1995
DOI: 10.1016/0016-7037(95)94443-j
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The role of organic matter in controlling aluminum solubility in acidic mineral soil horizons

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Cited by 201 publications
(170 citation statements)
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“…Al ox ranges from 0.54 cmol c kg À1 in a subsoil horizon to 2.02 cmol c kg À1 in an organic soil horizon. The sizes of the Al-pools in the soils in the two catchments are in the same range as in the acidic forest soils in Chongqing and Guiyang (Liao et al, 1997) and in acidic forest soils in Europe and North America (Berggren and Mulder, 1995;Koptsik and Koptsik, 1995;Koptsik and Silaeva, 1996). The concentration of exchangeable Fe is low, which may limit the availability of this important plant nutrient (Wang et al, 1989).…”
Section: Soil Chemistry In the Two Catchmentsmentioning
confidence: 77%
“…Al ox ranges from 0.54 cmol c kg À1 in a subsoil horizon to 2.02 cmol c kg À1 in an organic soil horizon. The sizes of the Al-pools in the soils in the two catchments are in the same range as in the acidic forest soils in Chongqing and Guiyang (Liao et al, 1997) and in acidic forest soils in Europe and North America (Berggren and Mulder, 1995;Koptsik and Koptsik, 1995;Koptsik and Silaeva, 1996). The concentration of exchangeable Fe is low, which may limit the availability of this important plant nutrient (Wang et al, 1989).…”
Section: Soil Chemistry In the Two Catchmentsmentioning
confidence: 77%
“…concentrations. Release of Al 3+ is an important acid buffering process in acid soils (Mulder et al, 1989;Berggren & Mulder, 1995;Larssen et al, 1999). Considering the depletion of base cations from the soil complex under N treatments (Fig 5a), a consequence of elevated H + production (low pH) is the dissolution of Al from soil (van Breemen et al, 1983;Schulze, 1989;Krusche et al, 2003).…”
Section: Accepted Articlementioning
confidence: 99%
“…Nonetheless, the levels of soil organic matter in all the agro-ecological zones were low. The low soil organic carbon content could be due to rapid decomposition of organic matter promoted by the prevailing high temperatures and high humidity [42], and continuous cropping without the return of crop residues to replenish the soil organic C stock [43]. The slightly low soil pH may be attributed to continuous cropping and leaching of soil basic cations [44].…”
Section: Discussionmentioning
confidence: 99%