Treesearch

Acid precipitation is not a new phenomenon. As long as water has fallen on the surface of the earth it has probably contained varying amounts of oxides of carbons, nitrogen and sulfur that increase hydrogen ion activity. This was certainly true when volcanism prevailed. With the appearance of life spasmodic geologic expulsions of elements into the atmosphere were supplemented by more rhythmic biochemical cycles of organic matter production and decomposition. Since the Industrial Revolution consumption of fossil fuel has increased additions of atmospheric contaminants. In the first two and...

The data presented here are based upon element balance investigations in a beech forest in Central Germany (Ellenberg 1971). Being located in an altitude of about 500 m above sea level with an annual precipitation of about 1000 mm, and an acid soil with loess as the main constituent, the test site represents a typical environment for many Central European forests. Situated apart from larger industrial centers or big cities, it may also for Central European conditions - be considered as a clean air region with a relatively low level of air pollution.

The typical values and probable ranges of acid-precipitation are evaluated in terms of their theoretical effects on pH and cation exchange equilibrium of soils characteristic of the humid temperature region. The extent of probable change in soil pH and the time required to cause such a change are calculated for a range of common soils. Hydrogen ion input by acid precipitation is compared to cation inputs from nutrient cycling and other sources. For example it can be calculated that 100 years of acid precipitation (10,000 cm at pH 4.0) could be expected to shift the percentage base saturatio...

The acidification of precipitation is an accomplished fact. The only question that remains is whether the present trend of acidification is to continue into the future, and if so, to what degree. A related question is, are the consequences of acid precipitation reversible and to what extent, or over what time period? Research conducted over the last twenty years has been addressed to the problem of monitoring the composition of rainfall (and precipitation in general) (e.g. Cogbill and Likens, 1974). Except for the rather obvious and blatant examples of the effects of acid precipitation...

Sulphur dioxide emissions have occurred on a gigantic scale at Sudbury from nickel-copper smelters. Soil erosion has followed the destruction of large areas of forest. Rainfall has been found highly acidic, frequently less than pH 3.0 in 1971. Metal accumulation in the soils (to distances of 50 km) have occurred for nickel and copper. The combination of heavy metal particulate fall-out and acid rainfall has caused soils to become toxic to seedling survival and establishment. Erosional loss has contaminated lakes and water courses with consequent long distance transport of metal loads. The...

Rain and snow in Alberta are seldom acid. The S content of snow is so low that the snow pack gives a deposition of less than 1 kg S/ha, even downwind from large SO2 emission sources. Rainfall contributes at the most 4 kg S/ha yearly near SO2 sources, and only about 1 kg S/ha in clean areas. However, rain intercepted by forest trees exposed to SO2 emission becomes acid (pH 3.5 to 4.5) and has a S content of 3 to 4 times greater than rain. Soils absorb large amounts of S from emissions (up to 50 kg S/ha annually) but much of the S is found in non-sulphate form. Soils are slowly acidified by...

Emissions of sulphur dioxide appear to have an acidifying effect on grossfall (open rainfall), throughfall, stemflow and soil solution at sites near major sources. Resulting effects on soil chemistry include elevated extractable acidity and aluminum and depressed exchangeable bases, especially calcium and magnesium. These changes are mostly in the incipient phases in the study area.

This paper deals with problems of measuring acidity in rainfall and the interpretation of these measurements in terms of effects on the soil-plant system. Theoretical relationships of the carbon-dioxide-bicarbonate equalibria and its effect on rainfall acidity measurements are given. The relationship of a cation-anion balance model of acidity in rainfall to plant nutrient uptake processes is considered. It was concluded that average H+ concentration calculated from pH measurements is not a satisfactory method of determining H+ loading from rainfall unless the rain is consistently acid....

Ion separation of acid air pollutants out of snow causes-sudden, deep pH-drops in lakes and running waters at an early stage of snowmelting. These pH-drops have drastic effects on fish populations and are suggested to be the main cause of Sphagnum invasion and changes in the microflora already at an early stage of acidification, i.e. when summer pH-values are about 6. These effects in turn reduce the nutrient recycling and accelerate the acidification process.

The two species of mole salamander that occur in the Ithaca, New York, region (Ambystoma maculatum and A. jeffersonianum) breed in temporary ponds that are formed by accumulation of melted snow and spring rains. Water in many of these pools during the breeding season is acid; pH values as low as 3.5 have been measured. In laboratory experiments A. maculatum tolerated pHs from 6-10 and had greatest hatching success at pH 7-9. Ambystoma jeffersonianum tolerated pH 4-8 and was most successful at pH 5-6. Mortality rose abruptly beyond the tolerance limits. The pH optimum shifted upward with...