Nitrogen mineralization and crop uptake of N from decomposing 15N labelled red clover and yellow sweetclover plant fractions of different age

Nitrogen mineralization from 15N labelled red clover (Trifolium pratense L.) and yellow sweetclover (Melilotus officinalis Lam.) plant fractions of three different ages (8-, 14- and 20-week old) was studied in an out-door pot experiment during 8.5 months. Individual plant fractions (leaves/stems/roots/flowers), 23 g dry matter pot-1 (corresponding to 7300 kg ha-1), were incorporated into a sandy soil. The net mineralization of N was measured as 15N recovery in spring wheat (Triticum æstivum L.), perennial ryegrass (Lolium perenne L.) following the wheat and in the soil mineral N pool. Dry matter and N yields of the wheat crop were largest in pots receiving the legume leaf materials and the oldest root fractions. The largest amount of net N mineralized was obtained after application of sweetclover leaves, 381 mg N pot-1 (38% of added N), and a smaller amount was measured from red clover leaves, 215 mg N pot-1 (26% of added N). The N release was much smaller from the stems, being on average 63 mg N pot-1 (15% of added N), with intermediate values obtained from roots, 152 mg N pot-1 (26% of added N). The effects of age of the legume fractions on net N mineralization were more pronounced for sweetclover than for red clover materials. Greater net N release was obtained from sweetclover leaves and roots with inceasing age, but the opposite was valid for stems. At final harvest of the ryegrass, an additional 2.8% of added legume N was mineralized, compared with at wheat harvest. The net N mineralized proportion of added N was significantly related to concentrations of N and cell wall constituents in the plant material. Differences in net N mineralization estimates were generally larger between plant fractions than between materials of different age, implying that leaf proportion of the above-ground biomass is of great importance when predicting net N mineralization from green-manure plant materials. In addition, the contribution from roots to net mineralized legume N could be substantial.     

Field measurement of symbiotic nitrogen fixation in an established lucerne ley using15N and an acetylene reduction method

Summary Lucerne is an important forage legume in the south and south-east of Sweden on well-drained soils. However, data is lacking on the apparent amount of nitrogen derived through N₂ fixation by field-grown lucerne. This report provides basic information on the subject. The experiment was performed in a lucerne ley grown 40 km north of Uppsala. The input of nitrogen through fixation to the above-ground plant material of an established lucerne (Medicago sativa L.) ley was estimate by¹⁵N methodology during two successive years. The amount of fixed N was 242 kg N ha^–1 in 1982 and 319 kg N ha^–1 in 1983. The proportion of N derived from the atmosphere (%Ndfa) was 70% and 80% for the two years respectively. The first harvest in both years contained a lower proportion fixed N. Both N₂ fixation and dry matter production were enhanced during the second year, particularly in the first harvest. The Ndfa was 61% in the first harvest in 1982, compared to 72% Ndfa during the same period in 1983. This demonstrates the strong influence of environment on both dry matter production and N₂ fixation capacity of the lucerne.In addition anin situ acetylene reduction assay was used in 1982 to measure the seasonal distribution of the N₂ fixation and in 1983 to study the effect of soil moisture on the N₂ fixation process. The seasonal pattern showed great dependence on physiological development and harvest pattern of the lucerne ley. The maximum rate of N₂ fixation occurred at the bud or early flower stage of growth and was followed by a rapid decline as flowering proceeded. After harvest the nitrogenase activity markedly decreased and remained low during at least two weeks until regrowth of new shoots began. Irrigation doubled the nitrogenase activity of the lucerne in late summer 1983, when soil moisture content in the top soil was near wilting point. No changes in nitrogenase activity did occur in response to watering earlier during the summer, when the soil matric potential was around –0.30 MPa.