Experimental and simulated soil mineral N dynamics for long-term tillage systems in northern France

2007 ◽  
Vol 94 (2) ◽  
pp. 441-456 ◽  
Author(s):  
K OORTS ◽  
F LAURENT ◽  
B MARY ◽  
P THIEBEAU ◽  
J LABREUCHE ◽  
...  
1997 ◽  
Vol 128 (3) ◽  
pp. 251-262 ◽  
Author(s):  
J. P. GRYLLS ◽  
J. WEBB ◽  
C. J. DYER

From 1985 to 1987, 20 experiments were carried out on shallow chalk soils, in which soil N reserves were expected to be small, to assess seasonal variations in the response of winter cereals to applied fertilizer N, and to relate these responses to measurements of soil mineral N (SMN), temperature and soil moisture deficits (SMD).Soil mineral N measured in autumn varied from 21 kg/ha (1986) to 73 kg/ha (1985), while SMN in spring ranged from 19 kg/ha (1987) to 91 kg/ha (1985), these values were typical of soils in long-term arable rotations. Estimates of apparent net N mineralization (AM) during the growing season were small at c. 26 kg/ha and suggested large seasonal variation. The small AM is considered to be due to the shallow topsoil drying out during the growing season. Whole crop N offtake without fertilizer N was only c. 40kg/ha. Crop N offtake, grain yield without fertilizer N and AFR (apparent recovery of fertilizer N) could not be reliably predicted by regression on SMN in autumn, SMN in spring or AM. Little or none of the variation in crop yield could be accounted for by regression on accumulated temperature over winter, maximum SMD in April to July or mean temperature in April to July.Despite optimum grain yields being only moderate at 6·59 t/ha for winter wheat and 6·78 t/ha for winter barley, response to applied fertilizer N was large, between 3·77 and 5·38 t/ha. In consequence the requirement for fertilizer N (c. 240–250 kg/ha) was also large, but differed little between seasons. This large requirement is concluded to be a result of limited fertilizer recovery and mineralization of soil N during the growing season.


2020 ◽  
Vol 298 ◽  
pp. 106975
Author(s):  
Mirjam Helfrich ◽  
Greta Nicolay ◽  
Reinhard Well ◽  
Caroline Buchen-Tschiskale ◽  
René Dechow ◽  
...  

2007 ◽  
Vol 37 (3) ◽  
pp. 313-320 ◽  
Author(s):  
Carol Melanie Schwendener ◽  
Johannes Lehmann ◽  
Marco Rondon ◽  
Elisa Wandelli ◽  
Erick Fernandes

Long term applications of leguminous green mulch could increase mineralizable nitrogen (N) beneath cupuaçu trees produced on the infertile acidic Ultisols and Oxisols of the Amazon Basin. However, low quality standing cupuaçu litter could interfere with green mulch N release and soil N mineralization. This study compared mineral N, total N, and microbial biomass N beneath cupuaçu trees grown in two different agroforestry systems, north of Manaus, Brazil, following seven years of different green mulch application rates. To test for net interactions between green mulch and cupuaçu litter, dried gliricidia and inga leaves were mixed with senescent cupuaçu leaves, surface applied to an Oxisol soil, and incubated in a greenhouse for 162 days. Leaf decomposition, N release and soil N mineralization were periodically measured in the mixed species litter treatments and compared to single species applications. The effect of legume biomass and cupuaçu litter on soil mineral N was additive implying that recommendations for green mulch applications to cupuaçu trees can be based on N dynamics of individual green mulch species. Results demonstrated that residue quality, not quantity, was the dominant factor affecting the rate of N release from leaves and soil N mineralization in a controlled environment. In the field, complex N cycling and other factors, including soil fauna, roots, and microclimatic effects, had a stronger influence on available soil N than residue quality.


2017 ◽  
Vol 246 ◽  
pp. 325-342 ◽  
Author(s):  
Caroline Buchen ◽  
Reinhard Well ◽  
Mirjam Helfrich ◽  
Roland Fuß ◽  
Manfred Kayser ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document