Apatite Loss in Pothwar Loess Plain (Pakistan) Fits a Simple Linear Reservoir Model
References (59)
- et al.
Pedogenesis, soil mass balance, phosphorus dynamics and vegetation communities across a Holocene soil chronosequence in a superhumid climate, South Westland, New Zealand
Geoderma.
(2011) - et al.
Experimental study of igneous and sedimentary apatite dissolution: Control of pH, distance from equilibrium, and temperature on dissolution rates
Geochim. Cosmochim. Acta.
(2003) - et al.
A study of two soil development sequences located in a montane area of Canterbury, New Zealand, III. Soil phosphorus transformations
Geoderma.
(1994) - et al.
Changes of organic matter, N, P and K content of soils in red soil areas under long-term experiment
Agr. Sci. China.
(2008) - et al.
Experimental evaluation of methods to quantify dissolved organic nitrogen (DON) and dissolved organic carbon (DOC) in soil
Soil Biol. Biochem.
(2006) - et al.
Phosphorus transformations and redistribution during pedogenesis of western Canadian soils
Geoderma.
(1996) - et al.
Phosphorus geochemistry in the Luochuan loess section, North China and its paleoclimatic implications
Quatern. Int.
(2006) - et al.
Inorganic phosphorus forms in some entisols and aridisols of Egypt
Geoderma.
(2007) - et al.
Crop yields, soil fertility and phosphorus fractions in response to long-term fertilization under the rice monoculture system on a calcareous soil
Field Crop. Res.
(2004) Phosphorus dynamic in soils and landscapes
Geoderma.
(1985)
The fate of phosphorus during pedogenesis
Geoderma.
Inorganic phosphorus fractions and phosphorus availability in a calcareous soil receiving 21-year superphosphate application
Pedosphere.
Relationship between phosphorus fractions and properties of highly calcareous soils
Aust. J. Soil Res.
Phosphorus forms in particle-size fractions of a toposequence from northeast Brazil
Soil Sci. Soc. Am. J.
Chloride and lithium transport in large arrays of undisturbed silt loam and sandy loam soil columns
Vadose Zone J.
Linking hydrology and biogeochemistry in complex landscapes
Prog. Phys. Geog.
The fate of soluble phosphate applied to soils
J. Soil Sci.
Fractionation of soil phosphorus
Soil Sci.
Calcium- and iron-related phosphorus in calcareous and calcareous marsh soils: Sequential chemical fractionation and 31P nuclear magnetic resonance study
Commun. Soil Sci. Plan.
An evaluation of ammonium fluoride as a selective extractant for aluminum-bond soil phosphate: III. Detailed studies on selected soils (1)
Soil Sci.
The fraction method for determining soil inorganic P in calcareous soils
Soils (in Chinese).
Phosphorus fractions in a loess toposequence. M. S. Thesis
Factors of Soil Formation: A System of Quantitative Pedology
A suggested fractionation scheme of inorganic phosphorus in calcareous soils
Fert. Res.
Phosphorous
Phosphate minerals
Routine procedure for rapid determination of soil carbonates
Soil Sci. Soc. Am. J.
Coagulation-flocculation of natural organic matter with Al salts: Speciation and structure of the aggregates
Environ. Sci. Technol.
Environmental Chemistry of Soils
Cited by (9)
Soil apatite loss rate across different parent materials
2018, GeodermaCitation Excerpt :The distribution of P in the parent materials conforms to those presented on a global scale (Yang et al., 2013). Previously, apatite-P of 680 mg kg− 1 was reported for undeveloped loess (Akhtar et al., 2014), 580 mg kg− 1 for highly developed loess soils (Hartmann, Durr, Moosdorf, Meybeck, & Kempe, 2012), 190 mg kg− 1 for coarse textured sand dunes (Syers & Walker, 1969), 230 mg kg− 1 for coarse texture greywacke derived alluvium (Shah, 1966), and 396 mg kg− 1 for sandstone. Apatite remained the largest contributor to total P in all the soils.
Growth benefits provided by different arbuscular mycorrhizal fungi to Plantago lanceolata depend on the form of available phosphorus
2018, European Journal of Soil BiologyCitation Excerpt :However, little is known about how mycorrhizal ‘quality’ is determined by the ability of the fungus to access and utilize different forms of P present in soils. Along with organic P pools [19,20], sparingly soluble (crystalline) P minerals such as apatites (Ca10X (PO4)6, where X = F−, Cl−, OH− or CO32−), may contribute significantly to the total phosphorus content of a soil, up to 75–90%, especially in the more calcareous soil types [21–24]. These Ca-phosphate species are often denoted by the term rock phosphates if they originate from a marine diagenetic mineral deposit [4,22].
Changes in Soil Organic Carbon Fractions Across a Loess Toposequence
2020, Journal of Soil Science and Plant Nutrition
Supported by the Higher Education Commission, Pakistan.