Assessment of Potential Nutrient Release from Phosphate Rock and Dolostone for Application in Acid Soils
References (69)
- et al.
Reaction of citric acid with calcite
Chem Eng Sci
(2007) - et al.
Aluminium fractionation and speciation in bulk and rhizosphere of a grass soil amended with mussel shells or lime
Geoderma
(2012) The lime-silicate question
Soil Biol Biochem
(2015)- et al.
Increase of apatite dissolution rate by Scots pine roots associated or not with Burkholderia glathei PML1(12) Rp in open-system flow microcosms
Geochim Cosmochim Acta
(2013) - et al.
Amelioration of acidity with time by limestone under contrasting tillage
Soil Till Res
(2003) The mechanism of dissolution of minerals in acidic and alkaline solutions: Part I. A new theory of non-oxidation dissolution
Hydrometallurgy
(2014)The mechanism of dissolution of the feldspars: Part I. Dissolution at conditions far from equilibrium
Hydrometallurgy
(2015)The mechanism of dissolution of minerals in acidic and alkaline solutions: Part VI. A molecular viewpoint
Hydrometallurgy
(2016)- et al.
Rock fragments evolution and nutrients release in vineyard soils developed on a thinly layered limestone (Tuscany, Italy)
Geoderma
(2009) - et al.
Long-term effects of lime and phosphogypsum application on tropical no-till soybean-oat-sorghum rotation and soil chemical properties
Eur J Agron
(2016)
Effect of beech (Fagus sylvatica L.) rhizosphere on phosphorous availability in soils at different altitudes (Central Italy)
Geoderma
A review on the dissolution models of calcium apatites
Prog Cryst Growth Ch
Effect of 1-naphthaleneacetic acid on organic acid exudation by the roots of white lupin plants grown under phosphorus-deficient conditions
J Plant Physiol
Effects of organic acids and dissolved oxygen on apatite and chalcopyrite dissolution: Implications for using elements as organomarkers and oxymarkers
Chem Geol
Rare earth element release from phosphate minerals in the presence of organic acids
Chem Geol
The dissolution kinetics and apparent solubility of natural apatite in closed reactors at temperatures from 5 to 50 °C and pH from 1 to 6
Chem Geol
Quantitative assessment of the fungal contribution to microbial tissue in soil
Soil Biol Biochem
The use of phosphate rock for direct application to soils
Adv Agron
Organic acid exudation by mycorrhizal Andropogon virginicus L. (broomsedge) roots in response to aluminum
Soil Biol Biochem
Stimulation of root acid phosphatase by phosphorus deficiency is regulated by ethylene in Medicago falcata
Environ Exp Bot
Rhizosphere interactions between microorganisms and plants govern iron and phosphorus acquisition along the root axis-model and research methods
Soil Biol Biochem
The analysis of soil cores polluted with certain metals using the Box-Cox transformation
Environ Poll
Interactions between ectomycorrhizal fungi and the bacterial community in soils amended with various primary minerals
FEMS Microbiol Ecol
Bio-fertilizer, ground magnesium limestone and basalt applications may improve chemical properties of Malaysian acid sulfate soils and rice growth
Pedosphere
Calcite, dolomite and magnesite dissolution kinetics in aqueous solutions at acid to circumneutral pH, 25 to 150 °C and 1 to 55 atm pCO2: New constraints on CO2 sequestration in sedimentary basins
Chem Geol
The reactivity of Tanzanian Minjingu phosphate rock can be assessed from the chemical and mineralogical composition
Geoderma
Tillage system and lime application in a tropical region: Soil chemical fertility and corn yield in succession to degraded pastures
Soil Till Res
Interaction between low molecular weight organic acids and hydroxyapatite with different degrees of crystallinity
Colloid Surface A
Kinetics of carbonate dissolution and its effects on the porosity and permeability of consolidated porous media
J Petrol Sci Eng
Lime: A soil amendment
Trace Elements in the Terrestrial Environment: Biogeochemistry, Bioavailability, and Risks of Metals
Dolomite: Perspectives on a perplexing mineral
Oilfield Rev
Local phosphate resources for sustainable development in Sub-Saharan Africa
Small-scale fertilizer production units using raw and partially solubilized phosphate
Cited by (30)
Shifting soil nutrient stoichiometry with soil of variable rock fragment contents and different vegetation types
2023, CatenaCitation Excerpt :The rock fragments contribute to the formation of large pores at both RF-RF and RF-fine soil interfaces (Ma et al., 2010; Sekucia et al., 2020), which can affect soil hydrological processes, such as increasing water infiltration and soil air capacity, and reducing surface runoff and soil erosion (Poesen and Lavee, 1994; Sekucia et al., 2020; Wang et al., 2012). In addition, considerable amounts of available nutrients can be released during weathering processes of RF, including dissolution of carbonate, and formation and transformation of secondary minerals (Heisner et al., 2004; Jin et al., 2010; Koele et al., 2010; Rafael et al., 2018; Ugolini et al., 1996). Previous studies found that rock fragment content (RFC) was positively related to soil nutrients (Johnson et al., 2012; Lai et al., 2021), and was conducive to reduce soil N loss and promote soil nutrient accumulation (Liao et al., 2019; Zheng et al., 2021; Zhou et al., 2020).
Soil fertility in slash and burn agricultural systems in central Mozambique
2022, Journal of Environmental ManagementCitation Excerpt :Because of this, the distinct parent material and related mineralogical assemblage appeared to be the main cause of the different soil pH values. TOC and HC were present in very low amounts, in line with the contents reported by Rafael et al. (2018) for Mozambican soils. However, since both TOC and HC contents were similar in the FF soils and were the highest in the Macate CF soil, deductions were that:
Phosphate bacterial solubilization: A key rhizosphere driving force enabling higher P use efficiency and crop productivity
2022, Journal of Advanced ResearchCitation Excerpt :Therefore, improving use efficiency of P fertilizers in terms of nutrient uptake and crop yield remains highly important. Unlike water-soluble P fertilizers, RP directly applied in agricultural soils could be an efficient P form for crop production in high P retention soils [12]. The agronomic efficiency of RP has been extensively studied and reported over the past 50 years [13], and the positive effects of its direct application on soil properties and plants growth have been well reported to rely mainly on RP solubility [14-16].
P-legacy effect of soluble fertilizer added with limestone and phosphate rock on grassland soil in subtropical climate region
2021, Soil and Tillage ResearchCitation Excerpt :The RP used as P source in the current study had more than 75 % coarse particles (2000−50 μm) and 4% particles smaller than 2 μm. Larger particles have lesser specific surface area for chemical reactions; therefore, they are lesser reactive and more recalcitrant in the soil (Mackay and Syers, 1986; Rafael et al., 2018; Syers et al., 1986). Moreover, the self-inhibiting dissolution mechanism takes place when the surface of the mineral particle starts the process of dissolving and releasing Ca2+ and P, which raises soil pH. Low Ca2+, P and H+ diffusion in soil solution enables the formation of a zone with high pH, and Ca2+ and P saturation levels around the particle.
Impacts of oxalic acid-activated phosphate rock and root-induced changes on Pb bioavailability in the rhizosphere and its distribution in mung bean plant
2021, Environmental PollutionCitation Excerpt :Contrary to them, phosphate rock (PR) is a low-cost amendment comprised of metal oxides, carbonates, silicates, and fluorides (Cao et al., 2002; Huang et al., 2016). Phosphate rock is usually utilized for the manufacturing of high-grade phosphate fertilizers for agricultural usage (Rafael et al., 2018). Although it contains essential micronutrients such as Ca, Mg, Fe, or Zn in different concentrations, it should be mentioned that concentrations of Cd can be also very high (Kabata-Pendias, 2011; Rochayati et al., 2011) and can be accumulated in soils amended with P fertilizers (Park et al., 2020).
Coffee by-products derived resources. A review
2021, Biomass and Bioenergy