<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Otieno, D. O.</style></author><author><style face="normal" font="default" size="100%">Mirzaei, H.</style></author><author><style face="normal" font="default" size="100%">Hussain, M. Z.</style></author><author><style face="normal" font="default" size="100%">Li, Y. L.</style></author><author><style face="normal" font="default" size="100%">Schmidt, M. W. T.</style></author><author><style face="normal" font="default" size="100%">Wartinger, M.</style></author><author><style face="normal" font="default" size="100%">Jung, E.</style></author><author><style face="normal" font="default" size="100%">Ribeiro, N.</style></author><author><style face="normal" font="default" size="100%">Pereira, J. S.</style></author><author><style face="normal" font="default" size="100%">Tenhunen, J.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Herbaceous layer development during spring does not deplete soil nitrogen in the Portuguese montado</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Arid Environments</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biomass development of the herbaceous vegetation</style></keyword><keyword><style  face="normal" font="default" size="100%">Mediterranean ecosystems</style></keyword><keyword><style  face="normal" font="default" size="100%">pasture</style></keyword><keyword><style  face="normal" font="default" size="100%">Plant and soil nitrogen pools</style></keyword><keyword><style  face="normal" font="default" size="100%">Portuguese montado</style></keyword><keyword><style  face="normal" font="default" size="100%">Root distribution and nutrient uptake</style></keyword><keyword><style  face="normal" font="default" size="100%">Soil moisture</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2011</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2011///</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://linkinghub.elsevier.com/retrieve/pii/S0140196310002922</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">75</style></volume><pages><style face="normal" font="default" size="100%">231 - 238</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Nitrogen (N) content in the soil and in the herbaceous biomass were monitored during spring of 2004e2006 to determine how the herbaceous layer development inﬂuences soil N availability in the montado ecosystem of southern Portugal. Highest (246.6 52.7 g m2 ) and lowest (123.2 89.5 g m2 ) peak biomass occurred in 2006 and 2005 respectively. Total soil N within the top 20 cm soil proﬁle ranged between 0.2 0.1% in February and 0.41 0.2% in May, while available soil N was lowest (5 2 mg g 1 soil) in February but increased three-to-ﬁve fold in March and was &gt;17.5 mg g 1 soil at senescence in May. Signiﬁcant (p &lt; 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</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record></records></xml>