Abstract:was lower than on adding manure+superphosphate. Other monoester P compounds, typically related to microbial biomass and processes were highest on adding pig manure+urea. When adding superphosphate+urea+pig manure a reduction of these P compounds was observed as well as the highest accumulation of inositol hexakisphosphate (IHP). Synthetic fertilisers increased Olsen-P, orthophosphate and other monoester and total IHP and largely decreased soil pH. The addition of pig manure greatly increased the stereoisomers … Show more
“…Increases in other-monoester compounds in organic C-enriched cropped soils amended with exogenous organic C have been related to microbial biomass and processes (Li et al, 2022a). In the present study, levels of other-monoesters increased in the organic C-enriched layer of crop-growing soil and incubated plantfree soils.…”
Section: Effects Of Growing Crops In Compost-amended Soilssupporting
confidence: 54%
“…However, the IHP in our soils was not related to the levels of microbial biomass or soluble C and it was not an important variable for the discrimination between C-enriched and C-depleted soils in the rst PCA axis, perhaps because of the IHP content in the compost itself. Indeed, higher abundances of IHP have been found during the composting process (Hashimoto et al, 2014) and after adding manures to soils (Li et al, 2022a).…”
Section: Effects Of Compost Amendmentmentioning
confidence: 99%
“…Agricultural management practices can affect P availability and Po pools (Faucon et al, 2015;Foereid, 2017;Cooper et al, 2018). Increases in Po have been found in minerally fertilised soils after applying P mineral fertilisers alone or combined with manures (Li et al, 2022a), whereas, in other studies, no signi cant changes were observed after applying only manures or plant residues (Annaheim et al, 2015;Jantamenchai et al, 2022). Increasing organic matter in soil favours Pi mobility (Haynes and Mokolobate, 2001), but its effects on Po pools are less clear.…”
Section: Introductionmentioning
confidence: 99%
“…Indeed, most P in organic amendments is in mineral form (Sharpley and Moyer, 2000;Koopmans et al, 2007;Takahashi, 2013), and applying organic amendments in croplands increase pools of organic C and labile Pi (Romanyà et al, 2017;Zhang et al, 2020). Moreover, the long-term application of organic fertilisers has been found to reduce the Po/Pi ratio, mainly in soils with large increases in organic C (Li et al, 2022a). In contrast, other studies reporting moderate increases or reductions in soil organic C after the application of organic fertilisers observed an increase or no change in the Po/Pi ratio (Romanyà and Rovira, 2009).…”
Background Microbiota can favour crop access to phosphorus (P) pools retained in soil. Microbial activity and P mobilization can be enhanced by soil carbon and root exudates.Aims We aimed to study the changes in organic and inorganic P (Po; Pi) forms and compounds in organically fertilised soils growing crops for two years.Methods Crops were grown in pots with compost added at the soil surface. We measured changes in microbial carbon, soluble carbon, total Po and Pi forms, the less labile EDTA-NaOH-Pi (-Po), and labile NaHCO3-Pi (-Po) in surface and subsurface soils from crop-free pots amended with compost and unamended, and from amended pots growing crops. P compounds in the EDTA-NaOH extract were measured by 31P-NMR.Results Compost addition increased the levels of Pi and although it had no effect on Po it increased inositol hexakisphosphate and other-monoesters. After the application of compost, the amount of total organic carbon, soluble carbon and P forms increased in surface soil, while in the subsurface soil there was a reduction in organic carbon and an increase in soluble carbon, total Pi, EDTA-NaOH-Pi and NaHCO3-Pi and the less labile EDTA-NaOH-Po and labile NaHCO3-Po. Growing crops reduced all measured Pi forms and had no observable impact on total Po in either organic C-enriched or organic C-depleted soils.Conclusions Crops mostly used Pi from the low P availability C-depleted layer. Large reductions in NaHCO3-Po and increased levels of other-monoesters in crop growing organic C-enriched layers may suggest microbial mobilization and crop use of this pool.
“…Increases in other-monoester compounds in organic C-enriched cropped soils amended with exogenous organic C have been related to microbial biomass and processes (Li et al, 2022a). In the present study, levels of other-monoesters increased in the organic C-enriched layer of crop-growing soil and incubated plantfree soils.…”
Section: Effects Of Growing Crops In Compost-amended Soilssupporting
confidence: 54%
“…However, the IHP in our soils was not related to the levels of microbial biomass or soluble C and it was not an important variable for the discrimination between C-enriched and C-depleted soils in the rst PCA axis, perhaps because of the IHP content in the compost itself. Indeed, higher abundances of IHP have been found during the composting process (Hashimoto et al, 2014) and after adding manures to soils (Li et al, 2022a).…”
Section: Effects Of Compost Amendmentmentioning
confidence: 99%
“…Agricultural management practices can affect P availability and Po pools (Faucon et al, 2015;Foereid, 2017;Cooper et al, 2018). Increases in Po have been found in minerally fertilised soils after applying P mineral fertilisers alone or combined with manures (Li et al, 2022a), whereas, in other studies, no signi cant changes were observed after applying only manures or plant residues (Annaheim et al, 2015;Jantamenchai et al, 2022). Increasing organic matter in soil favours Pi mobility (Haynes and Mokolobate, 2001), but its effects on Po pools are less clear.…”
Section: Introductionmentioning
confidence: 99%
“…Indeed, most P in organic amendments is in mineral form (Sharpley and Moyer, 2000;Koopmans et al, 2007;Takahashi, 2013), and applying organic amendments in croplands increase pools of organic C and labile Pi (Romanyà et al, 2017;Zhang et al, 2020). Moreover, the long-term application of organic fertilisers has been found to reduce the Po/Pi ratio, mainly in soils with large increases in organic C (Li et al, 2022a). In contrast, other studies reporting moderate increases or reductions in soil organic C after the application of organic fertilisers observed an increase or no change in the Po/Pi ratio (Romanyà and Rovira, 2009).…”
Background Microbiota can favour crop access to phosphorus (P) pools retained in soil. Microbial activity and P mobilization can be enhanced by soil carbon and root exudates.Aims We aimed to study the changes in organic and inorganic P (Po; Pi) forms and compounds in organically fertilised soils growing crops for two years.Methods Crops were grown in pots with compost added at the soil surface. We measured changes in microbial carbon, soluble carbon, total Po and Pi forms, the less labile EDTA-NaOH-Pi (-Po), and labile NaHCO3-Pi (-Po) in surface and subsurface soils from crop-free pots amended with compost and unamended, and from amended pots growing crops. P compounds in the EDTA-NaOH extract were measured by 31P-NMR.Results Compost addition increased the levels of Pi and although it had no effect on Po it increased inositol hexakisphosphate and other-monoesters. After the application of compost, the amount of total organic carbon, soluble carbon and P forms increased in surface soil, while in the subsurface soil there was a reduction in organic carbon and an increase in soluble carbon, total Pi, EDTA-NaOH-Pi and NaHCO3-Pi and the less labile EDTA-NaOH-Po and labile NaHCO3-Po. Growing crops reduced all measured Pi forms and had no observable impact on total Po in either organic C-enriched or organic C-depleted soils.Conclusions Crops mostly used Pi from the low P availability C-depleted layer. Large reductions in NaHCO3-Po and increased levels of other-monoesters in crop growing organic C-enriched layers may suggest microbial mobilization and crop use of this pool.
“…However, pig manure could effectively alleviate soil acidification ( Bei et al, 2018 ); in the present study, the M treatment had the highest pH value. Pig manure is enriched with organic matter and nutrients including nitrogen, phosphorus, and potassium ( Ding et al, 2017 ; Li et al, 2022 ); thus our results indicated general improvements in soil fertility after 12 years of combined application of pig manure and chemical fertilizers on aeolian sandy soil.…”
Soil microorganisms play crucial roles in nutrient cycling and determining soil quality and fertility; thus, they are important for agricultural production. However, the impacts of long-term fertilization on soil microbial community remain ambiguous due to inconsistent results from different studies. The objective of this study was to characterize changes in bacterial and fungal diversity and community structures after 12 years of different fertilization in aeolian sandy soil by analyzing 16S rRNA and ITS rRNA gene sequences and the soil properties to discover the driving factors. Eight different fertilizer treatments have been set up since 2009: no fertilizer (CK), chemical N fertilizer (N), chemical N and P fertilizer (NP), chemical N, P and K fertilizer (NPK), pig manure only (M), pig manure plus chemical N fertilizer (MN), pig manure plus chemical N and P fertilizer (MNP), pig manure plus chemical N, P, and K fertilizer (MNPK). The results indicated that the long-term application of chemical fertilizer reduced soil pH, whereas the addition of pig manure alleviated a decrease in soil pH value. Chemical fertilizer plus pig manure significantly improved soil available nutrients and soil organic carbon. Long-term MNPK fertilization resulted in changes in bacterial diversity due to effects on specific bacterial species; by contrast, all fertilization treatments resulted in changes in fungal diversity due to changes in soil properties. Principal component analysis indicated that fertilization had a significant effect on soil microbial community structure, and the effect of chemical fertilizer combined with pig manure was greater than that of chemical fertilizer alone. Soil available phosphorus, total phosphorus, and pH were the most important factors that influenced bacterial taxa, whereas soil pH, total phosphorus, organic carbon, ammonium nitrogen and nitrate nitrogen were the most important factors influencing fungal taxa after 12 years of fertilization in aeolian sandy soil.
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