emission control measures must be strengthened. In contrast, the surprising increases of NO2 concentration due to the continuous increasing in road traffic and lack of efficient NO
Overall, due to the rapid economical and industrial development, the nature of air pollution in the PRD region has been changing sharply. Essentially, the findings reported in this chapter indicated that the atmospheric oxidizing power in the PRD region has been continuously increasing. Even in the industrial city, which was more affected by primary pollutants like SO2, the vehicle emission and resulted photochemical pollution should be noticed. The enhancing atmospheric oxidizing power could change the atmospheric chemistry by triggering the secondary pollutant formation via increasing oxidation rate. The increasing secondary pollutants may exert a number of significant impacts on public health and regional climate. As most of secondary pollutants were related to transport of aged air mass, such findings emphasize the critical impacts of trans-boundary transportation and regional air pollutions. With an aim to control the secondary pollutants, cooperation with other provinces and even countries become more and more important. Besides, due to the enhanced atmospheric oxidation capacities, primary pollutants like SO2 and some of volatile organic compounds will be transformed to secondary fine particles more efficiently, and therefore, stricter implementation of local primary pollutant control was also necessary. In summary, in order to efficiently improve the regional air quality in the PRD region, local and regional efforts on air pollution control are both required.
We thank Hong Kong Observatory, Hong Kong Environmental Protection Department, Meteorological and Geophysical Bureau of Macao, Environmental Protection Bureau of Foshan and Meteorological Bureau of Foshan for providing the data. This study was supported by a key project of the Natural Science Foundation of Guangdong Province, China (No. 825102501000002), the National Natural Science Foundation of China (No. 40875075), a joint fund of the National Natural Science Foundation of China and Natural Science Foundation of Guangdong Province, China (No. U0833001), and Rosa Luxemburg Foundation.
© 2011 The Author(s). Licensee IntechOpen. This chapter is distributed under the terms of the Creative Commons Attribution-NonCommercial-ShareAlike-3.0 License, which permits use, distribution and reproduction for non-commercial purposes, provided the original is properly cited and derivative works building on this content are distributed under the same license.
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