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A demonstration of acid rain and lake acidification: wet deposition of sulfur dioxide

机译:酸雨和湖泊酸化的演示:二氧化硫的湿沉降

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Acid rain is a familiar environmental problem that is sometimes discussed in general chemistry lectures. Several demonstrations pertaining to acid precipitation have been published in this Journal (1-3) but none of these illustrate the dissolution of acidic oxides in airborne water droplets, or "wet deposition", in the manner in which it occurs in the atmosphere. nitrogen oxides come from cars and other combustion sources, whereas atmospheric sulfur oxides are a result of coal-fired power plants and the roasting of metal sulfide orea in smelters (4). Cloud droplets then scavenge these oxides. Acification of lakes in areas geographically removed from the source can results when this acidified precipitation is deposited in lakes with no natural buffering capacity. A lake underlain by limestone will be resistant to acidification due to the buffering capacity of CaCO_3 while a lake underlain by granite will not, since granite contains silicates rather than carbonates (5). In the United States, lake acidification has received the most attention in the Northeast where the bedrock is primarily granite (6).
机译:酸雨是一个常见的环境问题,有时会在常规化学讲座中讨论。在本期刊(1-3)中已发表了一些与酸沉淀有关的证明,但没有一个例证说明酸性氧化物以在大气中发生的方式溶解在空气中的水滴中或称为“湿沉降”。氮氧化物来自汽车和其他燃烧源,而大气中的硫氧化物是燃煤电厂和冶炼厂中金属硫化矿石的焙烧的结果(4)。然后,云滴清除这些氧化物。当这种酸化的沉淀物沉积在没有自然缓冲能力的湖泊中时,可能导致在地理上远离源头的地区使湖泊酸化。由于CaCO_3的缓冲能力,石灰岩下的湖泊将抗酸化,而花岗岩下的湖泊则不会,因为花岗岩包含硅酸盐而不是碳酸盐(5)。在美国,湖泊酸化作用在东北地区最为受关注,那里的基岩主要是花岗岩(6)。

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