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Vertical Distribution of Roots and Soil Nitrate: Tree Species and Phosphorus Effects
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Abstract
We hypothesized that trees can rapidly root into subsoil and capture NO
3
, which can accumulate in the subsoil of agricultural soils with high anion sorption. The vertical distribution of root length and inorganic N (NO
3
and NH
4
) to 3.95‐m soil depth was compared for 11‐mo‐old stands of eucalyptus (
Eucalyptus grandis
W. Hill ex Maiden), sesbania [
Sesbania sesban
(L.) Merr.], calliandra (
Calliandra calothyrsus
Meissner), markhamia [
Markhamia lutea
(Benth.) Schumann], and grevillea (
Grevillea robusta
A. Cunn. ex R. Br.) grown at two P levels (no added P and 500 kg added P ha
−1
) on a Kandiudalfic Eutrudox in Kenya. The trees were planted at a 1 by 1 m spacing in a randomized complete block with three replications. Added P had no effect on root length, soil NO
3
, and soil NH
4
even though the soil was low in available P. Total root length was greater for calliandra (15.5 km m
−2
) than other trees (1.2–5.6 km m
−2
). The slope for the model of natural logarithm root length density (cm cm
−3
) as a function of soil depth was affected by tree species (
P
< 0.01), indicating differences among trees in the tendency for deep rooting. Root length densities, averaged for the two P levels, were ≥0.1 cm cm
−3
to depths of 2.2 m with calliandra, 1.8 m with sesbania, 1.2 m with eucalyptus, 0.45 m with grevillea, and 0.3 m with markhamia. Calliandra and sesbania reduced soil NO
3
in the top 2 m by about 150 to 200 kg N ha
−1
within 11 mo after establishment and effectively captured subsoil NO
3
. Fast‐growing trees with high root length densities can rapidly reduce subsoil NO
3
.
Title: Vertical Distribution of Roots and Soil Nitrate: Tree Species and Phosphorus Effects
Description:
Abstract
We hypothesized that trees can rapidly root into subsoil and capture NO
3
, which can accumulate in the subsoil of agricultural soils with high anion sorption.
The vertical distribution of root length and inorganic N (NO
3
and NH
4
) to 3.
95‐m soil depth was compared for 11‐mo‐old stands of eucalyptus (
Eucalyptus grandis
W.
Hill ex Maiden), sesbania [
Sesbania sesban
(L.
) Merr.
], calliandra (
Calliandra calothyrsus
Meissner), markhamia [
Markhamia lutea
(Benth.
) Schumann], and grevillea (
Grevillea robusta
A.
Cunn.
ex R.
Br.
) grown at two P levels (no added P and 500 kg added P ha
−1
) on a Kandiudalfic Eutrudox in Kenya.
The trees were planted at a 1 by 1 m spacing in a randomized complete block with three replications.
Added P had no effect on root length, soil NO
3
, and soil NH
4
even though the soil was low in available P.
Total root length was greater for calliandra (15.
5 km m
−2
) than other trees (1.
2–5.
6 km m
−2
).
The slope for the model of natural logarithm root length density (cm cm
−3
) as a function of soil depth was affected by tree species (
P
< 0.
01), indicating differences among trees in the tendency for deep rooting.
Root length densities, averaged for the two P levels, were ≥0.
1 cm cm
−3
to depths of 2.
2 m with calliandra, 1.
8 m with sesbania, 1.
2 m with eucalyptus, 0.
45 m with grevillea, and 0.
3 m with markhamia.
Calliandra and sesbania reduced soil NO
3
in the top 2 m by about 150 to 200 kg N ha
−1
within 11 mo after establishment and effectively captured subsoil NO
3
.
Fast‐growing trees with high root length densities can rapidly reduce subsoil NO
3
.
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