酸雨
土壤酸化
分水岭
土壤水分
环境科学
硫黄
植被(病理学)
土壤pH值
氮气
环境化学
水文学(农业)
土壤科学
生态学
化学
地质学
生物
有机化学
岩土工程
计算机科学
医学
病理
机器学习
作者
Edward C. Krug,C. R. Frink
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1983-08-05
卷期号:221 (4610): 520-525
被引量:532
标识
DOI:10.1126/science.221.4610.520
摘要
Acid rain is widely believed to be responsible for acidifying soil and water in areas of North America and northern Europe. However, factors commonly considered to make landscapes susceptible to acidification by acid rain are the same factors long known to strongly acidify soils through the natural processes of soil formation. Recovery from extreme and widespread careless land use has also occurred in regions undergoing acidification. There is evidence that acidification by acid rain is superimposed on long-term acidification induced by changes in land use and consequent vegetative succession. Thus, the interactions of acid rain, acid soil, and vegetation need to be carefully examined on a watershed basis in assessing benefits expected from proposed reductions in emissions of oxides of sulfur and nitrogen.
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