avoid food shortages. However, the implementation of intensive agricultural practices such as excessive irrigation, tillage, and chemical fertilizers to increase crop productivity has devastated soil and farmland quality. [1,2] Particularly, acidification, salinization, and organic matter decomposition in soils typically coincide with agriculture practices, which adversely affect crop productivity and soil fertility. [3][4][5] Additionally, the inefficient absorption of conventional chemical NPK (i.e., nitrogen, phosphorus, and potassium) fertilizers by plants are among the main drivers of environmental eutrophication. [6] Therefore, many efforts are being made to develop novel strategies to overcome these drawbacks, including new types of fertilizers that can both maximize crop nutrient use efficiency and restore soil quality. [7,8] Novel smart fertilizer structures should not only be sensitive to crop rhizosphere, thus selectively releasing NPK or other crop macronutrients, but should also be made with non-toxic and low-cost materials. Crop nutrient use is maximized when the sensing ability of smart fertilizers is coupled with slow-releasing activity,
Structurally stable humic substances (HSs) in soils are tightly associated with soil fertility, and it is thus important to understand how soil HSs are naturally formed. It is believed that microbial metabolism on plant matter contributes to natural humification, but detailed microbial species and their metabolisms inducing humic functionality (e.g., direct plant stimulation) need to be further investigated.
We investigated the ability of microbial
volatile organic compounds
(MVOCs) emitted by Bacillus megaterium (a well-known MVOC producer) to modify the dissolution kinetics
and surface of hydroxyapatite, a natural soil mineral. Facilitated
phosphate release was induced by the airborne MVOCs in a time-dependent
manner. Use of each standard chemical of the MVOCs then revealed that
acetic and oxalic acids are crucial for the phenomenon. In addition,
the ability of such MVOCs to engineer the apatite surfaces was evidenced
by FT-IR spectra showing the COO– band variation
with incubation time and the prolonged acceleration of phosphate release
during the negligible acidification of the hydroxyapatite-containing
solutions. The formation of calcium oxalate was revealed through SEM-EDS
and XRD analyses, suggesting that MVOC oxalic acid interacts with
calcium ions, leading to the precipitation of calcium oxalate, thus
preventing the recrystallization of calcium phosphates. Gel- and soil-based
plant cultivation tests employing Arabidopsis thaliana and solid calcium phosphates (i.e., nano- and microsized
hydroxyapatites and calcium phosphate dibasic) demonstrated that these
MVOC mechanisms facilitate plant growth by ensuring the prolonged
supply of plant-available phosphate. The relationship between the
growth enhancement and the particle size of the calcium phosphates
also substantiated the MVOC sorption onto soil minerals related to
plant growth. Given that most previous studies have assumed that MVOCs
are a molecular lexicon directly detected by the dedicated sensing
machinery of plants, our approach provides a new mechanistic view
of the presence of abiotic mediators in the interaction between plants
and microbes via MVOCs.
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