2010
DOI: 10.1016/j.geoderma.2010.04.023
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Soil organic phosphorus fraction in pine–oak forest stands in Northeastern Germany

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Cited by 36 publications
(29 citation statements)
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“…Values reported were approximately ten times greater than those of NaHCO 3 -Pi, indicating that the labile P forms in these soils are mainly stored in organic forms. In P-deficient soils, as those studied, the organic fractions play a fundamental role in the P cycle and plant nutrition (SLAZAK et al, 2010). These fractions were significantly correlated with soil C content (R: 0.73 ** ), confirming that the presence of labile organic fractions is associated with organic matter accumulation.…”
Section: Resultssupporting
confidence: 58%
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“…Values reported were approximately ten times greater than those of NaHCO 3 -Pi, indicating that the labile P forms in these soils are mainly stored in organic forms. In P-deficient soils, as those studied, the organic fractions play a fundamental role in the P cycle and plant nutrition (SLAZAK et al, 2010). These fractions were significantly correlated with soil C content (R: 0.73 ** ), confirming that the presence of labile organic fractions is associated with organic matter accumulation.…”
Section: Resultssupporting
confidence: 58%
“…The labile organic P forms probably buffer the inorganic forms, maintaining the labile inorganic P contents unchanged, even after three Pinus crops, as also observed by SLAZAK et al (2010). Perennial plants have more time to take up P during the cycle than annual crops, so that slow-release forms, such as labile Po forms, can buffer the available P for the forest system.…”
Section: Resultssupporting
confidence: 53%
“…However, it must be emphasised that there are large differences in litter quality within deciduous and coniferous species (Reich et al 2005), and probably thus also in P pools. Furthermore, Talkner et al (2009) and Slazak et al (2010) found a higher organic P pool in mixed species stands compared to homogeneous stands, which they also attributed to higher litter turnover rates.…”
Section: Applicability Of Our Results To Other Forest Typesmentioning
confidence: 89%
“…At agricultural land available P content under grey alder (Alnus incana (L.) Moench) SRC increased from 22.53 to 47.20 mg kg -1 (0-20 cm soil depth) after 5 years (Uri et al 2002). According to Slazak et al (2010) available P also increased with age of trees in mixed pine (Pinus sylvestris L.)/oak (Quercus petraea (Matt.) Liebl.)…”
Section: Soil Improvementmentioning
confidence: 98%