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Assessing potassium reserves in northern temperate grassland soils: A perspective based on quantitative mineralogical analysis and aqua-regia extractable potassium

Andrist Rangel, Ylva (author)
Swedish University of Agricultural Sciences,Sveriges lantbruksuniversitet,Institutionen för mark och miljö,Department of Soil and Environment
Öborn, Ingrid (author)
Swedish University of Agricultural Sciences,Sveriges lantbruksuniversitet,Institutionen för växtproduktionsekologi,Department of Crop Production Ecology
Hillier, Stephen (author)
Swedish University of Agricultural Sciences,Sveriges lantbruksuniversitet,Institutionen för mark och miljö,Department of Soil and Environment
 (creator_code:org_t)
 
Elsevier BV, 2010
2010
English.
In: Geoderma. - : Elsevier BV. - 0016-7061 .- 1872-6259. ; 158, s. 303-314
  • Journal article (peer-reviewed)
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  • Increasing demand for locally produced farm products, with a lower input of mineral fertilisers, leads to a greater reliance on the inherent capacity of soils to supply plant nutrients. Typically 98% of all soil potassium (K) is found in K-feldspars and phyllosilicates, however the potential bioavailability of K from different mineral forms varies significantly. As a basis for improving sustainable nutrient management options for grassland systems we set out to determine 1) how soil parent material influences the amount of K in soils, 2) how the K is quantitatively distributed between mineral groups, 3) relationships between quantitative mineralogy (X-ray powder diffraction (XRPD)), total K (X-ray fluorescence) and the more widely available measurement of aqua-regia extractable K, and (4) how the studied soils could be ranked in terms of their long-term potential capacity to deliver K to plants. Soils representing eight of the most extensive soil associations (defined by different parent materials) under improved grassland in Scotland were analysed. Soil samples represented a wide range of total K concentrations, from 1.3 to 39 g kg(-1). Quantitative mineralogical data from XRPD were combined with mineral compositions to obtain the mineralogical apportionment of K. Apportionment of K varied significantly, from those soils with almost all K present in various phyllosilicates to others where almost all K is held in K-feldspars. Aqua-regia extractable K is related to K in phyllosilicates (excluding muscovite mica) and unrelated to K in K-feldspars. The studied soils are ranked in terms of their potential capacity to release K based on their mineralogical and geochemical characteristics. (C) 2010 Elsevier B.V. All rights reserved.

Subject headings

LANTBRUKSVETENSKAPER  -- Lantbruksvetenskap, skogsbruk och fiske -- Jordbruksvetenskap (hsv//swe)
AGRICULTURAL SCIENCES  -- Agriculture, Forestry and Fisheries -- Agricultural Science (hsv//eng)

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Öborn, Ingrid
Hillier, Stephen
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Geoderma
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