Herbaceous layer development during spring does not deplete soil nitrogen in the Portuguese montado
| dc.contributor.author | Otieno, D.O. | |
| dc.contributor.author | Mirzaei, H. | |
| dc.contributor.author | Hussain, M.Z. | |
| dc.contributor.author | Li, Y.L. | |
| dc.contributor.author | Schmidt, M.W.T. | |
| dc.contributor.author | Wartinger, M. | |
| dc.contributor.author | Jung, E. | |
| dc.contributor.author | Ribeiro, N. | |
| dc.contributor.author | Pereira, J.S. | |
| dc.contributor.author | Tenhunen, J. | |
| dc.date.accessioned | 2014-01-28T15:20:45Z | |
| dc.date.available | 2014-01-28T15:20:45Z | |
| dc.date.issued | 2010-11-26 | |
| dc.description.abstract | Nitrogen (N) content in the soil and in the herbaceous biomass were monitored during spring of 2004-2006 to determine how the herbaceous layer development influences soil N availability in the montado ecosystem of southern Portugal. Highest (246.6 ± 52.7 g m-2) and lowest (123.2 ± 89.5 g m-2) peak biomass occurred in 2006 and 2005 respectively. Total soilNwithin the top 20 cmsoil profile ranged between 0.2 0.1% in February and 0.41 0.2% inMay,while available soil N was lowest (5 ± 2 μg g-1soil) in February but increased three-to-five fold in March and was >17.5 μg g-1 soil at senescence in May. Significant (p < 0.001) increase in total N in the aboveground pool occurred between February and May. There was however, no decay in soil N content. Instead, the herbaceous vegetation enhanced soil N input and N retention in the ecosystem. Most of the herbaceous plants were annuals with large reserves of organic N at senescence, which returned to the soil as detritus. The herbaceous vegetation is a critical component of the montado that contributes to N recharge and cycling within the ecosystem. | por |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nd | |
| dc.identifier.authoremail | nmcar@uevora.pt | |
| dc.identifier.authoremail | jspereira@isa.utl.pt | |
| dc.identifier.authoremail | nd | |
| dc.identifier.citation | D.O. Otieno, H. Mirzaei, M.Z. Hussain, Y.L. Li, M.W.T. Schmidt, M. Wartinger , E. Jung, N. Ribeiro, J.S. Pereira, J. Tenhunen, (2011). Herbaceous layer development during spring does not deplete soil nitrogen. Journal of Arid Environments 75: 231-238 | por |
| dc.identifier.scientificarea | 578 | por |
| dc.identifier.sharewith | Departamento de Fitotecnia | por |
| dc.identifier.uri | http://www.sciencedirect.com/science/article/pii/S0140196310002922 | |
| dc.identifier.uri | http://hdl.handle.net/10174/10188 | |
| dc.language.iso | por | por |
| dc.peerreviewed | yes | por |
| dc.publisher | Elsevier | por |
| dc.rights | openAccess | por |
| dc.subject | Biomass development of the herbaceous vegetation | por |
| dc.subject | Mediterranean ecosystems | por |
| dc.subject | Portuguese montado | por |
| dc.subject | Pasture | por |
| dc.subject | Plant and soil nitrogen pools | por |
| dc.subject | Root distribution and nutrient uptake | por |
| dc.subject | Soil moisture | por |
| dc.title | Herbaceous layer development during spring does not deplete soil nitrogen in the Portuguese montado | por |
| dc.type | article | por |
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