Nitrogen (N) is the main fertiliser input to tea plantations because of the
large removal of this element with regular harvests of young shoots in the
field. The form of N supply is known to influence the uptake of other plant
nutrients, notably phosphorus (P), through its effect on soil pH in the
rhizosphere. A glasshouse study was conducted to test the effect of N form (NH
+4,
NO-3 , or both) on the
transformation of soil P in the rhizosphere and its availability to tea
(Camellia sinensis L.) plants fertilised with sparingly soluble Eppawala
phosphate rock (EPR). Four-month-old tea (TRI 2025) plants were grown in
rhizosphere study containers containing an Ultisol from Sri Lanka (pH 4
·5 in water) amended with EPR and KCl at 200 g P or K/g soil, and
mixed with
(NH4)2SO4
(100% NH+4 -N),
NH4NO3 (50%
NH+4 -N and 50%
NO-3 -N), and
Ca(NO3)2 (100%
NO-3 -N) at the rate of 200 g
N/g soil, with a control (no N fertiliser), as treatments.
Rhizosphere pH decreased compared with the bulk soil when N was supplied as
NH+4 or
NH+4
+NO-3 forms, and increased
when N was supplied as NO-3. The
cation{anion balance estimations in the plants showed that the plants had
taken up more NO-3 than
NH+4 even in
(NH4)2SO4
treated soil, suggesting high nitrification rates, especially in the
rhizosphere, in spite of using a nitrification inhibitor. More EPR dissolved
in the rhizosphere compared with that in the bulk soil, regardless of the N
form applied. The
(NH4)2SO4
treatment had the highest dissolution rate of EPR in the rhizosphere, whereas
Ca(NO3)2 treatment had the lowest,
reflecting the degree of acidification in the rhizosphere.
Resin-P and NaOH-Pi (inorganic P) concentrations were
lower and NaOH-Po (organic P) concentration was higher
in the rhizosphere than in the bulk soil. Plant and possible microbial uptake
of P is the main reason for the decrease in resin-P and
NaOH-Pi. The increase in NaOH-Po
concentration in the rhizosphere is believed to be due to transformation of
Pi to Po by the high microbial
activity in the rhizosphere. The
(NH4)2SO4
treatment caused the highest depletion of resin-P but lowest depletion of
NaOH-Pi, probably due to the fixation of P by the soils
at the low pH in the rhizosphere.
The study revealed that the use of the
NH+4 form of fertiliser can
increase acidification in tea rhizosphere compared with bulk soil and this can
enhance the effectiveness of PR fertiliser utilisation by tea plants.