2018
DOI: 10.1080/03650340.2018.1550747
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Cultivation affected the level of inorganic phosphorus more than the organic pool of the Pampas soils in Argentina

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Cited by 3 publications
(7 citation statements)
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“…In those cases, the used rates are close to 30–34 kg of P ha −1 year −1 , which result in positive net balances that gradually increase soil Pe levels (Ciampitti et al., 2011; Suñer et al., 2005; Wyngaard et al., 2013). The results of the P balances of these and our long‐term trials show the need to increase P rates (between 4 and 13 kg of P ha −1 ) to compensate the export by crops, despite the fact that in the current context of the Rolling Pampas, P does not strongly constraints plant productivity (Alvarez et al., 2018). However, relying solely on the use of mineral fertilizers generates a greater dependence on P derived from the phosphoric rock, which is a non‐renewable resource and current global reserves may be depleted in 50–100 years (Cordell et al., 2009).…”
Section: Discussionmentioning
confidence: 77%
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“…In those cases, the used rates are close to 30–34 kg of P ha −1 year −1 , which result in positive net balances that gradually increase soil Pe levels (Ciampitti et al., 2011; Suñer et al., 2005; Wyngaard et al., 2013). The results of the P balances of these and our long‐term trials show the need to increase P rates (between 4 and 13 kg of P ha −1 ) to compensate the export by crops, despite the fact that in the current context of the Rolling Pampas, P does not strongly constraints plant productivity (Alvarez et al., 2018). However, relying solely on the use of mineral fertilizers generates a greater dependence on P derived from the phosphoric rock, which is a non‐renewable resource and current global reserves may be depleted in 50–100 years (Cordell et al., 2009).…”
Section: Discussionmentioning
confidence: 77%
“…Additionally, it responded to the distribution of crop residues in the profile (Franzluebbers, 2004; Irizar et al., 2015). Below the A horizon, the observed TP increase towards the centre of the Bt1 horizon (40–50 cm) (Figure 1) results from the increased clay percentage (Arzuaga et al., 2005; Hernández et al., 1995; O'Halloran, 1993) and to the P enrichment of the OM with increasing depth (Alvarez et al., 2018).…”
Section: Discussionmentioning
confidence: 99%
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