Dp. Belesky et al., NITROGEN AND MINERAL-COMPOSITION OF AUTUMN-GRAZED PASTURE, Communications in soil science and plant analysis, 26(17-18), 1995, pp. 2941-2959
Grazing management in autumn can influence the botanical composition a
nd productivity of a sward. Cycling of nutrients as a result of grazin
g livestock activity and variable canopy growth rates may influence mi
neral nutrient supply and demand in a dynamic canopy. An experiment wa
s conducted to determine the influence of autumn grazing practices on
the growth and composition, including minerals in terms of ruminant re
quirements, of a grass/legume sward. Paddocks were established and thr
ee replicates grazed by growing lambs for 30-, 60-, or 90-d intervals
beginning in late summer. Herbage samples were collected at the beginn
ing of the grazing interval and at the end of each interval (closing d
ate). Herbage mass, and nitrogen (N), phosphorus (P), potassium (K), m
agnesium (Mg), calcium (Ca), and sulfur (S), as well as copper (Cu) an
d zinc (Zn) were examined in terms of the influence of sampling date,
closing date, year, and the interaction of these factors from stockpil
ed and grazed canopies. Soil mineral composition was determined as wel
l. Concentrations of all minerals declined with increasing soil depth
and P, Na, Mg, and Ca increased in soil over the course of the experim
ent. Soil N concentration was reflected in the pattern of herbage grow
th in autumn. In general, closing date had no influence on herbage min
eral composition and concentrations were within the recommended levels
for a range of livestock. Phosphorus was the exception and concentrat
ions in herbage were low in terms of requirements for high producing l
ivestock such as lactating dairy cattle. Uptake or mineral reallocatio
n within the plant remained constant during the autumn growth interval
, since mineral yields were stable as growth rates declined in 1991 an
d increased when growth rates were stable in 1992. Mineral related nut
ritional problems in grazed mixed-species pasture, would most likely b
e a function of mineral bioavailability or interactions, rather than l
ow concentrations in the herbage.