1997
DOI: 10.1007/bf01420218
|View full text |Cite
|
Sign up to set email alerts
|

Nitrogen immobilization and mineralization during initial decomposition of15N-labelled pea and barley residues

Abstract: The immobilization and mineralization of N following plant residue incorporation were studied in a sandy loam soil using 15N-labelled field pea (Pisum sativum L.) and spring barley (Hordeum vulgare L.) straw. Both crop residues caused a net immobilization of soil-derived inorganic N during the complete incubation period of 84 days. The maximum rate of N immobilization was found to 12 and 18 mg soil-derived N g-i added C after incorporation of pea and barley residues, respectively. After 7 days of incubation, 2… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

4
24
1
3

Year Published

1999
1999
2024
2024

Publication Types

Select...
5
2
1

Relationship

0
8

Authors

Journals

citations
Cited by 107 publications
(32 citation statements)
references
References 20 publications
4
24
1
3
Order By: Relevance
“…Calculation of net ammonification (a, Figure 3) and net nitrification (n), in order to have a comparative parameters between treatments, was performed by subtracting soil NH 4 + -N in the time x (t x ) from soil NH 4 + -N in the initial time (t 0 ) and NO 3 --N in the time x (t x ) from soil NO 3 --N in the initial time (t 0 ), respectively. Apparent microorganism NH 4 + -Nimmobilization (i) was calculated by subtracting soil NH 4 + -N microbial biomass in the organic amendment treatment from NH 4 + -N microbial biomass in the control treatment (soil without organic amendment) (Jensen 1997), using the fumigation-extraction method. NO 3 --N consumption (c) was calculated by subtracting soil NO 3 --N in the control treatment from soil NO 3 --N in the organic amendment treatment.…”
Section: Nitrogen Mineralization and Immobilizationmentioning
confidence: 99%
See 2 more Smart Citations
“…Calculation of net ammonification (a, Figure 3) and net nitrification (n), in order to have a comparative parameters between treatments, was performed by subtracting soil NH 4 + -N in the time x (t x ) from soil NH 4 + -N in the initial time (t 0 ) and NO 3 --N in the time x (t x ) from soil NO 3 --N in the initial time (t 0 ), respectively. Apparent microorganism NH 4 + -Nimmobilization (i) was calculated by subtracting soil NH 4 + -N microbial biomass in the organic amendment treatment from NH 4 + -N microbial biomass in the control treatment (soil without organic amendment) (Jensen 1997), using the fumigation-extraction method. NO 3 --N consumption (c) was calculated by subtracting soil NO 3 --N in the control treatment from soil NO 3 --N in the organic amendment treatment.…”
Section: Nitrogen Mineralization and Immobilizationmentioning
confidence: 99%
“…NO 3 --N consumption (c) was calculated by subtracting soil NO 3 --N in the control treatment from soil NO 3 --N in the organic amendment treatment. This is based on the assumption that the mineralization and losses of indigenous soil N were similar in control and residue-treated soils (Jensen 1997). Apparent ammonification (a) was significantly different (P < 0.05) during the incubation period for the majority of treatments (Table 2).…”
Section: Nitrogen Mineralization and Immobilizationmentioning
confidence: 99%
See 1 more Smart Citation
“…A high N concentration in soil solution is necessary for plant growth but facilitates N loss via leaching (Jensen 1997). Soil microbial biomass N plays an important role as a sink and source of N (Singh et al 1989), and microbial immobilization of soluble N would contribute to a decrease in N leaching when crop residues were added to soils (Herai et al 2006;Sugihara et al 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Estas reduções são atribuídas, principalmente, ao efeito da alta relação C/N. A imobilização líquida de nitrogênio poderá ocorrer nos períodos iniciais da decomposição (JENSEN, 1997). Entretanto, a continuidade do processo de decomposição dos resíduos diminui a relação C/N no solo, uma vez que o carbono é perdido na forma de CO 2 e o nitrogênio é conservado pela formação de massa celular microbiana (VICTORIA et al, 1992).…”
Section: Introductionunclassified