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Effects of sample pretreatment and sequential fractionation by centrifuge drainage on concentrations of minerals in a calcareous soil solution

Tyler, Germund LU (2000) In Geoderma 94(1). p.59-70
Abstract
Soil solution is the direct source of mineral nutrients to vascular plants. Soil solutions of sieved samples at water-holding capacity of a seminatural calcareous soil, never cultivated or treated by fertilizers, were collected by sequential centrifugation at 24-18,900 X g relative centrifugal force (RCF), followed by ultrafiltration (0.2 mu m), and analysed for Al, Ca, Fe, K, Mg, Mn, Mo, Na, P, S, Si and pH. Soil solution held by weak forces (low RCF applied) had higher concentrations of base cations, Fe, and Si than soil solutions obtained at higher RCF. Opposite relationships were measured for P-TOT, molybdate-reactive P and Mo, whereas concentrations of Mn and S did not vary much according to RCF level. A comparison between... (More)
Soil solution is the direct source of mineral nutrients to vascular plants. Soil solutions of sieved samples at water-holding capacity of a seminatural calcareous soil, never cultivated or treated by fertilizers, were collected by sequential centrifugation at 24-18,900 X g relative centrifugal force (RCF), followed by ultrafiltration (0.2 mu m), and analysed for Al, Ca, Fe, K, Mg, Mn, Mo, Na, P, S, Si and pH. Soil solution held by weak forces (low RCF applied) had higher concentrations of base cations, Fe, and Si than soil solutions obtained at higher RCF. Opposite relationships were measured for P-TOT, molybdate-reactive P and Mo, whereas concentrations of Mn and S did not vary much according to RCF level. A comparison between centrifugation of soil cores at undisturbed stratification and mixed samples uncovered no great differences in soil solution pH or concentrations of major constituents, though concentrations of Ca, Si and S were 10-20% lower in solution from undisturbed cores. Possible mechanisms accounting for the observations are discussed. (C) 2000 Elsevier Science B.V. All rights reserved. (Less)
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author
organization
publishing date
type
Contribution to journal
publication status
published
subject
in
Geoderma
volume
94
issue
1
pages
59 - 70
publisher
Elsevier
external identifiers
  • scopus:0033951488
ISSN
0016-7061
DOI
10.1016/S0016-7061(99)00080-4
language
English
LU publication?
yes
additional info
The information about affiliations in this record was updated in December 2015. The record was previously connected to the following departments: Plant Ecology and Systematics (Closed 2011) (011004000)
id
21313aa4-54b9-47a3-8cc2-d62b9735e54b (old id 147379)
date added to LUP
2016-04-01 16:47:50
date last changed
2022-01-28 22:12:18
@article{21313aa4-54b9-47a3-8cc2-d62b9735e54b,
  abstract     = {{Soil solution is the direct source of mineral nutrients to vascular plants. Soil solutions of sieved samples at water-holding capacity of a seminatural calcareous soil, never cultivated or treated by fertilizers, were collected by sequential centrifugation at 24-18,900 X g relative centrifugal force (RCF), followed by ultrafiltration (0.2 mu m), and analysed for Al, Ca, Fe, K, Mg, Mn, Mo, Na, P, S, Si and pH. Soil solution held by weak forces (low RCF applied) had higher concentrations of base cations, Fe, and Si than soil solutions obtained at higher RCF. Opposite relationships were measured for P-TOT, molybdate-reactive P and Mo, whereas concentrations of Mn and S did not vary much according to RCF level. A comparison between centrifugation of soil cores at undisturbed stratification and mixed samples uncovered no great differences in soil solution pH or concentrations of major constituents, though concentrations of Ca, Si and S were 10-20% lower in solution from undisturbed cores. Possible mechanisms accounting for the observations are discussed. (C) 2000 Elsevier Science B.V. All rights reserved.}},
  author       = {{Tyler, Germund}},
  issn         = {{0016-7061}},
  language     = {{eng}},
  number       = {{1}},
  pages        = {{59--70}},
  publisher    = {{Elsevier}},
  series       = {{Geoderma}},
  title        = {{Effects of sample pretreatment and sequential fractionation by centrifuge drainage on concentrations of minerals in a calcareous soil solution}},
  url          = {{http://dx.doi.org/10.1016/S0016-7061(99)00080-4}},
  doi          = {{10.1016/S0016-7061(99)00080-4}},
  volume       = {{94}},
  year         = {{2000}},
}