Transport of 14C-Sucrose and 14C-Benzyl Adenine in Winter Wheat (Triticum aestivum L.) in the Pre-Anthesis Period

A lysimeter trial is described in which the fate of ¹⁵N was monitored in a sand, loam and clay soil by using it over a period of 6 years. The following results were obtained.
1. The uptake of fertilizer nitrogen by plants, determined by using ¹⁵N, is lower than by using the conventional method ("difference method"). Nitrate ¹⁵N is better utilized by the plants than is ammonium ¹⁵N. The total nitrogen uptake only gives hints of these differences.
2. The extent to which plants utilize fertilizer ¹⁵N is between 38 and 58%; in the case of the method of differences this figure is between 48 and 68%.
3. Plants remove more nitrogen from the soil when fertilizer N is applied than when without fertilization. The influence of these two nutrient forms is of subordinate significance.
4. After a trial period of six years between 26 and 54 % of the fertilizer ¹⁵N remains in the soil. The resulting sequences are clay > loam > sand > and ammonium > nitrate.
5. The immobilization of the fertilizer ¹⁵N is most pronounced in the first four years but then decreased considerably; in the case of the sandy soil it is then even slightly regressive.
6. The biggest part of the ¹⁵N is deposited in the uppermost layer of the soil. The amount of ¹⁵N in the deeper layers is diminished appreciably. The type of soil has a greater influence than the form of nitrogen.
7. If the amount of fertilizer N left in the soil is compared with the N losses from the soil's reservoir (plants' uptake, leaching) there is a negative balance for the soil nitrogen which mainly is determined by the type of soil.