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Jimenez, M.A. ; Schmid, H.* ; von Lützow, M. ; Gutser, R.* ; Munch, J.-C.

Evidence for recycling of N from plants to soil during the growing season.

Geoderma 105, 223-241 (2002)
DOI
Open Access Green möglich sobald Postprint bei der ZB eingereicht worden ist.
In spite of the known below-ground biomass production of plant roots that concurrently introduce significant amounts of carbon and nitrogen into the soil, the effects of these inputs on N cycling in the soil-plant system are seldom considered. Here, we report on two field experiments carried out between 1995 and 1997 at the FAM Research Station Scheyern: (1) a N-turnover experiment to determine the N fluxes derived from N-15-labeled clover residues incorporated into the plough layer of defined plots, and (2) a root production experiment to assess the above (shoot) and below ground (gross and net root) biomass production of winter wheat in different fields, but nearby the N-15 plots. An initial 50% decrease in soil organic N-15 at 0-20-cm soil depth was recorded between fall, 1996 (incorporation of clover straw) and spring, 1997 (138 days after incorporation), which was then followed by a period of stability in N-15 levels in the soil organic N until the harvest of winter wheat (286 days after incorporation). This stability may be explained in two ways: (a) actual stability of clover-derived N-15 remaining in the second phase, e.g., due to recalcitrant compounds or microbial immobilization; or (b) apparent stability, e.g., because the actual mineralization of clover-derived N-15 in the soil was compensated by secondary inputs of organic 1 5 N (recycling). Further results showed that the first explanation was unlikely, as (1) between 138 and 286 days after clover incorporation, the mean N-15 signature in soil mineral N was 2.1 at.%, indicating a persistent mineralization of clover residues; and (2) a decrease in soil microbial biomass N-15 occurred in the second phase, indicating a continued N turnover in the soil, The amount of clover-derived N-15 accumulated below the plough layer at 20-110-cm soil depth (11.5%) between early spring and the harvest of wheat also corroborated the return of mineralized N-15 into the soil being due to the root N inputs by winter wheat. Based on the depth distribution of winter wheat net root biomass (root production experiment) and on soil organic N-15 depth distribution (1 5 N-turnover experiment), the root N input into soil was estimated to be 282 kg ha(-1), equivalent to 54% of total net N assimilation of winter wheat. Thus, the results of this study give substantial evidence for a N loop between soil and growing plants, whereby a part of the net mineralized N taken up by plants is continuously returned into the soil by their roots. The implications of this N loop for the interpretation of N-15 experiments and for plant nutrition are discussed.
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Publikationstyp Artikel: Journalartikel
Dokumenttyp Wissenschaftlicher Artikel
Korrespondenzautor
Schlagwörter nitrogen cycle; nitrogen mineralization; labeled N; root biomass production; soil microbial biomass; clover; MICROBIAL BIOMASS; NITROGEN MINERALIZATION; FIELD CONDITIONS; WINTER-WHEAT; DECOMPOSITION; RHIZOSPHERE; N-15; BARLEY; CROP; DEPOSITION
ISSN (print) / ISBN 0016-7061
e-ISSN 1872-6259
Zeitschrift Geoderma
Quellenangaben Band: 105, Heft: 3-4, Seiten: 223-241 Artikelnummer: , Supplement: ,
Verlag Elsevier
Nichtpatentliteratur Publikationen
Begutachtungsstatus Peer reviewed
Institut(e) Institute of Soil Ecology (IBOE)