1997
DOI: 10.1046/j.1365-2389.1997.00104.x
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Cryptopodzolic Soils in Switzerland

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Cited by 39 publications
(30 citation statements)
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“…The high C/N ratio of the plant litter from Nardus vegetation (C/N = 35) relative to that of the soil (10-12) suggests that N is immobilised during the initial decomposition of this litter (Bloemhof and Berendse, 1995;Parton et al, 1987), as found in our third laboratory experiment. The particular soil chemistry of the acidic cryptopodzolic soils also tends to promote the immobilisation of N in soil organic matter (Blaser et al, 1997). For camp areas, the low C/N ratio of the camp-area substrate (13) suggests a release of N already during the initial stages of decomposition (Bloemhof and Berendse, 1995;Parton et al, 1987), in agreement with the results of our third laboratory experiment.…”
Section: Discussionsupporting
confidence: 81%
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“…The high C/N ratio of the plant litter from Nardus vegetation (C/N = 35) relative to that of the soil (10-12) suggests that N is immobilised during the initial decomposition of this litter (Bloemhof and Berendse, 1995;Parton et al, 1987), as found in our third laboratory experiment. The particular soil chemistry of the acidic cryptopodzolic soils also tends to promote the immobilisation of N in soil organic matter (Blaser et al, 1997). For camp areas, the low C/N ratio of the camp-area substrate (13) suggests a release of N already during the initial stages of decomposition (Bloemhof and Berendse, 1995;Parton et al, 1987), in agreement with the results of our third laboratory experiment.…”
Section: Discussionsupporting
confidence: 81%
“…The bedrock is a mixed biotite plagioclase gneiss (Reinhard et al, 1962). The soils are silty and mainly of the 'cryptopodzol' type with extremely low pH, high aluminium content, and the accumulation of humic acids in the topsoil (Blaser et al, 1997). The system has been grazed during the summer for many centuries, as indicated by ruins of former stables and stone walls.…”
Section: Study Areamentioning
confidence: 99%
“…Parent material is a mixture of orthogneiss and gneiss. Soils are Cryptopodzols (FAO: Haplic Podzol; Blaser et al, 1997) with profile depths between 0.6 and 1.4 m and pH (CaCl 2 ) values below 5 throughout the whole profile. The soil texture is sandy with 72, 20 and 8% of sand, silt and clay, respectively.…”
Section: Study Sitementioning
confidence: 99%
“…Therefore, most of the time the soil conditions are much drier than indicated by the drought index of the model. A third explanation for the underestimation of soil carbon in Southern Alps is given by Blaser et al (1997). The soils of the Southern Alps are characterized by the iron-and aluminium-rich acid bedrock and a litter layer providing dissolved organic matter rich in polyphenolic substances with strong metal-binding properties.…”
Section: Evaluation Of the Yasso Modelmentioning
confidence: 99%