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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Soil use and management 17 (2001), S. 0 
    ISSN: 1475-2743
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract. The aim of this study was to investigate the effects of water submergence depth on radial oxygen loss (ROL), soil solution chemistry and rice growth performance in acid sulphate soils in southern Vietnam. ROL was measured in a solution culture. In a separate pot experiment the impact of water submergence depth on rice growth and soil solution chemistry was studied. Three submergence depths were used in the two experiments (5, 10 and 15 cm). ROL declined with submergence depth and was significantly greater in young roots (with no root hairs) than in older roots. In the pot experiment rice growth and soil solution chemistry were clearly affected by the submergence depth. During the first crop at 5 cm submergence, there was a significantly higher yield and a higher oxidation state (pe+pH) compared to 10 or 15 cm submergence. The Fe concentration was significantly greater at the 5 cm depth compared to the 10 or 15 cm depth. SO42– reduction was delayed at the 5 cm depth. Rice yield was c. 25% less at the 15 cm than at the 5 cm depth. During a second crop, there was a substantial SO42- reduction and H2S formation and almost no significant effects of submergence depth on either soil solution chemistry or crop yield. In a field experiment with a dry-season rice crop, yield and Fe, Al and SO42– concentrations were higher at a shallow submergence depth than at greater depths in the same field, showing similar depth trends to those found during the first crop in the pot experiment. Farmers should be advised to use a shallow submergence depth and, if possible, avoid deep-rooted rice varieties. A conceptual model is suggested, which summarizes the relationships between ROL and soil solution chemistry.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 87 (1996), S. 1-22 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Relationships between the concentrations of sulphate, nitrate and Al were studied in leachates from reconstructed soil profiles of a previously N fertilized Haplic Podzol. Half of the profiles were covered with the grassDeschampsia fexuosa (Trin.), and the other half were not. The soil profiles were subjected to different N loads, in the form of ammonium sulphate. The doses were 0.5 mmol ammonium-N during the first part of the experiment and 1.0 mmol ammonium-N during the later part. Uptake of N by the vegetation almost completely eliminated the effects of added ammonium, even when the soil profile was strongly nitrifying. Fertilizer treatment caused nitrate to leach from the non-covered soil profiles, although there was a net retention of N. The concentration of Al in leachates was positively correlated with nitrate. Fertilizer treatment increased the proportion of inorganic monomeric Al in leachates. Most sulphate retention seemed to take place in the O horizon. In the presence of vegetation sulphate concentration was enhanced to a greater degree than could be explained from differences in evapotranspiration estimated from the Cl−/S04 2− ratio in the leachates. Soil N dynamics on a forest clear-cutting are discussed with reference to the present findings.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-2932
    Keywords: Forest liming ; dolomite ; soils ; runoff ; calcium ; magnesium ; potassium ; aluminium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract The dry forest soils (80%) of a 3.3 ha catchment in Gårdsjön, were treated with 1.5 ton/ha dolomite in 1984. In half the catchment an additional dose of 4.5 ton/ha was added in 1986 (i.e. totaly 6 ton/ha). By 1991 the concentrations of exchangeable calcium and magnesium had increased by 450% to 800% in the humus layer and upper 0–5 cm of the mineral soils and by 500% and 300%, respectively, in the 5–10 cm and 10–20 cm soil depth in the 6 ton/ha part. By 1.5 ton, Ca and Mg increased in humus and 0–5 cm in the mineral soil. Potassium decreased in the humus and the mineral soil with both 1.5 ton and 6 ton per ha. The accumulated output of K by runoff was however only 1 kg during the 6 years until 1992, which indicates that the losses from the soil also may have resulted in increased uptake by the forest. Tree growth and nutrient content in current needles was, however, unchanged. Increased contents of Mg, Ca and Zn was observed in some species of ground vegetation. Nitrate and ammonium concentrations and fluxes in runoff were identical to the reference catchment, while inorganic Al and Mn decreased by 40–50% and H+ by 30%. The accumulated extra output by runoff of Mg was about 7% and of Ca 0.6% of the amounts applied by the two treatments in 1984 and 1986.
    Type of Medium: Electronic Resource
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