As a part of a National Fertilization Trial established in the second
half of the 1960s, on lime coated chernozem soil at Nagyhorcsok, conta
ining 3% humus, 5% CaCO3, originally supplied moderately with N and K,
and poorly with P and Zn, between the 13th and 20th years of the Tria
l No. B 17, studies were made on the long-term effect of N, P and K fe
rtilizations in winter wheat-maize diculture. During that period also
the trend in AL-soluble PK contents was followed. The main results can
be summed up as followe: On the soil originally with a poor P supply,
the cumulative P fertilization with a P2O5 rate of 50 kg/ha/year incr
eased significantly the grain yield of winter wheat by 1,9-3,0 t/ha, o
f maize by 0,8-3,0 t/ha, of sunflower by 0,4 t/ha between 13-20th year
s of the trial. By increasing the rate of P to 100 kg P2O5/ha/year the
grain yield of winter wheat rose additionally by 0,1-0,6 t/ha, while
it had no influence on the yield of sunflower, in maize it resulted ev
en in a significant decrease of 0,4-0,7 t/ha on the poorly supplied Zn
soil, due to Zn deficiency induced by P. By raising the N fertilizer
level from 50 kg/ha/year to 100 kg/ha/year it gave a significant incre
ase in 3 cases from 4 winter wheat years (0,1-1,0 t/ha), in maize in o
ne case from 3 years (0,1-0,6 t/ha), and also in the 9ne sunflower yea
r (0,2 t/ha). The rise of N rate from 100 to 150 kg/ha/year achieved,
however, in winter wheat a further yield surplus of only 0,1-0,2 t/ha,
in maize 0,0-0,7 t/ha, in sunflower 0,0 t/ha. The effects of K fertil
ization were generally depending on weather and kind of crop. The rate
of 100 kg/ha K2O had a yield increasing effect in 2 years from the 4
winter wheat years (0,0-1,0 t/ha), also in 2 years from the 3 maize pr
oducing years (0,4-0,6 t/ha), and in the one sunflower year it was als
o significant (0,3 t/ha). Among the interactions, the N x P was the st
rongest; it was, apart from one year, always statistically proved. In
the ploughed layer the AL-P2O5 content of the soil during the 8 years
in the non-fertilized treatment fell from 70 to 60 mg/kg, in the ferti
lization treatment of 50 kg/ha/year P2O5 from 110 to 100 mg/kg, and re
mained further on at the level of poor, moderate, resp. supply. During
the two rotations at 150 kg/ha P2O5 level the AL-P2O5 content rose fr
om 170 to 190 mg/kg, at P2O5 level of 200 kg/ha/year it rose from 180
to 240 mg/kg, what showed already a good, even a very good P supply. I
n the ploughed layer of plots without K fertilization, the AL-K2O cont
ent decrease from 180 to 130 mg/kg during the 8 years, between the 13t
h and 20th years of the trial. That meant a change from the upper limi
t of the moderate supply category to the lower limit ot the same categ
ory. On the effect of the yearly fertilization of 100 kg/ha K2O, as a
result of the positive K balance, the AL-K2O content rose from 210 to
230 mg/kg indicating a good K supply. The results of the long-term tri
al prove that besides the genetic characteristics of the crops, the si
ze of the yields vary mainly according to the nutrient and water suppl
ies of the soil.