Es. Kristensen et al., A SIMPLE-MODEL FOR ESTIMATION OF ATMOSPHERICALLY-DERIVED NITROGEN IN GRASS-CLOVER SYSTEMS, Biological agriculture & horticulture, 12(3), 1995, pp. 263-276
Atmospherically-derived nitrogen can be a major source of nitrogen in
organic or other low-input farming systems. lt is, however, in practic
e difficult to quantify the contribution of nitrogen from the atmosphe
re especially when dealing with grass-clover leys in the crop rotation
. In this study a simple model based on knowledge about the content of
clover in herbage and the time after establishment is presented and c
alibrated to a range of production conditions in Denmark. A statistica
l analysis of three experiments showed that the content of clover made
a satisfactory description of the variation in atmospherically-derive
d nitrogen above stubble height (harvested fixed-N-2). The variation i
n harvested fixed-N-2 was considerable (38-208 kg N ha(-1) year(-1)) d
ue to experimental manipulation by rate of N-fertilizer, cutting frequ
ency, soil type and irrigation. It was, however, also found that the t
ime after establishment of the grass-clover leys has a significant eff
ect in that way, that at a given content of clover harvested fixed-N-2
in the 3rd, 4th and 5th cropping year was only 2/3 of that in the 1st
and 2nd cropping year. Mineralization and immobilization of nitrogen
are discussed to predict accumulation of atmospherically-derived nitro
gen below stubble height. It is concluded that within the first two ye
ars after establishment there is a net accumulation of fixed-N-2 below
stubble height corresponding to 24-29% of harvested fixed-N-2. After
the 2nd year the total fixed-N-2 is assumed to correspond directly to
harvested fixed-N-2. Based on three classes of visual estimates of clo
ver content (10-29%, 30-49% or above 49%), the atmospherically-derived
nitrogen was estimated to be (kg ha(-1) year(-1)) 80, 157 or 248 in t
he first two years and 47, 84 or 128 in the 3rd, 4th and 5th years.