Johan Bergholm

Soil Acidification Induced by Ammonium Sulphate Addition in a Norway Spruce Forest in Southwest Sweden

The contributions of different acidifying processes to the total protonload (TPL) of the soil in control plots (C) and ammonium sulphate treatedplots (NS) were studied in a Norway spruce stand in Southwest Sweden during 1988–1998. The annual deposition of inorganic nitrogen and sulphate was on average 18 kg N and 20 kg S ha-1. In addition the NS treated plots received 100 kg N and 114 kg S ha-1 annually. The amounts of nutrients added to the ecosystem by wet and dry deposition and the leaching at 50 cm depth were calculated. The net atmosphericproton load, the proton load by nitrogen transformations in the soil, the sulphate sorption/desorption in the soil and the excess base cation accumulation in biomass were calculated. There was no leaching of inorganic nitrogen from control plots during the study period. The net atmospheric proton deposition, originating from sulphuric and nitric acid deposition, was the main contributor to TPL in control plots. The addition of ammonium sulphate increased the leaching of ammonium, nitrate, sulphate, magnesium and calcium but not of potassium. The TPL in NS plots was about ten times that in control plots. The nitrogen transformation processes were the main contributors to TPL to NS soil, in the beginning by ammonium uptake and later also by nitrification. The pH decreased by 0.4 units in the mineral soil. The between-year variation in TPL during the eleven year period in C plots (200–1500 molc ha-1 yr-1) and in NS plots (1000–13000 molc ha-1 yr-1) was mainly dependent on the sorption or release of sulphate. Both in C and NS, the TPL was buffered mainly by dissolving solid aluminium compounds, most probably some Al(OH)3 phase.

Vegetation establishment on a deposit of zinc mine wastes

Field trials concerning the establishment of plant cover on a deposit of wastes from the Ammeberg zinc mine in central Sweden were carried out during 1976-1985. Different soil conditioners and manures were applied and plant species cultivars were evaluated with regard to plant biomass, vigour, durability and content of zinc, lead and cadmium. Sewage sludge and topsoil led to better establishment of grasses than did municipal waste, straw and hydraulic seeding. After 2 years, Festuca rubra and Poa pratensis dominated the swards. Other species (Dactylis glomerata, Bromus inermis, Lolium perenne, Phleum nodosum, Festuca pratensis and F. arundinacea) constituted only a minor part of the stand. After 10 years, F. rubra was the most dominant species, while native Agrostis tenuis had invaded 20-50% of the area within the plots. Merlin was the clearly dominant red fescue cultivar. The concentration of zinc in shoots (616 mg kg(-1) dw) was about 10% of that in the soil. Zinc concentration decreased with increasing biomass above ground. It increased with age in Scots pine needles and was very high in birch leaves. Grasses survived longer than legumes in the zinc sand waste. Among the surviving grasses was a group with high (3800 mg kg(-1) dw) and a group with low (320 mg kg(-1) dw) zinc concentrations. The low group included Merlin red fescue and Sobel creeping bent. The cultivar Merlin contained a much lower zinc concentration than the other cultivars of red fescue (375 and 624 mg kg(-1) dw, respectively). A large amount of root biomass was present in plots with dominating Merlin red fescue (1715 g m(-2)), 97% of which was concentrated in the top 10 cm of the soil. The concentration of zinc in the roots was very high (13 000-25 000 mg kg(-1) dw). Nitrate fertilizer, especially ammonium nitrate, and acidic water (pH 4.3) increased zinc leaching.

Effects of enhanced supplies of nitrogen and sulphur on rhizosphere and soil chemistry in a Norway spruce stand in SW Sweden

Rhizophere and bulk soil chemistry were investigated in a Norway spruce stand in SW Sweden. The rhizosphere and bulk soil chemistry in water extracts in control plots (C) and plots repeatedly treated with ammonium sulphate (NS) were compared. Treatment regime was started in 1988. Cylindrical core samples of the LFH-layer and mineral soil layers were collected in 1992 and used for water extract analyses. Samples of soil from LFH-layer and mineral soil layers were taken in 1991 and 1993 for determination of CEC and base saturation. Soil pH and NH4-N, NO3-N and SO4-S, Al, Ca, K and Mg concentrations in water extracts were measured for rhizosphere and bulk soils. The pH-values of bulk and rhizosphere soils in NS plots decreased compared with those in control plots, whereas concentrations of NH4-N, NO3-N, SO4-S, base cations and Al in water extract increased. In both bulk and rhizosphere soils the concentration of NH4-N was much higher than that of NO3-N. A significant difference in the pH and Mg concentration of bulk and rhizosphere soil between the treated and control plots was found only in the 0–10 cm layer. For all layers, there was a significant difference in NH4-N concentrations in the bulk and rhizosphere soil between the NS treatment and control plots. Concentrations of exchangeable base cations and the base saturation level in the LFH-layer decreased in the NS plots. The concentration of extractable SO4-S increased in the NS plots. The NS treatment enhanced the amount of litter in L-layer, owing to increases in needle biomass and litterfall but led to losses of base cations, mainly K and Mg, from LFH-layer. It was concluded that the NS treatment displaced cations from exchangeable sites in the LFH-layer leading to higher concentrations of these elements in both rhizosphere and bulk soil.

Accumulation of Nutrients in Above and Below Ground Biomass in Response to Ammonium Sulphate Addition in a Norway Spruce Stand in Southwest Sweden

The effects of ammonium sulphate (NS) on the accumulation of nutrients in above and below ground biomass and soil were studied in a Norway spruce stand in south-west Sweden during 1988–1993. Ammonium sulphate addition resulted in nitrogen accumulation with 326 and 16 kg ha-1 in above and below ground biomass, respectively. Corresponding figures for the control plots (C) were 34 and 3 kg ha-1. Nitrogen accumulation in forest floor of NS was 266 kg ha-1 and 47 kg ha-1 in mineral soil. About 70% of added sulphate by fertiliser was retained in NS plots (482 kg S ha-1) of which 274 kg ha-1 was adsorbed in the mineral soil. The sulphate addition resulted in increased leaching of nitrogen, magnesium, calcium and sulphur. It is suggested that the spruce stand at the study site has a high capacity to accumulate nitrogen with a high above ground production. The high input of ammonium sulphate may in the long run result in increased losses of cations to ground water.