1990
DOI: 10.1071/sr9900593
|View full text |Cite
|
Sign up to set email alerts
|

Seasonal storage and release of phosphorus and potassium by organic matter and the microbial biomass in a high producing pastoral soil

Abstract: Seasonal and fertilizer effects on forms of soil phosphorus and potassium, partially decomposed organic debris and enzyme activities were studied over 2 years on a highly fertile yellow-brown loam (Typic Vitrandept) under grazed pasture. Fertilizer topdressing (potassic superphosphate) increased total inorganic phosphorus, NaHCO3-extractable inorganic phosphorus and NaHCO3- extractable potassium, but did not affect organic forms of phosphorus, microbial biomass potassium and phosphorus, or organic debris. Labi… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

5
46
1

Year Published

2007
2007
2021
2021

Publication Types

Select...
6
4

Relationship

0
10

Authors

Journals

citations
Cited by 86 publications
(52 citation statements)
references
References 24 publications
5
46
1
Order By: Relevance
“…The value of available P at surface soil ranged from 1.74 to 3.70 ppm and subsurface soils ranged from 0.63 to 2.56 ppm. The concentrations of P in soil depends on a combination of factors including plant uptake, adsorption-desorption and dissolutionprecipitation of inorganic P, the mineralization of organic P and microbial immobilization and fertilizer addition (Perrott et al, 1990;Frossard et al, 2000). However, the concentration of P in soils of the current study was influenced by other factors.…”
Section: Ajesmentioning
confidence: 60%
“…The value of available P at surface soil ranged from 1.74 to 3.70 ppm and subsurface soils ranged from 0.63 to 2.56 ppm. The concentrations of P in soil depends on a combination of factors including plant uptake, adsorption-desorption and dissolutionprecipitation of inorganic P, the mineralization of organic P and microbial immobilization and fertilizer addition (Perrott et al, 1990;Frossard et al, 2000). However, the concentration of P in soils of the current study was influenced by other factors.…”
Section: Ajesmentioning
confidence: 60%
“…The concentrations of P in soils depends on a combination of factors including plant uptake, adsorption-desorption and dissolutionprecipitation of inorganic P, the mineralization of organic P and microbial immobilization and fertilizer addition (Perrott et al, 1990;Frossard et al, 2000).…”
Section: Discussionmentioning
confidence: 99%
“…High plant uptake rates create a zone around the root which is depleted of P since the rate of P diffusion is slow [61]. According to Perrott et al [62] and Frossard et al [63], the content of soil available P largely depends on a combination of factors including the uptake of plant, adsorption-desorption, and dissolution-precipitation of inorganic P, organic P mineralization, microbial immobilization, and addition of fertilizer. Immobile forms of P to the soil solution were released by soil microbes and the microbes are responsible for the P immobilization [61].…”
Section: Relationship Between Soil Fertility and Growth Performance Omentioning
confidence: 99%