Report Released on Investigation of Acid Rain in TaiwanEnvironmental Information
「Report Released on Investigation of Acid Rain in TaiwanEnvironmental Information」於資料集「Environmental Policy Monthly」由單位「行政院環境保護署」的楊先生所提供，聯繫電話是(02)23117722#2217,(02)23117722#2216，最近更新時間為：2022-01-15 01:13:03。 欄位編號的內容是416 ， 欄位標題的內容是Report Released on Investigation of Acid Rain in Taiwan ， 欄位摘要的內容是The results of an investigation into acid rain in the Taiwan region were recently released. According to the report average rain water pH value is between 4.8 and 5.1, revealing that Taiwan's acid rain problem is not severe in comparison with neighboring countries. As far as the pollutants that contribute to acid rain, atmospheric sulfate concentrations appear to be decreasing yearly while nitrate concentrations are holding steady.
To better understand the state of acid rain in Taiwan, in 1990 the EPA brought together a number of domestic universities to research the current status, contributors and environmental impacts of acid rain in the Taiwan region. After eight years of work, an exhaustive report on this investigation has finally been released.
The EPA points out that CO2 stored in the atmosphere (about 330ppm) reacts with rain water to form carbonic acid naturally resulting in a low acidity that is translated as a pH of around 5.6. However, formic acid, acetic acid, and other organic acids produced in nature also lower the pH values in rain, so in recent years many advanced nations and scientists have used pH values below 5.0 to define acid rain which has been polluted by human activity. In fact, judgements about acid rain are not based solely on pH values. There are numerous other factors such as electrical conductivity, anions and cations, which influence the acid-base levels of rain water.
To gain command of the acid rain situation in Taiwan, an acid rain monitoring network has been established. The network generally uses the same sampling process and analysis methods as the U.S. EPA's National Atmospheric Deposition Program (NADP). There are a total of 12 stations set up in Taipei, Kuishan, Chungli, the Taichung harbor, and other locations throughout the island.
The data accumulated over the years by these stations reveals that average pH values in Taiwan range from 4.8 to 5.1. Compared with the average pH values of neighboring countries like Hong Kong (4.2) and Japan (4.8), and with other advanced countries like the U.S. (4.2) and Europe (4.1), Taiwan's acid rain problem seems less severe. Looking at metropolitan areas, the average pH levels at the Taipei and Chungli monitoring stations have risen from 4.27 in 1991 to 4.51 in 1998, a 42% improvement. The Kaohsiung station recorded an improvement of 24%, from 4.49 to 4.61. I-lan improved 70%, from 4.35 to 4.88. Only Taichung showed increasing acidity, with pH values falling from 4.7 to 4.3. The average pH values at non-urban monitoring stations in Kenting, Daimali, Jia-i, Penghu and Alishan were all above 5.2, showing no signs of acidification.
The two major contributors to the acidification of rain are sulfates and nitrates. Over the last eight years the average concentration of sulfates in rainfall have decreased from 3.5ppm in 1991 to 2.8ppm in 1998, an improvement of 20%. The concentration of nitrates have remained the same at 1.3ppm. As far as cations, the report shows that there is no obvious increase in ammonium ions (from the application of ammonia fertilizers) and calcium ions (from natural settling dust or limestone formations). From this the report infers that the reason behind the improvement in acid rain lies in the reduction of sulfate concentrations.
For this reason the EPA expressed that the decrease in sulfate concentrations is directly related to EPA policies to encourage the use of low-sulfur fuels over the years. Sulfur content in fuels first dropped from 2% in 1986 to 1% in 1993, and then starting in 1996 the EPA promulgated successive regulations reducing sulfur content in fuels to 0.5% in all counties and cities. Sulfur content in high-grade diesel fuels first dropped from 0.3% to 0.15%, and then in 1998 regulations were announced further lowering sulfur content to 0.05%. Since the implementation of these measures the air quality values at monitoring stations have significantly improved. Compared with ten years ago SO2 levels have improved 80%.
Beginning July 1998, the EPA also began collecting seasonal air pollution control fees for SOx and NOx based on pollutant type and actual emissions quantities. The fees are aimed to encourage industries to move independently to install pollution control equipment. Other measures, such as prohibiting the sale and use of high sulfur fuels like petroleum coke and raw coal without proper authorization and the collection of a pollution control fee of 1,000 NTD per/ton for the use of such fuels, have resulted in a large decrease in the number of factories using high-sulfur fuels. This has also contributed to the improvement of acid rain.
Based on a Central University professor’s research on SOx, almost 25% of SOx in Taiwan’s ambient air drifts in from outside Taiwan's boundaries. The other 75% comes from internal pollution sources. Taiwan sits on the edge of the Asian continent and the Pacific Ocean, and is downwind of many continental pollution sources. It is clear that over the years, the amount of SOx blown to Taiwan from seasonal northeast winds has increased. Taiwan’s air quality, and hence the problem of acid rain, will continue to worsen as mainland China and other east Asian countries increase pollutant emissions. Due to the difficulties of cross boundary pollution control this issue is likely to become a thorn in the side of future efforts to deal with acid rain. ， 欄位全文的內容是The results of an investigation into acid rain in the Taiwan region were recently released. According to the report average rain water pH value is between 4.8 and 5.1, revealing that Taiwan's acid rain problem is not severe in comparison with neighboring countries. As far as the pollutants that contribute to acid rain, atmospheric sulfate concentrations appear to be decreasing yearly while nitrate concentrations are holding steady.
To better understand the state of acid rain in Taiwan, in 1990 the EPA brought together a number of domestic universities to research the current status, contributors and environmental impacts of acid rain in the Taiwan region. After eight years of work, an exhaustive report on this investigation has finally been released.
The EPA points out that CO2 stored in the atmosphere (about 330ppm) reacts with rain water to form carbonic acid naturally resulting in a low acidity that is translated as a pH of around 5.6. However, formic acid, acetic acid, and other organic acids produced in nature also lower the pH values in rain, so in recent years many advanced nations and scientists have used pH values below 5.0 to define acid rain which has been polluted by human activity. In fact, judgements about acid rain are not based solely on pH values. There are numerous other factors such as electrical conductivity, anions and cations, which influence the acid-base levels of rain water.
To gain command of the acid rain situation in Taiwan, an acid rain monitoring network has been established. The network generally uses the same sampling process and analysis methods as the U.S. EPA's National Atmospheric Deposition Program (NADP). There are a total of 12 stations set up in Taipei, Kuishan, Chungli, the Taichung harbor, and other locations throughout the island.
The data accumulated over the years by these stations reveals that average pH values in Taiwan range from 4.8 to 5.1. Compared with the average pH values of neighboring countries like Hong Kong (4.2) and Japan (4.8), and with other advanced countries like the U.S. (4.2) and Europe (4.1), Taiwan's acid rain problem seems less severe. Looking at metropolitan areas, the average pH levels at the Taipei and Chungli monitoring stations have risen from 4.27 in 1991 to 4.51 in 1998, a 42% improvement. The Kaohsiung station recorded an improvement of 24%, from 4.49 to 4.61. I-lan improved 70%, from 4.35 to 4.88. Only Taichung showed increasing acidity, with pH values falling from 4.7 to 4.3. The average pH values at non-urban monitoring stations in Kenting, Daimali, Jia-i, Penghu and Alishan were all above 5.2, showing no signs of acidification.
The two major contributors to the acidification of rain are sulfates and nitrates. Over the last eight years the average concentration of sulfates in rainfall have decreased from 3.5ppm in 1991 to 2.8ppm in 1998, an improvement of 20%. The concentration of nitrates have remained the same at 1.3ppm. As far as cations, the report shows that there is no obvious increase in ammonium ions (from the application of ammonia fertilizers) and calcium ions (from natural settling dust or limestone formations). From this the report infers that the reason behind the improvement in acid rain lies in the reduction of sulfate concentrations.
For this reason the EPA expressed that the decrease in sulfate concentrations is directly related to EPA policies to encourage the use of low-sulfur fuels over the years. Sulfur content in fuels first dropped from 2% in 1986 to 1% in 1993, and then starting in 1996 the EPA promulgated successive regulations reducing sulfur content in fuels to 0.5% in all counties and cities. Sulfur content in high-grade diesel fuels first dropped from 0.3% to 0.15%, and then in 1998 regulations were announced further lowering sulfur content to 0.05%. Since the implementation of these measures the air quality values at monitoring stations have significantly improved. Compared with ten years ago SO2 levels have improved 80%.
Beginning July 1998, the EPA also began collecting seasonal air pollution control fees for SOx and NOx based on pollutant type and actual emissions quantities. The fees are aimed to encourage industries to move independently to install pollution control equipment. Other measures, such as prohibiting the sale and use of high sulfur fuels like petroleum coke and raw coal without proper authorization and the collection of a pollution control fee of 1,000 NTD per/ton for the use of such fuels, have resulted in a large decrease in the number of factories using high-sulfur fuels. This has also contributed to the improvement of acid rain.
Based on a Central University professor’s research on SOx, almost 25% of SOx in Taiwan’s ambient air drifts in from outside Taiwan's boundaries. The other 75% comes from internal pollution sources. Taiwan sits on the edge of the Asian continent and the Pacific Ocean, and is downwind of many continental pollution sources. It is clear that over the years, the amount of SOx blown to Taiwan from seasonal northeast winds has increased. Taiwan’s air quality, and hence the problem of acid rain, will continue to worsen as mainland China and other east Asian countries increase pollutant emissions. Due to the difficulties of cross boundary pollution control this issue is likely to become a thorn in the side of future efforts to deal with acid rain. ， 欄位年度的內容是2000 ， 欄位月份的內容是3 ， 欄位卷的內容是3 ， 欄位期的內容是3 ， 欄位順序的內容是1 ， 欄位倒序的內容是2 ， 欄位分類的內容是Environmental Information ， 欄位標題2的內容是Report Released on Investigation of Acid Rain in Taiwan ， 欄位檔案位置的內容是print/V3/V3-03 。
編號
416
標題
Report Released on Investigation of Acid Rain in Taiwan
摘要
The results of an investigation into acid rain in the Taiwan region were recently released. According to the report average rain water pH value is between 4.8 and 5.1, revealing that Taiwan's acid rain problem is not severe in comparison with neighboring countries. As far as the pollutants that contribute to acid rain, atmospheric sulfate concentrations appear to be decreasing yearly while nitrate concentrations are holding steady. To better understand the state of acid rain in Taiwan, in 1990 the EPA brought together a number of domestic universities to research the current status, contributors and environmental impacts of acid rain in the Taiwan region. After eight years of work, an exhaustive report on this investigation has finally been released. The EPA points out that CO2 stored in the atmosphere (about 330ppm) reacts with rain water to form carbonic acid naturally resulting in a low acidity that is translated as a pH of around 5.6. However, formic acid, acetic acid, and other organic acids produced in nature also lower the pH values in rain, so in recent years many advanced nations and scientists have used pH values below 5.0 to define acid rain which has been polluted by human activity. In fact, judgements about acid rain are not based solely on pH values. There are numerous other factors such as electrical conductivity, anions and cations, which influence the acid-base levels of rain water. To gain command of the acid rain situation in Taiwan, an acid rain monitoring network has been established. The network generally uses the same sampling process and analysis methods as the U.S. EPA's National Atmospheric Deposition Program (NADP). There are a total of 12 stations set up in Taipei, Kuishan, Chungli, the Taichung harbor, and other locations throughout the island. The data accumulated over the years by these stations reveals that average pH values in Taiwan range from 4.8 to 5.1. Compared with the average pH values of neighboring countries like Hong Kong (4.2) and Japan (4.8), and with other advanced countries like the U.S. (4.2) and Europe (4.1), Taiwan's acid rain problem seems less severe. Looking at metropolitan areas, the average pH levels at the Taipei and Chungli monitoring stations have risen from 4.27 in 1991 to 4.51 in 1998, a 42% improvement. The Kaohsiung station recorded an improvement of 24%, from 4.49 to 4.61. I-lan improved 70%, from 4.35 to 4.88. Only Taichung showed increasing acidity, with pH values falling from 4.7 to 4.3. The average pH values at non-urban monitoring stations in Kenting, Daimali, Jia-i, Penghu and Alishan were all above 5.2, showing no signs of acidification. The two major contributors to the acidification of rain are sulfates and nitrates. Over the last eight years the average concentration of sulfates in rainfall have decreased from 3.5ppm in 1991 to 2.8ppm in 1998, an improvement of 20%. The concentration of nitrates have remained the same at 1.3ppm. As far as cations, the report shows that there is no obvious increase in ammonium ions (from the application of ammonia fertilizers) and calcium ions (from natural settling dust or limestone formations). From this the report infers that the reason behind the improvement in acid rain lies in the reduction of sulfate concentrations. For this reason the EPA expressed that the decrease in sulfate concentrations is directly related to EPA policies to encourage the use of low-sulfur fuels over the years. Sulfur content in fuels first dropped from 2% in 1986 to 1% in 1993, and then starting in 1996 the EPA promulgated successive regulations reducing sulfur content in fuels to 0.5% in all counties and cities. Sulfur content in high-grade diesel fuels first dropped from 0.3% to 0.15%, and then in 1998 regulations were announced further lowering sulfur content to 0.05%. Since the implementation of these measures the air quality values at monitoring stations have significantly improved. Compared with ten years ago SO2 levels have improved 80%. Beginning July 1998, the EPA also began collecting seasonal air pollution control fees for SOx and NOx based on pollutant type and actual emissions quantities. The fees are aimed to encourage industries to move independently to install pollution control equipment. Other measures, such as prohibiting the sale and use of high sulfur fuels like petroleum coke and raw coal without proper authorization and the collection of a pollution control fee of 1,000 NTD per/ton for the use of such fuels, have resulted in a large decrease in the number of factories using high-sulfur fuels. This has also contributed to the improvement of acid rain. Based on a Central University professor’s research on SOx, almost 25% of SOx in Taiwan’s ambient air drifts in from outside Taiwan's boundaries. The other 75% comes from internal pollution sources. Taiwan sits on the edge of the Asian continent and the Pacific Ocean, and is downwind of many continental pollution sources. It is clear that over the years, the amount of SOx blown to Taiwan from seasonal northeast winds has increased. Taiwan’s air quality, and hence the problem of acid rain, will continue to worsen as mainland China and other east Asian countries increase pollutant emissions. Due to the difficulties of cross boundary pollution control this issue is likely to become a thorn in the side of future efforts to deal with acid rain.
全文
The results of an investigation into acid rain in the Taiwan region were recently released. According to the report average rain water pH value is between 4.8 and 5.1, revealing that Taiwan's acid rain problem is not severe in comparison with neighboring countries. As far as the pollutants that contribute to acid rain, atmospheric sulfate concentrations appear to be decreasing yearly while nitrate concentrations are holding steady. To better understand the state of acid rain in Taiwan, in 1990 the EPA brought together a number of domestic universities to research the current status, contributors and environmental impacts of acid rain in the Taiwan region. After eight years of work, an exhaustive report on this investigation has finally been released. The EPA points out that CO2 stored in the atmosphere (about 330ppm) reacts with rain water to form carbonic acid naturally resulting in a low acidity that is translated as a pH of around 5.6. However, formic acid, acetic acid, and other organic acids produced in nature also lower the pH values in rain, so in recent years many advanced nations and scientists have used pH values below 5.0 to define acid rain which has been polluted by human activity. In fact, judgements about acid rain are not based solely on pH values. There are numerous other factors such as electrical conductivity, anions and cations, which influence the acid-base levels of rain water. To gain command of the acid rain situation in Taiwan, an acid rain monitoring network has been established. The network generally uses the same sampling process and analysis methods as the U.S. EPA's National Atmospheric Deposition Program (NADP). There are a total of 12 stations set up in Taipei, Kuishan, Chungli, the Taichung harbor, and other locations throughout the island. The data accumulated over the years by these stations reveals that average pH values in Taiwan range from 4.8 to 5.1. Compared with the average pH values of neighboring countries like Hong Kong (4.2) and Japan (4.8), and with other advanced countries like the U.S. (4.2) and Europe (4.1), Taiwan's acid rain problem seems less severe. Looking at metropolitan areas, the average pH levels at the Taipei and Chungli monitoring stations have risen from 4.27 in 1991 to 4.51 in 1998, a 42% improvement. The Kaohsiung station recorded an improvement of 24%, from 4.49 to 4.61. I-lan improved 70%, from 4.35 to 4.88. Only Taichung showed increasing acidity, with pH values falling from 4.7 to 4.3. The average pH values at non-urban monitoring stations in Kenting, Daimali, Jia-i, Penghu and Alishan were all above 5.2, showing no signs of acidification. The two major contributors to the acidification of rain are sulfates and nitrates. Over the last eight years the average concentration of sulfates in rainfall have decreased from 3.5ppm in 1991 to 2.8ppm in 1998, an improvement of 20%. The concentration of nitrates have remained the same at 1.3ppm. As far as cations, the report shows that there is no obvious increase in ammonium ions (from the application of ammonia fertilizers) and calcium ions (from natural settling dust or limestone formations). From this the report infers that the reason behind the improvement in acid rain lies in the reduction of sulfate concentrations. For this reason the EPA expressed that the decrease in sulfate concentrations is directly related to EPA policies to encourage the use of low-sulfur fuels over the years. Sulfur content in fuels first dropped from 2% in 1986 to 1% in 1993, and then starting in 1996 the EPA promulgated successive regulations reducing sulfur content in fuels to 0.5% in all counties and cities. Sulfur content in high-grade diesel fuels first dropped from 0.3% to 0.15%, and then in 1998 regulations were announced further lowering sulfur content to 0.05%. Since the implementation of these measures the air quality values at monitoring stations have significantly improved. Compared with ten years ago SO2 levels have improved 80%. Beginning July 1998, the EPA also began collecting seasonal air pollution control fees for SOx and NOx based on pollutant type and actual emissions quantities. The fees are aimed to encourage industries to move independently to install pollution control equipment. Other measures, such as prohibiting the sale and use of high sulfur fuels like petroleum coke and raw coal without proper authorization and the collection of a pollution control fee of 1,000 NTD per/ton for the use of such fuels, have resulted in a large decrease in the number of factories using high-sulfur fuels. This has also contributed to the improvement of acid rain. Based on a Central University professor’s research on SOx, almost 25% of SOx in Taiwan’s ambient air drifts in from outside Taiwan's boundaries. The other 75% comes from internal pollution sources. Taiwan sits on the edge of the Asian continent and the Pacific Ocean, and is downwind of many continental pollution sources. It is clear that over the years, the amount of SOx blown to Taiwan from seasonal northeast winds has increased. Taiwan’s air quality, and hence the problem of acid rain, will continue to worsen as mainland China and other east Asian countries increase pollutant emissions. Due to the difficulties of cross boundary pollution control this issue is likely to become a thorn in the side of future efforts to deal with acid rain.
年度
2000
月份
3
卷
3
期
3
順序
1
倒序
2
分類
Environmental Information
標題2
Report Released on Investigation of Acid Rain in Taiwan
檔案位置
print/V3/V3-03
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每小時更新更新,161謝小姐 | 02-2311-7722#2386 | 2022-01-14 01:00:21
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每2月更新,151黃先生 | 02-23117722#2748 | 2023-08-06 01:04:33
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每小時更新更新,138謝小姐 | 02-2311-7722#2386 | 2022-01-14 01:05:09
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每1月更新,165顏先生 | 02-23117722#2109 | 2023-07-27 01:01:24
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每1月更新,151顏先生 | 02-23117722#2109 | 2023-08-07 00:59:56
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每小時更新更新,211陳小姐 | 02-23117722分機6216 | 2022-01-14 01:02:55
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不定期更新更新,271陳先生 | 02-2311-7722#2386 | 2023-07-30 01:01:48
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不定期更新更新,39劉小姐 | 02-2311-7722#2824 | 2022-01-14 01:23:27
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不定期更新更新,95劉先生 | 02-23117722#2743 | 2022-01-15 01:12:37
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每1月更新,164顏先生 | 02-23117722#2109 | 2023-08-07 01:00:00
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每年更新更新,199李小姐 | 02-2311-7722#2633 | 2022-01-14 01:24:44
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不定期更新更新,182王先生 | 02-23712121#6401 | 2022-01-14 01:18:45
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每2月更新,48黃先生 | 02-23117722#2748 | 2023-08-05 01:01:08
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每3月更新,188郭先生 | 2311-7722#2399 | 2023-08-07 01:02:03
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每小時更新更新,156謝小姐 | 02-2311-7722#2386 | 2022-01-14 01:00:40
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每月更新更新,52陳小姐 | 02-2311-7722#2159 | 2022-01-14 01:22:16
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每月更新更新,144邱小姐 | 02-23712121#6309 | 2022-01-14 01:18:31
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不定期更新更新,52陳先生 | 02-2311-7722#2386 | 2023-08-07 01:02:14
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每年更新更新,46方先生 | 02-2311-7722#2153 | 2022-01-15 01:09:45
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不定期更新更新,65蔡先生 | 02-23257399#55723 | 2023-08-09 01:04:24
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不定期更新更新,56許先生 | 02-2311-7722#2831 | 2022-01-18 01:24:47
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不定期更新更新,50程先生 | 02-2311-7722#2833 | 2023-08-09 01:04:14
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不定期更新更新,57陳小姐 | (02)2311-7722分機2932 | 2023-07-30 01:02:09
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