Tq. Zhang et al., LONG-TERM CHANGES IN MEHLICH-3 EXTRACTABLE P AND K IN A SANDY CLAY LOAM SOIL UNDER CONTINUOUS CORN (ZEA-MAYS L), Canadian Journal of Soil Science, 75(3), 1995, pp. 361-367
Rates of change of soil nutrient levels during crop production can be
used to evaluate the long-term economic value and sustainability of fe
rtilizer practices. Objectives were to quantify changes in Mehlich-3 e
xtractable P and K due to additions of inorganic and manure P and K in
corn (Zea mays L.) production. Surface (0-20 cm) and subsoil (20-40 c
m) samples were collected after harvest from 1984 to 1993 on a Chicot
sandy clay loam soil (Grey Brown Luvisol) fertilized with two rates of
inorganic P and K and with dairy manure. Manure P at 60 kg P ha(-1) p
lus inorganic fertilizer P at 132 kg ha(-1) yr(-1) increased extractab
le P 1.0 kg for every 4.2 kg added P if only topsoil was considered, f
or every 3.2 kg added P if corn grain P removal was deducted, and for
every 2.8 kg added P if subsoil increases were included but corn P upt
ake excluded, and 2.1 kg added P with subsoil P included and corn P re
moval deducted. Without manure, 132 kg P hal yr(-1) increased Mehlich-
3 extractable P by 1.0 kg for every 8.1 kg P added, or 5.3 kg P added
if corn P removal was deducted from added fertilizer P. At the low rat
e of 44 kg P ha(-1) with manure P, Mehlich-3 levels increased by 1.0 k
g P for every 5.2 kg added fertilizer P. Extractable P remained consta
nt when inorganic fertilizer P was added without manure, probably beca
use crop removals equalled fertilizer additions. Mehlich-3 extractable
K increased in both top soil and subsoil at rates of 141 and 332 kg h
a(-1) yr(-1) inorganic K except for the 141 K rate in the final four y
ears when no manure was applied. When both soil depths were included a
nd summed over all years, values of added K to increase extractable K
by 1.0 kg ranged from 4.2 to 5.5 kg, regardless of source or rate of a
dded K. To increase soil test P, manure combined with high P rates was
more effective per unit added P than low P rates or added P without m
anure. Either form or rate of added K was equivalent in increasing ext
ractable K.