Hauptseite > Publikationsdatenbank > Impact of phosphorus mineral source (Al-P or Fe-P) and pH on cluster-root formation and carboxylate exudation in Lupinus albus L. > print |
001 | 56266 | ||
005 | 20180211164307.0 | ||
024 | 7 | _ | |2 DOI |a 10.1007/s11104-007-9535-7 |
024 | 7 | _ | |2 WOS |a WOS:000253216200013 |
037 | _ | _ | |a PreJuSER-56266 |
041 | _ | _ | |a eng |
082 | _ | _ | |a 570 |
084 | _ | _ | |2 WoS |a Agronomy |
084 | _ | _ | |2 WoS |a Plant Sciences |
084 | _ | _ | |2 WoS |a Soil Science |
100 | 1 | _ | |a Shane, M. W. |b 0 |0 P:(DE-HGF)0 |
245 | _ | _ | |a Impact of phosphorus mineral source (Al-P or Fe-P) and pH on cluster-root formation and carboxylate exudation in Lupinus albus L. |
260 | _ | _ | |a Dordrecht [u.a.] |b Springer Science + Business Media B.V |c 2008 |
300 | _ | _ | |a 169 - 178 |
336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
336 | 7 | _ | |a ARTICLE |2 BibTeX |
336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
336 | 7 | _ | |a article |2 DRIVER |
440 | _ | 0 | |a Plant and Soil |x 0032-079X |0 9161 |v 304 |
500 | _ | _ | |a Record converted from VDB: 12.11.2012 |
520 | _ | _ | |a Lupinus albus L. were grown in rhizoboxes containing a soil amended with sparingly available Fe-P or Al-P (100 mu g P g(-1) soil/resin mixture). Root halves of individual plants were supplied with nutrient solution (minus P) buffered at either pH 5.5 or 7.5, to assess whether the source of mineral-bound P and/or pH influence cluster-root growth and carboxylate exudation. The P-amended soil was mixed 3:1 (w/w) with anion-exchange resins to allow rapid fixation of carboxylates. Treatments lasted 10 weeks. Forty percent and 30% of the root mass developed as cluster roots in plants grown on Fe-P and Al-P respectively, but cluster-root growth was the same on root-halves grown at pH 5.5 or 7.5. Mineral-bound P source (Al- or Fe-P) had no influence on the types of carboxylates measured in soil associated with cluster roots-citrate (and trace amounts of malate and fumarate) was the only major carboxylate detected. The [citrate] in the rhizosphere of cluster roots decreased with increased shoot P status (suggesting a systemic effect) and also, only for plants grown on Al-P, with decreased pH in the root environment (suggesting a local effect). In a separate experiment using anion exchange resins pre-loaded with malate or citrate, we measured malate (50%) and citrate (79%) recovery after 30 days in soil. We therefore, also conclude that measurements of [citrate] and [malate] at the root surface may be underestimated and would be greater than the 40- and 1.6-mu mol g(-1) root DM, respectively estimated by us and others because of decomposition of carboxylates around roots prior to sampling. |
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588 | _ | _ | |a Dataset connected to Web of Science |
650 | _ | 7 | |a J |2 WoSType |
653 | 2 | 0 | |2 Author |a citrate |
653 | 2 | 0 | |2 Author |a P-deficiency |
653 | 2 | 0 | |2 Author |a proteoid roots |
653 | 2 | 0 | |2 Author |a split-root design |
653 | 2 | 0 | |2 Author |a systemic signal |
653 | 2 | 0 | |2 Author |a white lupin |
700 | 1 | _ | |a Lambers, H. |b 1 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Gawthray, G.R. |b 2 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Kuhn, A. J. |b 3 |u FZJ |0 P:(DE-Juel1)129349 |
700 | 1 | _ | |a Schurr, U. |b 4 |u FZJ |0 P:(DE-Juel1)129402 |
773 | _ | _ | |a 10.1007/s11104-007-9535-7 |g Vol. 304, p. 169 - 178 |p 169 - 178 |q 304<169 - 178 |0 PERI:(DE-600)1478535-3 |t Plant and soil |v 304 |y 2008 |x 0032-079X |
856 | 7 | _ | |u http://dx.doi.org/10.1007/s11104-007-9535-7 |
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914 | 1 | _ | |y 2008 |
915 | _ | _ | |0 StatID:(DE-HGF)0010 |a JCR/ISI refereed |
920 | 1 | _ | |k ICG-3 |l Phytosphäre |d 31.10.2010 |g ICG |0 I:(DE-Juel1)ICG-3-20090406 |x 1 |
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981 | _ | _ | |a I:(DE-Juel1)ICG-3-20090406 |
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