Inoculation of phosphate-solubilizing bacteria improves soil phosphorus mobilization and maize productivity
Nutr Cycl Agroecosyst
https://doi.org/10.1007/s10705-023-10268-y
ORIGINAL ARTICLE
Inoculation of phosphate‑solubilizing bacteria improves soil
phosphorus mobilization and maize productivity
Isidro Beltran‑Medina · Felipe Romero‑Perdomo ·
Lady Molano‑Chavez · Angelica Y. Gutiérrez · Antonio M. M. Silva
German Estrada‑Bonilla
·
Received: 1 August 2022 / Accepted: 20 February 2023
© The Author(s) 2023
Abstract Phosphate-solubilizing bacteria represent
a bioalternative in making soil-immobilized phosphorus (P) available to plants, and consequently improve
agriculture sustainability and reduce nutrient pollution. In this study, we examined whether Rhizobium
sp. B02 inoculation can affect the soil P fractions.
Moreover, we investigated how inoculation influences the growth, physiological traits, and productivity of the maize crop. Field tests were carried out
to evaluate the combined application of strain B02
and reduced doses of P fertilizer. Soil P fractionation
was performed after crop harvesting, assessing the
Isidro Beltran-Medina and Felipe Romero-Perdomo have
contributed equally.
Supplementary Information The online version
contains supplementary material available at https://doi.
org/10.1007/s10705-023-10268-y.
I. Beltran‑Medina
Corporación Colombiana de Investigación Agropecuaria AGROSAVIA - C.I. Nataima, Espinal, Tolima, Colombia
F. Romero‑Perdomo · L. Molano‑Chavez ·
A. Y. Gutiérrez · G. Estrada‑Bonilla (*)
Corporación Colombiana de Investigación Agropecuaria AGROSAVIA - C.I. Tibaitatá, Mosquera, Cundinamarca,
Colombia
e-mail: ;
A. M. M. Silva
Departamento de Ciência do Solo, Escola Superior de
Agricultura “Luiz de Queiroz”, Universidade de São
Paulo, Piracicaba, São Paulo, Brazil
P dynamics. To study the plant response, samplings
were carried out in three phenological stages—the
vegetative stage of the 7 fully emerged leaves with
leaf collars (V7), the vegetative stage of the tassel (VT), and the reproductive stage of physiological maturity (R6). Using 50% of P fertilizer recommended, the strain inoculation increased the labile
inorganic P fraction by 14% compared to the control
treatment at the same dose, indicating that it favored
the Pi mobility. Under these same conditions in the
V7 and VT phenological stages, the inoculation significantly improved shoot length (28 and 3%) and
shoot dry weight (9.8 and 12%). B02 inoculation
increased grain yield by 696 kg ha−1 using 50% of
the recommended rate of P fertilizer, phenocopying
the complete P fertilization treatment without inoculation. Therefore, Rhizobium sp. B02 inoculation
replaced 50% of P fertilizer in maize and increased
the soil P availability.
Keywords Fertilization · PGPB · Phosphorus
availability · Phosphorus legacy · Phosphorus
recovery
Introduction
Phosphorus (P) is a fundamental and irreplaceable element for living organisms. It impacts agricultural productivity and environmental pollution.
Large amounts of P have accumulated in soils, but
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Nutr Cycl Agroecosyst
less than 5% are available for use by plants (Lambers 2022). It has been estimated that 5.7 billion hectares of land globally contain insufficient amounts of
available P for crop production, thus demanding P
fertilizer inputs (Drohan et al. 2019). However, part
of the applied P is fixed in soils due to high-affinity
reactions with soil particles. The amount of P applied
to the soil is markedly higher than the amount of P
absorbed by plants, leading to a surplus of soil P over
time (Gatiboni et al. 2020), and in some cases excessive doses of P fertilizers are applied to compensate
for P fixation (Alewell et al. 2020). Excess P in soil
causes deficiencies of micronutrients such as zinc
and iron (Xu et al. 2022). It also generates P runoff,
which causes nutrient over-enrichment in agricultural watersheds and possibly results in irreversible
effects on aquatic ecosystems (Wildemeersch et al.
2022). Therefore, improving P management is a priority when it comes to sustaining future food supplies
and sustainably managing the environment (Haygarth
et al. 2021).
Soil P recovery is an approach that closes the P
cycling and thus increases P availability (Withers
2019). One of the most crucial roles in this approach
is played by legacy P (Yuille et al. 2022). This represents the accumulated P in soil over the years (Doydora et al. 2020). Legacy P can be found in soils in
various chemical fractions, classified as labile, moderately labile, and non-labile P (Mezeli et al. 2020).
Legacy P in arable lands (i.e., Africa, South America, and Eastern Europe) is estimated at a minimum
of 347 kg P h a−1 within a 0–0.2 m deep soil layer,
which could be sufficient to sustain global P demands
for approximately 9–22 years (Rowe et al. 2015; Liu
et al. 2017). The potential use of legacy P would
reduce harmful P accumulation, provide economic
benefits in P fertilizer inputs, mitigate pressure on
phosphate rock reserves, and improve crop P use efficiency (Withers et al. 2020).
Cereal production worldwide stands out as having a low efficiency of P use, which varies between
9 and 12% (Yu et al. 2021). In particular, P is the
second most demanded nutrient by maize plants
(Zea mays L.) and its lack critically limits crop
development and yield (Yan et al. 2021). Low soil
P availability for maize strongly decreases root
growth, stem strength, crop quality, and grain yield
and leads to non-uniform and later crop maturity
(Zhang et al. 2021). Tropical and subtropical soils
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usually have strong P adsorption caused by hydroxides of aluminum and iron, as well as crystalline
and amorphous oxides, alongside accumulation processes or organic matter stabilization (Damian et al.
2020). Consequently, many countries are facing cost
overruns and non-self-sufficient production when it
comes to maize (Barbieri et al. 2022).
Soil microorganisms such as phosphate-solubilizing bacteria (PSB) are able to access legacy P, making it available to plants, and thus leading to a reduction in the P fertilizer needs of crops (de-Bashan et al.
2021). The most representative PSB genera are Pseudomonas, Bacillus, Gluconobacter, and Burkholderia,
while other genera, such as Rhizobium, have been less
investigated (Alori et al. 2017). The metabolic mechanisms of PSB to mineralize organic phosphorus (Po)
are the production of phytases, phosphomonoesterases, and phospholipases, while those to solubilize
inorganic phosphorus (Pi) are the synthesis of organic
acids and release of protons and hydroxyl or bicarbonate ions (Granada et al. 2018; Hinsinger 2001). The
metabolic activities of PSB have been widely investigated, mainly under in vitro conditions with insoluble
Pi sources (Zeng et al. 2022). Numerous studies have
focused on the influence of inoculation both on plant
development and the total P accumulation in the soil
(De Zutter et al. 2022; Bargaz et al. 2021). However,
whether PSB inoculation increases the availability of
soil legacy P remains largel (...truncated)